ANUARY 25. 1982
THE
NAUTILUS
1^«N ()()28-i:i44
Vol. 96
No. 1
A quarterly
devoted to
malacology and
the interests of
conchologists
Founded 1889 by Henn' A. Pilsbry. Continued by H. Burrington Baker.
Editor-in-Chief; R. Tucker Abbott
EDITORIAL COMMITTEE
CONSULTING EDITORS
Dr. William J. Clench
Curator Emeritus
Museum of Comparative Zoology
Cambridge, Mass. 02138
Dr. William K. Emerson
Department of Living Invertebrates
The American Museum of Natural History
New York, New York 10024
Dr. Aurele La Rocque
Department of Geology
The Ohio State University
Columbus, Ohio 43210
Dr. James H. McLean
Los Angeles County Museum of Natural History
900 Exposition Boulevard
Los Angeles, California 90007
Dr. Arthur S. Merrill
103 West 8th Avenue
Cudjoe Gardens
Summerland Key, Florida 33043
Dr. Donald R. Moore
Division of Marine Geology
School of Marine and Atmospheric Science
10 Rickenbacker Causeway
Miami, Florida 33149
Dr. Joseph Rosewater
Division of Mollusks
U.S. National Museum
Washington, D.C. 20560
Dr. G. Alan Solem
Department of Invertebrates
Field Museum of Natural History
Chicago, Illinois 60605
Dr. David H. Stansbery
Museum of Zoology
The Ohio State University
Columbus, Ohio 43210
Dr. Ruth D. Turner
Department of Mollusks
Museum of Comparative Zoology
Cambridge, Mass. 02138
Dr. Gilbert L. Voss
Division of Biology
School of Marine and Atmospheric Science
10 Rickenbacker Causeway
Miami, Florida 33149
Dr. Charles B. Wurtz
3220 Penn Street
Philadelphia, Pennsylvania 19129
EDITOR-IN-CHIEF
Dr. R. Tucker Abbott
American Malacologists, Inc.
Box 2255, Melbourne, Florida 32901
Mrs. Cecelia W. Abbott
Business and Subscription Manager
P.O. Box 22.55
Melbourne, Florida 32901
Tlie Nautilus (USPS 374-980)
ISSN 0028-1344
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Subscription Price: $12.00 (see inside back cover)
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THE
NAUTILUS
Volume 96, number 1 - January 25, 1982
ISSN 0028-1344
CONTENTS
Joseph Rosewater
A New Species oiHipjiopu^- (Bivalvia: Tridaciiidae)
Francesco B. Trama
Occurrence of the Asia^c Clam Corbicula Jluininea in the Raritan River,
New Jersey 6
William D. Shepard
Rediscovery of a Portion of the Isely Unionid Collections 8
Philippe Bouchet and Francoise Danrigal
Napoleon's Egyptian Campaign (1798-1801) and the Savigny Collection of Shells 9
Clement L. Counts, III and Robert S. Prezant
Shell Microstructure of Corbicula flmninea (Bivalvia: Corbiculidae) 25
Paul W. Parmalee and Walter E. Klippel
A Relic Population oi Obuvaria retussa in the Middle Cumberland River,
Tennessee 30
Publications Received 2 Recent Deaths 2
THE NAUTILUS
January 25, 1982
Vol. 96(1)
PUBLICATIONS RECEIVED
Brooks, Stanley Truman (1902-1960), Biobibliosraphy by
R. I. .lohnson in Ocr. fnpers MoUuaka. va]. 4, no. 59,
pp. 266-268(1981).
Clarke, Arthur H. 1981. The Tribe Alasmidontini (Unioni-
dae: Anodontinae), Part 1: Pegias, Alasmidon.la, and
A rcidenx. Smithsonian Contributions to Zoology, no. 326,
pp. iii + 1-101, 32 figs. Ecologic and taxonomic study with
illustrations of shell, soft parts, gloehidia, descriptions,
distributional maps, synonymies, and simple anatomical
test for sex determination. Alusmidontn mliusta n. sp..
extinct mussel from (jharlotte, N(" (not Vnio mlntatif
Sowerby, 1840).
Habe, T. and Iwao Taki. 1981. A Catalogue of Molluscs of
Wakayama Prefecture, the Province of Kii. 1. Bivalvia,
Scaphopoda and Cephalopoda. F'ubl. Seto Marine Biol.
Lab.. Special Series, vol. 7, no. 1, pp. xx 304, 13 pis. (One
in color). Based on Kuroda's Manuscript. Eleven new
species of .Japanese Bivalvia are described. Synonymies
very complete. 51 cephalopods treated by I. Taki (pp.
234-264).
.Johnson, Richard I. 1981. Recent and Fossil Unionacea and
Mutelacea (Freshwater Bivalves) of the Caribbean Islands.
Occasional Papers on Mollii.<!ks. vol. 4, no. 60. pp. 269-288.
•SI. 60 from Dept. Mollusks. Museum ('omparative Zool-
ogy, Cambridge, MA 02138.
Martins, Antonio M. Frias. 1981. Oxyrliilus. (Drouetia)
agosl.inhm New Species (Stylommatophora: Zonitidae)
from the Azores Islands, its Anatomy and Phylogenetic
Relationships. Occ. Papers on Mollwsks, vol. 4. no. 59.
pp. 245.
Rehder, Harald A. 1981. The Audubon Society Field Guide
to North .American Seashells. 894 pp., 705 color pis. An
excellent pocket guide of the common shells, with espe-
cially good photographs by James H. Carmichael, Jr.
Gives descriptions, habitats, range and both popular and
Latin names, but unfortunately omits all authors and
dates.
.Sharabati, Doreen. 1981. Saudi Arabian Seashells. 119 pp.
VNU Books International. A popular account with numer-
ous beautiful photographs, many of living mollusks.
T}iais. 1981. Publicaciones Diversas de la Sociedad Pana-
mena de Malacologia. No. 1 (La Fauna Malacologica
Panamena), 28 pp.; No. 2 (Lista Prelimininar de Referen-
cias Bibliograficas Sobre la Fauna Malacologica
Panamena), 59 pp. Both by Miguel C. Aviles E. Annual
subscription Balboa 10.00 (U.S. $10.00), Soc. Panamena de
Malacologia, Estafeta Universitaria, Panama, Rep. of
Panama.
RECENT DEATHS
Grab, Robert McKay, former President of the Naples Shell
Club, bom New York City on April 19, 1904, graduate
University of Michigan in 1926, died in North Carolina
September 1981.
Lyman, P>ank, long-time shell dealer, editor of "Shell
Notes" (1942-51), born in Lantana, Florida, June 10,
1895, died Oct. 11, 1981, in Ferandina Beach, Florida.
Sexauer, Howard T. 1981-82 President of the Sanibel
Captiva Shell Club, well-known poet, former resident of
Montpelier, Vermont, died at age 82 in Florida on Dec. 1,
1981.
Zeigler, Rowland Franklin, born .lune 1, 1915, in Greely-
ville, SC, formerly chief of obstetrics and gynecology at
McLeod Hospital in P'lorence, SC, author (with Porreca)
of "Olive Shells of the World" and articles in medical
journals, died at age 66, on Sept. 21, 1981, in Durham,
NC. His widow, Edna Jo continues his interests in olive
shells.
I'ln' I'irsI a>vrhfdogiral wtirk liij mi .■\mmcaii
jiuhHuhed in A mtn'icit.
THOMAS Savs CONCHOLOGY
1819
A beaut iful facsimile copy of the third
edition of Say's fiindeinental umrk from
Nicholson's British Encyclopedia
Philadelphia 1819
This rare work, never before reprotluced in full, con-
tains 20 pages and four lithograph plates of Say's new
land and freshwater species of mollusks. This is the
expanded version of the first (1816) and second (1818)
edition. 32 pages, paperbound.
The [ireface, by R. Tucker .Abbott, tells the history of
this article and gives brief biographies of the author,
the editor, the publisher and the printer. Limited edi-
tion. $5.00, including postage. F'oreign postage,
plea.se add $1.00.
Amki;i('an MALACOUHiisTS, Inc.
P.O. Box 2255
Mi-llMiurne. FL 32»(I1-I«2S
Vol. 96(1)
January 25, 1982
THE NAUTILUS
A NEW SPECIES OF HIPPOPUS (BIVALVIA: TRIDACNIDAE)
Joseph Rosewater
Department of Invertebrate Zoology
National Museum of Natural History
Washington, D.C. 20560
ABSTRACT
Hippopus porcellanus n. sp. is described from Sibutu Island, Sulu Archipelago,
Philippines, bringing the known members of the genus Hippopus to 3, including
H. hippopus (Linne, 1758), Recent, I ndo- Pacific, and H. gimteri Mansfield, 1937,
Fossil. Lower Miocene of Florida.
For several years shell dealers have received
large numbers of a rather distinctive giant clam
belonging to the genus Hippopus which they
refer to as the "China Clam", and which they
consider to be distinct from the "Horse's Hoof
or "Bear Paw", Hippopus hippopus (Linne,
1758). It is much thinner and smoother than the
usually elaborately sculptured H. hippopus, and
lacks most of the characteristic strawberry color
of the latter. When I reviewed the classification
of Tridacnidae this phenotype was believed to
intergrade completely with H. hippopus (Rose-
water, 1965, p. 361). Recent examination of
nearly two dozen specimens of the "China Clam"
and comparison with H. hippopus persuades me
that they are separate species.
Hippopus porcellanus new species
(Figs. 1-4)
Description: Shell reaching 216 mm (about 8
1/2 inches) in length, semicircular in outline and
globose in shape; usually only moderately in-
flated; with valves closed byssal orifice is very
narrowly gaping. Valves not excessively heavy,
markedly translucent, colored occasionally with
weak strawberry blotches arranged concentri-
cally or scattered; color of interior porcel-
laneous, of exterior grayish white. Surface of
valves remarkably clean, except for scattered
coralline algae and debris. Primary radial sculp-
ture consisting of 13 or 14 low rib-like folds
distributed over surface of valve, extending on-
to ventral slope where they become obsolete.
Secondary radial sculpture consisting of low rib-
lets which are nearly obsolete on primary folds
but are more prominent in their interstices.
Riblets varying somewhat in width, usually lack-
ing spines or evidencing only microscopic con-
centric imbrications. A few low tubular spines
present on primary fold bordering ventral slope
and occasionally on ventral portions of other
primary folds; folds usually smooth dorsally.
Concentric sculpture consisting of microscopic,
wavy, imbricate lines of growth. Dorsal margin
undulate, with series of 8-9 rounded to squarish,
medially projecting, interdigitating processes
representing extremities of rib interstices.
Hinge line usually longer than half the length of
valve. One oblong cardinal tooth in each valve; 2
elongate posterior laterals in right and a single
moderately sharp one in the left valve. Liga-
ment secondarily prosodetic. Umbos directed
postero-medially. Edge of byssal orifice with a
series of 8-12 light-yellow, rather poorly
developed plicae which remain fairly constant in
size or become only slightly larger posteriorly.
Ventral slope moderately concave. Hinge plate
suffused with orange. Pallial line entire, mod-
erately narrow. Muscle scars central, medium
sized; the posterior adductor scar round in both
valves, the posterior pedal retractor scar is
smaller and elongate, the two extending over
portions of two fold interstices in each valve.
Area within pallial line, excluding muscle scars,
dull; pallial line, muscle scars and areas to edge
of shell shiny. Prodissoconch unknown.
The anatomy and life history of this species
are unknown. Following my studies (Rosewater,
1965) several persons have achieved success in
studying the spawning and development of Hip-
THE NAUTILUS
January 25, 1982
Vol. 96(1)
Vol. 96(1)
January 25, 1982
THE NAUTILUS
popus hippopus (Jameson, 1976; Gwyther and
Munro, 1981).
Measurements (mm): Tridacnidae are indis-
criminately inequivalved, and the figures given
under "length" and "height" are always the max-
imum measurement. "Width" is the greatest
distance through opposed valves.
Lticality Sihiitu MaMmte
(Philippines) Zmtiliiiiniiia hi Id. SnIii Sra
Types: Holotype ANSP (The Academy of
Natural Sciences of Philadelphia) 246600, 157
mm length, 113 mm height; 3 paratypes ANSP
354770, 155 mm length, 115 mm height, 101 mm
length, 81 mm height, and 75 mm length, 53 mm
height; 1 paratype USNM (National Museum of
Natural History, Washington, D.C.) 807720, 133
mm length, 98 mm height.
Type locality: Sibutu Island, Tawi Tawi
Group, Sulu Archipelago, Philippines (4°46'N;
119°29'E), du Pont- Academy Expedition, 1958.
Other Material Examined: ANSP 209699
Zamboanga, Mindanao Island, Philippines, ex.
A. B. Bronson, 1956 (10 specimens, see Meas-
urements); ANSP 228977, Masbate Island,
Philippines, du Pont-Academy Expedition, 1958
(1 specimen, see Measurements); USNM, "Sulu
Sea", ex. A. D'Attilio and John Root (6 speci-
mens, see Measurements).
Distribution: Philippines, mostly known from
the Sulu Archipelago; 1 specimen from Masbate
Island, central Philippines.
Etymology: "porcellanus", an adjectival name
referring to the porcelain-like appearance of the
shell of this species.
Remarks: Shells of this new species are con-
sistently smoother, more semicircular in outline,
proportionately lighter in weight and thinner
than H. hippopus (see figs. 1-4). When viewed
apart from the latter they present a rather ro-
tund appearance although measurements show
they are no more obese, but, in fact, are often
less wide. Compared with H. hippopus. H.
porcellanus has a very narrow byssal orifice,
with the plicae less well developed and lighter in
color (fig. 4). The single posterior lateral tooth
of the left valve is moderately sharp in H.
porcellanus while in H. hippopus it is blunt.
The only other large bivalve species with
which H. porcellanus is likely to be confused is
Tridacna derasa (Roding, 1798). Specimens of
T. derasa, of the same length as H. porcellanus
(200 mm-f ), are smooth, may be similarly semi-
circular in outline and exhibit similar obesity. It
is quite likely that living T. derasa has a con-
siderably more colorful mantle, that of H. hip-
popus, at any rate, being rather sombre olive.
The shell of T. derasa is even smoother than
that of H. porcellanus, lacking in development
of tubular spines and having low primary and
secondary folds, although sometimes developing
strong, continuous, undulate concentric ridges
(Rosewater, 1965, pi. 281, fig. 1). Shells of T.
derasa lack the orange and yellow coloration
present in Hippopus in the areas of hinge and
byssal orifice. Byssal plicae number 6-7, are low
and elongate to nearly obsolete in T. derasa
while in H. pjorcellanus they are shorter and
number from 8-12. The posterior adductor
muscle/posterior pedal retractor scar complex is
comparatively larger in T. derasa and its umbos
tend to be less distinctly convoluted than in H.
porcellanus. although size for size the former
tends to have a heavier shell.
I originally thought that H. porcellanus dif-
fered from H. hippopus subspecifically rather
than specifically. As subspecies the two would
normally have more or less discreet geographic
ranges. While it appears that H. porcellanus
lives mostly in the southern Philippines, more
precisely the southern Sulu Sea, a specimen has
been reported from Masbate Id. in the central
Philippines. Furthermore, H. hippopus is
distributed in the same area besides having a
more extensive range in the western Pacific.
Since the ranges of the two species seem not to
be in any real way mutually exclusive, the sub-
specific status seems doubtful, and they are here
considered to be separate species within the
THE NAUTILUS
January 25. 1982
Vol. 96(1)
genus HippoptLs. It is quite obvious that the
known geographic range of H. porcellanus is
considerably more restricted than that of//, hip-
popus (see Rosewater, 1965, pi. 272).
ACKNOWLEDGMENTS
Special thanks are expressed to those who
assisted in gathering information and donating
specimens: Anthony D'Attilio, John Root,
Robert W. Morrison, R. T. Abbott, and Betty
and Robert Lipe. I am grateful to R. Robertson,
ANSP, for loaning specimens with accurate
locality data. R. D. Turner, and K. J. Boss,
Museum of Comparative Zoology, Harvard
University, and H. A. Rehder, and R. S.
Houbrick, USNM, offered helpful criticism.
LITERATURE CITED
Gwyther, J. and J. L. Munro. 1981. Spawning induction and
rearing of larvae of Tridacnid Clams (Bivalvia: Tridacni-
dae). AquaeuHurc 24:197-217.
Jameson, Stephen C. 1976. Early life history of the Giant
Clams Tridarna crocea Lamarck, Tridarna maxima
(Roding). and Hippopus hippopus (Linnaeus). Pacific
Science 30(3):219-233.
Rosewater, Joseph. 1965. The Family Tridacnidae in the
Indo-Pacific. Indo-Pacifie Mollusca l(6):347-396.
Shell Factory. 1963. Shells of the Winid. Catalog no. 109,
160 pp. Fort Myers. Florida. "China Clam" illustrated
on p. 45.
OCCURRENCE OF THE ASIATIC CLAM CORBICULA FLUMINEA IN THE
RARITAN RIVER, NEW JERSEY^
Francesco B. Trama
Department of Biological Sciences
Rutgers LTniversity
New Brunswick, New Jersey
ABSTRACT
The mid-Atlantic range of the Asiatic clam, Corbicula fluminea (Muller. 1771^)
is extended to the Raritan River in central New Jersey. A successfully breeding
population was found in the nontidal region near a water supply intake. These
clams have also colonized far upstream into the South Branch of the Raritan but
not the North. Branch. No reason for this difference is known. Living specimens
were found downstream in the tidal portion of the river which is freshwater but
polluted. There was no evidence of reproduction in this region of the river.
Since it was first observed in this country in
the Columbia River, Washington (Dundee and
Dundee, 1958) the Asiatic clam, Corbicula
fluminea (Muller, 1774; (alias manilensis Philip-
pi) has spread rapidly into many river systems
across the United States (Sinclair, 1971). Exten-
sion of its range to the mid- Atlantic region was
documented by Diaz (1974) in the James River,
'This study was supported iiy the Center for Coastal and En-
vironmental Studies. Rutgers University. Assistance of Joy
Bergelson in pierforming field collections is acknowledged.
Virginia, and by Fuller and Powell (1973) in the
Delaware River between Philadelphia, Pennsyl-
vania and Trenton, New Jersey. Diaz estimated
the year of introduction in the James River to be
1968 and Fuller and Powell concluded that Cor-
bicula was present in the Delaware River since
at least 1971 or 1970. Crumb (1977) later re-
ported it in the Delaware River between Tren-
ton and Burlington in September 1971.
On March 26, 1981 many empty shells and a
few living Corbicula were collected from a tidal
(Init freshwater) region of the Raritan River
Vol. 96(1)
January 25, 1982
THE NAUTILUS
near New Brunswick, New Jersey (Sta. 1, Fig.
1). Collections of macrobenthos taken from this
same region in September 1980 did not contain
any specimens of Corbicula. The largest shell
collected in March 1981 was 25 mm in length
and was estimated to be between 3 and 4 years
of age at the time of death. It was concluded
that the year of invasion was not later than 1978
and that the invasion site had to have been
upstream from this point of initial discovery.
During July and August 1981 the occurrence
and range of Corbicula in the Raritan River was
studied. Samplmg extended upstream from Sta.
1 (tidal but freshwater) into the North and South
Branches of the Raritan River (Fig. 1).
At Sta. 1 many empty shells were again
found. Many live specimens, however, were also
collected from current-swept bottoms covered
by gravel and small pebbles The livmg clams
fell into two size classes; largest specimen was
25 mm in length and had a grossly distorted
shell growth that appeared to commence from a
shell length of 20 mm. The smallest specimen
was 15 mm in length and appeared nt)rmal.
The greatest population density and evidence
of reproduction were found at Sta. 2 which is in
the vicinity of the Elizabethtown Water Com-
pany's intake on the Raritan River which is non-
tidal at this point. Largest living clams ranged
from 15 to 17 mm in length and a first year class
ranged from 2 to 6 mm in length. No Corbicula
were found in the Millstone River (Sta. 3) im-
mediately above its confluence with the Raritan
River. The substrate in this portion of the
Millstone River was soft muck and, therefore,
was not a preferred habitat for these clams.
Very few living Corbicula were taken at Sta-
tions 4 and 5, and these ranged from 7 to 10 mm
in length. Many empty shells were found at Sta.
4. Even though a suitable type substrate existed
at Stations 6, 7 and 8 only one specimen of Cor-
bicula (10 mm) was found at Sta. 6. None was
found at Stations 7 or 8, nor was there evidence
of dead Corbicula shells anywhere in the North
Branch of the Raritan River. On the other hand,
tliere were significant populations in the South
Branch. Specimens ranged from 2.5 to 10 mm in
length at Stations 9, 10 and 11. No dead
no. 1. Samjile files ,„, the Ranta,, Hirer. Netr Jersey. Samplvngfor Corbicula look place belween July 2:1 and
August 2ti. 1981.
8 THE NAUTILUS
January 25, 1982
Vol. 96(1)
specimens or empty shells were found in those
locations.
It seems that the Asiatic clam has established
itself in the tidal and nontidai, freshwater (even
polluted) regions of the Raritan River. The
population center (initial colonization?) is in the
nontidai waters of the main stem in the vicinity
of the intake of the Eiizabethtown Water Com-
pany. Furthermore, this foreign species has suc-
cessfully colonized the South Branch of the
Raritan River but for some reason has not as yet
moved very far into the North Branch of the
Raritan River. This discovery extends the north-
ern range of Corbicula in the mid-Atlantic
region.
LITERATURE CITED
Crumb, S. E. 1977. Macrobenthos in the tidal Delaware
River between Trenton and Burlington, New .Jersey.
Chesapeake Science 18:253-265.
Diaz, R. J. 1974. Asiatic clam, Corbicula manilensis (Philip-
pi), in the tidal James River, Virginia. Chesapeake Science
15:118-120.
IXindee, D. S. and H. A. Dundee. 1958. Extension of known
ranges of four mollusks. The Nautilus 72:51-53.
Fuller, S. L. H. and C. E. Powell. 1973. Range extensions
(jf Corbicula manilensis (Philippi) in the Atlantic drainage
of the United States. The Nautilus 87:59.
Sinclair. R. M. 1971. Annotated bibliography on the exotic
bivalve Carbicula in North America, 1900-1971. Sterki-
anaNo. 43:11-18.
REDISCOVERY OF A PORTION OF THE
ISELY UNIONID COLLECTIONS
William D. Shepard
Oklahoma Biological Survey
Norman, Oklahoma 73019
During a recent renovation of the Inverte-
brate Range at Stovall Museum of Science and
History (University of Oklahoma), a collection of
unionids was found carefully wrapped in old
newspapers and stored away. Part of these were
labeled as collected by F. B. Isely in Oklahoma
between 1908 and 1912. The remaining unionids
were also from Isely's collections. Upon inquiry
with several malacologists, it appears that this
is the largest extant portion of Isely's collec-
tions. These are part of the specimens collected
by Isely for his study of the clams of Eastern
Oklahoma, which appeared in 1925.
After rearrangement of the above specimens
and merging of several other collections, a
series of unlabeled unionids were found. These
differed from all the other specimens, however,
in that they had small, circular, numbered, cop-
per tags wired to the shells. On further examina-
tion it was determined that these were a portion
of the specimens used by Isely in his classical
migration study (Isely 1914). They were also col-
lected in Oklahoma.
The rediscovery of these specimens is impor-
tant for several reasons. They were used by Ise-
ly and therefore are now voucher specimens for
liis works. Their presence also allows some in-
sight into the taxonomy of his time or at least
Isely's interpretation of it. Secondly, the
specimens have a historical importance in that
some of the streams Isely collected have now
been altered so as to deplete the original unionid
fauna. Finally, some of these specimens repre-
sent the only collections from various streams in
Oklahoma.
Isely's specimens plus others donated to
Stovall Museum form a nucleus for a growing
collection of Oklahoma unionids. The Stovall col-
lection combined with that located at OU's
Biological Station on Lake Texoma (Texas-
Oklahoma border) represents perhaps the major
collections of Oklahoma unionids.
LITERATURE CITED
Isely, F. B. 1914. Experimental study of the growth and
migration of freshwater mussels. Bureau of Fisheries
Document, No. 792.
1925. The freshwater mussel fauna of Eastern
Oklahoma. I'rur. OkUi. Acad. Sci. 4:43-118.
Vol. 96(1)
January 25, 1982
THE NAUTILUS
NAPOLEON'S EGYPTIAN CAMPAIGN (1798-1801)
AND THE SAVIGNY COLLECTION OF SHELLS
Philippe Bouchet and Francoise Danrigal
Museum National d'Histoire Naturelle
55, Rue de Buffon
75 Paris (5°), France
ABSTRACT
During the Napoleonic campaign to Egypt a collection of Red Sea, Mediter-
ranean and continental niollut^k^ ivas brought together by Savigny who published
upon them in 1817 as folio engravings. These served as type figures for a number
of species described by 19th ceyitury malacologists, including Audouin,
Ehrenberg, Deshayes, Philippi, Hupe, Landrin, Jonas, Issel, Morlet, Vaillant, P.
Fischer, Tapparone-Canefri. von Martens, Weinkauff, Monterosato, Jousseaume,
H. Fischer and finally Pallary. A checklist and illustrations of 86 of these
original types frmn the Savigyiy collection, now in the Paris Museum, are
presented, supplemented by reproductions of the unpublished color vellums of
opisthobranchs and cephalopods.
Jules Cesar Savigny was born at Provins,
France, on April 5, 1777. In 1793, in the middle
of the Revolution, the Convention transformed
the Royal Gardens into a "Museum d'Histoire
naturelle". Savigny was then 16 years old and
was sent to Paris to study at the "Ecole de
sante" and the Museum. His professors were
Lamarck, Cuvier, Daubenton; they noted the
young student's assiduity and also took note
that he was always wearing the same Nankin
costume.
Lamarck was then writing the "Nouvelle En-
cyclopedie" and assigned Savigny his first work,
the drafting of the part on the sorrel plant. This
paper showed the wealth of his knowledge and
soon he was named professor of botany at the
"Ecole Centrale" in Rouen. Cuvier advised him
to wear a wig to look older and more serious!
But Savigny was never to go to Rouen. Napo-
leon Bonaparte was already preparing the
Egyptian Campaign.
Bonaparte not only wanted to conquer the
country but also make it a model of French
culture. He added to the expedition troops a
"Commission des sciences et des arts", con-
sisting of scholars, painters, architects and
others. Bonaparte asked his friend Cuvier to
name the naturalists who would join the expedi-
tion. Savigny and Geoffroy Saint Hilaire were
selected for the zoological part. Savigny was
then 21 years old; he had been trained as a
botanist, but Cuvier's opinion was that "he
would become a zoologist when he would decide
to".
The Expedition
After the Battle of Campoformio in 1797,
Bonaparte realized that he could not invade
England, so he decided to make war on Egypt.
In 1798, 38,000 men gathered at Toulon on 335
ships; among them were the members of the
"Commission des Sciences et des Arts". On
Floreal 30th, year VI, (i.e. May 19th, 1798)
Geoffroy Saint Hilaire and Savigny left Toulon.
They were to reach Alexandria 41 days later.
Savigny was placed in the 4th class of the Com-
mission, with a very low salary, but thanks to
Geoffroy Saint Hilaire, he was soon admitted to
the first class.
The Nile was flooding and the expeditionary
forces were directed to Cairo which they en-
tered on July 23 after the Battle of the Pyra-
mids. During this time the Commission settled
in Rosetta for a month. Savigny and Geoffroy
Saint Hilaire stayed for several weeks in the
islands of Lake Menzale; in September they
visited Salahied and Damiette. They worked all
during the autumn in the delta and left Damiette
for Cairo in December. Geoffroy Saint Hilaire
was exhausted, but Savigny was in very good
condition. A current joke of the time in Cairo
was to call scholars, the donkeys, then used as
"taxis", because the members of the Commission
were always travelling on donkeys.
Reprints of this article are available for U.S. $7.00
(postage paid) from American Malacologists. Inc..
P.O. Box 2255, Melbourne. FL. ;32901, U.S., A.
10 THE NAUTILUS
January 25, 1982
Vol. 96(1)
Between August 1 and 2, Nelson defeated the
French Naw in Aboukir and cut all contacts
with F" ranee. In Cairo, Bonaparte organized the
country under his rule and founded the "Institut
d'Egypte". He then prepared the expedition to
Syria 13,000 infantrymen and the cavalry left
in the beginning of February, 1799. After sev-
eral victorious battles, Bonaparte was finally
stopped at Saint Jean d'Arce, where 4,000 were
killed. On June 14 the army was back in Cairo,
Savigny was the only naturalist to follow the
troops.
In August, Bonaparte turned over the com-
mand to Kleber and returned to Paris, where
the "Directoire" was weakened. The members of
the "Commission" were sent to Suez at the end
of 1 799. Savigny was very e.xcited by the wealth
and beauty of the Red sea fauna. But Kleber had
to face the Turks and the British and the
scholars were sent back to Cairo. Kleber was
murdered shortly after he won the Battle of
Heliopolis; France was then finally defeated at
Canope in 1801.
The journey of the 45 members of the "Com-
mission" back to France was rather unfortu-
nate. On April 6, 1801, they left Cairo for Alex-
andria. On their arrival they were quarantined
by the French general, Menou. They were trans-
ferred to a brig, and waited 21 days for permis-
sion to leave the bay. The British troops stopped
them, took them to Abukir, then back to Alexan-
dria. Menou had surrendered on terms stipulat-
ing that the collections gathered by the "Com-
mission" in Egypt should be given to the British.
The scholars rebelled and threatened to destroy
the collections. Finally, on September 26, 1801,
they were allowed to go back to France with
their collections.
The Original Plates
Savigny returned to Paris in February, 1802.
He did a great amount of work on the material
he took back with him and published various
papers and memoirs between 1801 and 1810.
Among them were the study of 1,200 insects
and his famous "Histoire naturelle et mytholo-
gique de I'Ibis" (1805). In 1817, he published
125 plates for the atlas of the "Expedition
d'Egypte", in "grand-aigle" size (71.5 x 52 cm);
in 1826 they were reprinted by Panckoucke in
reduced size (68.5 x 52 cm). These engraved
plates were prepared from the original colored
vellums now preserved in this Museum's library.
They had beon drawn very accurately, with a
wealth of details, by the best artists of the time.
Because the "Commission" judged that they
were too difficult to reproduce in color, only
black and white copies were printed.
Savigny suffered progressively failing eye-
sight, approaching blindness after 1815, for
which reason he never published any text to ac-
company the plates. But Cuvier found that this
iconography was unique and Audouin was cho-
sen to write an explanatory part. Audouin was a
professor of entomology at the Museum, and
was not prepared for this work. But he was the
son-in-law of Brongniart, a member of the "In-
stitut", director of the Sevres manufacture, and
a friend of the powerful Cuvier.
There is considerable difficulty in determining
the exact dates of publication of the "Explica-
tion sommaire des planches", of which two edi-
tions were printed.
The first edition bears on the title page "public
par les ordres de sa majeste I'Empereur
Napoleon Le Grand" and is dated 1809 on the
cover page, but was evidently published much
later (Laissus, 1973); the Mollusca are treated in
tome 1, part 4, and begin with a copy of a letter
dated Nov. 1, 1825! The register of the letters
and declarations of the "Commission d'Egypte",
kept in the Manuscript Department of the Na-
tional Library, Paris, shows that the Natural
History section belongs to the third issue of
reports. On April 13, 1826 the last manuscript
by Audouin concerning shells was sent to the
"Imprimerie Royale", but we could not deter-
mine whether the first edition, third issue, was
actually printed before the end of 1826.
However it seems wise to assume that Sherborn
(1897:287) was right and that this part "may be
safely regarded as dated 1826."
Almost simultaneously a second edition,
"dediee au roi", was being printed by
Panckouke. This bears 1827 on the title page but
it appears also that this date is a fake. Pallary
accepted this date (1827) in a bibliography, but
mentioned 1829 in the text (Pallary 1926). In
fact the earliest date we can ascertain is July 19,
1828 (Bibliographie de la France, 1828).
The text was published while Savigny was still
alive. When he became aware of the contents, he
became very irritated and sent a letter to the
Academy of Sciences. Later on, L. Pfeiffer pro-
nounced similarly .severe judgement, and re-
proached Audouin with the fact that he had
taken all the benefit of Savigny's work. P.
Fischer and Pallary had the same opinion. In the
checklist, we have given references to both edi-
tions of Audouin's text because the first one is
apparently very rare in libraries.
Vol. 96(1)
January 25, 1982
THE NAUTILUS 1 1
Savigny's work, despite its unfinished condi-
tion, was to interest naturalists for a long time.
The very short explanations by Audouin were
later completed, first by Issel (1869), then by
Pallary (1926). But many other authors referred
to Savigny, among them, Jonas (1846), Pfeiffer
(1846), Vaillant (1865), P. Fischer (1865, 1870,
1871), von Martens (1866), Tapparone-Carnefri
(1875), Jousseaume (1888). Many of the speci-
mens depicted by Savigny have therefore be-
come the types of new species, which are
enumerated below.
The Collection
From Egypt, Savigny brought back a rich col-
lection of birds, fishes, mammals, insects and
shells. Included were also mollusks in alcohol,
given by Savigny to Cuvier in 1802; later on
these were said to be deposited in the Gallery of
Anatomy but we have been unable to trace
them.
In 1853, the manuscripts, notes and collec-
tions of Savigny were offered to the town of
Versailles. Curation was entrusted to the
"Societe des sciences naturelles et medicales de
Seine et Oise". Deshayes once planned to publish
a report on the Mollusca collection but never did
(Landrin, 1865). In 1864, the Society realized its
inability to curate the material properly and
asked for help from the Museum. Valenciennes
and Gratiolet were contacted, but the Society
and the Museum lacked the sum of 2,500 francs
to fund the naturalist who intended to work at
Versailles. The collection then sank into obli-
vion. In 1919, the council of the "Societe des
Sciences naturelles" was disbanded because of
World War I. The librarian of the Versailles
library took this opportunity to transfer the col-
lection in a very rough fashion to a cellar in
order to gain some space.
In 1926, when Pallary wrote his "Explication
des Planches", the vellums and collections of
Savigny were considered to be lost. In April
1927, he visited his friend the bryozoologist,
Canu, in Versailles and realized that some shells
in the cellar of the municipal library matched
exactly some depicted on Savigny's plates. Be-
tween August and September, he carefully
studied the shells which were finally to join the
national collections in 1930, together with the 5
volumes of vellums.
Pallary (1931, 1932, 1934) produced a very
detailed history of the expedition and the collec-
tions together with a biography of Savigny. He
evidently had planned to publish a report on the
collection after he had rediscovered it, but only a
small part was published (1932); this concerned
only the shells not depicted in the plates.
We are therefore producing here the latest
chapter of this two centuries-old story with the
realization of the nomenclatorial importance of
this material.
Acknowledgements
We are grateful to the librarians who helped
us during this work and to A. Foubert for
Figures 1-51, Mrs. Guillaumin, Centre de
Microscopie du C.N.R.S. for Figures 52-84 and
P. Lafaite for the colorslides of the vellums.
Figures 93-101. We wish to thank Mr. Richard
E. Petit of South Myrtle Beach, South Carolina,
for making possible the publication of the color
plate.
Checklist of the names based partly or entirely on
Savigny's plates.
It has been our intention to simply list the
material on which a name is based, when the
original description refers to the 1817 plates.
Lectotype designation is the affair of the mala-
cologist actually engaged in a process of revi-
sion of a group and should not be done for the
mere sake of it, as is too often the case in such
checklists.
We are aware of the fact that, strictly, only
the very specimen depicted on Savigny's plate
should be considered the tyyje of later authors. It
is, indeed, possible to recognize the ty^ie when it
is a large and distinct shell, but it is not so when
dealing with the many microgastropods, of
which Savigny appears to have been the earliest
collector in the Indo-Pacific.
(legyptmcii Ehrenberg, 1831 (Siuxinen) Fig. (51
Savigny 1817: pi. 2, fig. 24
Ehrenberg 18.31: (no page number). Signature E.
Name based on an unknown number of animals from
Damiette and Savigny's figure. One shell in coll. Savigny.
Ehrenberg collection in the Berlin Mu.seum may contain
specimens.
iwgyptidcd Chenu, \8A5 (Tridacna)
Savignv 1817: pi. 10, fig. 1-2
Chenu '1845: 2, pi. 7. fig. 1-2
Name based on Savigny's plate and a number of subfossil
shells from the Suez area. .Judging from the illustrations,
however. Chenu's shells have nothing to do with Savigny's,
and are tyjjical Tridacna mfuimd (Rbding).
affinis Issel, 1869 (Chiton) Fig. .') I
Savignv 1817: pi. 3, fig. 8
lsseri869: 234
Name based on Savigny's figure and seven specimens from
the Gulf of Suez, now in MGD (Genoa, Italy). One specimen
in coll. Savigny. See also sariynyi Pilsbry 1892.
(irsMomsin Issel, 1S69 (Turbo) Fig. 2.5
Savigny 1817: pi. 5, fig. 28
12 THE NAUTILUS
January 25, 1982
Vol. 96(1)
Issel 1869: 220
Name based on Savignv's figure and a subfossil shell which
could not be traced in MGU. Five shells in coll. Savigny.
audouini Jonas, 1846 (Fasciolaria) Fig. 42
Savignv 1817: pi. 4, fig. 17
Jonas i846a: 63
Name based on Savigny's figure. A single specimen in coll.
Savigny is considered to be the holotype.
audouini Jousseaume, in Lamy, 19lH(Pristis) Fig. 86
Savignv 1817: pi. 8, fig. 11
Lamy 1918: 30
Name based on Savigny's figure and two specimens from
Suez, now in MNHN. No Savigny material left.
bacillum Issel, 1869 (Cerithium) Fig. 77
Savignv 1817: pi. 4, fig. 28
Issel 1§69: 340
Name based on Savigny's figure. A single specimen in coll.
Savigny is considered to be the holotype.
bertholleti Issel, 1869 (Rissoina) Fig. 38
Savignv 1817: pi. 4. fig. 2
Issel 1869: 208
Name based on Savigny's figure, named by Audouin 'Rissoa
de Bertholett'. Two shells in coll. Savigny.
bourguignati Landrin, lS65(Unio) Fig. 4
Savigny 1817: pi. 2, fig. 3
Landri'n 1865: 5, fig. 1-3
Name based on Savigny's figure and specimens collected by
Savigny in Damiette (Landrin actually saw the collection).
Three syntypes in coll. Savigny.
brongnartii Audouin, \S26 (Tricoiia) Fig. 26
Savignv 1817: pi. 5, fig. 23
Audouin 1826: 41; 1828: 181
Name based on Savigny's figure. A single specimen in coll.
Savigny is considered to be the holotype.
aiillaudi von Martens, 1866 iSpatka) Fig. 1
Savignv 1817: pi. 7, fig. 1
von Martens 1866: 9
Name based on Savigny's figure and specimens in the collec-
tions of Caillaud, Mousson, Leiden Museum and British
Museum. Two bivalve specimens and one valve in coll.
Savigny.
calloiia P. Fischer, 1 871 (Gen.a) Fig. 32
Savigny 1817: pi. 5, fig. 10
Fischer 1871: 218
Name based on Savigny's figure and specimens collected at
Suez by Gaudry, which could not be traced. Two shells in
coll. Savigny; the small one (3.2 mm) is here depicted. The
larger one (5.8 mm) is chipped and smaller than the natural
size shell depicted fig. 10,5 in Savigny.
carinata Pallarv, 1926 (Risella isseli var.)
Savigny 1817: pi. 5, fig. 34
Pallary 1926: 84
Name based on Savigny's figure and an unknown number of
shells from Suez. See under isseli.
ringulata Issel, 1869 (Eulimella) Fig. 73
Savigny 1817: pi. 3, fig. 25
Issel 1869: 182
Name based on Savignv's figure and 3 specimens from Suez,
two of which are in MGO (Genoa). One shell in coll. Savignv.
The name was changed to TurboniUa isseli by Trvoii
<1886:339) because it is supposedly congeneric with fur-
bonilla nngutatn Dunkcr 1860.
Issel 1869: 177
Name ba.sed on Savigny's figure and a specimen from Suez.
There are two shells with tnis locality m the Issel coll. in
MGD. One specimen in coll. Savigny.
c/j/ppomoru-s Jousseaume. \SSS {Clypeomorus) Fig. 40-41
Savigny 1817: pi. 4, fig. 10
.Jousseaume 1888: 171
Name based on Savigny's figure and an unknown number of
specimens from the southern Red Sea. In the Jousseaume
coll. (MNHN), there are 33 shells from Massawa and 12
shells from Obock. Two shells in coll. Savigny.
eoenobita VaiWant, IS65 (Mytilus) Fig. 12
Savigny 1817: pi. 11, fig. 3
Vaillant 1865: 115, 122
Name based on Savigny's figure and several specimens from
Suez, now in MNHN. One specimen in coll. Savigny.
mncentrica Audouin, 1826 (Doris)
Savigny 1817: Gasteropodes pi. 1, fig. 5
Audouin 1826: 14; 1828: 128
Name based on Savigny's figure. No material left.
Fig. 97
Fig. 18
corbieri JoTtus, lSi&(Chama)
Savigny 1817: pi. 14, fig. 8
Jonas 1846c: 126
Name based on Savigny's figure. Two complete specimens in
coll. Savigny.
craticulata Issel, 1SG9 (Odontostomia) Fig. 75
Savigny 1817: pi. 3, fig. 39
Issel 1869: 180
Name based on Savigny's figure and subfossil specimens,
which could not be traced in MGD (Genoa). One shell in coll.
Savigny.
ruvieri Audouin, l&2G(Emargmula)
Savigny 1817: pi. 1, fig. 9
Audouin 1826: 27; 1828: 152
Name based on Savigny's figure. No material left.
Fig. 89
Fig. 37
dautzenbergi Pallary, 1926 (Donovania)
Savigny 1817: pi. 4, fig. 20
Pallary 1926: 71
Name based on Savigny's figure. A single specimen in coll.
Savigny is considered to be the holotype.
desgenettii "Risso" Audouin, \S2G (Bul.lal Fig. 55
Savignv 1817: pi. 5, fig. 6
Audouin 1826: 39; 1828: 178
Name based on Savigny's figure. Five shells in coll. Savigny.
desmarestii Audouin, 1826 (/Sissoaj
Savigny 1817: pi. 3, fig. 21
Audouin 1826: 36; 1828: 171
Name based on Savigny's figure. No material left.
Fig. 91
Fig. 74
dysmatica Issoi. \St'^>lOdontostomia)
Savigny 1817: pi. 3, fig. 36
Fig. 72
doliiformis Pallary, l92(ifPyrgulina)
Savigny 1817: pi. 3, fig. 42-43
Pallary 1926: 63
Name based on Savigny's figure and several specimens from
Suez, which could not be traced. Five shells in coll. Savigny.
dnrbignii Audouin, \S26IRissoa) Fig. 68
Savignv 1817: pi. 3, fig. 22
Audouin 1826: 36; 1828: 171
Name based on Savigny's figure. A single specimen in coll.
Savigny is considered to be the holotype.
dftrbigvii Audouin, \?<2(>(Snssurella) Fig. 63
Siivignv 1817: pi. 5, fig. ,30
Audouin 1826: 42; 1828: 183
Name based on Savigny's figure. Five shells in coll. Savigny.
Vol. 96(1)
January 25, 1982
THE NAUTILUS 13
doriae Issel, 1869 (Stomatella) Fig. 48
Savigny 1817: pi. 5. fig. 8
Issel 1869; 228
Name based un Savigiiy's figure and 10 specimens from
Suez, which could not tje traced in MGD. Seven shells in coll.
Savigny.
draparnaudi Audomn, IS26 (Tricolia) Fig. 46
Savigny 1817: pi. 5, fig. 19
Audouin 1826: 41; 1828: 181
Name based on Savigny's figure. Two shells in coll. Savigny.
elata Semper, in Issel, 1869(Sfa/io/a^ Fig. 84
Savigny 1817: pi. 3. fig. 15
Issel 1869: 330
Name based on Savigny's figure. Fifteen shells in coll.
Savigny.
elegans Audouin, 1S2G (Tritonia)
Savigny 1817: Gasteropodes pi. 2, fig. 1
Audouin 182?: 15; 1828: 130
Name based on Savigny's figure. No material left.
Fig. 94
Fig. 24
eroopotitanus Issel, 1&Q9 (Turbo)
Savigny 1817: pi. 5, fig. 27
Issel 1§69: 219
Name based on Savigny's figure and one specimen from Suez
which could not be traced in MGD. Six shells in coll. Savigny.
erythraea Hupe, 1SS4 (Blanivillia) Fig. 94
Savigny 1817: pi. 8, fig. 6
Hupe 1854: 223
Name based on Savigny's figure. Two valves in coll. Savigny.
erythraea Issel, 1869 (Nassa costulata var.) Fig. 44
Savigny 1817: pi. 6, fig. 4
Issel 1869: 126
Name based on Savigny's figure and specimens from Suez
which could not be traced in MGD. One shell in coll. Savigny.
erythraealsse], 1SQ9( Lticina) Fig. 20
Savigny 1817: pi. 8, fig. 8
Issel 1869: 84, pi. 1, fig. 9
Name based on Savigny's figure and 3 specimens from Suez
which could not be traced in MGD. One shell in coll. Savigny.
erythrofa Issel, 1869 (Area lactea var.)
Savigny 1817: pi. 10, fig. 7
Issel 1869: 89
Name based on Savigny's figure and 6 specimens from Suez.
Six paired valves in coll. Savigny.
favrei Landrin, 1865 (Helix) Fig. 21
Landrin 1865: 2, fig. 1-3
Name based on a shell from the Savigny coll., not depicted in
the atlas. Holotype in coll. Savigny.
ferussacii Audouin, 1826 (Scalaria) Fig. 81
Savigny 1817: pi. 3, fig. 13
Audouin 1826: 35; 1828: 169
Name based on Savigny's figure. One shell in coll. Savigny is
considered to be the holotype.
feuilletii Audouin, 1826 (Neritina) Fig. 28
"Savigny 1817: pi. 5, fig. 11
Audouin 1826: 40; 1828: 179
Name based on Savigny's figure. A single shell in coll.
Savigny is considered to be the holotype.
fourierii Audouin, 1S2& (Bulla) Fig. 54
Savigny 1817: pi. 5, fig. 5
Audouin 1826: 39; 1828: 178
Name based on Savigny's figure. A single shell in coll.
Savigny is considered to be the holotype.
Ireminvillii Audomn, lS2(\(Kist;ua) Fig 67
Savigny 1817: pi. 3, fig. 20
Audouin 1826: 36; 1828: 170
Name based on Savigny's figure. A single shell in coll.
Savigny is considered to be the holotype.
gennesi H. Fischer, 1901 (Claneulus) Fig 49
Savigny 1817: pi. 3, fig. 3
Fischer 1901: 123, pi. 4, fig. 11-12
Name based on Savigny's figure and one specimen from
Djibouti, now in MNHN. Five shells in coll. Savigny.
gevtiluomiana Issel, lS69(Eulima) Fig. 78
Savigny 1817: pi. 3, fig. 32
Issel 1869: 183
Name based on Savigny's figure and four shells from Suez.
There are 6 shells witfi this locality in MGD. Three .speci-
mens in coll. Savigny.
quenni Audouin. 1826 fTrico/ia^
Savigny 1817: pi. 5, fig. 24
Audouin 1826: 41; 1828: 181
Name based on Savigny's figure. Pallary argued that this is
only a color form of T. brongnarti. No material left.
girardi Audouin, 182& (Bulla) Fig. 52
Savigny 1817: pi. 5, fig. 3
Audouin 1826: 39; 1828: 178
Name based on Savigny's figure. A single shell in coll.
Savigny is considered to be the holotype.
hemprichi Ehrenberg, 1831 (Helix) Fig. 27
Savigny 1817: pi. 2, fig. 12
Ehrenberg 1831: Helix no. 4 (no page number)
Name based on a number of snails collected near Alexandria
and on Savigny's figure. 24 shells in coll. Savigny. The
Ehrenberg coll. is supposedly in Berlin.
hemprichi \&se\, \i>%9 (Trochus) Fig. 22
Savigny 1817: pi. 3, fig. 6
Issel 1869: 329 _
Name based on Savigny's figure. Six shells in coll. Savigny.
/wjrn'dMS Orbigny, li,2() (Octopus) Fig. 100
Savigny 1817: Cephalopodes pi. 1, fig. 2
Orbignv 1826: 144
Name based on Savigny's figure. No material left.
kumboldti Audouin, \B2() (Anatola)
Savigny 1817: pi. 5. fig. 1
Audouin 1826: 39; 1828: 177
Name based on Savigny's figure. No material left.
immaculata Audouin, 1826 (Doris)
Savigny 1817: Gasteropodes pi. 1, fig. 2
Audouin 182?: 13; 1828: 126
Name based on Savigny's figure. No material left.
Fig. 85
Fig. 93
infracostata Issel, \SS9(Riselln) Fig. 64
Savigny 1817: pi. 5, fig. 40
Issel 1869: 195
Name based on Savigny's figure and three specimens from
Suez, which could not be traced in MGD. Three shells in coll.
Savigny.
i'sseli Semper, in Issel, 1869 (Risella) Fig. 65
Savigny 1817: pi. 5, fig. 35
Issel 1869: 194
Name based on Savigny's figure and several specimens from
Suez and Zanzibar. There are 2 shells from Zanzibar with a
label in Semper's handwriting in MGD. Five shells in coll.
Savigny.
isseli Nevill & Nevill, 1875 (Marginella)
Nevill & Nevill 1875: 95
Fig. 57
14 THE NAUTILUS
January 25, 1982
Vol. 96(1)
New name for Marginelta pygmaea Issel 1869, non Sowerby
1846. See pygmaea.
isseli Trvon, XSSQ (TurhoniUa)
New name for Eulimella cingulata Issel 1869. See this
name.
tstfemicuTO Issel, 1869 ^Cardwmj F'g- 1^
Savignv 1817: pi. 9, fig. 11
Issel 1§69: 74 , , • f
Name based on Savigny's figure and several sp?cirneris from
Attaka, near Suez, which could not be traced in M(,t). One
valve in coll. Savigny.
jmnardi Audouin, 1 826 (Scalaria) Fig' '^'^
Savignv 1817: pi. 3, fig. 4
Audouin 1826: 3.5; 1828: 169 . . , u „ ■ ii
Name ba.sed on Savigny's figure. A single shell in coll.
Savigny is considered to be the holotype.
hi n th a Audouin , 1 826 (Cypraea) Fig. 33
Savigny 1817: pi. 6, fig. 27
Audouin 182?: 4.5; 1828: 190 . . , u „ ■ u
Name based on Savigny's figure. A single shell in coll.
Savigny is considered to be the holotype.
lamarckii Audouin, 1826(PMpa^ Fig. 83
Siivignv 1817: pi. 2, fig. 1
Audoufn 1826: 31; 1828: 161 . , . „ ■
Name ba.sed on Savigny's figure. A single shell in coll.
Savigny is considered to be the holotype.
teroii Landrin, 1 865 (Helix) Fig. 23
Landrin 1865: 4, fig. 1-4 , , ^ . . .. „
Name based on a shell collected by Savigny at the Fyra-
mides, not depicted in the atlas. Holotype in coll. Savigny.
lessepsianus Vaillant, 1865 iLUhodomus) Fig. 1 1
Savignv 1817: pi. 11, fig. 1
Vaillant 1865: 123 , • .
Name based on Savigny's figure and several specimens trom
the gulf of Suez, two of which are in MNHN. One specimen
in coll. Savigny.
Fig. 17
mareoticum Pallarv, 192S (Cardiiim)
Savigny 1817: pi. ?), fig. 10
PallarVl926: 109
Name ba.sed on Savigny's figure. One specimen in coll.
&ivigny is considered to be the holotype.
marmorata Audouin, 1 826 (Doris) Fig. 95
Savignv 1817: Gasteropodes pi. 1, fig. 7
Audoutn 1826: 14-15; 1828: 129
Name based on Savigny's figure. No material left.
marmorata Pallary, 1926fGCTta; Fig. 31
Savigny 1817: pi. 5, fig. 9
Pallarv 1926: 76
Nameoased on Savigny's figure. Four shells in coll. Savigny.
marfen-si Issel, 1869 (Alaba) Fig. 71
Savignv 1817: pi. 3, fig. 26
Issel lJi69: 206
Name based on Savigny's figure and a subfossil specimen
from the Red sea, which could not be traced in MGI). Four
shells in coll. Savigny.
rtwngii Audouin, 1826rB»/W Fig. 58
&vi'gny 1817: pi. 5, fig. 7
Audouin 1826: 39; 1828: 178
Name based on Savigny's figure. A single specimen in coll.
Savigny is considered to be the holotype.
oblongun Audouin. \&2i\ I FJ nun ibrnnchus) Fig. 98
Savigny 1817: Gasteropodes pi. 3. fig. 1
Audouin 1826: 20-21; 1828: 140
Name based on Savigny's figure. No material left.
olivaefonni'i Issel, 1869 (Tomatina) Fig. 56
Savigny 1817: pi. 6, fig. 25
Issel 1869: 171 , , .
Name based on Savignv's figure and three specimens trom
Suez, one of which is in MGD. One shell in coll. Savigny.
perlntus Issel , 1869 (Triforis) Fig. 79
Savigny 1817: pi. 4, fig. 4
Issel 1869: 152 ,,,.., ■ ,
Name based on Savigny's figure and subfossil specimens, ot
which one is in MGD with the data 'Red sea'. One shell in coll.
Savigny. See also savignyanus.
pharaonis P. Fischer, 1871 (Area) Fig. 7
Savignv 1817: pi. 10, fig. 9
Fischer 1871: 213 , , • ,
Name based on Savigny's figure and several specimens trom
Suez which could not Be traced. One valve in coll. Savigny.
iMraonis P. Fischer, 1870 (Mytilus) Fig. 10
Savigny 1817: pi. 11, fig. 5
Fischer 1870: 169 , ■ r
Name based on Savignv's figure and several specimens trom
Suez, of which six bivalve specimens and one valve are m
MNHN. One specimen in coll. Savigny.
philippii Issel, 1869 (Cydostremn) Fig. 66
Savigny 1817: pi. 5, fig. 33
Issel 1869: 189 , . • ^ c
Name based on Savignv's figure and 6 specimens trom Suez
which could not be traced in MGD. Two shells in coll.
Savigny.
pulvis Issel, 1869 (Cerithium) ' Fig. 35
Savigny 1817: pi. 4, fig. 5
Isseri869: 1.50 , ,
Name based on Savigny's figure and one or several
specimens from Suez of which one is in MGD in Genoa. One
shell in coll. Savigny.
miqmaea Issel, 1869 (Marginella) Fig. 57
Savigny 1817: pi. 6, fig. 26
Issel 1869: 150 , c, ■ ■ r ,
Name based (with question mark) on Savigny s figure anti
one shell from Suez, now in MGD. Four shells in coll.
Savigny.
reticulata Philippi, 1853 (Scissurella) Fig. 62
Savignv 1817: pi. 5, fig. 29
Philippi 18.53: 38, pi. 6, fig. 11 ^,. , , . ,.
New name fi)r "Scissurella decussatn Orbigny. .-^ucJouin
(1826:42; 1828:183), not Orbigny, 1824. Therefore the name
is based on Savignv's figure; Phihppi also refers to
specimens from thp Red Sea collected by Hempnch and
Ehrenberg. Four shells in coll. Savigny.
richardi Audouin, 182& (Cardiuvi) Fig. 14
Savigny 1817: pi. 9, fig. 14
Audouin 1826: 51; 1828: 201
Name based on Savigny's figure. One specimen m coll.
Savigny is considered to be the holotype.
rissoi Audouin, 1826 (Tricolia) Fig. 47
Savignv 1817: pi. 5, fig. 18
Audouin 1826: 41; 1828: 181
Name based on Savigny's figure. Two shells in coll. Savigny.
rissoi Weinkauff, 18S5 (Rissoina)
Savignv 1817: pi. 4, fig. 1
Weinkauff 1885: 63. pi. 15d
Fig. 76
,. „„, ^ fig. 13
Name based on the name 'Manzelia de Risso' Audouin (1828:
171) and a shell from Mauritius. Two shells in coll. Savigny.
Vol. 96(1)
January 25, 1982
THE NAUTILUS 15
roemeriana Issel, IS&d (Verms) Fig. 62
Savigny 1817: pi. 8, fig. 3
Issel 1869: 64
Name based on Savigny's figure and 7 valves from Suez, now
in MGD. Seven valves in coll. Savigny.
savigniana Audouin. IS26 (Bursatella) Fig. 99
Savigny 1817: Gasteropodes pi. 2, fig. 2
Audouin 1826: 17-18; 1828: 134
Name based on Savigny's figure. No material left.
saifignyana Ehrenberg, 1831 (Helix)
Savigny 1817: pi. 2, fig. 20
Ehrenberg 1831: Helix no. 9 (no page number)
Name based on three specimens collected near Alexandria
and Savigny's figure. Pallary however (1926: 47) argues that
Ehrenberg's species is different from the one on Savigny's
figure, which indeed depicts Zonites algirus (^Linne),
represented by 4 shells in coll. Savigny. If Ehrenberg s types
proved to be lost (they are supposedly in the Berlin
Museum),. the present material appears to be formally avail-
able for lectotype designation if it proves necessary for
nomenclature stability.
savignyanus delle Chiaje, 1828 (Murex)
Savigny 1817: pi. 4, fig. 4
delle C"hiaje 1828: 222. pi. 49, fig. 32-34
Name based on Savigny's figure and additional material
from southern Italy, presumably lost. One shell in coll.
Savigny. See also perlatus.
smngnyi Blainville, 1827 (Sepi'a^
Savigny 1817: Cephalopodes pi. 1, fig. 3
Blainville 1827: 285
Name based on Savigny's figure. No material left.
Fig. 101
Fig. 45
sarngnyi Deshayes, \S44 (PlarKucis)
Savigny 1817: pi. 4, fig. 29
Deshayes 1844d: pi. 109 (with two unnumbered pages of
text)
Name based on Savigny's figure and an unknown number of
specimens from Madagascar, which could not be traced.
Three shells in coll. Savigny.
savignyi Deshayes, 1844 (Purpura) Fig. 30
Savigny 1817: pi. 6, fig. 1
Deshayes 1844a: 112
Name based on Savigny's figure. A single specimen in coll.
Savigny is considered to be the holotype.
sarignyi Jor\2LS, 1S46 (Cytherea) Fig. 15
Savigny 1817: pi. 8, tig. 17
Name based on Savigny's figure. Eight bivalve specimens
and three valves in coll. Savigny.
savignyi P. Fischer, \S€i5 (Cerithium) Fig. 39
Savigny 1817: pi. 4, fig. 8
Fischer 1865: 244
Name based on Savigny's figure and several specimens from
Suez which could not be traced. Two shells in coll. Savigny.
savignyi Vaillant, 1865 (Diplodonta) Fig. 9
Savigny 1817: pi. 8, fig. 7
Vaillant 1865: 124
Name based on Savigny's figure and several specimens from
El Toueneb bank. Red sea, two of which are in MNHN. Two
specimens in coll. Savigny.
savignyi Issel, 18&9 (Litiopa) Fig. TO
Sa\'ignv 1817: pi. 3, fig. 19
Issel 1§69: 197
Name based on Savigny's figure and ten shells from Suez, of
which seven are in MGD. Ten shells in coll. Savigny.
savignyi Issel, \9i%9 (Marginella)
Savigny 1817: pi. 6, fig. 18
Fig. 88
Issel 1869: 115
Name based on Savigny's figure and a number of specimens
from Suez, of which two are in MGD. No Savigny material
left.
sanqnyi P. Fischer, 1871 iPeclunculus) Fig. 3
Savigny 1817: pi. 10, fig. 14
Fischer 1871: 219
Name based on Savigny's figure and one sjiecimen from
Suez, which could not be traced. Two shells in coll. Savigny.
savignyi Tapparone-Canefri, IHlh (Fasciolana) Fig. 43
Savigny 1817: pi. 4, fig. 14
Tapparone-Canefri 1875: 612
Name based on Savigny's figure. A single shell in coll.
Savigny is considered to be the holotype.
samgiiyi Morlet, \S7S (RingieuLa) Fig. 59
Savigny 1817: pi. 6, fig. 7"
Morlet"l878: 117, pi. 5, fig. 1
Name based on Savigny's figure and one shell from the gulf
of Suez, now in MNHlSl. Two shells in coll. Savigny.
savignyi Jousseaume, 1888 (Mesodesma) Fig. 5
Savigny 1817: pi. 8, fig. 5
Jousseaume 1888: 206
Name based on Savigny's figure and two left valves from
Cameron island. Red sea, apparently lost. One specimen in
coll. Savigny.
savignyi Pilsbry, 1892 (CaUistochiton keterodon var.)
Savngny 1817: pi. 3, fig. 8
Pilsbry 1892: 277, pi. 60, fig. 16 (copied from Savigny)
Name based on Savigny's figure. It is therefore an objective
synonym of Chiton affinis Issel 1869. which is based on the
same figure.
savignyi Monterosato, 1899 (Meleagrina) Fig. 2
Savigny 1817: pi. 11. fig. 8-9
Monterosato 1899: 392
Name based on Savigiiy's figure and many specimens from
Cyprus and Alexandria, proliably in the Museo Comunale,
Roma. Two specimens in coll. Savigny.
savignyi Pallary, 191% (Fissurella) Fig. 50
Savigny 1817: pi. 1, fig. 5; Pallary 1926: 34
Name based on Savigny's figure and .several specimens from
Suez, which could not be traced. Two shells in coll. Savigny.
.•OTr/'gwV? Pallary, l'i2f>(Gastrochaenal Fig. 13
SavignV 1817: "pi. 1, fig. 15; Pallary 1926: 39
Name based on Savigny's figure and one specimen from
Suez, which could not be traced. One bivalve specimen and 5
valves, some being fragmentary, in coll. Savigny.
savignyi ? aWaxy , 1926 (Lioconcha) Fig. 6
Savigny 1817: pi. 9, fig. 5; PallaiT 1926: 107
Name based on Savigny's figure. One shell in coll. Savigny is
considered to be the holotype.
savignyi Pallary, 1926 (Nassa) Fig. 90
Savigny 1817: pi. 6, fig. 3; Pallary 1926: 87
Name based on Savigny's figure. No material left.
savignyi Pallary, 1926 (Sculus) Fig. 92
Savigny 1817: pi. 1, fig. 10; Pallary 1926: 35
Name based on Savigny's figure. No material left.
savigniji "?\\\\vpp\" Krauss, \^i?, (Siphonaria)
Savigny, 1817: pi. 1, fig. 1; Pallary 1926:28
Krauss, 1848:61; Reeve, vol. 9, pi. 5, sp. 20.
3 syntjpes in MNHN,
seguenziana Issel, 1869 (Rissoina) Fig. 82
Savigny 1817: pi. 4, fig. 3
16 THE NAUTILUS
January 25, 1982
Vol. 96(1)
Issel 1869: 209
Name based on Savig7iy's fig:ure. A single sl^ell in coll.
Savigny is considered to be the holotype.
seynperiana Issel, lS&9(Lucina) Fig. 19
Savignv 1817: pi. 8, fig. 12
Issel lS69: 82
Name based on Savigny 's figure and one specimen from
Suez, which could not be traced in MCID. A single shell in
coll. Savigny.
sismondiana Issel, 1869 (Rissoa) Fig. 87
Savigny 1817: pi. 3, fig. ,33
Issel 1^69; 205
Name based on Savigny's figure and three shells from Suez,
two of which are now in M(jD. No Savigny material left.
sue2irasi'.s' Issel. 1869(A/(iryjnW;o; Fig. 60
Savigny 1817: pi. 6, fig. 17
Issel ito: 115
Name based on Savigny's figure and several shells from
Suez, six of which are in MOD. Si.x shells in coll. Savigny.
siigillata Jonas, 1846 (CythereaJ Fig. 8
Savigny 1817: pi. 9, fig. 3
Jonas i846a: 64
Name based on Savigny's figure and two additional shells
which could not be traced. Two bivalve specimens and one
valve in coll. Savigny.
tiberiana Issel, 1869 (Cingula) Fig. 69
Savigny 1817: pi. 3, fig. 16
Issel 1^69: 199 ^ ^
Name based on Savigny's figure and several specimens from
Suez, of which si.x are in MGD. About three dozen shells in
coll. Savigny.
tigrina .Audouin, 1826(Dorrs^
Savigny 1817; Gasteropodes pi. 1. fig. 3
Fig. 96
Audouin 1826: 13; 1828: 127
Name based on Savigny's figure. No material left.
tninrala (Ferussac m,s) Audouin, "[S'l^lPhysa) Fig. 29
Savigny 1817: pi. 2, fig. 27
Audoum 1826: 34; 1828: 166
Name based on Savigny's figure. Two shells in coll. Savigny.
There are also several shells from Syria, collectea by
Bruguiere and Olivier, in the Ferussac coll. (MNHN).
undata Pallary, 1926 (Risella isseii var.)
Savigny 1817: pi. 5. fig. 35.3
Pallary" 1926: 84 ^
NameDased on Savigny's figure and a number of shells from
Suez, which could not De traced. See under isseii.
unicolor Dautzenberg, in Pallary, 1926 (Cassis turgida var.)
Savignv 1817: pi. 6, fig. 6
Pallary 1926: 88
Name based on Savigny's figure and an additional shell in
Dautzenberg's private collection, which could not be traced
by Abbott (1968: 199). One shell in coll. Savigny.
venusta Issel, 1869 (Turbonilla) Fig. 34
Savigny 1817: pi. 3, fig. 34
Issel 1869: 175
Name based on Savigny's figure and three shells from Suez,
now in MGD. Nine specimens in coll. Savigny.
rillae Issel, 1869 (Cingula) Fig. 80
Savigny 1817: pi. 3, fig. 17
Issel 1869: 198
Name based on Savigny's figure and six shells from Suez,
four of which are in MGD. Seven shells in coll. Savigny.
villersii Audouin, IS'ZG (Bulla) Fig. 53
Savigny 1817: pi. 5, fig. 4
Audouin 1826: 39; 1828: 178
Name based on Savigny's figure. Two shells in coll. Savigny.
FIGS. 1-84. Specimens from the Snvinny Egyptian collec-
tion yww in the Musinim National il'Hi^toire Naturelle in
Paris. France.
1, Spatha caillaudi van Martens, 68 mm.
2, Melcagrina savi^nyi Monterosato, 58 mm.
3, Pectunculus savigiivi P. Fischer, 18 mm.
4, Unio bourguignati Landrin, 2.i mm.
5, Mesodesma savignyi Jousseaume, 20 mm.
6, Lioconcha savignyi Pallary, ,W mm.
7, Area pharaonis P. Fischer, J,8 mm.
8, Cytherea sugillata Jona^, 3J, mm.
9, Diplodonlii savignyi Vnillant, 28 mm.
10, Mylilus pharaonis P. Fischer, .12 mm.
11, Lithodomus lessepsianus Vaiilant, 10 mm.
12, Mylilus coenobita Vaiilant, 7 mm.
13, Ga.sirochaena savignyi Pallary, 11 mm.
14, Cardium richardi Audouin. 10 mm.
15, Gytherea savignyi Jona.s, 35 mm.
16, Cardium isthmic'um Issel, SJ, mm.
17, Cardium mareoticum Pallary, 2J, mm.
18, Chama corliierei ,)onas, .H7 mm.
19, Lucina semiieriana Issel, 4 mm.
20, Lucina erythruea Issel, 16 mm.
21, Helix favroi Landrin, 12 mm.
22, Trochus liemprielii Issel, 2 mm.
23, Helix leroii Landrin. 7 mm.
24, Turbo cr(<opolitanus Issel, ;l mm.
25, Turbo tiisinoensis Issel. J, ynm.
26, Tricoiia brongnartii .4Mrfo»(ii, I, mnL
27, Helix hemprichi Ehri-nlierg. IJ, mm.
28, Neritina feuilietii ,4 «(/.<»)«. /, mm.
29, Physa truncata Audauin, 5 mm.
30, Purpura savignyi Deshayes, iO mm.
31, Gena marmorata Pallary, Jf.7 mm.
32, Gena callosa P. Fischer, 3.2 mm.
33, Cypraea kunthii .Audouin, 22 mm.
34, Turbonilla venusta Issel. 6 mm.
35, Cerithium pulvis Issel, 3 mm.
36, Scalaria jomardi Audouin, 3 mm.
37, Donovania dautzenbergi Pallary. 5 mm.
38, Rissoina bertholleti /,s.sr/. 6' mm.
39, Cerithium savignyi P. Fischer, iO mm.
40, Clypeomorus clypeumorus jDM.s'.-JcaMme. 18 mm.
41, Clyi)eomorus clypeomorus ,/()M.s'.-;c(j»mc. 9 mm.
42, Fasciolaria audouini Jonaii. 135 mm.
43, Fasciolaria savignyi Tapparone-Canefri, 30 mm.
44, Nassa erythraea Issel, 9 mm.
45, Planaxis savignyi Deshayes, 17 mm.
46, Tricoiia draparnaudii j4M(foui>i, 6 mm.
47, Tricoiia rissoi Ai/rfouin, 7 mm.
48, Stomatella doriae Issel, 1, mm.
49, Clanculus gennesi H. Fischer, 8 mm.
50, Fissurella sasngnyi Pallary, 13 mm.
51, Chiton affinis Issel. 9 mm.
52, Bulla girardi .4Miy<min. 2.5 mm.
Xi, Bulla villersii /IwftoMin, 1.25 mm.
54, Bulla fourieri .Audouin. 2.6 mm.
55, Bulla desgenettii .Audouin, 1.8 mm.
56, Tornatina olivaeformis /.s.s-e/. 3.4 mm.
57, Marginella isseii Nerill & Nevill, H mm.
58, Bulla niongii Audouin, 1.6 mm.
59, Ringicula savignyi Morlet, 2.8 mm.
Vol. 96(1)
January 25, 1982
THE NAUTILUS 17
18 THE NAUTILUS
January 25, 1982
Vol. 96(1)
Vol. 96(1)
January 25, 1982
THE NAUTILUS 19
20 THE NAUTILUS
January 25, 1982
Vol. 96(1)
Vol. 96(1)
January 25, 1982
THE NAUTILUS 21
22 THE NAUTILUS
January 25, 1982
Vol. 96(1)
60, Marginella sueziensis Isse.l, 2.95 tmn.
61, Succinea aeg>'ptiaca Ehrenberg, 6.5 mm.
62, Scissurella reticulata Philippi, 1.75 mm.
63, Scissurella dorbignii Audomn, 1.75 mm,.
64, Risella infracostata hsel, 1.15 mm.
65, Risella isseii St-niper in Issel, 1.15 mm.
66, Cyclostrenia philipii /sse/, 1.6 mm..
67, Rissoa freminvillii Audouin, 3.0 mm.
68, Rissoa dorbignii Audouin, 2.5 mm.
69, Cingula tiberiana /sse^, 1.25 mm.
70, Litiopa savignyi Issel, 2.55 mm.
71, Alaba martens"! Issel, 2.3 mm.
72, Odontostomia clysmatica Issel, 2.7 mm.
73, Eulimella ciiijjiilata Issel. 2.6 mm..
74, Pyrgulina doliiformis Paltary. 2.1 mm.
75, Odontostomia craticulata I.'isel. 2.05 mm.
76, Rissoina rissoi Weinkauff, 3.Jt mm.
77, Cerithium bacillum Issel, 3.75 mm.
78, Eulima gentiluomiana Issel. 2.6 mm.
79, Triforis perlatus Issel, i.7 mm.
80, Cingula villae Issel, 2.0 mm.
81, Scalaria {erassa.ci\ Audouin. 1.95 mm.
82, Rissoina seguenziana Issel. 2.8 mm.
83, Pupa lamarckii Audouin, 2.2. mm.
84, Scaliola elata Semper in Issel, 2.05 mm.
87
''%\^
89
■^i.^
90
FIGS. 8.5-92. Types fiffun's copied from Savigny (no type
m.aterial found in SurK/nii inlltrtion).
85, Anatola humboldti .-1 udoum, 35 mm (?).
86, Pristis audouini Jousseaume, 31 mm..
87, Rissoa sismondiana Issel, 2.5 mm.
92
88, Marginella savignyi Issel. h mm..
89, Emarginula cuvieri Audauin, 9.5 mm.
90, Nassa savignyi Pallary, 9 mm.
91, Rissoa desmarestii Audouin, 3 mm..
92, Scutus savignyi Pallary, 7 mm.
<■'■'■' ■" ■ ■ ;. i.-.m, 3.9 mm.
FIGS. 96-103. Savigny's unpublished color vellum.s of
opisthobranchs and cephalopods in Bibliotheque Centrale,
MNHN. Only black and white prints were previously
published.
>^^--^3
t
V -vi?^
96, Doris immaculata Audouin. i6 mm.
*.#
%^ ■ r f. -^
%.
97, Tritonia elegans Audouin, 50 mm.
98, Doris marmorata /I Mrfoitiw, 30 mm.
99, Doris tigrina Audouin. 22 mm.
100, Doris concentrka Audouin. 21 mm.
' )-^**&:::
^
■•i-i^'
,1 ■■ ' ap*";
102, Bursatella savignyana Audouin. 130 mm.
101, Fleurobranchus obiongus .Audouin, 30 ?«/«,
\y^
103, Octopus horridus Orhigny. mantle length 30 mm.
24 THE NAUTILUS
January 25, 1982
Vol. 96(1)
FIG. 94. Blainvillia erythraea Hnpe. 58 mm.
FIG. 95. Sepia savignyi BlainviUe, mantle length 85 mm.
From an unpublished color vellum in the Bibliotheque Cen-
trale, MNHN.
LITERATURE CITED
Abbott. R. T. 1968. The Helmet shells of the World (Cassi-
dae). Part 1. Indv-Paafic Mollusca 2(9):7-202, pi. 1-187.
Audouin, V. 1826. Explication sommaire des planches de
Mollusques de I'Egypte et de la Syrie publiees par J. C.
Savigny. Description de I'Egypte ou recueil des observa-
tions et des recherches qui ont ete faites en Egypte pend-
ant I'expedition de I'armee fran^aise, publie par les ordres
de sa majeste I'empereur Napoleon le grand. Histoire
Naturelle, Animaux invertebres l(4):7-56. Imprimerie
imperiale, Paris.
1828. (same title), 2 erne edition, dediee au roi,
22:117-212. Panckouke, Paris. [1827 on title page is in-
accurate].
BlainviUe, H. M. Ducrotay de 1827. Dictionnaire des sciences
naturelles, 48. Levrauft, Strasbourg. 572 pp.
Chenu, J. C. 1845. Illustrations Conchyliologiques, vol. 2:
Bivalves marins. Genus Tridaena. 2 pp., 8 pi. Paris.
Chiaje, S. delle 1828. Memorie sulla storia e anatomia degli
animali senza vertebre del regno di Napoli, 3:1-232, pi.
31-49. Napoli.
Deshayes, G. P. 1844a. Histoire naturelle des animaux sans
vertebres, 2eme edition, 10. Baillere, Paris. 638 pp.
, 1844b. (no title). Mag. Zool.. Mollusques: pi. 109
(with two unnumbered pages of text).
Ehrenberg, C. G. 1831. Animalia Mollusca, in: Hemprich &
Ehrenberg: Symbolae Physicae, IV: Animalia Everte-
brata. Unnumbered pages. 3 plates.
Fischer, P. 1865. Note sur les launes conchyliologiques des
deux rivages de I'isthme de Suez. Jour. Conchyt. 13:
240-248.
1870. Sur la faune conchyiiologique marine des
baies de Suez et de I'Akabah. Jour. Conchyl. 18:161-179.
1871. Sur la faune conchyiiologique marine de
la bale de Suez. Joar. Conchyl. 19:209-226.
Fischer, II. 1901. Liste des coquilles recueillies par M. de
Gennes a Djibouti et Ali-Sabieh, avec la description de
plusieurs formes nouvelles. Jour. Conchyl. 49:96-130,
pi. 4.
Hup^, H. 1854. Note sur un nouveau genre de Mollu.sque
acephale, genre Blainvillie (Blainvillia). Re^>. Mag. Zool.,
(2)6:219-224.
Issel, A. 1869. Malacologia del Mar Rosso. Ed. della Biblio-
teca Malacologica, Pisa. 387 pp., 5 pi.
Jonas, J. H. 1846a. Beitrag zur Erklarung der in der Des-
cription de I'Egypte abgebildeten, nebst Beschreibung
einiger anderer in rothen Meere und den angrenzenden
Landem lebender Mollusken. Z. Malak. 3:59-64.
1846b. Unbeschriebene Konchylien des rothen
Meeres. Z. Malak. 3:65-67.
1846c. Beitrag zur Erklarung der in der Des-
cription de I'Egypte abgebildeten . . . Z. Malak.
3:120-127.
Jousseaume, F. 1888. Description des Mollusques recueillis
par Mr. le Dr. Faurot dans la mer Rouge et le golfe d'Aden.
Mem. Soc. Zool. France 1:165-223.
Krauss, F. 1848. Die sildafrikanischen Mollusken. 140 pp.
Stuttgart.
Laissus, Y. 1973. Napoleon et rimprimerie. Description de
I'Egypte; bilan scientifique d'une expedition militaire, iyi
L'art du Livre a I'lmprimerie Nationale: 190-205. Im-
primerie nationale, Paris. 295 pp.
Lamy, E. 1918. Les Tellines de la mer Rouge (d'apres les
materiaux recueillis par M. le Dr. Jousseaume). Bull.
M2(.s. natn. hist. nat. 24:26-33.
Landrin, A. 1865. Coquilles nouvelles. Aubert, Versailles.
6 pp., 1 pi.
Martens, E. von 1866. Uebersicht der Land- und Siisswasser
Mollusken des Nil-Gebietes Ma/.aA-. Bl. 7:1-21.
Monterosato, A. di 1899. Coquilles marines de Chypre. Jour.
Conchyl. 47:392-401.
Morlet, L. 1878. Monographie du genre Ringicula Deshayes
et descriptions de quelques especes nouvelles. Jour.
Conchyl. 26:113-133, pi. 5.
Nevill, G. and H. Nevill 1875. Descriptions of new marine
Mollusca from the Indian Ocean. Jour. Asiatic Soc. Bengal
44(2):83-104, pi. 7-8.
Orbigny, A. d' 1826. Tableau methodique de la classe des
Cephalopodes. Ann. Sci. Nat. 7( separate reprint).
Pallarv, P. 1926. Explication des planches de J. C. Savigny.
Mm. Inst. Egypte ll:Viii -h 138 pp., pi. 1-18.
1931. Marie Jules-Cesar Savigny. Sa vie et son
oeuvre. Premiere partie. Mem. Inst. Egypte 17:1-106.
Deuxieme partie (1932). Ibid. 20:1-112. 'Troisieme partie
(1934). Ibid. 23:1-202.
1932. Inventaire de la collection malacologique
de Savigny. Bull. Mus. natn. hist. nat.. 2nd ser., 4(3):
313-321. ■
1933. Les sources d'information concernant les
savants et artistes de I'Expedition d'Egypte. Bull. Inst.
Egypte 15:221-228.
Philippi, R. A. 1853. Die Gattungen Delphinula, Scissurella
und Globulus. Systematisches Conenylien-Cabinet von
Martini und Chemnitz ("second" edition), 2(4):l-57, pi.
1-8. Von Bauer & Raspe, Niirnberg.
Pilsbry, H. A. 1892. Manual of Conchology 14: Polyplaco-
phofa. 350 pp., 68 pi. Philadelphia.
Savigny, J. C. 1817. Description de I'Egypte, ou recueil des
observations et des recherches qui ont ete faites en Eg^'pte
pendant I'Expedition de I'armee fran^aise, publiee par
ordre du gouvernement. Histoire naturelle. Planches, vol.
II. Imprimerie royaie, Paris.
1826. (same title), 2 eme edition, dediee au roi.
Pjinf rCouf kp P urm
Sherborn, C. D. 1897. On the Dates of the Natural History
portion of Savigny's 'Description de I'Egypte'. Proc. Zool.
Soc. Lond.. 1897:285-288.
Ta|iparone-Canefri, C. 1875. Studio monografico sopra i
Muricidi del Mar Rosso. .Ann. Mus. Civ. St. nat. Genova
7:564-640, pi. 19.
Tr>'on, G. W. 1886. Manual of Conchology 8. Philadelphia.
Vaillant, L. 1865. Recherches sur la faune malacologique
de la bale de Suez. Jour. Conchyl. 13:97-127, pi. 6.
Weinkauff, H. C. 1885. Die Gattungen Ris.'ioina und Rts.wa.
Systematisches Conchylien-Cabinet, 2nd ed., l(22):l-205,
pi. 1-25. Bauer & Raspe, Nuremberg.
Vol. 96(1)
January 25, 1982
THE NAUTILUS 25
SHELL MICROSTRUCTURE OF CORBICULA FLUMINEA
(BIVALVIA: CORBICULIDAE)i
Clement L. Counts, III and Robert S. Prezant
College of Marine Studies
University of Delaware
Lewes, DE 19958 U.S.A.
ABSTRACT
The shell microstructure ofCorbicula tluminea was examined using scanning
electron microscopy. The interface between the periostracum and calcareous shell.
and a marginal periostracal loop, are described with a discussion of possible func-
tions. Surface morphology of shells with periostracum chemically removed re-
waled periodic concentric surface ridges. The complex crossed-lamellar
crystalline arrangement of the shell is confirmed.
Shell structure of bivalves in the genus Cor-
bicula (Miihlfeld, 1811) has been examined by
several investigators (Tsujii, I960; Toots and
Fox, 1972; Taylor et al., 1973; Mackie, 1978).
Tsujii (1960) reported that three shell layers
(periostracum, prismatic and pearl [nacreous of
other authors]) are present in C. japonica Prime,
1864, collected from brackish waters of the Tose
River at Tsu, Japan.
Taylor et al. (1973) reported that shells of Cor-
bicula flumin-ea (Miiller, 1774), C. occidens
(Deshayes, 1854), C. cuneiformis (Sowerby,
1817) and the fossil species C. cordata (Morris,
1854) are composed totally of aragonitic calcium
carbonate. Toots and Fox (1972) found that
aragonite, as is typical of this mineral through
geologic time, had metamorphosed to calcite in
fossil shells of Corbicula (Leptesthes) fracta
collected in the Upper Cretaceous strata of
Wyoming.
The outer calcareous shell layers of Corbicula
fluminea and C. occidens are arranged in a finely
crossed lamellar pattern, the inner layers are
complex crossed lamellar and an indistinct myo-
stracum occurs at the pallial line (Taylor et al.,
1973). The complex crossed lamellar layer of C.
fluminea and C. occidens consists of laths ar-
ranged in regular columns as in the Limopsacea
(Taylor et al., 1969).
'University of Delaware College of Marine Studies Contribu-
tion No. 155.
Mackie (1978) examined the shell structure
and mineralogy of Corbicula fluminea in a com-
prehensive ultrastructural study of the fresh-
water Sphaeriacea. Corbicula fluminea has the
thickest shell of the 23 species of sphaeriaceans
studied. Mackie reported that the individual
layers of the complex crossed lamellae, which
are found in all Sphaeriacea, are inclined in op-
jx)site directions. No pallial myostracum, nacre-
ous or outer prismatic layer is present. Mackie
(1978) postulated that thicker-shelled species of
sphaeriaceans have correspondingly thicker
periostraca that protect the shell from dissolu-
tion in acid waters of organically enriched
habitats in which they are found (Ingram et al.,
1953; Mackie and Qadri, 1973).
No single study has carefully examined the
ultrastructure of the interior and exterior sur-
face features of the shell of the Asiatic clam. The
present paper presents such an analysis of the
shell of Corbicula fluminea. using scanning elec-
tron microscopy. The outer surface morphology
is emphasized.
MATERIALS AND METHODS
Specimens of Corbicula fluminea were col-
lected, through the kindness of Dr. Ralph W.
Taylor, from Tygarts Creek, Carter County,
Kentucky, in October 1978. The bivalves were
first relaxed in 7% magnesium chloride or pro-
pylene phenoxytol solutions. Periostracum was
tlien removed with a 5% sodium hjTJOchlorite
26 THE NAUTILUS
January 25, 1982
Vol. 96(1)
solution. Shells were washed in distilled water,
dehydrated through 70% ethanol and placed in a
hot air oven (73°C) for 48 hours to dry. Shells
were then fractured and shell fragments were
selected from the posterior and anterior adduc-
tor muscle scars, the hinge and ligament, the
growing edge, the outer surface near the grow-
ing edge, the pallial line, and the purple inner
surface. Dried shell fragments were mounted on
aluminum SEM pin stubs with double adhesive
tape and silver paint and stored in the hot air
oven (73°C) until coated with metal.
Fractured shells with intact periostracum
were dehydrated in a series of increasing con-
centrations of ethanol solutions to 100% in
which they were stored. Periostracum was also
prepared on whole shells by fixation in 3%i
gluteraldehyde for 7 days. Shells were fractured
and fragments placed in 50% ethanol (5 min.)
and 100% ethanol (28 hrs.). All specimens were
dried in a Denton DCP-1 critical point drying ap-
paratus using carbon dioxide as a transfer
agent. Specimens were then mounted on pin
stubs.
Mounted specimens were coated with a thin
layer of gold in a Denton Vacuum Evaporator
and examined in a Philips PSEM 501 SEM.
RESULTS
A well-developed periostracum covers the
calcerous shell oi Corhicula jlmrdnea. This layer
consists of an extremely smooth external sur-
face, is internally homogenous, and averages 10
ym in thickness. It is firmly conjoined with the
underlying aragonitic crystals.
The periostracum terminates along the ven-
tral shell margin in a reflective loop before in-
FIG. 1. Pi'notitnicat loop al vetitral shell margin. Uirectiun
of growth to the top. Hortzonlal field width = i!55 piw.
gressing to the secretory mantle (Fig. 1). Thus,
upon emergence from the mantle, the periostra-
cum remains disattached from internal calcer-
ous shell and extends up to 580 \j.m beyond the
shell edge in a loop that often bends back over
the outer shell margin. Where the periostracum
closely overrides the outer shell surface, the at-
tachment is very tight and rarely is this organic
layer seen to peel away from the calcareous ex-
oskeleton.
Ultrastructural examination of fractured shell
fragments confirms the complex crossed lamel-
lar structure reported by Taylor et al. (1973) and
Mackie (1978) (Fig. 2). Bands of crystalline laths
are arranged approximately normal to each
other. Individual layers or bands have an
average thickness of 10 ^im (Fig. 3) while in-
dividual crystalline laths are approximately 0.7
\jin in diameter.
A cursory examination of the outer surface oi
shells from which periostacum has been re-
moved with sodium hj'pochlorite reveals annula-
tions or major ridges visible to the unaided eye
that are separated by fine, concentric striations
FIGS. 2-7. 2, Radially fractured shell o/ Corbicula fluminea demo iist rat iri.y complex crossed lamellar structure. Direc-
tion of growth lo the right. Horizontal field width = 900 lim. 3, Normally arranged crystalline laths composiyig the com-
plex crossed lamellar shell. Direction of growth to the right. Horizontal field width = 8 (jto- 4, Outer shell surface.
periostracum removed, showing concentric major annulationis (arrows), unequally spaced, and finer, subannular concen-
tric striae helween major annulae. Direction of growth lo the right. Horizontal field width = 5.3 mm. 5, Shell surface,
perkmlnwum removed, in fractured specivwn. Two growth zones are found in association with the major annulae (ar-
rows). Direction of growth lo the right. Horizontal field width = 2.J, mm. 6, Growth zones demonstrating rugose, perforate
zones terminating in a thick band of shell, the periphery of which apparently marks the end of a growth peri.od (A), a
smooth hand oj shell that becoines rugose, perforate, and grooved and then smooth, terminating in a small ridge (B) and a
wide band of nigi.se. perforate shell (C). Direction of growth to the left. Horizontal field uidth = .'ISO urn.. 7, Rugose, per-
forate bond oj oilier shell surface sculpture organized into radial ridges and grooves with surj'ace perforatiuris. Direction
of growth In the nght. U'jrlzonhil field width = 82 \im.
Vol. 96(1)
January 25, 1982
THE NAUTILUS 27
(Fig. 4). Under higher magnification (Fig. 5)
three major striations are often found in
association with each large concentric annula-
tion. The surface morphology of a single major
ridge system (Fig. 6) changes with growth,
showing different patterns of rugosity that ap-
Vol. 96(1)
January 25, 1982
THE NAUTILUS 28
pear to be associated with cessation of growth
and that alternate with smooth areas at the ap-
parent beginning of renewed shell growth. The
largest region of rugose shell was found in areas
preceeding an apparent growth halt (Fig. 7).
This region demonstrated an overall pattern of
perforations and grooves that are radially
oriented. The grooves were either interrupted
or anastomosing and had an average width of
1-2 fjim. Perforations within this zone (Fig. 8)
were of various sizes, ranging from the ir-
regularly ovoid largest holes measuring 0.75 x
1.00 nm at their greatest dimensions, to the
smallest, more circular holes with an average
diameter of 0.5 j^m. The largest perforations
usually occurred at the bottom of the radial
grooves. The small perforations were usually
found on walls bordering grooves. No perfora-
tions penetrated very deeply into the interior of
the shell (Fig. 9). This rugosity is a natural oc-
currence on the calcareous shell of Corbicula
fiwminea and is not an artifact caused by
chemical removal of the periostracum. This is
evidenced by the alternating smooth areas.
The zone of perforated grooves terminates in
a narrow (approximately 20-30 f.im) band of
thick, radially arranged microstructures (Fig.
10). This calcareous band is continuous with the
FK.S. 8-10. o, hiny.-ijroove sculplnre ikrminstrntiHn varying Kizes of perforations. Direction of yrowth to the right.
Horhotit'it fielil u-idlh = li) nm. 9, FrnHitrc section of shell with periostracum removed. Note .luperficinl perforations.
Direction of ijrowlh to the right. Horizontal field width = S2 tim. 10. Thick, concentric hand (D) terwinatimj the ridge-
groon sralplurc. \,w shell (E) appears to be laid down from beneath this band. Direction of growth to the lejl. Horizontal
field ic'dth = I,,-; ii7,i.
Vol. 96(1)
January 25, 1982
THE NAUTILirS 29
FIG. 11. Thr 5 fjiiii ridge (B) xcpdnilutg smoolh bam! (F)
from rugose band (C) of shell. Perforation's of the. rugose band
are r}ot organized into ridge-groove patterns at this stage.
Tile sntiMith hand has few. scattered perfdrolnois. Dinclidii
of groiiili III Hie right. Hnrizniiliil field ivnllli = to jj/h.
radial-perforate zones, and has few perfora-
tions. The leading edge of this zone apparently
represents the end of a growing period.
A concentric ridge averaging 5 ytm in width
was found 110 ^m from the band of apparent
growth cessation (Fig. 6). Between these two
points, three transitional surface patterns were
found; a band of smooth surfaced shell averag-
ing 25 [im in width with diffuse perforations, a
25 fim-wide band of grooved, perforate surface
similar to that preceeding the thickened calcium
band before the apparent growth pause, and a
60 yim wide band of smooth surfaced shell that
terminates in the 5 ^^m-wide ridge.
Immediately following the 5 \xm ridge, the
shell surface becomes more rugose with perfora-
tions averaging 2-4 \xm in diameter (Fig. 11).
These perforations are heterogeneous but
gradually gain organization as they meld with
the ridge-groove pattern found later in the
growth period (Figs. 6, 7, and 8) and terminate
in the thickened surface sculpture (Fig. 10).
DISCUSSION
The periostracum tightly fills the irregular
contours of the underlying calcareous shell sur-
face as shown in Figin-e 10. Presumably the
periostracum has fully polymerized prior to the
initiation of calcium carbonate deposition on this
organic template (Waite and Wilbur, 1976), so
that this intimate association is more likely a
result of aragonitic nuclei being deposited in
rugosities of a preformed periostracal mold. In
any event, the tight fit between periostracum
and calcareous shell typically leaves an intact
outer organic layer over the aragonitic shell and
the only evidence of periostracal wear occurs
around the umbones.
The marginal periostracal looj) is an interest-
ing morphological feature whose function is
unclear. The periostracal extension might allow
free range of motion of the mantle so that upon
withdrawal of the mantle the periostracum
would easily follow. Thus upon adduction perio-
stracum would form an effective seal at the shell
edge.
The curvature of the periostracal loop, if
maintained during mineralization might offer a
mold for formation of calcareous concentric
shell ridges. Loop size corresponds well with
that of major concentric ridge size, lending sup-
port to this hypothesis. Extensive periostracal
folding along the mantle margin occurs com-
monly in many marine bivalves [for example.
Area zebni (Waller, 1980)]. "Excess" marginal
periostracum is probably a reflection of perio-
stracal growth exceeding development of cal-
careous shell. This phenomenon still requires
careful analysis.
Morton (1977) found that populations of Cor-
bicula Jluminea in Plover Cover Reservoir,
Hong Kong, spawn twice a year. He pointed out
that shell growth appeared to stop during these
episodes as energy is redirected to gonadal
development. The first spawning in the spring
of the Plover Cover population was the most in-
tensive, followed by a less intensive one in the
fall or late summer (Morton, 1977). Although
Morton (1977) reported no shell surface changes
that correspond to spawning seasons, if metabo-
lism is redirected so that only gonads are
developed and shell growth ceases, this halt
should be reflected in the surface morphology of
the shell. Fuziwara (1975, 1978) reported Cor-
hirula leana spawns biannually in response to
thermal stimuli and while portions of the gonad
ai'e mature throughout the year, the overall rate
of gametogenesis is unknown. Jones (1981)
recently reported variations in shell growth in-
crements that correspond to thermal variation
30 THE NAUTILUS
January 25, 1982
Vol. 96(1)
in the marine environment. The pattern of .sur-
face shell sculpture seen in the Tygarts Creek,
Kentucky, population may be the result of
redirected energetics during gametogenesis and
change in surface sculpture seen in Figure 10
represents the terminal period of shell growth
before gonadal development or a response of the
bivalve to fluctuations in thermal regime.
ACKNOWLEDGMENTS
We thank Dr. Ralph W. Taylor, Department
of Biological Sciences, Marshall University,
Huntington, West Virginia, for his assistance in
the collection of the bivalves used in this study.
We are also indebted to Dr. Melbourne R. Car-
riker, College of Marine Studies, University of
Delaware, Lewes, for his review of the manu-
script and Dr. Gerald L. Mackie, Department of
Zoology, University of Guelph, Ontario, for his
comments and discussion. Appreciation is also
extended to Mr. Walter H. Denny, Department
of Mechanical and Aerospace Engineering, Uni-
versity of Delaware, Newark, for his technical
assistance, Ms. Pam Palinski for her photo-
graphic help, and Ms. Linda Leidy for typing the
final versions of the manuscript.
LITERATURE CITED
Fuziwara, T. 197.S. On the reproduction of Carhiculii Icana
Prime. Venus 34(l):54-56.
1978. On the ovulation n{ Ciirhiruin lennn Prime.
VV?!«.s 37(l):22-28.
Ingram, W. M., U. G. Rallinger and A. K. Gaul'in. 19.'):i. Ke-
latitmship of Sphaerium nolidum Prime to organic pollu-
tants. Ohio J. Sci. 53(4):230-235.
Jones, D. S. 1981. Annual growth increments in shell.s of
Sjiisula soLidissima record marine temperature varia-
bility. Science 211(4778):165-166.
Mackie, G. L. 1978. Shell .structure in freshwater Sphae-
reacea (Bivalvia: Heterodonta). C'nuidian Jour. ZooL
56(l):l-6.
Mackie, G. L. and S. V . Qadri. 1973. Abundance and dis-
tribution of Mollusca in an industrialized portion of the
Ottawa River near Ottawa - Hull, Canada. Jour. Fish.
Res. Bd. Canada. 30:167-172.
Morton, B. 1977. The population dynamics of Corbicula
fluminea (Bivalvia: Corbiculidae) in Plover Cove Reser-
voir, Hong Kong. Jour. ZooL. London, 181(l):21-42.
Taylor, .J. D., W. I. Kennedy and A. Hall. 1969. The shell
structure and mineralogy of the Bivalvia. Introduction.
Nuculacea - Trigonacea. Bull. British Mus. (Nat. Hist.).
ZooL Suppl. 3. pp. 1-125.
1973. The shell structure and mineralogy of the
Bivalvia. II. Lucinacea - Clavagellacea. Conclusions. Bull.
British Mus. (Nat Hist.) ZooL. 22(9):2,55-294.
Toots, H. and J. E. Fox. 1972. Inversion of aragonite to
calcite in Corbicula (Leptesthes) fracta from upper Creta-
ceous strata of Wyoming. Contrib. Geol. 12:11-14.
Tsujii, T. 1960. Studies of the mechanism of shell and pearl
formation in molluscs. Jour. Fac. Fish.. Prefect. Univ.
M(V 5:1-70.
Waite, J. H. and K. M. Wilbur. 1976. Phenol oxidase in the
periostracum of the marine bivalve Modiolus demissus.
Jour. Exper. ZooL. 195:359-367.
Waller, T. R. 1980. Scanning electron microscopy of shell
and mantle in the order Arcoida (Mollusca: Bivalvia).
Smithsonian Cuntr. ZooL 313: 58 pp., 46 figs., 1 table.
A RELIC POPULATION OF OBOVARIA RETUSA IN THE
MIDDLE CUMBERLAND RIVER, TENNESSEE
Paul W. Parmalee and Walter E. Klippel
Department of Anthropology
University of Tennessee
Knoxville, TN 37916 '
ABSTRACT
Recovery in 1980-1981 of three specimens o/Obovaria retusa (Lamarck, 1819)
from cull piles left by commercial shelters provides additional evidence of an ex-
tant relic population of this naiad in the middle Cumberland River, Trousdale
County, Tennessee.
The fornior dir-triliution of Obovaria retusa
(Lamarck, 1819) included the Ohio, Cumber-
land, and Tennessee River systems. This mus-
sel, called by the common name Golf Stick by
Vol. 96(1)
January 25, 1982
THE NAUTILUS 31
Boepple and Coker (1912) and known variously
as Pink, Ring Pink, Ram's Horn Pink, Pink
Pigtoe or Rosebud by commercial shellers,
typically inhabits the deep stretches of a river
having swift current and a substrate composed
of coarse sand and gravel. Obovaria retusa has
been extirpated throughout most of its former
range. Stansbery (1970) stated that "A popula-
tion still living in the impounded lower Ten-
nessee [below Pickwick Dam] had apparently
not reproduced since impoundment and is ex-
pected to die out. The only known breeding
population of this once widespread species is a
small one in the Green River near Munfordville,
Kentucky." Stansbery has since commented
(Personal Communication, October 1980) that
the Green River population appears to be no
longer viable and very possibly has been entirely
eradicated. Commercial shellers still occasion-
ally take a large old relic individual from
stretches of the Tennessee River below Pick-
wick Dam, but the animal is extremely rare
judging by the limited numbers encountered.
Prior to impoundment, 0. return occurred
throughout the Cumberland River "although by
no means abundant anywhere" (Wilson and
Clark, 1914). However, Neel and Allen (1964). in
their study of the mussel fauna of the upper
Cumberland River basin before impoundment,
found it to be fairly common on the big stream
bars below the falls. 0. rptui^n was not found
during a collection made by Stansbery (1969)
after impoundment of the same general area
surveyed by Neel and Allen (1964). Tennessee
Valley Authority biologists (TVA, 1976), how-
ever, reported finding the Ring Pink (numbers
and location not given) at a sheller's cook-out
area during their mussel survey of the middle
Cumberland River in Wilson, Trousdale, and
Smith counties (CRM 270.0-305.0). Although a
few valves of 0. retusa were recovered from two
prehistoric Indian rock shelter middens (Wood-
land Period, c. 1000 B.C. - A.D. 1000) in Smith
County by Parmalee, Klippel and Bogan (1980),
no fresh specimens were taken by brailing or
found in sheller's cull and stock piles during
their three year middle Cumberland River naiad
survey in Smith County.
Examination of a series of cull and stock pile
belonging to a commercial sheller operating
from a location along the Cumberland River
(CRM 275.2), c. 6.5 km south of Hartsville,
Trousdale County, Tennessee were made No-
vember 14, 1980 and January 8 and September
17, 1981. In addition to the various piles of shell,
sorted on the basis of species, size, and/or nacre
color, several hundred naiads had been dis-
carded at the water's edge. It was in this area
that the first specimen of 0. retusa was found; it
was a very large female (in mm: length, 83;
height, 79, breadth, 50) and, by all appearances,
old with a heavily eroded umbo and slightly
deformed posterior margin (Figure 1). It is very
similar in size and apparent age to those speci-
mens taken in the Tennessee River below Pick-
wick Dam. The second specimen, another fe-
male and represented by the right valve, was
recovered January 8, 1981 from a large cull pile
of "pinks" (£'?h'pfio spp., Cyclonaias tuberculata,
Lampsilis orhiculata, Epioblasma sulcata).
Measurements (mm) of this valve are as follows:
length, 64, height, 60, estimated breadth of
paired valves, 40.
During re-examination of these abandoned
cull piles (no commercial shelling in this area
since summer 1980) on September 11, 1981, the
/ •
VU'i. 1. Sf)ecirnens o/ Obovaria retusa taken hy commercial
shelters. .>iummer 1980. in the Cumberland River. Trouxdale
County, Tennessee. Top shell 8.3 mm in length.
32 THE NAUTILUS
January 25, 1982
Vol. 96(1)
left valve of another female was found. This
specimen was slightly larger than the one repre-
sented by a right valve and measured 71 mm in
length, 63 in height, and estimated 44 mm in
breadth of paired valves. Diligent searches
failed to locate the other valves of these two in-
dividuals (Figure 1).
Admittedly three specimens or even several
do not represent a viable population, but they do
provide evidence for the continued existence of
0. retusa in the middle Cumberland River.
Although the two smallest of the three speci-
mens appear to be considerably younger than
the large individual, the outer rest-lines are
crowded and too obscure to establish even an
estimated age with any degree of certainty.
Their smaller size and the lesser extent of umbo
erosion suggests individuals somewhat younger
than the larger female, but it has been found
that in the case of certain species (e.g.
Epiobbtsma brevidens. Cyprogenia irrorafa) or
individuals that impoundment has the effect on
naiads of causing the production of extremely
heavy and thick but stunted shells (Parmalee.
Klippel, and Bogan, 1980).
The assemblage of naiad species from this sec-
tion of the river (CRM c. 273.0-278.0) where the
specimens of 0. retusa were taken exhibits some
interesting differences from the one reported by
Parmalee. Klippel, and Bogan (1980) at CRM
291.0-296.8. Although many species such as
Lampsilis orbiculata appear to occur in about
the same frequency in the stretch of river below
Hartsville as they do upstream some 16-18 km,
others, including Actinonaias ligamentina and
Ptychobranchvisfasciolare, are much rarer in oc-
currence. In contrast, Quadrula quadruLa ap-
pears in greater numbers below Hartsville. It is
of interest to note that a relic population of
Epioblasma sulcata continues to survive in
the Cumberland River below Hartsville; we sal-
vaged 38 specimens (all males) of this endan-
gered naiad from the cull piles. It is evident
from the paucity of specimens taken during the
past five years that 0. retusa continues to exist
only as a relic population in the middle Cumber-
land River and that, as Stansbery (1970) com-
mented regarding the population of this naiad in
the lower Tennessee River, it can be expected to
die out.
ACKNOWLEDGMENTS
We thank Miles Wright, Frank H. McClung
Museum, University of Tennessee, Knoxville,
for photographing the specimens in Figure 1
and Betty W. Creech for typing the manuscript.
LITERATURE CITED
Hiiepple, J. V. and R. E. Cuker. 1912. Mussel resources ol
ihe Holston and Clinch rivers of eastern Tennessei-.
Bureau of Fisheries Document No. ?65.'3-13.
Neel, Joe K. and William R. Allen. 1964. The mussel fauna
of the upper Cumberland Basin before its impoundment.
Malacologia l(.3):427-4.59.
Parmalee, Paul W., Walter E. Klippel and Arthur E. Bogan.
1980. Notes on the prehistoric and preserit status of the
naiad fauna of the middle Cumberland River, Smith Coun-
ty, Tennessee. The Nautilus 94(3):93-in5.
Stansbery, David H. 1969. Changes in the naiad fauna of
the Cumberland River at Cumberland Falls in eastern
Kentucky. The Ann^r-ican Malacol'igical l.'nion Annual
Reports for 1969. pp. 16-17.
1970. Eastern freshwater mollusks (1) the Mis-
sissippi and St. Lawrence River systems. In; Proceedings
of the Ajnerican Malafological Union Sympostum on Rare
and Endangered Mollusks. Malacologia 10(l):9-22.
Tennessee Valley Authority. 1976. Mussel fauna of the
Cumberland River in Tennessee. Unpub. Report: Div.
Environmental Planning and Div. Forestry, Fisheries, and
Wildl. Develop.
Wil.son, Charles B. and H. Walton Clark. 1914. The mussels
of the Cumberland River and its tributaries. Department
of Commerce, Bureau <if Fisheries Document No. 781.
63 pp.
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1 LIBRARY i NAUTILUS
II /\Y 1 iqfl? t Volume 96, number 2 - April 21, 1982
MAY 6 WOd j ISSN 0028-1344
!
CONTENTS Woods_Ho!MiaH:---.'
Joseph Charles Bequaert (1886-1982)
An Obituary by William J. Clench 35
Terrence J. Frest and R. Sanders Rhodes II '
Oxychilus drapamaldi in Iowa 36 I
Piet Kaas !
Ischnochitcm. dilatosculptiis, A New Species from Florida
(Polyplacophora: Ischnochitonidae) 40
Hans Bertsch and Loyal J. Bibbey I
A New Tropical Eastern Pacific Ovulidae (Gastropoda) A'andarovu^a hammesi 42
Jesus Ortea
A New Favorinus (Nudibranchia: Aeolidoidea) from the Canary Islands 45
Ralph W. Taylor and Beverly D. Spurlock
The Changing Ohio River Naiad Fauna: A Comparison of Early Indian I
Middens with Today 49 I
Richard J. Neves and Alexander V. Zale
Freshwater Mussels (Unionidae) of Big Moccasin Creek, Southwestern Virginia 52 ]
George N. Wiley, Ronald C. Circe and John W. Tunnell, Jr.
Mollusca of the Rocky Shores of East Central Veracruz State, Mexico 55
Twila Bratcher and Walter 0. Cernohorsky
Six New Species of Indo-Pacific Terebridae (Gastropoda) 61
Ralph W. Taylor '
The Freshwater Mussels (Naiads) of Big Indian Creek, a Small Southern
Indiana Tributary of the Ohio River (Bivalvia: Unionidae) 66
Jack T. Moyer, William K. Emerson and Michael Ross I
Massive Destruction of Scleractinian Corals by the Muricid Gastropod,
Drupella, in Japan and the Philippines 69
Dorothea S. Franzen
Succinea avara Say from the Southern Great Plains of the United States 82
I
Recent Deaths 68 Meetings and Shell Shows 68
34 THE NAUTILUS
April 21, 1982
Vol. 96(2)
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Vol. 96(2)
April 21, 1982
THE NAUTILUS 35
JOSEPH CHARLES BEQUAERT
1886-1982
Dr. Joseph C. Bequaert, Agassiz Professor of
Zoology emeritus of the Museum of Compara-
tive Zoology, Harvard University, died in
Amherst, Massachusetts, at the age of 95, after
a lingering illness, on January 12, 1982.
Dr. Bequaert was born in the small town of
Thourout, near Bruges, Belgium, and as a
schoolboy was interested in plants and mollusks.
In 1908 he received his Ph.D. in botany from the
University of Ghent, and he spent the rest of his
long and productive life studying many facets of
the natural world.
His first entomological field work was in the
Belgian Congo where he was Entomologist for
the Belgian Sleeping Sickness Commission from
1910 to 1912. He stayed on in Africa after the
Commission gained control of the disease by
isolating its victims, and between 1913 and 1915
he continued his botanical work, being in charge
of botanical explorations for the Belgian Colo-
nial Government. During his time in Africa he
collected mollusks, many of them new, from the
Congo River, throughout the jungles to the
mountainous Ugandan border. This material
was studied by Dr. Henry A. Pilsbry and formed
the basis of his two-volume work on the mol-
lusks of the Belgian Congo, the second volume
of which was written in collaboration with Dr.
Bequaert.
In 1916 Joe Bequaert immigrated to the
United States, and by 1921 he was a naturalized
citizen. His first position in the U.S. was at the
American Museum of Natural History as Re-
search Associate in Congo Zoology. He left the
American Museum in 1922 for Boston, where he
was first Instructor (1923-1925) and then Assis-
tant Professor in the Department of Tropical
Medicine at the Harvard Medical School,
1925-1945. In 1927 he married Frances Brown
of Ohio; they had two children, Helen and
Frank.
After his retirement from Harvard in 1956, he
sought warmer climes and went to the Univer-
sity of Texas as a Visiting Professor in biology.
In 1960 he moved to Tucson, Arizona as he was
Visiting Entomologist and Curatorial Assistant
at the University of Arizona, where he orga-
nized the mollusk collection and continued to
collect and study the little known land and fresh-
water snails of the area. His last paper was on
the "Mollusks of the Arid Southwest" with
Walter B. Miller, published in 1973.
In 1980 he and his wife Frances moved to
Amherst, Massachusetts, to be near their
daughter. Dr. Helen Holmes. He died there at
the age of 95, on January 12, 1982.
Dr. Bequaert's prolific bibliography (over 250
papers, more than 50 of them on mollusks) at-
tests to his broad background and interests. His
work includes medical research on sleeping sick-
ness and schistosomiasis, extensive molluscan
studies, particularly of the Achatinidae and
Strophochelidae, many works on wasps and
other insects, botanical papers, and even a
paper on the use of the fauna of putrefaction to
determine time of death. He was a member of
many scientific societies, president of the
American Malacological Union in 1954, and an
Honorary Associate in Entomology and Mala-
cology at the Museum of Comparative Zoology
from the time of his retirement. Dr. Bequaert,
affectionately called Uncle Joe by the many
young students then at the MCZ, was available
to advise and help at all times. He was an in-
credible linguist (said he grew up on the streets
of Belgium speaking four languages) and was
always willing to help translate difficult
passages in any of the European languages.
Dr. Bequaert's contribution to malacology and
to the Mollusk Department of the MCZ will be
appreciated by students for many generations.
Memorial contributions to support research in
land molluscan systematics may be given to
either the Friends of the Department of Mol-
lusks, Museum of Comparative Zoology, Har-
vard University, Cambridge, MA 02138 or the
American Malacological Union, 3706 Rice
Boulevard, Houston, Texas 77005.
William J. Clench, Curator Emeritus
Department of Mollusks
Museum of Comparative Zoology
36 THE NAUTILUS April 21, 1982
OXYCHILUS DRAPARNALDI IN IOWA
Vol. 96(2)
Terrence J. Frest and R. Sanders Rhodes II
Department of Geology
University of Iowa
Iowa City, lA 52242
ABSTRACT
Feral and greenhouse colonies o/Oxychilus draparnaldi (Beck, 1837) in Iowa
City, Johnson Co., Iowa constitute the first Iowa record for an introduced land
snail. The species has now been reported as feral in 13 states and in greenhouses
in 13 states and the District of Columbia. The feral colony was established in or
prior to 1966, occupies approximately 2,U00 sq. ft., and contains several hundred
individuals. Differences in land snail faunas in adjacent areas with and without
0. draparnaldi, plus feeding experiments, suggests that 0. draparnaldi reduces
local populations of some land snail species.
Records of introduced mollusks in Iowa are
extremely rare. Barnhard (1978) lists two slugs
and one fresh-water snail: as far as we know this
paper constitutes the first record for an intro-
duced land snail in Iowa. In addition, the Iowa
City 0. draparnaldi occurrence is of signifi-
cance because it is the only Midwest feral colony
and because some information as to date of in-
troduction (and hence rate of spread) is
available.
In the course of a systematic survey of the
land snails of Johnson County, Iowa in 1976-78
a single dead specimen of 0. drapanaldi was
recovered from a drift pile along a fence in the
northwest corner of Hickory Hill Park, a city
facility in northeastern Iowa City. Subsequent
intensive searches for the species resulted in the
discovery of living specimens in July 1978 on the
west side of a ravine just southwest of the south
terminus of St. Clements Street in Iowa City
(SEV4 NWV4 SWV4 SWV4 sec. 2,T. 79 N., R. 6
W., Iowa City West IVz' topographic quadran-
gle: Fig. 1). Repeated visits to the site were
made in March - August 1979 and 1980 to collect
0. draparnaldi and define the limits of the col-
ony. Litter and drift samples were taken from
the colony and adjoining areas to assess the ef-
fects, if any, of the introduction. A laboratory
colony was maintained for one year to check
feeding preferences. Also a visit made to one
local greenhouse (Pleasant Valley Orchards and
rv-^'
'■■:'■• OAK LAN P
fMfT^Y \
FIG. 1. Portion uflow<i ( 'itij W'l si ?'/■>' topoyrtiiiliic iptadran-
<jle fihoiving location of Oxychilus draparnaldi (Beck, 1837)
colony (black dot). Scale bar (lower left) length: 0.3 km (ap-
proximately 0.2 mi.).
Nursery, Inc., 1302 S. Gilbert) turned up addi-
tional 0. dra;panialdi.
Three species of Oxychilus {allarius, cellarius
and draparnaldi) are common introductions in-
to the United States. Hanna (1966, p. 19) was of
the opinion that the three "cannot be separated
consistently from shell characters", but Burch
(1960, 1962) and Ellis (1969) suggest distin-
guishing shell features as well as soft body
characters enabling relatively easy discrimina-
tion of adults of all three. Adult allarius are
small (6-7 mm diameter), the spire is nearly flat,
and the animal is very dark. The larger cellarius
Vol. 96(2)
April 21, 1982
THE NAUTILUS 37
(pa. 9 mm diameter) has a more lunate aperture,
higher spire, and the animal is pale gray. 0.
drapamaldi is the largest of the three (diameter
12-16.5 mm), has a flattened spire and aperture
as in allarius but the animal is blue-gray. Our
specimens (Fig. 2) fit most readily into drapar-
naldi: mean diameter of the 10 largest speci-
mens is 11.8 mm, the largest (Fig. 2) is 13.2 mm
in diameter, and the body is blue-gray. As a fur-
ther check the Iowa City Oxychilus were com-
pared with authenticated European allarius
and cellarius provided by C. R. C. Paul (Liver-
pool University). Available material (43 speci-
mens) shows little variation in shell, animal col-
or, or spire height.
Occurrence and Ecology
The feral colony occupies a 200 ft. stretch of
overgrown steep slope (height 10-15 ft.: area
about 2400 sq. ft.) on the west side of a small
ravine (Fig. 1). Abundance seems to fluctuate
yearly even under seemingly identical weather
and moisture conditions: our best estimate is
that a minimum of 400 individuals are normally
present. Abundance also varies widely on the
slope with individuals most common under
debris near its top. Because the area formerly
was a brickyard the present slope configuration
is in part artificial. It was still in operation as
late as 1935, when the site was collected for
Pleistocene (Peoria Loess) land snails
(Cameron, 1935). After abandonment the site
was largely filled with mixed junk and earth and
housing constructed over it. According to the
present landowner, filling ceased in 1966.
Among the last materials dumped were a con-
siderable quantity of discarded greenhouse
stock, including "spoiled" tulip bulbs. It is very
likely that the snails were introduced with this
material. Following cessation of dumping the
slope has been little disturbed, and much of the
trash is now overgrown by weeds and fast-grow-
ing trees, e.g. elms and cotton woods. At pre-
sent, the site is moist and shaded into late sum-
mer, but leaf litter and ground cover are sparse.
A 2-liter litter sample and hand collecting shows
that the site provides adequate habitat for a
small land snail fauna of 11 species (Table 1).
Eggs and young have been observed in the
TABLE 1. Comparison of land snail faunas in ecologically
similar areas with and mthout Oxychilus draparnaidi (Beck,
1837) at Iowa City, Iowa.
With iMthout
draparnaidi draparnaidi
FIG. 2. Oxychilus draparnaidi iSU 1 1,9535) from Iowa City,
Iowa: respectively top, apertural, and bottom views, x3.
Scale bar length is 5 mm. Actual diameter 13.2 mm.
Al logona profunda (Say , 1321)
Angu ispira alternata (Say, 1916)
Tnodopsis multilineata (Say, IB21)
Mesodon clausus (Say, 1821)
Stenotrema f raternum (Say, 1824)
Stenotreina barbatum (Clapp, 1904'
Cat inella avara (Say. 1824)
Gastrocopta contracta (Say . 1822)
Gastrocopta pentodon (Say, 1821)
Hawai la minuscula (Bmney, 1840)
Hel icodiscus parallelus (Say, 1821)
Vertigo tndentata Wolf. 18 70
Vallonia parvula Sterki, 189J
Zcnitoides arboreus (Say, 18161
Ret inei la indentata (Say, 1823)
38 THE NAUTILUS
April 21, 1982
Vol. 96(2)
wild from April to August. Captives maintained
in a temperature-controlled room, however, laid
eggs as early as March. The species is reported
to be carnivorous by preference (Ellis, 1969, p.
247), but captive specimens would readily eat a
variety of plant and vegetable matter, as well as
other land snails. Litter sampling (2 liters) and
hand collecting of adjacent dump areas without
drapamaldi yielded 15 species. Comparison of
the two faunas (Table 1) shows considerable
overlap, but areas without drapamaldi have
several additional large species.
Feeding tests, while incomplete, indicate that
the Iowa drapamaldi are snail carnivores, and
that absence (more likely, reduced numbers: the
small sample size precludes certainty as to real
abundance of the larger species.) of some
species in areas with drapamaldi is due to selec-
tive carnivory, rather than competition for food.
Three species available in large numbers, Trio-
dopsis multilineata (Say), Anguispira altemata
(Say), and Stenotrema fratemum (Say), were
presented to drapamaldi alone, with a favorite
vegetable food (cucumber slices), in pairs, and
all together. 0. drapamaldi would eat all three
snails, but showed a marked preference for S.
fratemum. A. altemata was least favored, be-
ing often neglected in favor of cucumbers. T.
jnullilineata was eaten frequently, but when
paired with S. fratemum the latter was prefer-
red. Attempts to induce 0. drapamaldi to eat
smaller species (Z. arboreus and G. contracta)
were unsuccessful. In summary, Iowa 0. dra-
pamaldi can subsist on a variety of plant and
animal foods, and shows a moderate preference
for animal matter, particularly relishing S.
fratemum. It seems probable that absence (or
rarity) of some large native species from areas
inhabited by 0. drapamaldi is due to predation
by the introduced snail.
Because of the proximity of a city park, the
Iowa City colony will probably persist. Although
some intervening areas are presently unsuitable
for snails, maintenance of Hickory Hill Park in a
relatively undeveloped state makes available a
large area suitable for colonization. The nearest
good habitat is 0.3 mi. (0.3 km) southeast in the
same ravine (Fig. 1), and finds of occasional
drift specimens in the intervening stretch make
continued spread highly probable. The colony is
within 0.7 mi. (1.1 km) of the Iowa River valley:
the ravine in which it is situated drains into
Ralston Creek 0.6 mi. (0.9 km) down valley.
Though both waterways are locally heavily ur-
banized, both will provide adequate habitat for
0. drapamaldi. If the present rate of spread
{i.e. 200 ft. in 14 years: 15 ft/yr.) is now main-
tained), 0. drapamaldi would reach Ralston
Creek in 211 years and would require around
1000 years to reach the Iowa River via Ralston
Creek, a distance of approximately 6 mi. (13.2
km). These figures are probably conservative: to
cite a well-known example, 50 years after the
deliberate introduction of Triodopsis fosteri
(Baker) into Burlington, New Jersey by W. G.
Binney, the species had progressed a minimum
of 8 miles to Plum Point, New Jersey via the
Delaware River valley (Pilsbry, 1940), a rate of
845 ft/yr.
U. S. Distribution
Counting the Iowa records, introductions of
0. drapamaldi are reported from 13 states as
feral colonies and 13 states and the District of
Columbia as greenhouse colonies (Table 2): the
scattered literature is well summarized in
Pilsbry (1946), Hanna (1966) and Dundee (1974).
Judging from the number of greenhouse cita-
tions in states which have been surveyed in
detail {e.g. New York, 25 counties: Wurzinger,
1975, p. 37), many more feral colonies probably
exist, and the potential for continued accidental
introduction is great. The Iowa colony is signifi-
cant in that it is the first Midwest feral colony to
be reported: others are concentrated on the east
and west coasts or in long-settled areas of the
U.S. (Fig. 3). Burch (1960, p. 25-26) reports the
original distribution of 0. draparnaldi to in-
clude much of Europe, the Orkney and Shetland
Islands, the Outer Hebrides, Asia Minor, North
Africa, and Madeira. Both U. S. and foreign
distributions suggest a synanthromorph with
broad environmental tolerances making much of
the continental U. S. potential habitat. The
species does not appear to be a major agricul-
tural pest. The greatest potential for ecological
disruption seems to be in its possible tendency to
prey on native snails, combined with its poten-
Vol. 96(2)
April 21, 1982
THE NAUTILUS 39
TABLE 2. U. S. occurrences o/Oxychilus draparnaldi (Beck.
tially wide distribution. It is somewhat
analogous to the native Haplotrema concavum
in its environmental and feeding preferences;
thus the possibility of its being directly com-
petitive with the latter should be investigated.
LITERATURE CITED
Barnhart, M. C. 1978. Three introduced gastropods in Iowa.
The Nautilus 92:106-107.
Burch, J. B. 1960. Some snails and slugs of quarantine
significance to the U. S. Sterkiana 2:13-53.
1962. How to know the Eastern land snails.
Wm. C. Brown Co., Dubuque, Iowa. 214 p.
Cameron, C. C. 1935. A comparative study of the fossils of
two loess sections at North Liberty and Iowa City, Iowa.
Unpublished M.S. thesis. University of Iowa, 46 p.
Dundee, D. S. 1974. Catalog of introduced MoUusca of east-
ern North America (north of Me.xico). Sterkiana 55:1-36.
Ellis, A. E. 1969. British snails. A guide to the non-marine
Gastropoda of Great Britain and Ireland. O.xford Uni-
versity Press, London. 298 p.
Hanna, G. D. 1966. Introduced mollusks of western North
America. Occ. Papers California Acad. Sci. 48, 108 p.
Pilsbry, H. A. 1940. Land Mollusca of North America (North
of Mexico), V. 1, pt. 2. Acad. Nat. Se. Phil., Mon. 3(1):
575-994.
1946. Land Mollusca of North America (North
of Mexico), V. 2, pt. 1. Acad. Nat. Sc. Phil. Mon. 3(2):
1-520.
Wurzinger, K-Hans. 1975. The land snails of New York-
preliminary report. Sterkiana 57:33-39.
FIG. 3. County map of U. S. shou'ing localities unth feral Oxychilus draparnaldi iBeck.
1837). Note concentration on west and east coasts.
40 THE NAUTILUS
April 21, 1982
Vol. 96(2)
ISCHNOCHITON DILATOSCULPTUS, A NEW SPECIES FROM FLORIDA
(POLYPLACOPHORA: ISCHNOCHITONIDAE)
Piet Kaas
Steenvoordelaan 104, 2284 CZ Rijswijk
The Netherlands
My friend, Mr. Richard A. Van Belle, Sint-
Niklaas, Belgium, showed to me two Ischno-
chiton specimens which he had received from
collectors in Florida. One of them proved to be
correctly identified by Van Belle as Ischnochiton
(I.) pseudovirgatus Kaas, 1972. It is a fine,
7-valved, dried and flattened specimen, col-
lected by Mr. A. Crovo at Long Reef, off Elliott
Key, Florida, 18th August 1968, in the base of a
"sea-fan", and sent to Van Belle by Mr. D.
Steinke. The specimen, measuring 3.2 mm long,
1.8 mm wide, 0.6 mm high, is no. 2601 in the col-
lection of Van Belle. In all respects it is identical
to the holotype from Curasao, and the single
paratype from Aruba, Lesser Antilles.
Seven-valved specimens of Polyplacophora
are rather rare, but well-known. Acanthochitona
crinita (Pennant, 1777), and the holotype of
Callochiton septemvalvis (Montagu, 1803) are
abnormally seven-valved (vide Kaas, 1978).
The other specimen could not be identified as
it differs from all known species of Ischnochiton.
It was collected by Mr. R. Lyles in 1968, off Fort
Lauderdale Beach, Florida, in a depth of 12 m.
Although only one specimen was procured, its
characteristics are decisive enough to attach a
new name to it:
Ischnochiton dilatosculptus n. sp.
(Figs. 1-9)
Material: 1 specimen, dry. Off Fort Lauder-
dale Beach, Florida, U.S.A., 12 m. R. Lyles,
leg., now in the Rijks Museum van Natuurlijke
Historie, Leiden, Holotype 55382.
Diagnosis: Animal elongate oval, moderately
elevated, hardly carinated, angle of divergence
±110°, the valves only slightly beaked, side
slopes a little convex (Fig. 1). Head valve semi-
circular, quincuncially granulated, the anterior
margin somewhat dentated by a row of large
granules. Total length of animal: 14.5 mm;
width 8.5 mm.
Intermediate valves (Fig. 2) not sharply di-
vided into central and lateral areas as the latter
are not raised, only marked by a sculptural divi-
sion. The dorsal part of the central area is ir-
regularly granulose, more or less reticulate.
Towards the pleurae the granules rapidly in-
crease in size, forming curved longitudinal
chains, strongly converging close to the division
between central and longitudinal areas, where
they meet the chains of granules sculpturing
these parts of the valves, which are diverging
towards the anterior and side margins, thus giv-
ing the valves a fan-like, or feather-like, ap-
pearance. On the lateral areas the granules
make the sutures dentate.
Mucro of the posterior valve subcentral, not
very prominent, the back slope slightly concave.
Antemucrona! area sculptured like the central
areas of the intermediate valves, postmucronal
area like the head valve. Both areas are divided
by a rib formed by larger granules.
The articulamentum is well-developed, por-
celaneous, somewhat transparent; the color of
the tegmentum showing through; apophyses
evenly rounded, separated by a wide, bay-like
sinus; insertion plates smooth, with 8 inequidis-
tant slits in the anterior valve; 1-1 slits in the in-
termediate valves, and 11 slits in the posterior
valve; the slit-rays well-marked, the eaves solid.
The tegmentum is cream-colored, with irregu-
lar light greenish gray spots, especially towards
the side margins of the valves.
Girdle dorsally clothed with imbricating
scales, 66 ^^ wide, 48 ^i high, the base narrowly
diamond-shaped; the strongly convex dorsal
side with 8-10 strong, narrow riblets, converg-
ing towards the broadly rounded top of the
scale; interstices twice as wide as the ribs (Fig.
Vol. 96(2)
April 21, 1982
THE NAUTILUS 41
I
Js" '-■/ .''^' .* ■(!
I -3 '""■■? '■"■■J '"? -'^ I '^$ ''* %•
0kl.- -7 -J '.4 ^4 4 I'
CRT" , . y" ■cf^^ jf' . *-'^. ,.;■■' .jv" ■ - ,
T
2_
r _. J
FIGS. 1-9. Ischnochiton dilatosculptus new species. 1, OffFort Lauderdale Beach, Fliirida. Holotype
(12 mm): 2, Left half of valve VI ( x 20): 3, Dorsal girdle scale, 66 ^ broad: 4, Ventral girdle scales (the
largest Jfg jj x 16 jj): 5, Major lateral radula tooth (side view): 6, Cusip of major lateral radula tooth: 7,
Central iimlh of radula: 8, First lateral tooth of radula: 9, Minor lateral tooth.
3). There is no marginal fringe. Ventral side of
girdle paved with radiating rows of rectangular
flat scales, about 48 x 16 f.i (Fig. 4).
Central tooth of the radula (Fig. 7) twice as
long as wide, reversed pear-shaped at the base,
distally sharply pointed, the second (major)
lateral tooth with a strongly developed triden-
tate cusp (Figs. 5, 6) and an interior projection
just below the cusp. Minor lateral tooth strongly
curved, gradually widening distally, ending in a
blunt point, non-cuspidate (Fig. 9).
Discussion: Ischnochiton (I.) dilatosculptus un-
doubtedly belongs to the group of /. (I.) striola-
fus (Gray, 1828), erythronotus (C. B. Adams,
1845), and papillosus (C. B. Adams, 1848), well
known from the Caribbean region (including
Florida and Bermuda), from which it markedly
differs in its quite peculiar sculpture, the dif-
42 THE NAUTILUS
April 21, 1982
Vol. 96(2)
ferently, more sparsely ribbed dorsal girdle
scales, and the differently shaped central
radular tooth.
It is to be hoped that more specimens will turn
up in due course, although I have the impression
that it is rather rare in this well-investigated
area.
LITERATURE CITED
Kaas, P. 1972. Polyplacophora of the Caribbean Region.
Stud. Fauna CMrafao41(137):l-165, figs. 1-247,' pis. 1-9.
(The Hague, M. Nijhoff)
1978. Notes on Loricata, 10. On the European
Callochiton species. Basteria 42:73-75.
A NEW TROPICAL EASTERN PACIFIC OVULIDAE (GASTROPODA):
XANDAROVULA HAMMESI
Hans Bertsch and Loyal J. Bibbey
Ciencias Marinas
Universidad Autonoma de Baja California
Ensenada, B.C., Mexico
In a recent review of the Ovulidae, Cate (1973)
listed 7 species from the Panamic province
(tropical west America). Since then, although
more than 25 additional new taxa of ovulids
have been proposed from I ndo- Pacific and
Caribbean waters (e.g., Azuma, 1972; Cate,
1974b, 1975, 1976a, and 1978; and Petuch,
1979), only one new species has been named
from the Panamic region (Cate, 1976b). Emer-
son and Old (1965) had previously reported the
Galapagan occurrence of Pseudocypraea adam-
sonii, an Indo-Pacific ovulid. To these tropical
eastern Pacific ovulid species we add the follow-
ing: 2 species from Panama, one known only
from the type locality and the other a widely
ranging taxon in the western Pacific:
Xandarovula hammesi
Bertsch & Bibbey, sp. nov.
(Figs. 1-6)
Description: Thin, white glossy shell, quite
large for the genus; ovalish, with both ends
pointed; bulbous in the middle; adapical terminal
protrudes sharply, completely on right-half of
shell, distinctly set off from the left side of the
bulbous body whorl; abapical terminal much
more gently narrowing along the left side;
smooth except for extremely fine longitudinal
growth striae, and faint, fine transverse line
more prominent terminally and on the columel-
la; outer lip evenly rounded, circular rather than
oval; no lip callus; apertural opening comprises
nearly 1/2 the total area of the ventral side;
aperture terminals open slightly to the side
adapically, but straight abapically (anteriorly);
anterior columellar region thin and narrow,
forming a fragile edge to the anterior gutter-
shaped siphonal canal; posterior axis delicately
tortuous, twisting a full 180° from its proximal
juncture with the body whorl to its distal ter-
mination.
Type locality: All three specimens examined
were collected in shrimp nets from about 1000
feet, off Cebaco Island (approx. 7°30'N;
81°30'W), Pacific coast of Panama, approxi-
mately in September of 1979. Holotj'pe: San
Diego Natural History Museum, Marine Inver-
Vol. 96(2)
April 21, 1982
THE NAUTILUS 43
FIGS. 1-4. Xandarovula haiiiniesi. 1 a ml 2, Holotype (SDNHM Marine Invertebrates T.S. 513). 3? mm in length. 3 and 4,
Paratype (SDNHM Marine Invertebrates T.S. 517). (Photon by Bertsch.)
have a slight callus and sulphur yellow colora-
tion along the margin of the outer lip; by con-
trast, the outer lip of X. hammesi has no
thickening and is the same white as the rest of
the shell. This new species most resembles X
figgisae Gate, 1973, but can be immediately
distinguished by the shape of the adapical
(posterior) terminal. In X. figgisae the col-
umellar portion of the terminal extension is
relatively broad and short (width greater than
1/2 the length). Comparative illustrations of
European and western VaQ\i.\c Xandarovula can
be found in Gate (1973: figs. 66 to 71) and Azuma
(1972: figs. 2 and 3; radula, fig. 7) and 1976: pit.
1, figs. 14 and 15).
Etymology: This new species honors Mr. Terry
Hammes, of Panama.
FIGS. 5 and 6. Xandarovula hammesi n. sp. Paratype in tlte
Hammes' collection. Length: 33 mm. (Photos by Bertsch)
tebrates, Type Series 513.
S.D.N.H.M., Type Series 517.
Paratype:
Disciission: This new species is separated
from the other 5 known species oi Xandarovula
by geographic location (X. patula occurs in
European waters, and the other 4 species are
western Pacific, from Japan to Australia) and
morphology. Xandarovula hammesi has an
evenly rounded outer lip, but the lip flares
adapically inX pagoda Gate, 1973, and flares (is
broader, wider) adapically in X. patula (Pen-
nant, 1777). Xandarovula xanthochila (Kuroda,
1928) and X. formosana (Azuma, 1972) both
Phenacovolva brevirostris (Schumacher, 1817)
(Figs. 7-8)
Description: Smooth pale-apricot shell, with 3
transverse brownish bands; spindle-shaped;
thick callus on outer lip, orange-colored,
straight anteriorly, angles sharply at each end;
funiculum faintly crenate.
Measurement: 20 mm x 9 mm; in the collec-
tion of the American Museum of Natural
History, Department of Invertebrates, AMNH
198612.
Locality: This specimen was live-collected
near Los Zurrones, west Panama, by Royce E.
Hubert, in 1979. Mr. William E. Old, Jr., first
44 THE NAUTILUS
April 21, 1982
Vol. 96(2)
FIC.S. 7 and 8. Fhenacovolva brevirostris from western
Panama (AMNH 198612). (Photos by Barbara Myers)
identified and recognized the significance of this
specimen.
Discussion: Two recent papers have sum-
marized the known Indo-Pacific gastropod
mollusks that occur in tropical west America
(Emerson, 1978; Bertsch, 1979). The related
family Cypraeidae has about 10 Indo-Pacific
species in the Panamic province, but this is only
the second ovulid with pan-Pacific distribution.
Previous records of the present species include
the east Asian mainland, the Japanese Ryukyus,
Philippine and Cook Islands, Celebes-Sulu Sea
(Gate, 1969:364-365), Queensland and Sydney,
Australia (Allan, 1956:132) and Hawaii (Kay,
1979:204). This, however, is the first record of
the species from the Pacific coast of the
Americas.
Detailed comparison of internal and external
(shell) anatomy will be necessary to determine
the relationship between Phenacovola
brevirostris and P. lenoreae Cardin & Walls,
1980.
ACKNOWLEDGMENTS
We thank Barbara Myers (SDNHM) for the
photographs; Dr. William K. Emerson and
William E. Old, Jr. (AMNH) for advice and the
loan of the Phenacovolva specimen, and Terry
Hammes for allowing us to examine his Xan-
daroimla specimens.
TABLE 1. Species of Ovulidae in the eastern Pacific.
Distribution Key: P signifies a Panamic species (tropical
west America); C a Califomian species, and IP indicates
Indo-Pacific distribution. Generic tisuages after Cate
(I'njal. McLean (1978). and Schilder and Sehilder (1971).
Cymbomda Cate, 1973
Cymbovula bratcherae (Cate, 1973) P
Cyphoma Roding, 1798
Cyphoma eynarginatum (Sowerby, 1830) P
Delonovolva Cate, 1973
Delonovolva aequalis aequalis (Sowerby, 1832) P
Delonovolva aequalis vidleri (Sowerby. 1881) C
Delonovolva macleani Cate. 1976 P
Jenneria Jousseaume, 1884
Jenneria pustulata (Lightfoot, 1786) P
Neosimnia Fischer, 1884
Neosimnia avena avena (Sowerby, 1832) P
Pedicularia Swainson, 1840
Pedicularia califomica Newcomb, 1864 C
Phenacovolva Iredale, 1930
Phenacovolva breinrostris (Schumacher. 1817) P & IP
Pseudocypraea Schilder, 1927
Pseudocypraea adamsonii (Sowerby, 1832) P & IP
Simnialena Cate, 1973
Simnialena inflexa (Sowerby, 1832) P
Simnialena rufa (Sowerby, 1832) P
Spiculala Cate, 1973
Spieulata barbarensis (Dall, 1892) C
Spiculata loebbeckeana (Weinkauff. 1881) C
Subsimnia Cate, 1973
Suhsimnia bellamaris (Berry, 1946) C
Xandarcnnda Cate, 1973
Xandarovula hammesi Bertsch & Bibbey sp. nov. P
LITERATURE CITED
Allan. Joyce. 1956. Cowry shells of world seas. Georgian
House, Melbourne, x + 170 pp.; 15 pis.
Azuma, Masao. 1972. Descriptions of four new gastropods
from South China Sea. Japanese Journal of Malacology,
Venus 31(2):55-61; 10 text figs. (30 July 1972)
1976. Systematic studies on the recent Japanese
family Ovulidae (Gastropoda)-IV. Genera Lacrima Cate,
1973, Globoimla Cate, 1973, Pseudosimnia Schilder,
1927 and Xandarovula Cate, 1973. Japanese Journal of
Malacology 35(3):106-117; 1 pi.; 7 text figs. (20 October
1976)
Bertsch, Hans. 1979. Tropical fauna! affinities of opistho-
branchs from the Panamic province (eastern Pacific). The
Nautilus 93(2-3):57-61. (23 April 1979)
Vol. 96(2)
April 21, 1982
THE NAUTILUS 45
Gate, Crawford Neil. 1969. Two new species of the genus
Volva Roding, 1798 (Ovulidae Fleming, 1828). The Veliger
ll(4):364-366; pi. 56. (1 April 1969)
1973. A systematic revision of the recent
Cypraeid family Ovulidae (Mollusca: Gastropoda). The
Veliger 15(Supplement):l-116; 51 pis. (31 January 1973)
1974a. The Ovulidae: a key to the genera, and
other pertinent notes (Mollusca: Gastropoda). The Veliger
16(3):307-313. (1 January 1974)
1974b. Five new species of Ovulidae from the
western Pacific (Mollusca: Gastropoda). The Veliger
16(4):381-384; 1 pi. (1 April 1974)
1975. New Cypraeacean species (Mollusca:
Gastropoda). The Veliger 17(3):255-261; 2 pis.; 1 text fig.
(1 January 1975)
1976a. Three new Cypraeacean species (Mollus-
ca: Gastropoda). The Veliger 18(4):383-384; 1 pi. (1 April
1976)
1976b. Five new species on Ovulidae (Mollusca:
Gastropoda). Th£ Veliger 19(2):159-162; 1 pi. (1 October
1976)
1978. Recently discovered new species of Ovuli-
dae, chiefly from off Wakayama Prefecture, Japan (Mol-
lusca: Gastropoda). Japanese Journal of Malacology.
Venm 37(4):191-204; 2 pis. (November 1978)
Emerson, William K. 1978. Mollusks with Indo-Pacific
faunal affinities in the eastern Pacific Ocean. The Nautilus
92(2):91-96. (27 April 1978)
Emerson. William K. and William E. Old, Jr. 1965. New
molluscan records for the Galapagos Islands. The Nautilus
78(4):116-120. (April 1965)
Iredale, Tom. 1930. Queensland molluscan notes. No. 2.
Memoirs Queensland Museum 10(l):73-88; 1 pi. (28
August 1930)
Kay. E. Alison. 1979. Hawaiian marine shells. Reef and
Shore Fauna of Hawaii. Section 4: Mollusca. Bernice P.
Bishop Museum Special Publication 64(4):xviii -i- 652 pp.;
195 text figs. (December 1979)
Kuroda, Tokubei. 1928. New Japanese Mollusca. Venus
1(1):10-15; 1 pi.
Pennant, Thomas. 1777. British Zoology. Vol. IV. Crusta-
cea, Mollusca, Testacea. Benjamin WTiite, London viii -i-
10 + 154 pp.; 93 pis.
Petuch. Edward J. 1979. New gastropods from the AbroUos
Archipelago and reef complex, Brazil. Proc. Biol. Soc.
Washington 92(3):510-526; 4 text figs. (18 October 1979)
Schilder, M. and F. A. Schilder. 1971. A catalogue of living
and fossil cowries. Taxonomy and bibliography of Trivia-
cea and Cypraeacea (Gastropoda Prosobranchia). Institut
Royal des Sciences Naturelles de Belgique Mewaries,
Deuxieme Ser. 85:246 pp. (31 July 1971)
Schumacher, C. F. 1817. Essai d'un nouveau systeme des
habitations des vers testaces. Copenhagen, pp. 1-287;
22 pis.
(Contribution number 2 from the Escuela de
Ciencias Marinas, U.A.B.C, Ensenada, B.C.,
Mexico.)
A NEW FAVORINUS (NUDIBRANCHIA: AEOLIDOIDEA)
FROM THE CANARY ISLANDS
Jesus Ortea
Department of Zoology, Oviedo University, Spain
ABSTRACT
Favorinus vitreus, a new nudibranch is described from the Canary Islands with
a discussion of other Atlantic species.
In July 1980, among material collected from
Tenerife, during a trip supported by the Junta
de Canarias and La Laguna University, we
found 40 species of Ascoglossa and Nudibran-
chia; of the latter, I collected two specimens of a
small Favorinm with two white swellings in the
rhinophores which is here described as a new
species.
Favorinus vitreus n. sp.
(Figs. 1-3)
Type locality: Los Cristianos beach (26°00'N;
16°30'W), Tenerife, Canary Islands, 23 July
1980, two specimens found on the brown algae
(Sargasum sp. and Cystoseira sp.) with small
polyzoans and spaws of an undetermined Poly-
ceridae.
46 THE NAUTILUS
April 21, 1982
Vol. 96(2)
I I white pigment
FIG. 1. Favorinus vitreus n. sp.: A, dorsal view of li ping
animal; B, rhinophores.
Holotype: I deposited in the Museum national
d'Histoire Naturelle, Paris.
Description: The two living animals are 3 mm
in length; oral tentacles, elongate, 1 mm; rhino-
phores 0.5 mm; foot 0.3 mm; and cerata up to
0.7 mm. Animals translucent white (glassy) with
the head, rhinophores, oral tentacles and cerata
white opaque. Body translucent, with an opaque
white marking in both specimens. This broad
band is discontinuous in one specimen (fig. 1,A)
and continuous in the other. Rhinophores have
two small and inconspicuous white bulbs (fig.
FIG. 2. Favorinus vitreus n. sp. Left: radular tooth: right:
jaw.
1,B). Cerata arranged in arches in the first and
second group; the third and fourth groups ar-
ranged in rows. The fifth group is a solitary
ceras. The second arch is nearly a row. The
number of cerata per a arch or row in the 3-mm-
long holotype are as follows: left side: 6, 5, 3, 2,
1; right side: 6, 4, 3, 2, 1.
We have not observed any cnidosacs in the
cerata. Liver branches in the cerata not visible
in the living animal, as the white surface of
the cerata is opaque. Liver ducts in body com-
pletely transparent. Foot transparent, with two
translucent anterior corners. Cardiac area not
prominent.
The animal did not autotomize its cerata when
it was poked with tweezers, nor when narco-
tized with magnesium chloride. There is a dorsal
indentation to the jaw (fig. 2) the masticatory
border is not complete but has several irregular
rows of pointed teeth (fig. 2,E). The radula has
17 teeth, 30-35 fjm in height. Each tooth has a
strong central cusp with four or five acutely
pointed denticles on each side (fig. 2). The penis
is unarmed.
Derivation of name: This species is called F.
vitreiis, because of the transparency of its body
(vitreo = glassy).
Discussion: The Atlantic species of Favorinus
can be artificially divided into two groups ac-
cording to the color of the rhinophores:
a) animals with brown rhinophores.
F. branchialis (Miiller) from Northern Europe
Vol. 96(2)
April 21. 1982
THE NAUTILUS 47
1 mm
FIG. 3. Atlantic species of Favorinus. E, F. branchialis.
animal from Asturias (northern of Spain): F, F. blianus,
animal from Galicia (northern Spain); G, F. auritulus,
drawing adapted from Marcus (19801: H, F. ghanensis,
dramng adapted from Edmunds (1968).
and the Mediterranean (Thompson & Brown,
1976), Morroco (Pruvot-Fol, 1953) and Cape
Verde Islands (Eliot, 1906 as F. cameus), found
also in the Canary Islands (personal observa-
tion); F. ghanensis Edmunds, from Ghana (Ed-
munds, 1968; 1974); and F. auritulus Marcus,
from the tropica! west Atlantic (Edmunds, 1964;
Marcus, 1955; Marcus & Marcus, 1963, 1970;
Marcus & Hughes, 1974 and Edmunds & Mar-
cus, 1977) possess brown rhinophores.
b) animals with white rhinophores.
F. blianus Lemche & Thompson (fig. 3,F),
from Northern Europe (British Isles and Scan-
dinavia) (Lemche & Thompson, 1974; Hunnam
& Brown, 1975), found also in the northern
Spain (Ortea & Urgorri, 1981); andF. vitreus n.
sp. from Tenerife possess white rhinophores. A
Favorinus sp. which possibly belongs to this sec-
ond group, has been reported by Eliot (1906, p.
159) from the Cape Verde Islands.
F. blianus differs from F. vitreus by having
voluminous bulbs on the rhinophores and by the
distribution of the white opaque pigment in its
body, with discontinuous patches on the cerata
and anterior corners of the foot. It also reaches
a larger size, and its radular teeth lack denticles
on the sides of the large central cusp.
Among the species with brown rhinophores,
F. ghanensis seems to be a clearly defined
species due to its penial stylet and because it
feeds upon bryozoans, an exceptional diet for an
eolid nudibranch (Edmunds, 1974). However, F.
branchialis also feeds upon Bryozoa when the
edible spawn of opisthobranchs is scarce, as we
have been able to observe in Asturias, northern
Spain, where it is frequently collected during
the winter on Bugula fastigiata and B. fulva.
When F. branchialis eats Bugula, the color of
the liver in its cerata is violet-brown, as in those
of F. ghanensis. Three rhinophoral bulbs may
also be rarely present in F. branchialis, so that,
the differences between these species is limited
to the existence of the penial stylet in F. ghanen-
sis and small details of coloration (few white
dots on the body of F. ghanensis, a dorsal band
in F. branchialis).
The difference between F. branchialis and F.
auritulus is mainly in the 3 bulbs usually present
in F. auritulus. The spawn, which may help to
separate species, is only known from F. bran-
chialis, and it consists in a regular and con-
48 THE NAUTILUS
April 21, 1982
Vol. 96(2)
centric spiral cord (Loven, 1841; Alder & Han-
cock, 1845-55; Meyer & Mobius, 1865 and
Vayssiere, 1888) with eggs of 65-70 ^^m in dia-
meter in northern Spain (personal observation),
while Haefelfinger (1962) observed eggs of
45-60 yim from a spawn from Villefranche-sur-
Mer, Vayssiere (1888) noted eggs of 50 ^^m from
the Mediterranean and Rasmussen (1951) of 70
Jim from Copenhagen (Denmark).
RESUMEN
Descripcion de una nueva especie, Favorinus
vitreus. recolectada en Tenerife, islas Canarias,
caracterizada por tener rinoforos blancos y con
dos bulbos, tentaculos orales largos (1/3 del
cuerpo) y ceratas, pigmentados uniformemente
de bianco en la superficie.
ACKNOWLEDGMENTS
I wish to thank Dr. Terrence Gosliner and the
editor, R. Tucker Abbott, for assistance with the
manuscript.
LITERATURE CITED
Alder, J. and Hancock, A. 1845-1855. A monograph of the
British Nudibranchiate Mollusca. London, Ray Society.
Edmunds, M. 1964. Eolid Mollusca from Jamaica, with
description of two new genera and three new species. Bull.
Mar. Set. Gulf. Caribbean 14:1-32.
1968. Opisthobranchiate Mollusca from Ghana.
Proc. Malac. Sor. London 38:8.3-100.
1974. An eolid nudibranch feeding on Bryozoa.
Veliger 17:269-270.
Edmunds, M. and Marcus, E. 1977. On Favorinus auritulus
Marcus and Favorinus hranchialis (Miiller). ./. moll. Stud.
43:200-201.
Eliot, C. N. E. 1906. Report upon a collection of Nudibran-
chiata from the Cape Verde Islands, with notes by C.
Crossland. Proc. Malac. Soc. London 7:131-159.
Haefelfinger, H. K. 1962. Quelques faits concernant la nutri-
tion chez Favorinua branchialis (Rathke, 1806) et Stiliger
vesicidosu.s (Deshayes, 1864). deux mollusques opistho-
branches. i?«'. Suisse Zool. 69(2):31 1-316.
Hunnam, P and Brown, G. 1975. Sublittoral nudibranch Mol-
lusca (sea slugs) in Pembrokeshire waterns. Field Studies
4:131-159.
Lemche, H. and Thompson, T. E. 1974. Three opisthobranch
gastropods new to the British fauna. Proc. Malac. Soc.
Lowrfon 41:185-193.
Loven, S. L. 1841 Bidrag till Kannedomen of Molluskernas
utveckling. K. Vet. Acad. Himdl. Stockholm for ar 1839:
227-241.
Marcus, E. 1955. Opisthobranchia from Brazil. Bol. Fac. Fit
Cien. Let., Univ. S. Paulo. Brazil, Zoologia. 20:89-261.
Marcus, E. and Marcus, E. 1963. Opisthobranchs from
the Lesser Antilles. Studies on the Fauna of Curasao
and other Caribbean islands. Stud. Fauna Curasao
19(79):l-76.
1970. Opisthobranchs from Cura(;ao and faunis-
tically related regions. Studies on the Fauna of Curasao
and other Caribbean islands. Stud. Fauna Curagcui
33:1-129.
Marcus, E. and Hughes, H. P. I. 1974. Opisthobranch Mol-
lusks from Barbados. Bull. Mar. Sci. 24:498-532.
Meyer, H. A. and Mobius, K. 1865. Fauna der Kieler Bucht.
Die Hinterkeimer oder Opisthobranchier. Leipzig. Engel-
mann l:l-xxx:l-88.
Ortea, J. and Urgorri, V. (1981). Opistobranquios nuevos
para el literal Iberico colectados en Galicia. Boletin Insti-
tuto Espanol de Oceanografia 6(288):49-60.
Pruvot-Fol, A. 1953. Etude de quelques opisthobranches de
la Cote Atlantique du Maroc et du Senegal. Trav. Ins. Sci..
Cherifien Zool. 5:1-105.
Rasmussen, E. 1951. Faunistic and biological notes on
marine invertebrates. 2. The eggs and larvae of some
Danish marine gastropods. Vidensk. Meddel. Naturh,
Foren. 113:201-249.
Thompson, T. E. and Brown, G. H. 1976. British Opistho-
branch Molluscs. Synopses of the British Fauna (New
Series) 8:1-201.
Vayssiere, A. 1888. Recherches zoologiques et anatomiques
sur les mollusques Opisthobranches du Golfe de Marseille.
Pt. 2, Nudibranches et Ascoglosses. Ann. Mus. Hist. Nat.
Marseille 3(.4yA-ieO.
PHILLIP W. CLOVER
COLLECTOR & DEALER IN
WORLD WIDE SPECIMEN
SEA SHELLS p. o. Box 83
GUn Ellen, CA 95442
FREE SHELL AND
BOOK LISTS
SPECIALISTS IN RARE
CYPRAEA, CONUS, VOLUTA
MARGINELLA, MITRA, MUREX
Specimen Shells
Offering microscopic and miniature (to '/t inch) shells
from the Florida Keys, urith accurate locality data. Also
unsorted grunge; write for list.
Margaret Teskey
P.O. Box 273
Big Pine Key. Ft. 330J,3
Vol. 96(2)
April 21, 1982
THE NAUTILUS 49
THE CHANGING OHIO RIVER NAIAD FAUNA: A COMPARISON
OF EARLY INDIAN MIDDENS WITH TODAY
Ralph W. Taylor and Beverly D. Spurlock
Department of Biological Sciences
Marshall University
Huntington, West Virginia 25701
ABSTRACT
In prehistoric times the upper Ohio River supported a population of at least 32
species of freshwater mussels. By the turn of the Twentieth Century at least seven
species had been extirpated from the river. At the present time there are only 13 of
the original 32 species still occasionally found in the river. The river habitat has
been modified by man and at least 15 species new to the river have moved in. While
the total number of individuals currently living in the river is only a small
percentage of what it was prehistorically. the total number of species has only
changed from 32 to 28.
A survey of the freshwater naiads of the upper
Ohio River was conducted by a team of biolo-
gists from Marshall University during the sum-
mer of 1979 (Taylor, 1980). This work was con-
ducted with support by the United States Army
Corps of Engineers, Huntington/Pittsburgh
Districts. As a result of the survey, it was found
that today there exists a fairly diverse naiad
faunal assemblage (composed of at least 27 resi-
dent species) in this part of the river. Upon com-
paring these data with those presented by Ort-
mann (1921) it is immediately obvious that radi-
cal changes in the faunal make-up have taken
place since the turn of the century.
Within the past 200 years man has severely
modified the river through industrial and human
pollution, damming and dredging. The Ohio
River is a much different river from the pristine
Ohio that freely flowed for eons of time prior to
the coming of European man. Native Ameri-
cans, in apparently large numbers, had lived in
harmony with the river utilizing its resources in
moderation and adding nothing which would
seriously harm or modify the river.
The habit by some American Indians of dis-
posing of their wastes in garbage pits has pro-
vided contemporary paleoecologists with a very
useful tool through which much can be learned
about the lifestyle of these primitive people. A
major component of most midden piles, along
this portion of the river, is a large amount of
well-preserved freshwater mussel shell mate-
rial. Early man used the mussel meat as a food
at least part of the year, and the shells were
ground and used as a tempering agent in the
manufacture of clay pottery. Relatively few of
the shells were incorporated into pottery; the
majority was discarded after the flesh had been
removed for human consumption. These shells
remain so well preserved that even today, using
conchological characters only, they can be read-
ily identified to species level.
Method
The initial phase of this study was a boat
survey of the freshwater mussels which present-
ly (1979) inhabit a 340-mile long portion of the
Ohio River between Pittsburgh, Pennsylvania
and Greenup, Kentucky. Collecting techniques
included brailing, handpicking in the shallows
and collecting on the banks where muskrats had
disposed of empty shells after eating the flesh.
The shells were then identified, cataloged and
accessioned into the Marshall Univeristy Mala-
cological collections.
Literature records from Parodiz (1953) and
Stansbery (1977) provided information on two
sites. We report the results, in this paper, of the
excavation of three additional sites. Figure 1
50 THE NAUTILUS
April 21, 1982
Vol. 96(2)
PENN.
BARILEn— BIRD
W. VA.
FIG. 1. Map of the upper Ohio River showing the approx-
imate location of the archeological sites bearing freshwater
naiads.
shows the respective archeological sites, while
Table 1 gives additional pertinent information.
In addition, the published works of Ortmann
(1921) and Rhoads (1899), in conjunction with
Carnegie Museum records, were used to deter-
mine the status of freshwater mussel popula-
tions in the upper Ohio River at the turn of this
century.
Results and Discussion
By combining the data derived from all five ar-
cheological studies we were able to produce a
composite list which shows that within the last
2,000-or-so years at least 32 species of mussels
have lived in this part of the Ohio. By the middle
1800's the radical modification of the Ohio River
(required for navigation) had begun, and in addi-
tion the large industrial complexes and cities
along the Ohio began using the river as a waste
disposal system. Because of these alterations
Ortmann in 1921 was unable to find seven of the
32 species used by the Indians. Those species
which were present in goodly numbers in earlier
times, but which were extinct in the river by
1900, are listed in Table 2.
The misuse and modification of the river has
continued until the present. Between the years
of 1900 and 1980 an additional 12 species have
been eliminated (Table 3). Of the original 32
species of mussels which inhabited the Ohio
River in large numbers as recently as the 1600's,
only 13 were found in the 1979 survey. Nineteen
species had been extirpated from the entire up-
per Ohio over a relatively short period of time.
The picture is not, however, as bleak as it may
seem. Although the river is still far from being
clean, steps have been taken by state and
federal agencies that will insure a continued im-
provement in water quality and thus improve
the habitat. The fact remains that while water
quality may someday improve to an acceptable
Table 1. Additional information on the archeological sites.
Site Name
Investigator
Exca\-at ion
Date
Habi tat 1 un
Date
Species Identified
7
24
32 species
Vol. 96(2)
April 21, 1982
THE NAUTILUS 51
TABLE 2. Mussel species which became extinct in the Ohio
River between 1600 and 1920.
Plethobasus cicatricosus (Say, 1829)
Pleurobema claim (Lam., 1819)
Pleurobem.a sintoxia (Raf., 1820)
Pleurobema rubrum (Raf., IS20) { = plenum)
Epioblasma Jlex-itosa (Raf., 1820)
Epioblasma torulosa (Raf., 1820)
Ptychobranchus fasciolaris (Raf., 1820)
TABLE 3. Species extirpated Jrnw the Ohio River between
1920 and 1980.
Plethobasus striatus (Raf., 1820)
Plethobasus cyphyus (Raf., 1820)
Quadrula cylindrica (Say, 1817)
Elliptio dilatata (Raf., 1820)
Cyprogenia stegaria (Raf., 1820)
Actinonaias I. carinata (Barnes, 1823)
Obovaria retusa (Lam., 1819)
Obovaria suh-otunda (Raf., 1820)
Ligumia recta (Lam., 1819)
Lampsilis abrupta (Say, 1831) i = orbiculata)
Lampsilis ovata (Say, 1817)
Obovaria olivaria (Raf., 1820)
TABLE 4. Mussel species which have established residence
in the upper Ohio River in historical times.
Anodonta imbecillus Say, 1829
Anodonta g. grandis Say, 1829
Anodonta g. corpulenta Cooper, 1834
Strophitus u. undulatus (Say, 1817)
Lasmigona costata (Raf., 1820)
Lasmigona complanata (Barnes, 1823)
Lasmigona compressa (Lea, 1829)
Qiiadrula quadrula (Raf., 1820)
Fusconaia flava (Raf., 1820)
Unionwrus tetralasmus (Say, 1830)
Leptodea fragilis (Raf., 1820)
Potamilus alatus (Say, 1817)
Potamilus ohiensis (Raf., 1820)
Toxolasma parvus (Barnes, 1823)
Villosa i. iris (Lea, 1829)
level the river is irreversibly altered as a result
of damming. The river exists today as a series of
impoundments rather than a free-flowing river.
As the river habitat became intolerable for
some naiad species, it became acceptable for
others. There is a totally new mussel fauna
presently found in the Ohio River. In addition to
the 13 remaining species of the original fauna,
there are 15 species which have established
residence within the last century (Table 4). None
of these species has been found in the archeolog-
ical material from the five test sites. While none
of these species is presently found in commer-
cially harvestable quantities, most are found in
goodly numbers throughout the entire upper
Ohio. One noteworthy example is Quadrula
quadrula. Rhoads (1899) stated that this species
did not extend above Cincinnati, but it is
presently found in many large beds throughout
the study area.
ACKNOWLEDGMENTS
We wish to express our appreciation to the
U.S. Army Corps of Engineers, Huntington/
Pittsburgh Districts, for support of parts of this
study. As always, many thanks are due Dr.
David H. Stansbery of the Ohio State University
Museum of Zoology for his help in identification
and/or confirmation of some of our specimens.
LITERATURE CITED
Ortmann, A. E. 1921. A monograph of the Naiads of Penn-
sylvania. Annals of the Carnegie Museum 8:1-384.
Parodiz, J. J. 195.5. Shell remains from the Globe Hill Site.
Appendix 2:29-30 in Myers-Oaks, W. J. 1955. Excavations
at the Globe Hill Shell Heap (46HK34-1), Hancock County,
West Virginia. West Virginia ArcheoL Soc. 3. 32 pp.
Rhoads, S. M. 1899. On a recent collection of Pennsylvania
Mollusks from the Ohio River system below Pittsburgh.
The Nautilus. 12(12):12:133-137'.
Stansben,', D. H. 1977. The Molluscan fauna from Neale's
Landing. Appendix C:l-4 in Hemmings, E. T. 1977.
Neale's Landing: An archeological study of a Fort Ancient
settlement on Blennerhassett Island. West Virginia. Un-
published manuscript on file at the Archeological Section,
W. Va. Geol. and Econ. Surv., Morgantown, West Vir-
ginia.
Taylor, R. W. 1980. A survey of the freshwater mussels of
the Ohio River from Greenup Locks and Dam to Pitts-
burgh, Pa. U.S. Army Corps of Engineers, Huntington,
West Virginia. District. 71 pp.
52 THE NAUTILUS
April 21, 1982
Vol. 96(2)
FRESHWATER MUSSELS (UNIONIDAE) OF BIG MOCCASIN CREEK,
SOUTHWESTERN VIRGINIA
Richard J. Neves
Virginia Cooperative Fishery
Research Unit'
Department of Fisheries
and Wildlife Sciences
Virginia Polytechnic Institute
and State University
Blacksburg, Virginia 24061
and
Alexander V. Zale
Florida Cooperative Fishery
and Wildlife Unit^
Newins-Ziegler Hall
University of Florida
Gainesville, FL 32611
ABSTRACT
A survey of the micssel fauna of Big Moccasin Creek, an 88-km tributary of the
North Fork of the Holston River, was conducted during 1979 and 1980. Eight
species were collected, in comparison with fourteen taken during an earlier
survey in 1915. The endangered fine-rayed pigtoe, Fusconaia cuneolus, has seem-
ingly been extirpated from this stream.
The Upper Tennessee River drainage histori-
cally contained one of the most diverse naiad
faunas in the world. Ortmann's (1918) summary
of early mussel surveys recorded an abundant
and diverse fauna in major headwater tributar-
ies, which included the Clinch, Powell, and
Holston Rivers, Virginia. Recent mussel
surveys in these rivers (Stansbery 1972; Hill et
al. 1974; Stansbery and Clench 1973, 1974;
Bates and Dennis 1978; Ahlstedt and Brown
1979; Neves et al. 1980) have demonstrated a
significant decline in species diversity and abun-
dance, due largely to habitat alteration and
water quality degradation.
The loss of mussel populations in Virginia has
been greatest in the North Fork of the Holston
River between Saltville and the Virginia-
Tennessee state line (120 km of river). The 38
mussel species that once occurred in this section
of river (Ortmann 1918) were eradicated by
chemical waste inputs from a now defunct chem-
'The Virginia Unit is jointly supported by the U.S. Fish and
Wildlife Service, the Virginia Commission of Game and In-
land Fisheries, and Virginia Polytechnic Institute and State
University.
'The Florida L'nit is jointly supported by the U.S. Fish and
Wildlife Service, the Florida Game and Freshwater Fish
Commission, and the University of Florida.
ical plant at Saltville. Big Moccasin Creek
(BMC), the largest tributary of the North Fork,
was not affected by these chemical wastes. Ort-
mann (1918) reported 14 mussel species from
two sites on BMC, including the now endan-
gered fine-rayed pigtoe, Fusconaia cuneolus.
Because the naiad fauna of this creek had not
been examined for more than 60 years, we sur-
veyed several sites on BMC during 1979 and
1980 to determine what changes in species com-
position had taken place and whether F.
cuneolus still occurred in the stream.
Study Area
Big Moccasin Creek, an 88-km tributary of the
North Fork Holston River, flows through Rus-
sell and Scott counties in southwestern Virginia
(Fig. 1). The creek has a mean discharge of 0.37
m^/s, mean gradient of 3 m/km and drains 247
km^ of Valley and Ridge Province, which is
characterized by sedimentary strata of lime-
stones, dolomites, shales, and sandstones.
Roughly 58% of the watershed is forested; most
of the remaining land is used for grazing of live-
stock and cultivation of tobacco. Upstream
water chemistry measurements during low flow
in October 1979 were as follows: temperature.
Vol. 96(2)
April 21, 1982
THE NAUTILUS 53
FIG. 1. Stations (1-9) suri'eyed for mussels in Big Moccasin
Creek, Virginia.
14°C; pH, 8.2; dissolved oxygen, 9 mg/i; con-
ductivity, 250 fimhos; and hardness, 175 mg/i.
Methods
Seven sites on Big Moccasin Creek were sur-
veyed by at least three biologists with water-
scopes during low water flows in 1979 and 1980.
Two of these sites were at locations surveyed
earlier in this century by Ortmann (1918). Live
specimens or recently dead (lustered) shells
were recorded at each station, which included
about 0.4 km of stream bottom. Collections at
two additional sites (stations 3 and 7) sampled
during summer 1977 (Steve Ahlstedt, TVA, per-
sonal communication) are included with our sur-
vey results. Reference material is housed at
Virginia Polytechnic Institute and State Univer-
sity.
Collecting Stations
1. Above confluence with the North Fork of the Holston
River on state route 614, 2.2 km east of route 23 at Wil-
helm (river kilometer 0.0; lat. 36°36'32"N long.
82°32'40"W; Scott County). Mussels were uncommon.
2. Adjacent to a state picnic area on state route 23, Moc-
casin Gap (river kilometer 4.0; lat. 36°38'00"N, long.
82°33'10"W; Scott County). No mussels were collected.
3. Adjacent to state route 613 north of Snowflake (river
kilometer 28.8; lat. 36°41'17"N, long. 82"27'56"W; Scott
County). Mussels were uncommon.
4. McConnell Mill at intersection of state routes 613 and
687 (river kilometer 32.8; lat. 36''4r43"N, long.
82°26'56"W, Scott County). Mussels were uncommon.
5. Bridge on state route 613. 100 m east of state route 891
intersection (river kilometer 4.5.1; lat. 36°42'30"N. long.
82°23'55"W; Scott County). Mussels were uncommon.
6. Dean's Farm on state route 613, 1.9 km west of Russell-
Scott county line (river kilometer 52.6; lat. 36°43'00"N,
long. 82°21'1.5"W; Scott County). Mussels were abun-
dant.
7. Adjacent to state route 613 ju.st south of Collinwood
(river kilometer 58.4; lat. 36°44'00"N, long. 82°19'15"W;
Russell County), Mussels were uncommon.
8. Fugate's Farm on state route 613, 0,4 km south of Wil-
low Spring (river kilometer 75.6; lat. 36"46'30"N, long.
82°14'18"W; Russell County), Mussels were common.
9. Owen's Farm at the intersection of state routes 676 and
677 (river kilometer 82.6; lat. 36°47'30"N, long.
82"ir50"W; Russell County). Mussels were abundant at
this site, having an average density of 18.7 mussels/m'
(Zale and Neves 1982).
Results and Discussion
A total of eight species of freshwater mussels
were collected in Big Moccasin Creek (Table 1).
Ortmann (1918) reported 14 mussel species at
Moccasin Gap (our station 2) and two species at
Willow spring (our station 8). We collected two
species from Moccasin Gap and six species near
Willow Spring. Based on the earlier and current
collection records, the following species have
apparently been extirpated from the creek:
Ptychobranchus subtentum, Lampsilis ovata,
Dysnomia capsaejormis, Quadrula cylindrica,
Pegias fabula. Alasmidonta marginata, and
Fusconaia cuneolus. Lexingtonia dolabelloides
was not reported by Ortmann (1918), but we col-
lected this species at three stations. No recent
or relic shells of the endangered F. cuneolus
were found.
Results of this survey and water quality data
from the U.S. Geological Survey and the Vir-
ginia State Water Control Board (1976) indicate
that the lower 10 km of Big Moccasin Creek has
been subjected to water quality degradation
from urban development. At Moccasin Gap,
stream alterations resulting from road construc-
tion, housing development, and channelization
were readily apparent. The State Water Control
Board (1976) reported that treated sewage dis-
charge at Gate City and raw sewage discharge
from Weber City created severe pollution with
fecal coliform bacteria and high biological ox-
ygen demand in BMC, particularly during sum-
mer. This degradation in water quality surely
has adversely affected all downstream biota.
The diverse mussel fauna that once occurred
54 THE NAUTILUS April 21, 1982
Table 1. Checklist of mussel species collected (X) from Big Moccasin Creek, 1977-1980.
Vol. 96(2)
Mussel Species
1
Station No.
4 5 6
7
Anodontinae
Alasmidonta minor {Lea, 1845)
Lampsilinae
Lampsilis fasciola (Rafinesque, 1820)
Medionidus conradicus (Lea, 1834)
Villosa nebulosa (Conrad, 1834)
Villosa vanuxemi (Lea, 1838)
Unioninae
Fusconaia barnesiana (Lea, 1838)
Lexinqtonia dolabel loides (Lea, 1840)
Pleurobema ovi forme (Conrad, 1834)
X X X X X X X
X X X X X X X X
X XXXXXXX
XXXXX XXX
X XXXXXXX
X XX
X XXXXXXX
in lower Big Moccasin Creek has been elimi-
nated. In contrast the upper watershed has re-
mained rural, and the water quality and biota
have apparently remained essentially un-
changed over the past 70 years. Recent im-
provements in water quality below Moccasin
Gap may allow the gradual recolonization by
mussels either from upstream areas or from the
North Fork of the Holston River.
ACKNOWLEDGMENTS
We thank Lynn Russell Weaver and Jane Bain
for assisting with the mussel survey, Steve
Ahlstedt for providing the two complementary
collections, and Uavid H. Stansbery of the Ohio
State University for confirming several iden-
tifications. Funding for this work was provided
by the Virginia Commission of Game and Inland
Fisheries.
LITERATURE CITED
Ahlstedt. S. A. and S. R. Brown. 1979. The naiad fauna of
the Powell Kiver in Virpnia and Tennessee (Bivalvia;
Unionacea). Bull. Amer. Mai Union 1979:40-43.
Bates. J. M. and S. D. Dennis. 1978. The mussel fauna of the
CHnch River, Tennessee and Virginia. Sterkiana
69-70:3-23.
Hill. D. M., E. A. Taylor and C. F. Saylor. 1974. Status of
faunal recovery in the North Fork Holston River, Tennes-
see and Virg:inia. Proc. Southeust. Assoc. Game Fish
amim. 28:398-413.
Neves, R. J., G. B. Pardue, E. F. Benfield and S. D. Dennis.
1980. An evaluation of endangered mollusks in Virginia.
Va. Comm. Game Inland Fish. Proj. Rep. E-F-1. 140 p.
Ortmann, A. E. 1918. The nayades (freshwater mussels) of
the Upper Tennessee Drainage with notes on synonymy
and distribution, Proc. Amer. Phil. Soc. 57:521-626.
Stansbery, D. H. 1972. A preliminary report on the naiad
fauna of the Clinch River in the southern Appalachian
Mountains of Virginia and Tennessee (Mollusca: Bivalvia:
Unionoida). Bull. Amer. Mai. Union 1972:20-22.
Stansbery, D. H. and W. J. Clench. 1973. The Pleuroceridae
and Unionidae of the North Fork Holston River above
Saltville, Virginia. Bull. Amer. Mai. Union 1973:33-36.
Stansbery, D. H. and W. J. Clench. 1974. The Pleuroceridae
and Unionidae of the Middle Fork Holston River in Vir-
ginia. Bull. Amer. Mai. Union 1974:51-54.
Virginia State Water Control Board, 1976, Tennessee and
Big Sandy River Basins, Comprrhensiw Water Resour.
Plan Vol."V-A, Pt. 2 of 3. 298 p.
Zaie, A. V. and R. J. Neves. 1982. Reproductive biologj' of
four freshwater mussel species (Mollusca:Unionidae) in
VWirixim. Freshwater invert. Biol. 1:17-28.
Vol. 96(2)
April 21, 1982
THE NAUTILUS 55
MOLLUSCA OF THE ROCKY SHORES OF EAST CENTRAL
VERACRUZ STATE, MEXICO
George N. Wiley, Ronald C. Circe and John W. Tunnell, Jr.
Division of Biology
Corpus Christi State University
Corpus Christi, Texas 78411
ABSTRACT
The molluscan fauna ofthePunta del Morro-Punta Delgada region, of east cen-
tral Mexico located approximately 75 km north of Veracruz, was studied during
June, 1973, August, 1976. and March and October, 1977. One hundred twenty-one
species (55 alive) consisting of 80 Gastropoda, 36 Pelecypoda, 3 Polyplacophora,
and 2 Cephalopoda were collected or observed from the volcanic rocky shores of
this region.
The lack of natural rocky shores in the north
and northwestern Gulf of Mexico excludes ex-
tensive hard-bottom shore communities. Lim-
ited fauna and flora, however, have become
established on the various man-made jetties
along the Gulf coast (Whitten, et al., 1950). The
most northern natural rocky shore areas in the
southwestern Gulf are located on the eastern
coast of Mexico. The first is a minor limestone
proturberance at Punta Jerez, Tamaulipas, and
the second is an intrusive Cenozoic volcanic out-
cropping in the Punta del Morro-Punta Delgada,
Veracruz, region (Galtsoff, 1954).
This paper is based upon the mollusks col-
lected from the Punta del Morro-Punta Delgada
region, Veracruz, Mexico (Atlantic). The pur-
pose of this investigation is to describe the rocky
shore molluscan populations of this unique Gulf
of Mexico shore community, especially noting
habitat distribution and ecological zonation.
The molluscan fauna of the southwestern Gulf
of Mexico was first reported by F. C. Baker
(1891). This expedition, under the direction of
Professor Angelo Heilprin, collected mollusks
from the beaches, islands, and shallow reefs
around Veracruz. Sixty-seven years later,
Moore (1958) collected 24 species of molluscs by
wading and snorkeling on Blanquilla Reef, lo-
cated approximately 90 km south-southeast of
Tampico. Chavez, et. al. (1970) listed 126 species
from the lagoon of Lobos Reef, about 10 km
south of Blanquilla Reef. A few species of mol-
lusks common to or characteristic of different
ecological zones at La Blanquilla Reef, located
off Veracruz, were reported by Villalobos
(1971). Tunnell (1974) conducted a comprehen-
sive study of the mollusks of Lobos Reef and
Enmedio Reef, 15 km southeast of Veracruz,
during May and June, 1973. He reported 220
species from Lobos and 219 from Enmedio (290
together). Included in his study were discussions
concerning the zoogeographical distribution and
ecological distribution of species within the dif-
ferent reef biotic zones.
Rice and Kornicker (1962 and 1965, adden-
dum) provided environmental and distributional
data for 149 species from Alacran Reef along
the outer edge of the Campeche Bank. Ekdale
(1974), who sampled the benthic invertebrate
fauna on the western side of the Yucatan Strait,
collected 316 species of molluscs. He grouped
the mollusks into five major habitat assem-
bleges, each with a set of characteristic species.
Molluscan investigations in the Caribbean
have been published from Puerto Rico and the
Virgin Islands by McLean (1951); Coomans
(1958); Usticke (1959); Warmke and Abbott
(1961); and Weber (1961). Rehder (1962) and
Work (1969) reported on Los Roques, Vene-
zuela, and Abbott (1958) on Grand Cayman.
Mollusks from the Yucatan Peninsula have
been listed by Weisbord (1926) and Jaume
(1946). Olsson and McGinty (1958) and Radwin
(1969) compiled a list of molluscs from the Carib-
56 THE NAUTILUS
April 21, 1982
Vol. 96(2)
bean coast of Panama, and Houbrick (1968) did
the same for Costa Rica.
Study Area
The Punta del Morro-Punta Delgada region
lies approximately 75 km north of Veracruz
(Fig. 1). These volcanic outcroppings are the
eastern most extension of the Volcanic Cor-
dillera which extends across Mexico from the
west coast to the east coast.
Seven prominent volcanic rocky points are
found in the Punta del Morro-Punta Delgada
region (Fig. 2). Much confusion exists concern-
ing the names of the various points. Ernesto
Chavez of the Escuela Nacional de Ciencias
Biologicas, Mexico, D.F. {pers. comm.) has pro-
vided a list of the more commonly used names of
these points. Names which are occasionally used
FIG. 1. Mapofth: ii-ealnyiGulfofMexiroshov'tngllu'Piintit
del Morro-PwnXa r>etg<ida region. Bathymetry contoured in
fathoms.
FIG. 2. Map of the Punta del Morro-Punta Delgada region
showing the seven prominent rocky points. (Adapted from:
Comision Intersecretarial Coordinadora Del Levantamiento
De La Carta Geografica De La Republica Mexicana Vera-
cruz UQ-VJ)
by either local residents or listed on other maps
are in parentheses following the names provided
by Chavez.
Extensive collecting was done exclusively at
two points: Punta del Morro (19°52'15"N,
96°27'30"W); and Punta Boquilla de Piedras
(19°51'15"N, 96°26'45"W). These points were
chosen for their accessibility and differing physi-
ographical features.
There is a large variation in available types of
habitats on these rocky shores, ranging from
steep, rough jagged boulders, which receive full
energy of the waves breaking on them (Figure 3)
to high and low tide pools (Figure 4) to shallow
calm-water areas which are commonly lined
with small, smooth rocks and pebbles located on
sandy beaches and behind larger boulders (Fig-
ure 4 and 5). The large grapsid crab Gra-psiis
Vol. 96(2)
April 21, 1982
THE NAUTILUS 57
FIG. 3. Sfeep rocky cliffs, approximately 60 m high, at Pun-
ta Los Munecos fPvnta Boca Andrea).
FIG. 4. Large, steep jagged boulders and high to low tide
pools at Punta del Morro (Punta Delgada).
grapus (Linnaeus) is commonly observed scurry-
ing over the outer rocks in the supratidal zone
and the small acorn barnacle Chthamalus
fragilis Darwin dominates the upper intertidal
to lower supratidal zones. The mid to lower in-
tertidal areas are dominated by sabellariid
polychates and luxurient algal growths, primari-
ly browns with some reds and greens. Subtidally
the rocks are covered to a great extent by the
zooanthid anemone Palythoa mamrnillosa (Ellis
and Solander), and the sea urchin Echinometra
lucunter (Linnaeus) is also very abundant.
The Punta del Morro-Punta Delgada region
has an annual temperature range of 22-26°C
'^.^
««i^ .'..'»,:a*j^
FIG. 5. Large, steep jagged, boulders, protected rocky tide
pool, a7id sandy beach at Punta del Morro in the foreground.
Low profile headland, similar to Punta Boquilla de Piedras.
in the background.
with an annual rainfall of 1200-1500 mm (Gar-
cia, 1970).
Methods
Specimens were collected and observed dur-
ing four trips to the area: June, 1973; August,
1976; and March and October, 1977.
Techniques utilized in the collection of
mollusks included: collection and examination of
sediment samples from tidepools, beaches, and
subtidal substrates for micromollusks; collecting
intertidal algae samples for associated mollusks;
gathering rock samples for boring and attached
species; snorkeling, when weather permitted,
for subtidal species; and general collecting in-
volving walking and wading, examining cracks,
crevices, tidepools, and overturned rocks.
All samples were put in Whirlpak plastic bags
and placed in buckets containing 10% formalin
for fixation. Specimens were returned to the
lab, washed with freshwater and placed in a 45%
solution of isopropanol for preservation. Sedi-
ment samples were rinsed with freshwater and
placed in an oven for 24 hours at 100°C. After
drying, micromollusks were picked from each
sample. Algae samples were rinsed over a U.S.
Standard Sieve #35 (500u), and any mollusks re-
tained were kept for identification. Algae
58 THE NAUTILUS
April 21, 1982
Vol. 96(2)
samples were also examined under a dissecting
microscope for attached species.
All mollusks reported in this paper are de-
posited in the Corpus Christi State University
museum collections.
Results
A total of 121 species of Mollusca (55 alive)
v^ere collected from the Punta del Morro-Punta
Delgada region. The 121 species represented 61
families, 87 genera, and consisted of 80 species
of gastropods, 36 species of bivalves, 3 chitons,
and 2 cephalopods. The most abundant families
of gastropods were Columbellidae (7 species),
Littorinidae (4 species), and Neritidae (4
species). Arcidae (8 species), Veneridae (4
species), Chamidae (3 species), and Isogno-
monidae (3 species) were found to be the most
abundant bivalve famiHes.
Table 1 contains a list of mollusks collected or
observed from the Punta del Morro-Punta Del-
gada region. Included in the table are notations
SYSTEMATIC LIST OF MOLLUSCS COLLECTED OR OBSERVED
FROM THE PUOTA DEL MORRO-PUNTA DELCADA REGION
Species Ecological
_^ Notation +
Class Cascropoda
Subclass Prosobranchla
Order Archaeogastropoda
Flssurellldae
*Dl_od_ora caycnensls (Lamarck, 1822) Int
*Fla8urella barbadensls (Cinclin. 1791) Int
ACRiaeldae
*Acnaea leucopleura (Cinelln, 1791) int
Trochldac
Calllostoma euglypCum (A. Adams, 1854) bd
C. Jububinum (Cinelln, 1791) bd
Tefjula fasclata (flcrn, 1778) bd
Turbinldae
Astraea tecta Llghtfoot, 1786 bd
Phaslanellidap
•Tricolia afflnis
(C.B, Adams, 1850)
Norltidae
•Serita fulgurane Cmclln. 1791
*N. tgsspUata Cmelin. 1791
■N. versicolor Cmelin. 1791
•Nerltlna virglnca (Linnaeus, 1758)
Order HesoK3"Cropoda
. Littorinidae
*Lictorlna llncolatn QrblRny, 1840
*L. nrleoRrla (Potlez and Hlchaud, 1838)
*L. nebulowa (Lamarck, 1922)
*L. ilciac (Coelln, 1791)
Vltrincllldae
Vitrtnclla floridana Pllsbry and McGlnty, 1946
Parviturbqidos IntirruptuB (C.B. Adans, 1850)
Atchitceionlcidac
Arch 1 tec tonicn noblllw Rodlng, 1709
Hejjacyj* hiBulcatuB (Orblgnv, 1842)
H. cyllndrlcus {Gmflln, 1791)
Caecldae
*'-i''£.'^ p"lchellun Stimpaon, 1851
'C. rvi'-iu'iltiim Folln, 1867
't- Ke^iJl"^ (OrblRny. IStl)
Vcrsfit Idrti^ ~
'Pttnloronchun var Una (Orbignv, 1841)
Csrlthidai!
CTlChlun IjitoBiin Mt-nke. 182R
sab
sab
Order Mytllolda
Vol. 96(2)
April 21, 1982
THE NAUTILUS 59
TABLE 1 (continued)
•Collected Alive
+Ecological notation: spt-supratidal zone, int-Intertidal zone, sbt-subtidal
zone, al-algae associated, sab-sabellariid colony, sed-sediment samples,
tp-tidepool, ob-observed, bd-beach drift (shell only)
designating whether the moUusk was collected
alive or dead, the specific collecting site or zone,
and, in some cases, a notation relating to some
ecological aspect which deserves mention. The
systematic list follows Keen (1971) except for
genera or families which are absent from her
coverage of tropical West America, in which
case Abbott (1974) was employed. The species
are arranged alphabetically within each genus.
Supratidal zone
Littorina-Nerita zonation, common in many
rocky shore areas throughout the Caribbean,
characterized the supratidal zone. Littorina
zizac and L. lineolata were commonly found on
supratidal rocks and boulders in the upper por-
tion of the supratidal zone. Littorina zizac was
usually found above L. lineolata whenever they
occupied the same substrate. Two individuals of
L. nebulosa were collected from Punta Boquilla
de Piedras but are considered uncommon. Lo-
cated between the Littorina zone and the
water's edge, Nerita fulgurans was observed in
large numbers. Nerita tessellata and A^. ver-
sicolor were also considered uncommon as only
two individuals of each species were collected
both from Punta Boquilla de Piedras in March,
1977. Planaxis nucleus was observed in close
proxhnity to A^. fulgurans in the lower portion of
the supratidal zone and upper portion of the in-
tertidal zone but was less abundant.
Intertidal zone
Fifteen species of mollusks (11 Gastropoda, 1
Pelecypoda, and 3 Polyplacophora), were col-
lected from the intertidal zone; only the subtidal
zone yielded more species (18). The intertidal
zone of the Punta del Morro-Punta Delgada
region can be divided into 3 sub-zones: upper,
middle and lower intertidal. Each zone can be
characterized by certain mollusks.
The upper intertidal zone is characterized by
Siphonaria pectinata, Nerita fulgurans, and
Thais haemastoma. These species were also
found in the supratidal zone but were more
abundant in the upper intertidal zone.
Two keyhole limpets, Diodora cayenensis, and
Fissurella barbadensis. and the muricid Pur-
pura patula were the characteristic species of
the middle intertidal zone. Fissurella was the
most abundant limpet. One specimen of Acmaea
leucopleura was collected but considered uncom-
mon. In calm-water tide pools under rocks right
at the water line Planaxis lineatus appeared
gregarious often in clusters of 15-20 in-
dividuals, but sometimes as many as 80-100.
The lower intertidal zone was more of an in-
terface with the subtidal zone. Petaloconchu^
varians formed extensive mats in this area.
Brachidontes exustus and Isognomon hicolor
|:|
60 THE NAUTILUS
April 21, 1982
Vol. 96(2)
were commonly found attached to Petaio-
conchus. The polyplacophorans collected were
found in this zone, but only one specimen of each
was collected and were considered uncommon.
Of two muricids mentioned above, Purpura
patula was common on rough water, outer rocks
and Thais haemastoma was more common on
rocks found in moderate to slight wave energy
areas.
Subtidal zone
Barbatia domingensis, found to be most abun-
dant in turbulent environments on the Bermuda
platform by Bretsky (1967), was the most abun-
dant ark collected from the subtidal zone. Area
imbricata, Arcopsis adamsi, and Barbatia
Candida, which are perhaps the most con-
spicuous arks in the shallow waters of Lobos
Reef (Tunnell, 1974), were only occasionally col-
lected or observed in the subtidal zone. Locally
abundant in the upper portion of this zone were
clusters of Brachidontes exustus and Isognomon
bicolor. Aplysia of. brasiliana, A. dactylomelo
and two unidentified nudibranchs were collected
in 1976 while snorkeling.
Algae
Numerous species of mollusks are found asso-
ciated with marine algae. Warmke and Almodo-
var (1963) presented data on mollusk-algae
associations of Puerto Rico. They collected 90
species of molluscs from 25 species of algae.
Four species of algae, Sargassum cf. filipen-
dula C. Agardh, Padina vickersiae Hoyt, Caul-
perpa racemosa (Forskal) J. Agardh, and Ulva
lactiica Linnaeiis were collected at Punta Bo-
quilla de Piedras and examined for mollusks.
These four species appeared to be the dominant
algae.
Nine species of gastropods were found asso-
ciated with the four algal species collected. Only
two species, Tricolia affinis and Caecum
pulchellum, were found exclusively on the algae.
Littorina meleagris was also found intertidally
on the rocks. Caecum vestitum and Fossarus or-
bignyi were found in the sabellariid polychaete
colonies, as well as on algae. Planaxis lineatus
was collected both from calm-water tidepools
and algae, while Nitidella laevigata was found
crawling subtidally on the rocks among the
algae.
Sabellariid polychaete colonies
Sebellariid polychaete colonies were com-
monly observed covering portions of intertidal
boulders. These colonies formed a layer approx-
imately 2-10 cm thick and were composed of ag-
glutinated tubes of sand grains. Larger holes
and channels probably formed by wave action
were inhabited by numerous crustaceans, poly-
chaetes, and mollusks, Fossarus orbignyi,
Brachidontes exustus, and the nestling bivalve
Sphenia antillensis were the most common
mollusks collected from the sabellariid colonies.
Discussion
Although the majority of the molluscan fauna
collected from the Punta del Morro-Punta Del-
gada region is considered to be Caribbean in
origin, many of the families and genera were
represented by only one or two species. Tunnell
(1974) stated that southwestern Gulf reefs ap-
pear to have several reduced or lacking tropical
elements which are generally common in areas
more centrally located within the Caribbean
Province. This situation appears to be the case
in the Punta del Morro-Punta Delgada region
also. Although not universally accepted, the in-
shore northern boundary of the Caribbean prov-
ince is located in the vicinity of Cabo Rojo
(Briggs, 1974). This places the study area near
the periphery of the Caribbean province where
physical and ecological conditions are favorable
for tropical species, but are far from being op-
timal. The molluscan fauna of the Punta del
Morro-Punta Delgada rocky shores would there-
fore, most accurately be described as "depau-
perate Caribbean."
ACKNOWLEDGMENTS
The authors would like to gratefully thank the
Direccion General de Pesqueras, Departamento
de Pesca for allowing us to collect and study in
Mexico.
Vol. 96(2)
April 21, 1982
THE NAUTILUS 61
LITERATURE CITED
Abbott, R. T. 1958. The Marine Mollusks of Grand Cayman
Island, British West Indies. Monograph 11. Acad. Nat.
Sci. Phila.. 138 pp., 5 pis.
Abbott, R. T. 1974. American Seashelh. Van Nostrand
Reinhold Co., New York, 663 pp.
Baker, F. C. 1891. Notes on a collection of shells from South-
ern Mexico. Proc. Acad. Nat. Sci. Phil. pp. 45-55.
Bretsky, S. S. 1967. Environmental factors influencing, the
distribution of Barbatia domingensis (Mollusca: Bivalvia)
on the Bermuda platform. PostiUa. Peabody Museum of
Nat. Hisf., Yale Univ. 108:14pp.
Briggs, J. C. 1974. Marine zoogeography. Mc-Graw-Hill,
New York, 475 pp.
Chavez, E. A., E. Hidalgo, and M. L. Sevilla. 1970. Datos
acerca de las comunidades bentonicas del arricife de
Lobos, Veracruz. Revista de la Sociedad Mexicana de
Historia Natural 31:211-280.
Coomans, H. E. 1958. A survey of the littoral Gastropoda of
the Netherlands Antilles and other Caribbean islands.
Study. Fauna Curaeao 8:42-111.
Ekdale, A. A. 1974. Marine molluscs from shallow-water en-
vironments (0 to 60 meters) off the northeast Yucatan
coast, Mexico. Bull. Mar. Sci. 24(3):638-668.
Galtsoff, P. S. ed. 1954. Gulf of Mexico, its origin, waters,
and marine life. U.S. Fish Bull. 55(89):604 pp.
Garcia, E. 1970. Los climas del estado de Veracruz. Ann.
Inst. Biol. Univ. Anton Mexico 41(Ser. Bot l):3-42.
Houbrick, J. R. 1968. A survey of the littoral marine mol-
lusks of the Caribbean coast of Costa Rica. The Veliger
ll(l):4-23.
Jaume, M. L. 1946. Moluscos marinos litorales del Cabo
Catoche, Yucatan, Mexico. Revista Soc. Malac. Carlos de
la Tor-re 4(3):95-100.
Keen, A. M. 1971. Sea shells of tropical west America. Stan-
ford Univ. Press, Stanford, Calif., 1064 pp.
McLean, R. A. 1951. The pelecypod or bivalve mollusks of
Porto Rico, and the Virgin Islands. Sclent. Surv. Porto
Rico. N.Y. Acad. Sci. 17(1):1-183.
Moore, D. R. 1958. Notes on Blanquilla Reef, the most north-
eriy coral formation in the western Gulf of Mexico. Puhl.
Inst. Mar. Set. Texas 5:151-155.
Olsson. A. A. and T. L. McGinty. 1958. Recent marine mol-
lusks from the Caribbean coast of Panama with the de-
scription of some new genera and species. Bull. Amer
Paleo. 39(177):58 pp.
Radwin, G. E. 1969. A recent molluscan fauna from the
Caribbean coast of southeastern Panama Trans. San Diego
Soc. Nat. Hist. 15(4):229-236.
Rehder, H. A. 1962. Contribucion al conocimiento de los
moluscos marinos del archipielago de Los Roques y La
Orchila. Mems. Soc. Sctenc. nat. Xa Salle' 22:116-138.
Rice, W. H. and L. S. Kornicker. 1962. Molluscs of Alacran
Reef, Campeche Bank, Mexico. Puhl. Inst. Mar. Sci..
Texas 8:366-403.
1965. (Addendum to 1962 paper). Puhl. Inst.
Mar. Set.. Texas 10:172.
Tunnell, J. W., Jr. 1974. Ecological and geographical distri-
bution of Molluscs of Lobos and Enmedio coral reefs,
Southwestern Gulf of Mexico. Ph.D. Dissertation. Texas
A&M Univ., 158 pp.
Usticke, G. W. N. 1959. A checklist of the marine shells of St.
Croix. U.S. Virgin Islands, unth random annotations.
Lane Press, Burlington, Vermont, 90 pp.
Villalobos, A. 1971. Estudios ecologicos en un arrecife cora-
lino on Veracruz, Mexico. Pp. 532-545 in Symposium on
investigations and resources of the Caribbean Sea and ad-
jacent regions, preparatory to CICAR, organized jointly
by UNESCO and FAO.
Warmke, G. L. and R. T. Abbott. 1961. Caribbean seajshells.
Livingston Publishing Co., Narbeth, Penn., 348 pp.
Warmke, G. L. and L. R. Almodovar. 1963. Some associa-
tions of marine molluscs and algae in Puerto Rico. Mala-
cologia 1(2):163-177.
Weber, J. A. 1961. Marine shells of Water Island, Virgin
Islands, The Nautilus 75(2):55-60.
Weisbord, N. E. 1926. Notes on marine mollusks from the
Yucatan Peninsula, Mexico. The Nautilus 39(3):81-87.
Whitten, H. L., H. F. Rosene, and J. W. Hedgepeth. 1950.
The invertebrate fauna of Texas coast jetties; a pre-
liminary survey. Publ. Inst. Mar. Sci.. Texas 1:53-87.
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mollusks of Los Roques, Venezuela. Bull. Mar. Sci.
19(3):614-711.
1^
SIX NEW SPECIES OF INDO-PACIFIC TEREBRIDAE (GASTROPODA)
Twila Bratcher
8121 Mulholland Terrace
Hollywood, CA 90046
and
Walter 0. Cernohorsky
Auckland Institute and Museum
New Zealand
While doing research for a forthcoming book,
we have come across a number of undescribed
terebrid species, some in museums, others from
private collectors. Some other species were
62 THE NAUTILUS
April 21, 1982
Vol. 96(2)
FK ;S 1 i):Tcrebra mactanensis Bratcher & Cemohorsky. new species. Holotype, LACM no. 1968. oi.i mm. 2 & 9.
Terebra ■o^.-^.v..- Bratcher & Cemohorsky. n^ species. Holotype. LACM no. 1969. 26.1 mm. 3& 8: Dupl.cana mozambiquen-
sis Bratcher & Cemohorskv. new species. Holotype NM no. H78iS. 22.3 mm. 4 & 12: Terebra caddeyi Bratcher & Cemohorsky.
new mcie.s. Holotype LACM no. 1967. 52.7 mm. 5 & 11: Duplicaria baileyi Bratchei- & Cemohorsky. new species. Holotype
LACM no. 1070. ii.f m.m.. 6 & 7: Terebra burchi Bratcher & Cemohorsky. new .species. Holotype MNHN. 17.9 mm.
Vol. 96(2)
April 21, 1982
THE NAUTILUS 63
represented only by a single specimen, and we
will wait for more material before describing
them. Six are being described here.
Terebra burchi new species
(Figs. 6. 7)
Diagnosis: A pure-white shell with small
brown dots scattered at random just below the
suture and with a broadband of yellowish brown
on the base of the body whorl.
Description: Shell about 18 mm in length, with
12 whorls of teleoconch; color pure-white with
small yellowish brown dots scattered at random
immediately anterior to the suture and with the
same color on the base of the body whorl; outline
of whorls convex; protoconch with IV2 whorls
remaining (paratype with intact protoconch of
3V2 amber conical whorls); sculpture of slightly
arcuate axial ribs from suture to suture, 13 on
penultimate whorl; ribs well-developed, quite
sharp, and narrower than interspaces; inter-
spaces with 5 evenly-spaced grooves, the
posterior being deep; interstical grooves not
crossing ribs; no subsutural band; body whorl
with ribs fading at periphery; 8 grooves anterior
to periphery, 6 posterior; aperture quadrate,
with basal plication; columella recurved.
Dimensions: Holotype 17.9 x 4.3 mm. Para-
types from 18.8 x 4.3 to 22.4 x 5.4 mm.
Type locality: Northern Mozambique Channel
(12 45'S; 45 18;E), at 15 -20 m, Benthedi Ex-
pedition sta. 32.
Type Material: Holotype MNHN Paris. Para-
types LACM no. 1971 (1); MNHN (2); Bratcher
coll. (2): Cernohorsky coll. (2): Tursch coll. (2).
Distribution: From Mozambique and Papua
New Guinea; 2 to 20 m. Also Philippines.
Discussion: There are several other Indo-
Pacific terebrids with dark areas anterior to the
periphery of the body whorl and scattered spots
below the suture. None of them has a pure-white
background. Terebra amoena Deshayes, 1859,
T. conspersa Hinds, 1844, and T. pertv^a (Born,
1778), all have larger shells with beige to tan
backgrounds and have obvious subsutural
bands.
This species is named in honor of a late friend
and colleague, R. D. Burch.
Terebra caddeyi new species
(Figs. 4, 12)
Diagnosis: A long, slender, flat-sided terebrid
shell, shiny tan, and with 3 or 4 spiral grooves
per whorl.
Description: Shell long, slender, with 25
whorls; color shiny tan; outline of whorls
straight; protoconch missing; 3 spiral bands,
each defined by a spiral groove, occur anterior
to suture; posterior band narrow, without
nodes; center band of obsolete nodes; anterior
band flatter and scarcely noded; no axial sculp-
ture except axial striae; body whorl with deep
groove posterior to periphery, followed by 3
weak grooves; aperture small, quadrate; col-
umella curved, with moderately heavy parietal
callus; siphonal notch broad.
Dimensions: Holotype 52.7 x 6.9 mm. Para-
types from 44.4 x 5.4 to 53.4 x 6.6 mm.
Type Locality: Korere Village, Rabaul, Papua,
New Guinea, 3 m. in depth, on volcanic sand.
Type Material: Holotype LACM no. 1967.
Paratypes Bratcher coll. (1); Caddey coll. (2).
Distribution: Known only from type locality.
Discussion: Terebra lima Deshayes, 1857, also
has a flat-sided shell, but it lacks the sheen of
this species and has almost cancellate sculpture
with spiral cords and axial sculpture forming
small nodes at intersections. T. jenningsi Burch,
1965, has a concave outline, a cord at the periph-
ery of the body whorl, and more spiral grooves.
It also lacks sheen. This species is named for P.
T. Caddey, who collected the type lot.
Terebra mactanensis new species
(Figs. 1. 10)
Diagnosis: A long, extremely slender terebrid
shell with dark spots between axial ribs anterior
to the suture.
Description: Shell extremely slender, long;
color, shiny brown with black spots between ax-
ial ribs anterior to suture and a row of small
white dots at periphery of body whorl; outline of
whorls convex; protoconch of 3 white, conical
whorls; sculpture of axial ribs from suture to
suture, narrower than interspaces; ribs on body
whorl terminating at periphery in a white spot;
aperture elongate; columella recurved, white;
siphonal fasciole extremely heavy, long.
64 THE NAUTILUS
April 21, 1982
Vol. 96(2)
Di7nensions: Holotype 54.4 x 7.2 mm. Para-
types from 47.8 x 6.1 to 62.1 x 8.1 mm.
Type Locality: Punta Egano, Mactan Island,
Cebu, Philippine Islands at 200 m.
Type Material: Holotype LACM no. 1968.
Paratypes Bratcher collection. (1); Marrow col-
lection. (1).
Distribution: This species is known only trom
the type locality.
Discussion: One of the paratypes is light
orange-brown with dark brown spots between
the ribs anterior to the suture. The other is
white with a few brown areas anterior to the
suture and with extremely faint brown spots at
the periphery of the body whorl. All have similar
sculpture. There is no Indo-Pacific terebrid
species with which T. mactanensis could be con-
fused. The white paratype might be compared
with T. fortunae Deshayes, 1857, which has an
inflated shell with longer whorls, has more
spiral sculpture; and has no brown ornamenta-
tion. The type lot was collected by Max Marrow.
Terebra marrowae new species
(Figs. 2, 9)
Diagnosis: A cream-colored terebrid shell
with a few small orange-brown dots and with an
exceptionally large, blackish mamillate proto-
conch.
Description: Shell medium-sized for the
genus; color, cream with a few small scattered
orange brown dots, protoconch and first whorls
of teleoconch brown; outline of whorls concave
in early whorls, flat in later ones, with convex
subsutural band; protoconch of IV2 broad, ma-
millate blackish brown whorls; subsutural band
of large pearl-like nodes, occasionally spotted
between by orange-brown; suture shallow; sub-
sutural groove deep, narrow; subsutural band
followed by a narrow, almost smooth, inconspic-
uous band, becoming slightly nodulous on last 2
whorls; remainder of whorl finely concellate
with 2 spiral cords per whorl, forming shallow
pits between intersections; body whorl with
finely cancellate sculpture ending posterior to
periphery, spiral cords only continuing to
siphonal fasciole; aperture short, quadrate; col-
umella recurved.
Dimensions: Holotype 26.1 x 5 mm. Para-
types from 21.4 x 4.8 to 32.1 (Apex missing) to
6.4 mm.
Type Locality: Cleaverville, N.W. Australia;
intertidal.
Type Material: Holotype LACM no. 1969.
Paratypes Bratcher coll. (1); Caddey coll. (2);
Cernohorsky coll. (1); Cooper coll. (2).
Distribution: Northwest Australia, intertidal.
Discussion: The most outstanding feature of
this species is the extremely large blackish
brown or purplish brown mamillate protoconch,
with a lighter brown or purplish area extending
through two to four whorls of the teleoconch,
becoming progressively lighter. The sculpture of
some of the paratypes is finer than that of the
holotype, with smaller nodes on the subsutural
band. The color varies from white to yellowish
white with a white subsutural band. All speci-
mens except one have a few tiny scattered
brown dots, and that one was collected dead.
Two of the paratypes have brownish pin-point
dots at the periphery of the body whorl.
There are several other Indo-Pacific terebrid
species with cancellate sculpture, all of which
are easily separable from Terebra marrowae. T.
swobodai Bratcher, 1981, is more slender, has
convex whorls and very heavy, rough sculpture
with small nodes forming where axial and spiral
cords cross. T. elliscrossi Bratcher, 1979, and T.
amanda Hinds, 1844, both have slender, non-
mamillate protoconchs of more than IV2 whorls.
Although T. fenestrata Hinds, 1844, has a
mamillate protoconch, it is about Vs as large as
that of T. marrowae, and the sculpture of the
teleoconch is extremely coarse and heavy. This
species is named in honor of Lorna Marrow, who
collected the holotype.
Duplicaria baileyi new species
(PI. 5, 11)
1965 Duplicaria australis (E. A. Smith), J. Gate & R. D.
Burch, Veliger 6(3): 145; 1967 Cernohorsky, Mar. SMls
Pacific 1;208, pi. 52, fig. 392. [non Terebra australis E. A.
Smith, 1873).
1966 Duplicaria (Duplicaria) sp. Cernohorsky & Jennmgs,
Veliger 9(1):58, pi. 6, fig. 44.
1978 Terebra australis (E. A. Smith), Hinton, Guide Austra-
lian Shells, pi. 59, fig. 6. [non Terebra australis E. A.
Smith, 1873].
Vol. 96(2)
April 21, 1982
THE NAUTILUS 65
Diagnosis: A beige Duplicaria shell with a few
■yellowish brown splotches scattered irregularly
and with brown anterior to the periphery of the
body whorl.
Description: Shell medium sized, with 13
whorls of teleoconch; color, beige with a few
reddish brown splotches and dots scattered at
random, and with the same color anterior to the
aeriphery of the body whorl; outline of whorls
5lightlyconvex; protoconch of 4V2 pink, translu-
cent, conical whorls; axially ribbed subsutural
mnd defined by shallow groove, with deeper
junctations between ribs; remainder of whorl
vith straight axial ribs contiguous with ribs on
)and; interspaces about equal to ribs, smooth;
)ody whorl with ribs ending at periphery; peri-
)hery marked with light band between rib end-
ngs and light-brown area; aperture elongate;
:olumella recurved; siphonal fasiole striate, with
noderate keel.
Dimensions: Holotype 24.9 x 5.3 mm. Para-
ypes 21.5 x 4.5 to 40.0 x 7.9 mm.
Type Locality: Guadalcanal, Solomon Islands
9 25'S; 159 56'E); in sand at 20 m.
Type Material: Holotype LACM no. 1970.
^aratypes ANSP no. 352482 (1); AM no.
]132464 (1); CAS no. 60674 (1); MCZ no. 290426
1); MORG no. 21.275; NM no. H-766 (1); USNM
10. 782262 (1); Bratcher coll. (2); Cernohorsky
oil. (2); Morrow coll. (2).
Distribution: Mozambique to the Philippines
.nd the Solomon Islands; from intertidal to
;00m.
Discussion: The number of axial ribs varies
rom 20 to 29 on the penultimate whorl, and the
■asic color varies slightly from cream to beige,
'he brown splotches may vary in number and
.ize, but they are always inconspicuous. Dupli-
aria teramachii Burch, 1965, is somewhat
imilar in color pattern although it has a broad
and of reddish brown instead of the occasional
iterrupted blotches. It also has a narrower
pical angle, flatter subsutural band, and
horter whorls. This species is named in honor
f Brian Bailey who collected the holotype.
Duplicaria mozambiquensis neu^ species
(Figs. 3, 8)
Niiii Terehm gracilis Reeve, Conch. Icon. 12, pi. 24, fig. 1.31
[non Lea 1833; non Gray, 1834] Hab.: Africa; holotype
BM(NH). 1874.10.29.2; 22.0 mm.
Diagnosis: A Duplicaria with extremely in-
flated early whorls, a punctate subsutural
gi-oove, and a narrow, noded subsutural band.
Description: Shell color light-brown with ivory
ribs, nodes, and narrow peripheral stripe on
body whorl; outline of whorls convex; proto-
conch mamillate with IVz brown, moderately in-
flated embryonic whorls; sculpture of early
whorls of teleoconch consisting of a narrow sub-
sutural band with wide-spaced round nodes (8 or
9), and below each node an arcuate rib almost
noded in center, giving an angulate outline to
the early whorls; a punctate subsutural groove
developing after the 3rd whorl of teleoconch;
ribs on remainder of whorl remaining wide-
spaced, sharp, and arcuate, but losing the
angulate form on later whorls (12 on penulti-
mate whorl); nodes on subsutural band angulate
on later whorls; body whorl with sharp ribs con-
tinuing below periphery to keel of siphonal
fasciole; aperture elongate; columella almost
straight.
Dimensions: Holotype 22.3 x 5.6 mm. Para-
types from 17.0 x 4.4 to 33.0 x 6.8 mm.
Type Locality: Mozambique, trawled off
Chinde Island.
Type Material: Holotype Natal Museum no.
H7843/T2541. Paratypes in BM(NH) 198021;
Natal Museum nos. J2973/T2542 (1), 566/T2543
(1), B2137/T2544 (1), H765/T2545 (2); Bratcher
coll. (1).
Distribution: From Durban, South Africa, to
Mozambique.
Discussion: Four of the paratypes are the
same color as the holotype; one is peach color;
and two are ivory. Some individuals have small,
inconspicuous nodes at the posterior end of the
axial ribs. Some have more numerous, less wide-
ly spaced ribs.
Duplicaria spectabilis (Hinds, 1844) has
similar sculpture, but it has a distinctive color
pattern of rich brown and cream stripes, and a
protoconch of 2V2 whorls. Duplicaria evoluta
Deshayes 1859, has a broad subsutural space but
no groove. It has axial ribs on the subsutural
band instead of round nodes, and the early
66 THE NAUTILUS
April 21, 1982
Vol. 96(2)
whorls are quite flat in outline. This is the same
species as Terebra gracilis Reeve, 1844, a name
which was preoccupied.
Abbreviations have been used for a number of
institutional collections cited in this paper. They
are:
AM - Australian Museum
ANSP- Academy of Natural Science of Phila-
delphia.
CAS - California Academy of Sciences.
LACM-Los Angeles County Museum of Natur-
al History.
MCZ- Museum of Comparative Zoologj-, Har-
vard University.
MNHN - Museum National d'Histoire Naturelle,
Paris.
MORG-Museu Oceanografico de Rio Grande,
Brazil.
NM- Natal Museum, South Africa.
ACKNOWLEDGMENTS
We wish to thank the following for the loan of
tjpe material for this study: Brian Bailey of
Honiara, Solomon Islands; Dr. Philippe Bouchet
of MNHN Paris; P. T. Caddey of N.S.W., Aus-
tralia; Dr. George Davis of ANSP; Dr. R. Kil-
burn of NM; Max Marrow of Victoria, Australia;
Dr. Ben Tursch of Brussels, Belgium; Dr.
Joseph Rosewater of USNM.
LITERATURE CITED
Born, Ignatius. 1778. Index Rerum NaturcUium Caesaeri
Vindobonensis. Testacea.
Bratcher, Twila L. 1979. Taxonomic Changes in Eastern Pa-
cific Terebridae, with Description of a New Species. The
Veliger 22(l):61-64; figs. 1-12.
1981. Four Previously Undescribed Indo-Pacific
Terebrids. The Veliger 23(4):329-332; figs. 1-8.
Burch, Robert D. 1965. New Species from the Indo-Pacific
Ocean and from the Gulf of Mexico. The Veliger
7(4):241-253: pi. 31, figs. 1-10.
Deshayes, G. P. 1857. Description d'especes nouvelies du
genre Terebra, Jour, de Conchy I. 6:65-102, pis. 3-5.
1859A. General review of the genus Terebra,
and a description of new species. Proc. Zool. Soc. London.
p. 270-321.
Hinds, R. B. 1844. Synopsis of the known species of Terebra.
Proc. Zool. Soc. London for 1843, pt. 11:149-168.
THE FRESHWATER MUSSELS (NAIADS) OF BIG INDIAN
CREEK, A SMALL SOUTHERN INDIANA TRIBUTARY OF THE
OHIO RIVER (BIVALVIA: UNIONIDAE)
Ralph W. Taylor
Department of Biological Sciences
Marshall University
Huntington, West Virginia 25701
ABSTRACT
A 1979-81 survey of Big Indian Creek in southern Indiana prodiLced a total of
16 species of freshwater mussels (Naiads). In addition to these unionid species, the
exotic clam Corbicula fluminea was also found to be present throughout the
stream. The faunal make-up proved to be typically Ohioan in nature. The most
common species were Lampsilis r. luteola, Lampsilis ventricosa and Amblema p.
plicata. Lampsilis fasciola, Leptodea fragilis and Toxolasma parvus were each
represented by a single specimen.
In their Revision of the Mollusca of Indiana, together, in a condensed form, all the early
Goodrich and van der Schalie (1944) brought work done on the freshwater mussels in Indiana
Vo). 96(2)
April 21, 1982
THE NAUTILUS 67
streams. A more recent work by Krumholz et al
1970) provided valuable information on the
vVhite and Wabash Rivers. Most of the pub-
ished information available on the mussels of
Indiana is in fact concerned with the naiad
aunas of the larger rivers. There appears to be
I dearth of information available on the mussels
)f small streams, and in particular those
streams of southeastern Indiana. It is the pur-
)ose of this paper to report work on such a
.tream, Big Indian Creek, a tributary of the
)hio River located in southern Indiana.
Big Indian Creek originates in the low-rolling
ill section of southeastern Indiana, locally
nown as Floyd Knobs, and flows in a generally
outhwesterly direction to its confluence with
he Ohio River at the village of New Amsterdam
ome fifty river miles downstream of Louisville,
Kentucky. The stream presently exists in a fair-
-' undisturbed condition. Big Indian Creek flows
irough land that has for over a hundred years
een dedicated to agricultural use. A good per-
entage of the lower portion of the creek flows
irough Harrison/Crawford State Forest. The
nly towns of any size in this drainage are the
illages of Crandall and Corydon, with a com-
ined total population of less than one thousand
ihabitants. Water quality is apparently good,
s the only possible source of pollution would be
lat which results from limited agricultural ac-
vities within the floodplain. The substrate is
rimarily limestone bedrock with an occasional
and and gravel bar. There is very little
vidence of excessive silt deposition anywhere
long the stream's course.
Methods
During the summers of 1979 and 1981, Big In-
ian Creek was surveyed for freshwater mussels
t irregular time intervals. Seven collecting sta-
ons were established. Fresh dead shells were
andpicked from the water and shore line. Very
Id, severely weathered specimens were dis-
irded and only specimens of those species con-
dered to be part of the present naiad fauna are
icluded in this report. Specimens were cleaned
nd cataloged in the Marshall University Mala-
)logical Collections. Voucher specimens have
been placed in the Ohio State University Muse-
um of Zoology. Scientific names are those used
by Stansbery (1980).
Collecting Stations
Under bridge on Indiana St. Rt. 335, .4 mi S of St. Rt. 64,
1 mi N of village of Crandall; Harrison County, Indiana.
Take St. Rt. 335 SW of Crandall to Bethlehem" Cemetan,-
Rd., .5 mi N on Cemetary Rd. to Indian Creek; Harrison
County, Indiana.
Take St. Rt. 135 S of village of New Salisbury to un-
named, unimproved dirt road, .4 mi S of Southern Rail-
way tracks, .7 mi E on dirt road to bridge; Harrison
County, Indiana.
Take St. Rt. 135, 3.7 mi S of New Salisbury to Conrad
Cemetary Rd., .3 mi E to Creek; Harrison County, In-
diana.
Take St. Rt. 135 2.5 mi SW of Corydon to Heidleburg
Church Rd, then Mathis Rd. 1 mi to Creek; Harrison
County, Indiana.
Take St. Rt. 135 to Heidleburg Church Rd., then to Val-
ley View Rd. 1 mi to creek, Ca 3.5 mi SW of Corydon;
Harrison County, Indiana.
Indiana St. Rt. 335, .1 mi E of Indiana St. Rt. 135, Ca 2
mi S of New Salisbury; Harrison County, Indiana.
Table 1. Freshwater Naiads collected 1979-81 from Big Indian Creek.
Species listed by site.
Anodonta
grandis Say, 1829
Strophitus u. undiilatus (Say, 1817)
Alasmidonta vindis (Raf., 1820)
Lasmigona complanata (Barnes, 1823)
Lasmigona costata (Raf.. 1820)
Aroblcma £. plicata (Say, 1817)
Fusconaia flava (Raf.. 1820)
EUiptlo dilatata (Raf., 1820)
Leptudea fragiUs (Raf., 1820)
Potamilus alatus (Say. 1817)
Toxolasma parvus (Barnes, 1823)
VI 1 Ipsa I, ins (Lea, 1829)
Vlllosa lienosa (Conrad, 1834)
l.ampai 1 is radiata luteola (faoi., 1819)
LampBi 1 IS vcntncosa (Barnes, 1823)
Lampsilis fasciola Haf . . 1820
corbicula fluminea
68 THE NAUTILUS
April 21, 1982
Vol. 96(2)
Summary
Survey collecting at seven stations along Big
Indian Creek yielded a total of sixteen species of
freshwater Naiads plus the exotic Asiatic import
Corbiculajluminea (Table 1). Most species were
present in good numbers at several different lo-
calities. Five species (Anodonta grandis, Lepto-
dea fragilis, Elliptio dilatata, Toxolasma par-
vus and Lampsilis fasciola) were, however,
found at only one locality each.
None of the species found is currently con-
sidered to be rare or endangered. The faunal
make-up of this small stream is typically Ohioan
and is fairly similar to that found in Floyd's Fork
and Salt River (Taylor, 1980) which enter the
Ohio River from the south in the proximity of
the mouth of Big Indian Creek which enters
from the north.
LITERATURE CITED
Goodrich, Calvin and H. van der Schalie. 1944. A Revision of
the Mollusca of Indiana. The Amer. Mid. Nat. 32(2):
257-326.
Krumholz, Louis A., R. L. Bingham and E. R. Meyer. 1970.
A Survey of the Commercially Valuable Mussels of the
Wabash and White Rivers of Indiana. Proc. of the Indiana
Acad, of Set. 79:20.5-226.
Stansbery, David H. 1980. Naiad Mollusks of the Ohio River
Drainage System. The Ohio State University Museum of
Zoology, 1 p. mimeo.
Taylor, Ralph W. 1980. Mussels of Floyd's Fork, A Small
Northcentral Kentucky Stream. The Nautilus 94(1):
13-15.
MEETINGS
July 14-17. CO. A. (Conchologists of America).
Sanibel Island, Florida.
July 19-23. A.M.U. (American Malacological
Union. New Orleans, Louisiana.
SHELL SHOWS
July 30 - Sept. 1. Jacksonville Shell Show.
Jacksonville Beach, Florida.
June 20-23. 15th annual meeting of the West-
ern Society of Malacologists at the University
of Redland, CA.
RECENT DEATHS
Wataru W. Sutow, M.D., well-known cancer
expert, author of medical textbooks, and active
member of the Houston (Texas) Shell Club, died
Dec. 20, 1981, at the age of 69. He was born
Aug. 3, 1912, in Guadalupe, California. See
American Malacologists (1973), p. 457 and Texas
Conchologist (1982), vol. 18, no. 2, p. 25.
^<^^MMA^AM^^^W^^^^^«MMMVMM^W^V^VVN^^^
Carlos G(uillermo) Aguayo, leading Cuban
malacologist, exiled in Puerto Rico, died Feb.
12, 1982, at the age of 83, in Puerto Rico. He
was born in Havana, Cuba on Dec. 19, 1899, and
became a professor at the University of Puerto
Rico in Mayaguez in 1958. He published over
130 papers on mollusks, especially those of
Cuba, and was a Guggenheim Foundation Fel-
low at Harvard in 1931-33. (see American
Malacologists (1973), p. 188).
LICENSED APPRAISALS
AND
IDENTIFICATION SERVICE
Collections of shells and libraries of shell
books expertly appraised for estate, gift and
tax purposes. Moderate fees, plus travel ex-
penses. Services confidential. Inquire below.
Professional identifications of marine mol-
lusks for biological surveys, environmental
studies and private shell collectors. Fees bas-
ed on hourly basis. Minimum $20.00.
R. Tucker Abbott, Ph.D.
P. 0. Box 2255
Melbourne, Florida 32901
U.S.A.
Vol. 96(2)
April 21, 1982
THE NAUTILUS 69
MASSIVE DESTRUCTION OF SCLERACTINIAN CORALS BY THE
MURICID GASTROPOD, DRUPELLA, IN JAPAN
AND THE PHILIPPINES'
Jack T. Moyer
Tatsuo Tanaka Memorial Biological Station
Ako, Miyake-jima, Izu Islands, Japan 100-12
William K. Emerson
American Museum of Natural History
New York, New York 10024, U.S. A
and
Michael Ross
Bureau of Fisheries and Aquatic Resources
Region 7 District Office
Cebu City, Philippines
ABSTRACT
Aggregates of the muricid gastropods Drupella fragum, at Miyake-jima, Japan,
and Drupella rugosa, at Mactan Island, Cebu. Philippines, were noted to result in
widespread destruction of scleractinian corals. Destruction was limited to fast-
growing foliate forms such as Montipora, Acropora, Pocillopora, etc., but other
genera, e.g. Porites, Goniopora, Favia, Fungia, etc.. were avoided. Muricid pre-
dation at Mactan appeared to represent a biological control on coral reef struc-
ture, "weeding out" fast growing forms and providing space and settlement sites
for other coral species, thus increasing diversity over time. At Miyake-jima, in the
warm, temperate waters of southern Japan, Acropora spp. are dominant. Coral
destructio7i by Drupella fragum has been massive on Acropora reefs at Miyake-
jima, amounting to as much as 35% of our study reef (Toga Reef No. 1) in two
years. The sudden population explosion o/D. fragum in 1976 at one site on the
island and in 1980 at another location correlates with massive siltation from
heavy bulldozing on the volcanic island, followed by heavy rainfall. A hypothesis
to explain this correlation is presented.
Although many marine animals are known to
feed on hermatypic corals (Robertson, 1970;
Reese, 1977; Taylor, et ai, 1980), only the
asteroid Acanthaster planci has previously been
reported as representing a serious threat to
coral reefs (Randall, 1972; Branham, 1973; En-
dean, 1973; and others). Robertson (1970) re-
ported that certain species of prosobranch gas-
tropods of the muricid genus Drupella are
known as predators on scleractinians of various
genera and that some have been found living in
fairly large colonies among the branches of and
under stony corals. However, to our knowledge.
'Contribution Nc
Station.
36. Tatsuo Tanaka Memorial Biological
population explosions of Drupella with
widespread coral destruction have yet to be
reported.
Since 1976, population explosions of varying
sizes involving Drupella fragum (Blainville,
1832) have been observed annually at the island
of Miyake-jima (34°05'N, 139°30'E), one of the
Izu Islands of southern Japan. The combination
of heavy predation of D. fragum and Acan-
thaster planci (see Moyer, 1978) have destroyed
much of the island's coral fauna. Since 1979, a
similar phenomenon, but with less destructive
results, has been under observation at Mactan
Island, Cebu, Philippines (10°18'N, 123°54'E),
involving Drupella rugosa (Born, 1778) and
various species of branching corals. In this
70 THE NAUTILUS
April 21, 1982
Vol. 96(2)
paper we document the role of Drupellafragum
and D. rugosa in the destruction of corals and
identify them as potentially harmful to coral
reefs.
Methods and Materials
Early observations of Drupella predation at
Miyake-jima were made incidental to behavioral
studies on reef fishes from 1976 to 1979. The ex-
tent of the damage caused by the gastropods
was not realized until 1980. Accurate measure-
ments and observations of Drupella destruction
were obtained for two months in 1980 and one
month in 1981. Data were collected both diur-
nally and nocturnally using scuba. Specimens
were collected as they fed on coral polyps 2 to 4
hours after sunset and as they were concealed
under coral branches by day. At Mactan Island,
three transects, each measuring 100 m in
length, were placed parallel to shore, 4 m apart
and at depths ranging from 1-2 m, at two study
sites (Tambuli Beach and Malingin Beach) for
the purpose of coral community studies. At
every .25 m point along these transects, a point
sample was made using a small weight (5 mm in
diameter). This provided 1200 points of informa-
tion for each reef site. Data were collected from
1979-1981. The percent of dead and grazed cor-
als was recorded at each site according to speci-
fic genera of corals and observations of Drupel-
la rugosa swarms were recorded, both diurnally
and nocturnally. Specimens were collected as
they aggregated under coral branches by day.
All specimens from both Japan and the Philip-
pines are deposited in the mollusk collection of
the American Museum of Natural History
(AMNH). Underwater photographs were taken
by Moyer at Miyake-jima and by Ross at Mactan
Island.
The four species of neogastropods observed
feeding on the corals at Miyake-jima and Mactan
are referable to the superfamily Muricacea.
Three are species of Drupella, a genus assigned
to the Thaidinae, a subfamily of the Muricidae
(Emerson and Cernohorsky, 1973; Ponder,
1973). The fourth species belongs to the nomi-
nate genus Coralliophila. of the Coral lio-
philidae, which are anatomically similar to the
Muricidae, but lack a radula. The radular denti-
tion of Drupella is atypical of the Muricidae, in
which three teeth are aligned in each transverse
row, with the central tooth commonly armed
with three cusps and the triangular lateral teeth
distally cuspid. In Drupella, the much larger and
more slenderly elongated lateral teeth are com-
monly basally denticulate on the inner margin
and distally terminate in a hooked tip (Cerno-
horsky, 1969, pp. 303-307, figs. 8-11). These
radular modifications probably reflect an adap-
tation to a specialized mode of feeding (Cooke,
1895; Arakawa, 1958; Wu, 1965; Robertson,
1970; and others). The reed-like lateral teeth
apparently sweep the polyps of coral onto the
basal denticles of the lateral teeth and the cusps
of the central teeth where the food particles are
abraded (cf. Cernohorsky, 1969, p. 304;
Fankboner, 1970, p. 15; Taylor, 1976, p. 185).
Results
Species identification
Japan: The two Miyake-jima forms of Dru-
pella clearly represent distinct species. The
specimens that were found in massive clusters
on coral are identified as Drupella fragum
(Blainville, 1832). These specimens (Figs. lA,
IB), which attain a maximum height of 23-)-
mm, have weakly developed axial ribs (12 per
whorl) and an essentially white aperture. The
exterior is pale orange-ochre, giving a yellowish-
white appearance to the shell. Many specimens
have a spirally arranged, brownish maculation
between the axial ribs, especially on the body
whorl. In some specimens, as many as six faint,
orange spots occur on the outer lip and in the in-
terior of the siphonal canal. The identification of
these specimens must remain tentative until
comparison can be made with the typological
specimens of Purpura fragum in Blainville's col-
lection, which is deposited in the Museum Na-
tional d'Histoire Naturelle, Paris. In the original
description, Blainville (1832, p. 203, pi. 9, fig. 4)
noted that the yellowish-white shell possessed
dark rose nodules and a white aperture. In the
present specimens, the nodules in some individ-
uals are dark to pinkish brown.
The second Miyake-jima species, Drupella
e^ata (Blainville, 1832, p. 207, pi. 11, fig. l)[ = D.
Vol. 96(2)
April 21, 1982
THE NAUTILUS 71
FIGS. 1-3. lA iind IB, Drupella fraguni {Blainville). Miyake-jima. Jajjan; A, all white form. AMNH 203816a: B, maculated
form. AMNH ■203816h: x2. 2A and 2B, Drupella elata (Blainville), Miyake-jima. Japan, AMNH 202766; x2. 3A and 3B,
Drupella rugosa (Blainville). Marian Island. Philippines; A, all white form, AMNH 20266I,a; B,/orm mith colored nodules and
tannish orange aperture, AMNH 2027J,6b; x2.
'.pectrum (Reeve, 1846)], numerous individual
specimens of which were observed on the corals,
las a more massive shell with fewer (9 per
vhorl) axial ribs that are more obtuse. These
specimens, the largest of which examined by the
iecond author measures 28 + mm in height, are
vhite within and without, but the edge of the
)uter lip is tinged with greenish-yellow. The
;pecimens are largely overgrown with calcare-
)us algae and bryozoans (Figs. 2A, 2B). It
■hould be noted that this species was previously
)laced in the synonmy of Drupella cornus
Roding, 1798), see Cernohorsky (1969, pp. 304,
;05, pi. 48, figs. 12, 12a, b, and figs. 14, 14a [fide
Cernohorsky, 1978, p. 70]). H. A. Rehder (in
delville, 1980), however, notes that "D. comus
is restricted to the Indian Ocean . . . [and] D.
elata ... is found in the Pacific from Indonesia
eastwards." On morphological grounds, largely
the color of the aperture (orange in D. comus,
white in D. elata), Rehder does not believe the
two forms are conspecific, although he does not
rule out the possibility that D. elata may prove
to be a geographic subspecies of D. comns. We
follow Dr. Rehder in referring the western
Pacific specimens of this complex to D. elata
(Blainville).
The third muricacean gastropod observed
preying on corals at Miyake-jima is the wide-
ranging Indo-Pacific species, Coralliophila
violacea (Kiener, 1836) [=Murex neritoideus
Gmelin, 1791, not Linne, 1767; =C. diversi-
72 THE NAUTILUS
April 21, 1982
Vol. 96(2)
formis (Kiener, 1836); = C. squamulosa (Reeve,
1846)]. This distinctive suctorial-feeding species
is characterized by the dark violet aperture and
whitish squamulosely striate exterior (Cerno-
horsky, 1972, p. 131, pi. 37, fig. 5).
Philippines: The muricid snails found swarm-
ing on corals at Mactan Island are referable to
Dnipella rugosa (Born, 1778, p. 303) [=D. con-
catmata (Lamarck, 1822)]. These specimens
(Figs. 3A, 3B), the largest of which measures
24.6 mm in height (mean height approximately
18 mm in a sample of 360 specimens), has a con-
spicuously nodular appearance. The body whorl
is sculptured with 3 to 4 rows of prominent
nodules, which are reduced to a single row on
the penultimate whorl. The color varies consid-
erably, ranging from creamish-white specimens
to ones with dark brown or tannish nodules. The
aperture and siphonal canal may be entirely
white or a bright tannish-orange. Two speci-
mens of Drupella elata (Blainville, 1832) were
among the 348 specimens of D. rugosa collected
in one of the sites sampled on Mactan Island.
The larger specimen (AMNH catalogue no.
202766) measures 29.6 mm in height.
Field observations
Although situated at more than 34° North
latitude, Miyake-jima supports a surprisingly
diverse tropical fauna (Ida and Moyer, 1974;
Shepard and Moyer, 1980; Tribble and Randall,
MS). Tribble and Randall (MS) identified 92
species of scleractinian corals representing 45
genera. These are widely scattered in small out-
croppings, rather than as true coral reefs such
as those typically found at tropical latitudes.
Some relatively large Acropora patches are
present in scattered locations around the island,
the largest of which is located at Toga Bay on
the southwest side of the island. This patch
covers an area of approximately 1200 m\ and
will hereafter be referred to as Toga Reef No. 1.
"Swarming" of Drupella fragum was first
noted on a large platform of Acropora sp. (1.5 m
in diameter) in Igaya Bay, on the northwest side
of Miyake-jima, in August, 1976. Recent evi-
dence of gastropod predation was evident in the
form of fresh, white coral skeletons and small
swarms of D. fragum, but when the entire plat-
form was found dead and overgrown with algae
in the Spring of 1977, it was not known whether
it was killed by D. fragum, Acanthaster planci
(which appeared on the island's corals in the
winter of 1976-77; Moyer, 1978), or from silta-
tion from construction near the bay followed by
heavy rains.
A similar Acropora platform at Igaya Bay was
used as a cleaning station by a juvenile labrid
fish, Thalassoma lutescens, in 1978, and was
photographed and repeatedly observed at that
time (Fig. 4A). During September and October,
1978, a swarm of D. fragum appeared on this
coral, which was subsequently totally destroyed,
apparently by Drupella predation (Fig. 4B).
Accurate observations and measurements of
D. fragmn destruction were not possible until
the autumn (September and October) of 1980,
when one of us (JTM) was engaged in daily
Acanthaster monitoring as part of a removal
program. At this time, sizeable areas of freshly
killed white Acropora spp. were discovered,
with the area of destruction widening on a daily
basis. Careful searches in and under the corals
disclosed only swarms of Drupella fragum. Dur-
ing an evening dive, 17 September 1980, an in-
festation of several thousand Drupella fragum
was found massed around the border between
living and dead corals, devouring the polyps.
The snails were bunched around and on top of
each other in such numbers that it was impossi-
ble to estimate how many individuals were pre-
sent. Between 20:25 h and 21:00 h, a total of
about 1,500 were collected, 662 of which were
kept and later deposited at AMNH (catalogue
no. 203816). The remaining specimens were dis-
carded. Hundreds of others fell through the cor-
al branches and could not be recovered. In-
terestingly, all 12 AMNH specimens selected at
random for radular study were found to be
females. This swarm of D. fragum seemed to
disperse as waters cooled in winter, however, an
area of 35 m^ of reef was destroyed by their
predation during the two month period of obser-
vations (Fig. 5). No egg cases were observed on
or under the corals, suggesting that the
gastropods were swarming to feed. There was
no noticeable evidence that the swarms were
Vol. 96(2)
April 21, 1982
THE NAUTILUS 73
"IG. 4. A. Healthy Acropora coral platfimn at Miyake-jima. Japan. !!)?:). with the juvenile fish. Thaiassoma lutescens
I.'ifindae). cleaning Chromis flavoniaculata (Pomacentridae): B. Same Acropora platform in 1981. totally dead and overgrown
filli algae, after invasion o/" Drupella fragum. Note faviid coral lo7i far side in both photographs) remains unharmed by
II 1st ropcid invasio n.
74 THE NAUTILUS
April 21, 1982
Vol. 96(2)
FIG. 5. A. /";/"(
Japan, Sept. I'JSO.
, , \. ;. i/-,.ir. jniin. Japan, 1979, prior to Drupella fragum irM^aston; B, Toga Reef No. 1. Miyake-jimi
• il imik i/f Drupeila explosion: 5C, (on opposite page) Dead reef at same location in October. 1981.
Vol. 96(2)
April 21, 1982
THE NAUTILUS 75
FIG. 6. Toga Reef No. 1. Miynkejniia. Jiijiini, during Drupella fnigiini rxphision, Norcinhfr, i:lsi. A'nlc evidence of
movement from left to right in photo, with fresh algal growth over earlier coral kill at the left of photo.
76 THE NAUTILUS
April 21, 1982
Vol. 96(2)
directly related to reproductive purposes, but an
indirect relationship (intensive feeding either
directly before or directly after the reproductive
season) cannot be discounted.
A similar explosion of D. fragum was moni-
tered at Toga Reef No. 1 throughout the month
of November, 1981 (Fig. 6). During this period,
a total of 17 m^ of coral was destroyed. The com-
bined damage observed during two months in
1980 and one month in 1981 amounted to more
than 4% of the 1200 m^ reef being destroyed by
what was unquestionably predation by D.
fragum. Between 1979 and 1981, approximately
35% of Toga Reef No. 1 was destroyed. Records
from a carefully monitored ^ca?ii/iaster removal
program carried out in Toga Bay in 1980 and
1981 strongly suggest that Drupella fragum.
predation was responsible for most of the coral
destruction at Toga Reef No. 1. Acanthaster
were rarely seen at that reef, but were present
in small numbers at Toga Reef No. 2 and, more
commonly, at isolated patches deeper in the bay.
Surveys in November, 1981, at Igaya Bay, site
of the first detection of Drupella fragum out-
breaks in 1976, disclosed numerous patches of
freshly killed Acropora spp., similar to those at-
tributed to probable Acanthaster predation in
1978-1980. Close observation in and under the
branches of such corals invariably disclosed
clusters of D. fragum and numerous individuals
of the much larger D. elata (Blainville, 1832).
Relatively low numbers of Acanthaster were
removed from Igaya Bay, in spite of intensive
searches during the Acanthaster removal pro-
grams in 1979-1980. This fact, plus incidental
observations oi D. fragum outbreaks from 1976
to 1980 and the widespread occurrence of iso-
lated patches of corals under Drupella attack in
1981 (when the first intensive searches for the
muricids were attempted), suggest in retrospect
that a large amount of the massive Acropora
destruction at that site (perhaps as much as 50%
or more) is attributable to population explosions
of Drupella fragum.
Failure to discover the important role of muri-
cid predation at the onset of coral destruction at
Miyake-jima resulted from (1) presence of mod-
erate numbers oi Acanthaster planci at various
locations around the island and the perhaps
understandable assumption that fresh coral kill
resulted from asteroid predation, and (2) the
secretive behavior of D. fragum, which ag-
gregate far back under coral branches by day,
coming out at night to feed on coral polyps (Fig.
7). Observations in 1981 suggest t\\aL.tD. fragum
are more active during the dark phases of the
moon than around the full moon (more were visi-
ble on both night and day dives around the new
moon than at the full moon, and more fresh cor-
al kill was noted, although accurate measure-
ments on a daily basis could not be obtained, due
to the position of the study site on the windward
side of the island). D. fragum, also appeared to be
negatively phototactic. Many dropped between
the coral branches when caught in the flashlight
beam or as the strobe flashed.
At Mactan Island, data on swarming by Dru-
pella rugosa were collected from three different
sites, two at Tambuli Beach (AMNH catalogue
nos. 202763, 202764) and one at Malingin Beach
(AMNH catalogue no. 202765), see Table 1. On
Philippine reefs studied by the third author,
these snails are usually found widely dispersed,
in small groups or as individuals, and they ap-
parently are restricted to shallow waters. Since
April, 1980, it has been noted that at the Mactan
study sites, D. rmgosa has occurred on numerous
occasions in higher densities, including swarms
of up to 1500 individuals per .5 m\ comparable
to swarms of D. fragum on Acropora corals at
Miyake-jima (Fig. 8). Significant destruction of
specific corals was noted in localized areas; how-
ever, massive reef destruction, such as reported
above on the reefs at Miyake-jima, has not been
observed. Grazing by swarms oi D. rugosa, like
D. fragum, is nocturnal, with observed preda-
tion to date limited to the Astrocoeniina, specifi-
cally, Acroporidae and Pocilloporidae. These
corals, including the genera Montipora, Acro-
pora, Seriatopora and Pocillopora, are all small
polyped and branching or foliate in growth form
(Table 2). For these commonly grazed corals,
unlike the Japanese situation, predation appears
random and incomplete, resulting in scattered
patches of surviving corals in the grazed areas.
Corals with larger polyps (greater than 1 mm)
and massive growth forms are avoided and not
subject to predation by these molluscs, either in
/ol. 96(2)
April 21, 1982
THE NAUTILUS 77
FIG. 7. A, Diurnal aggregation (//' Drupella fragum under Acropora sp. at Toga Reef No. 1, Miyake-jima.
Japan, November. 1981; B, Nocturnal feeding y/'Drupella fraguni on Acropora sp. at Toga Reef No. 1. Miyake-
jima. Japan. November. 1981.
78 THE NAUTILUS
April 21, 1982
Vol. 96(2)
Vol. 96(2)
April 21, 1982
THE NAUTILUS 79
Table 1. Composition of dominant corals on
Mactan Island study sites
'able 2. Grazing preferences of Drupel la rugosa
at Mactan Island
^omnonly Grazed Corals
tontipora fruatiaosa
I. gvasi lis
1. alaiaormia
1. ramosa
1. foliosa
1. prolifera
^eriatopora hystrix
loderately Grazed Corals
'ocillopora vermoosa
^eriatopora oaliendmm
^onmonly Avoided Corals
tontipora aactus
1. verpuaosa
'OT^ tes
''avia
'avi tes
'latygyra
'■oniastrea
■oniopora
'yphastrea
■ardenoseris
'oeloseris
H.ploc2strea
Aaropora formosa
A. tenuis
A. florida
A. palifera
A. robusta
A. humilus
Aaropora hyaointhus
A. millipora
Galaxea
Pavona
Merulina
Euphyllia
Hydnophora
Peotinia
Lobophyllia
Symphy I Ha
Fimgia
Polyphyllia
Cyalosevis
Eahinopora
warms or as individuals (Table 2). Contrary to
he report by Demond (1957), wliich found Dru-
lella elata "most frequently on Porites sp.", and
hat of Taylor (1980) of Z). rugosa predation on
Writes colonies, Porites spp. appear to be en-
irely avoided by Drupella rugosa in the Philip-
lines. In addition, several highly tuberculate
(course surface projections) species of the most
commonly grazed genus, Montipora, are also
entirely avoided, suggesting a degree of host
selection.
Discussion
Robertson (1970) reported that species of
Drupella are known to be associated with scler-
actinian corals, and Fankboner (in Robertson,
1970) described feeding of Drupella comus
(Roding, 1798) on polyps of stony corals. Taylor
(1976, pp. 178, 185; 1978, pp. 95, 98) records
that Drupella comus and D. nigosa (Born, 1778)
feed on coral polyps. The literature, however,
suggests that not all the species of Drupella, at
least at the presently recognized generic alloca-
tions, may be obligate coral associates (Cerno-
horsky, 1969, p. 304; Robertson, 1970; Taylor,
1978, p. 99). This is further suggested by the
fact that four individuals of D. elata (Blainville,
1832) appeared on a species of Goniopora (Pori-
tidae) within a week after 6 of 8 parasitic muri-
cacean gastropods, Coralliophila uiolacea
(Kiener, 1836), were removed from the coral at
Miyake-jima. The coralliophilids had been ob-
served regularly over a period of six months in
the same Goniopora sp. with no appearance of
muricid predators during that period (M. Zaiser,
pers. cornm.). It is tempting to speculate that the
parasitic relationship of C. violacea and its
host may include some elements of mutualism.
Taylor (1978, p. 99), however, found on Can
Island, Addu Atoll, Maldives, that Drupella cor-
nus and Coralliophila violacea occur mostly on
different species of stony corals, and, as noted
above, Drupella rugosa avoids Poritidae in the
Philippines, but such avoidance is not necessar-
ily the case elsewhere (Taylor, 1980). The possi-
bility of competitive interactions between C.
violacea and Drupella spp. is currently under in-
vestigation by the senior author.
Our information on the composition of living
and grazed corals at the Mactan Island reef sites
suggests a degree of host selection by Drupella
rugosa, with specific preferences for Montipora
and Acropora and an obvious avoidance of
Porites, which is more common at Mactan than
Acropora (Tables 1 and 2). The effect of such
80 THE NAUTILUS
April 21, 1982
Vol. 96(2)
prey-preference is similar to that reported for
Acanthaster planci by Goreau, et al. (1972), and
Glynn (1976). These studies revealed a parallel
selection by Acanthaster for numerically com-
mon, fast growing species of Acropora, Monti-
pora. Pocillopora. Striatopora, and Stylophora.
as well as some faviids and fungiids. Other cor-
als appeared to be resistant to Acanthaster, e.g.
Millepora, Heliopora, Goniopora, and certain
species of Porites and Pocillopora (Goreau, et
al., 1972). Under "normal" conditions on tropical
reefs, such as those at Mactan, the results of se-
lective predation both by Acanthaster and Dru-
pella appear to be the same, i.e., a periodic
"weeding out" of the fast-growing, foliate
species (particularly the very abundant Monti-
pora at Mactan), providing space and settlement
sites for other corals and thus increasing diver-
sity over time. As discussed by Goreau, et al.
(1972) for Acanthaster predation, there will be
understandably different immediate and long
term effects as far as diversity and coral cover
are concerned, depending upon the intensity of
predation. At Mactan, Drupella rugosa appears
to represent an additional biological control
(with Acanthaster) on the coral community
structure. This seems to be characteristic on
tropical reefs elsewhere. R. Randall {pers.
comm.) reports that at Guam Drupella sp. feeds
exclusively on Pocillopora. Entire Pocillopora
colonies are destroyed, but destruction of large
segments of the reef, such as that occasionally
caused by Acanthaster population explosions,
does not occur.
The situation in the warm temperate waters
at Miyake-jima is quite different. As noted, true
coral reefs do not occur there, although coral
diversity is remarkable for such a high latitude.
Acropora spp. are dominant and form large
patches at certain localities, e.g. Toga Reefs
Nos. 1 and 2. However, other corals are rela-
tively scattered in isolated, small colonies on
the lava substrate (Tribble and Randall, MS).
Patches of branching Acropora are preferred
prey by Drupella fragum, and we have never
seen evidence of this snail feeding on other coral
genera.
Why Dnipella J'nuvun population explosions
began to occur in about 1976 at one site on
Miyake-jima and in 1980 at another site is a
puzzling question. The senior author has worked
on both sites since 1957, finding no evidence of
widespread coral destruction until 1976. It may
be more than a coincidence that heavy silting
from construction programs near the study sites
preceded each outbreak by from 2 to 4 years in
both cases. Beginning in 1972 and continuing
until 1974, large amounts of sand were pumped
with seawater through a large sandpipe from
the sandy interior of Igaya Bay to a filtering
center on shore, where the sand was collected.
The murky water, containing fine sediments,
flowed back into the bay, settling over coral
patches. Occasional breaks in the sandpipe
added to this siltation. During the same period,
a large pasture for dairy cattle was constructed
on the volcanic mountain above the bay. Lum-
bering, followed by bulldozing to level the land,
preceded the planting of cattle feed. Five dry
river beds run into Igaya Bay, all of which pass
through this recently constructed pasture.
Heavy rains during the period of bulldozing
flooded the rivers with muddy water and cut
visibility in the bay (normally 15-40m) to less
than 2 m on many occasions during this period.
Drupella destruction was noted from 1976, four
years after the beginning of both sand mining
and pasture construction.
Similarly, in 1976 a road was constructed to
Toga Bay for the purpose of development of a
marine park featuring Toga Bay's two large
coral patches (Toga Reef No. 1 and Toga Reef
No. 2). Silting from this road into the bay began
immediately, but increased greatly in 1978,
when the road was paved and drainage ditches
constructed to a point about 300 m above the
bay. Erosion along the remaining 300 m of road
since 1978 has been massive. Drupella destruc-
tion in Toga Bay first appeared in 1980, four
years after the construction of the road and two
years after severe siltation.
Although the relationship between massive
siltation and population explosions of Drupella
fragum at Miyake-jima must remain purely
speculative at this time, it is of interest to con-
sider the gastropod population explosions in the
light of Birkeland's (in press) hypothesis relating
Vol. 96(2)
April 21, 1982
THE NAUTILUS 81
cycles of Acanthaster planci destruction with
long periods of drought followed by heavy rains.
Birkeland presents evidence to show that heavy
rainfall following an extended dry season or
drought results in great increases in nutrients,
especially phosphorus, from terrestrial runoff
into the shallow waters near shore, thus stimu-
ating unusually lush blooms of phytoplankton.
This increased food supply permits Acanthaster
arvae to survive in much higher densities than
inder normal conditions, resulting in population
explosions and extensive coral damage three
/ears later, when the postlarvae reach maturity.
A similar phenomenon may account for the
Drupella fragum. explosions at Miyake-jima;
leavy siltation from human activities accom-
)anies tyjihoon or rainy season downpours, thus
ntroducing nutrients into coastal waters. Many
ihallow water marine invertebrates experience
)utbreaks at irregular intervals (Coe, 1956), and
;uch outbreaks have been related to terrestrial
lutrient runoff (see Sutcliffe, 1972, 1973). J. B.
Taylor (1975) identified 14 species of thaidid
'eligers (all four-lobed) in the plankton of
Caneohe Bay, Hawaii, including Drupella elata
as D. comtis). It is possible that Drurpella larvae
■at phytoplankton and that the heavily silted
orals may be unable to consume these larvae in
lumbers sufficient to control their population.
)f course, we recognize that this is pure conjec-
ure, but we present it for the purpose of stimu-
ating research on this intriguing problem.
ACKNOWLEDGMENTS
We thank the Fishermen's Cooperative of
Jiyake-jima and the Fisheries Divisions of the
I >\ernments of Tokyo Prefecture and Miyake-
ima for financial and logistic support during
his study. The efforts of J. A. Dalton, J. L.
)icksved, G. Hodgson, T. Takada, K. Tateyama,
1. Umeda and M. J. Zaiser in field observations
nd data collection are greatly appreciated. R.
uiiidall is thanked for sharing observations of
h-iipeUa predation at Guam. Dr. C. Birkeland
itidly offered expert advice and supplied impor-
int literature. Drs. R. T. Abbott, H. A. Rehder,
Is. B. W. Myers, and Mr. A. D'Attilio gener-
usly provided information on the taxonomy of
the Thaidinae and C. J. Ferraris, Jr. on Philip-
pine corals. Dr. J. Rosewater kindly supplied a
needed reference. W. E. Old, Jr. and S. S.
Horenstein and M. Werner, respectively, pro-
vided bibliographic assistance, photographed
the specimens (Figs. 1-3), and tj-ped the
manuscript. We are indebted to Dr. R. Robert-
son for critically reading the manuscript. We
also thank P. Kott and M. Cope.
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82 THE NAUTILUS
April 21, 1982
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species. Japan. Jour. Ichthyol. 21(3):113-128.
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Moyer, J. T. 1978. Crown of thorns starfish invades Miyake-
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Ponder, W. F. 1973. The origin and evolution of the Neo-
gastropoda. Malacologia 12(2):295-338.
Porter, W. P. 1972. Predation by Acanthaster and its effect
on coral species diversity. Amer. Natur. 106(950):
487-492.
Randall. J. E. 1972. Chemical pollution in the sea and the
crown-of-thorns starfish (Acanthaster planci). Biotropica
4(3): 132- 144.
Reese, E. S. 1977. Coevolution of corals and coral feeding
fishes of the family Chaetodontidae, p. 267-274. Third
International Coral Reef Symposium Proc. vol. 1, Univ.
Miami. Miami, Florida.
Robertson, R. 1970. Review of the predators and parasites
of stony corals, with special reference to symbiotic proso-
branch gastropods. Pacific Sn. 24(l):43-54.
Shepard, J. W. and J. T. Moyer. 1980. Annotated checklist
of the fishes of Miyake-jima, Japan. Pt. 1, Pomacentridae,
Chaetodontidae, and Pomacanthidae. Publ. Seto Mar.
Biol. Sta. 15(l-4):227-241.
Sutcliffe, W. H., Jr. 1972. Some relations of land drainage.
nutrients, particulate material, and fish catch in two east-
ern Canadian bays. Jour. Fish. Res. Bd. Canada 29(2):
357-362.
1973. Correlations between seasonal river dis-
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Taylor, J. B. 1975. Planktonic prosobranch veligers of
Kaneohe Bay. Ph.D. Diss. Univ. Microfilms Inst., Ann
Arbor, Michigan, 331 p.
Taylor, J. D. 1976. Habitats, abundance and diets of muri-
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1980. Diets and habitats of shallow water preda-
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B. (ed.) Univ. Hong Kong Press, p. 163-180.
1978. Habitats and diet of predatory gastropods
at Addu Atoll, Maldives, Exp. Mar. Biol. Jour. 3(1):
83-103.
Taylor, J. D., N. J. Morris and C. N. Taylor. 1980. Food
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Tribble, G. W. and R. Randall. [MS]. Description of coral
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SUCCINEA AVARA SAY FROM THE SOUTHERN GREAT PLAINS
OF THE UNITED STATES
Dorothea S. Franzen
Illinois Wesleyan University
Bloomington, Illinois 61701
ABSTRACT
Succinea avara Sa?/, 182Jt, was described from shells collected from the North-
west Territory. This study is o/S. avara collected at 21 stations in four states of
the Southern Great Plains Region of the United States. Shells and anatomical
structures are described and illustrated; habitats of a selected representative
series from the 21 stations are described.
Succinea avara Say, 1824
Sucnnea avara Say, 1824, p. 250; pi. 15, Fig. 6.
Succitiea avara Say, Pilsbry, 1948, pp. 837-840;
Fig. 442. B, b, C, c, D.
Shells of Succineidae present only a few dis-
tinctive characteristics; specific determinations
depend largely upon anatomical characteristics
of the soft parts. It is questionable whether the
anatomy of the soft parts as now identified with
a species actually corresponds to the anatomy of
the soft parts of the holotypes and paratypes
which are known only from their shells. It is im-
V^ol. 96(2)
April 21, 1982
THE NAUTILUS 83
possible to determine the exact location of the
type locality when geographically it is desig-
nated only as being in a general area, as iorSue-
Hnea avara Say, "Inhabits the Northwest Terri-
:ory" (Say, 1824, p. 260). The succineas taken
Tom a locality today may not be representative
)f the fauna existing fifty to a hundred or more
/ears ago. Such are the problems concerning
;he identification of S. avara Say.
The shells of the holotype and paratj^aes of
'^uccinea avara, Academy of Natural Science
Philadelphia No. 59542, are small and probably
mmature.
^ype description:
"S. avara. Shell suboval, pale reddish-yellow,
subdisphanous, fragile, covered with an earthy
crust; whorls three, minutely wrinkled; body
whorl very large; spire small; aperture large,
subovate, about two-thirds of the whole length
of the shell. Length three-twentieths of an
inch. Inhabits the North-west Territory. This
small species of Succinea occurs in humid
places very frequently under stones and near
the water. The shell is always completely in-
crusted with a coating of earth. It may at once
be distinguished from either the ovalis or of
campestris by its very small size. PI. 15,
fig. 6." (Say, 1824, p. 260.)
Pilsbry (1948, pp. 837-840, Fig. 455 and Fig.
42, A, a, B, b, C, c, D) described what he con-
idered to be S. avara. Fig. 442, B, b, are draw-
igs of the reproductive system of a specimen
rom Warm Spring Canyon, Arizona, collected
y Ferriss in 1909; C, c, are of a specimen from
lurricane Fault, Arizona.
The purpose of this paper is to describe shell
nd anatomical features, as well as habitats, of
uccinea avara Say of the Southern Great
'lains of the United States. Collections were
lade by Artie L. Metcalf and by me at 21 sta-
ons located in the western half of Texas, east-
rn and southern New Mexico, southern and
orthwestern Oklahoma and southwestern Kan-
as (Fig. 1).
Succineidae are generally regarded as being
mphibious- living on wet ground, in woods,
long shores, or appearing on the surface
allowing a rainfall heavy enough to soak the
round. However, we have sometimes found
Fid. 1 . Four-state map shomng locations of the 21 collecting
sidlionti.
them in habitats far removed from wet areas.
At the stations where S. avara was obtained,
the annual precipitation ranges from about 9 to
44 inches. All stations are subjected to periods
of from 3 to 5 months in which the precipitation
is less than an inch per month (Yearbook of
Agriculture, 1941). S. avara included in this
study were taken in early spring, summer, and
early winter months during which time the
snails were either active or aestivating. They
were found in damp places under rocks, logs,
boards or dead stems of Yucca sp. The following
are the locations of the 21 collecting sites and
descriptions of habitats of a selected representa-
tive series often of those sites. The field number
designations and descriptions of habitats are by
Artie L. Metcalf. My field numbers, enclosed in
parentheses, serve as a reference to my records.
Sites of my collections are indicated by my field
numbers and the descriptions of such habitats
are mine.
Stations
1. Field No. ALM 968 (DSF 402); 30 June, 1969, along the
Cimarron River, along New Mexico Rd. 325; 7.5 mi W of its
junction with New Mexico Rd. 370, Union County. New Mex-
ico. Altitude: 5,250 ft. above mean tide (AMT). Annual
precipitation about 17". Habitat: under logs on moist
floodplain of the river and also under rocks on adjacent
hillside.
2. Field No. ALM 1058 (DSF 412); 30 ,Iuly, 1970; 2.5 mi N
of Mt. Dora, Union County, New Mexico.
84 THE NAUTILUS
April 21, 1982
Vol. 96(2)
3. Field No. ALM 1060 (DSF 41 1); 31 July, 1970; valley of
North Canadian River, 0.1 mi N of bridge over river on New
Mexico Rd. 370; about 22 mi N NW of Clayton (S 33, T 29 N,
R 52 W), Union County, New Mexico.
4. Field No. ALM 673, DSF .342; 8 May, 1966; .5 mi SE of
Rincon; HW^ 1-25 at junction with Engle Road, Dona Ana
County, New Mexico. Altitude: 4370 ft. AMT. Annual pre-
cipitation about 9.5". The locality is in Jornada del Muerto-
a basin between two mountain ranges. Habitat: Succinea
avara were aestivating on dead stems of Yucca data
Engelm. growing in a "tobosa grass swale" where the
predominant plant is tobosa grass, Hilaria mutica (Buckl.)
Benth. The snails were found on the side of the dead Yucca
stems lying on the ground where there was a trace of
moisture.
5. Field No. ALM 948 (DSF 398); 19 November, 1968:
valley of Tularosa River and falls, 0.5 mi SW of bridge over
Tularosa River, U.S. Hwy 70; 8.5 mi SW of Tularosa (NW '/i,
SW 'A, S 32, T 13 S, R 11 E), Otero County. New Mexico.
6. Field No. ALM 946 (DSF 397); 19 November, 1968;
Mescalero Indian Reservation, Valley of the Tularosa River,
1.05 mi S of Tularosa Spring (SW 'A.SW 'A. S 7, T 14 S, R 13
E), Otero County, New Mexico.
7. Field No. ALM 998 (DSF 407); 11 October, 1969, and
19 September, 1970; junction of Pehasco and Cox Canyons
(SW 'A, S 3, T 17 S, R 13 E), Otero County, New Mexico.
.•Mtitude: 7200' AMT. Annual precipitation about 22".
Habitat: grassy, riparian meadow where the Penasco River
is about 5 ft. wide. The canyon wall is wooded with pre-
dominantly Ponderosa pine.
8. Field No. (DSF 492); collected by Artie Metcalf 23
September, 1978; east-central part of Nash Draw Basin
(center of S 15, T 22 S, R 30 E), 20 mi E of Carlsbad, Eddy
County, New Mexico.
9. Field No. ALM 670; 8 February, 1966, and DSF 339, 7
May, 1966; Franklin Mountains (S 27, T 28 S, R 4 E), about 5
mi NE Canutille, El Paso County, Texas. Altitude: 4900 ft.
AMT. Annual precipitation about 9". Habitat: under dead
Dasylirion sp. and under moist limestone rocks. A light rain-
fall which occurred the first of May resulted in certain areas
being relatively moist.
10. Field No. ALM 1396 (DSF 426); 9 August, 1972; 0.6
mi SW of Dalhart on southeast side of U.S. Hwy 54 and
bordering Rita Blanca Creek, Hartley County, Texas.
11. Field No. ALM 1283 (DSF 418); 19 June, 1971; 2.3 mi
W Channing, south side of Texas Farm Rd. 767, Hartley
County, Texas.
12. (DSF 389); collected by Artie Metcalf 23 August,
1968; flood plain of Wolf Creek, 1 mi E of dam on Lake
Fryer, Ochiltree County, Texas.
13. (DSF :',90); collected by Artie Metcalf 23 August,
1968; bluffs along north shore of Lake Fryer, Ochiltree
County. Texas. Altitude: 2650 ft. AMT. Annual precipitation
about 19.31". Habitat: under loose limestone below scarp in
Ogallala Formation.
14. (DSF 392); collected by Artie Metcalf 13 September,
1968; bluffs on southeast .-side of Buffalo Lake, 3 mi S of Um-
barger, Randall County. Texas.
15. Field No. ALM 1801 (DSF 476); 20 March. 1977; 9 mi
ENE or 6.6 mi W of junction of Ranch Rd. 2084 (to
Christoval) with Texas Hwy 29. S side of Texas Hwy 29.
Schleicher County, Texas.
16. Field No. ALM 1451 (DSF 430); 16 April, 1973; east
side of conical hill immediately E of old Fort Lancaster; N of
U.S. Hwy 290, Pecos County. Texas. Altitude: 2075 ft.
AMT. Annual precipitation about 19". Habitat: under lime-
stone rocks on E side of conical hill. The vegetation consists
of sparse grass and low xeric shrubs.
17. Field No. ALM 1458 (DSF 428); 18 April, 1973; under
limestone rocks opposite Judge Roy Bean Visitor Center,
Langtry, Val Verde County, Texas.
18. Field No. DSF 422; 14 July, 1972; Buffalo Bayou,
Texas Hwy 6, 1 mi S of junction with HWY I-IO, near Ad-
dicks, Harris County, Texas. Altitude: 50 ft. AMT. Annual
precipitation about 44". Habitat: Succinea avara found
aestivating on a trunk of a pecan tree up to 7' above ground
level and on a fence rail 5' above ground level. The ground
vegetation comprised nettles and grasses which may have
been too dense for the succineas; therefore, they sought
more open areas.
19. Field No. DSF 387, 28 July, 1968, and 17 July, 1972;
west bank of a bay of Lake Texoma, University of Oklahoma
Biology Station, 2 mi E of Willis and Oklahoma State HWT
99, Marshall County, Oklahoma. Altitude: about 500 ft.
AMT. Annual precipitation about 38". Habitat: the snails
were aestivating under boards and logs lying on the un- '
shaded bank of the lake; temperature at time of collection,
95°F.
20. Field No. ALM 1066 (DSF 414); 1 August, 1970; 6 mi
S Turpin; IV2 mi N of Beaver Creek, Beaver County, Okla-
homa. Altitude: 2600 ft. above AMT. Annual precipitation I
about 18". Habitat: under stones of bluff of Ogallala Forma-
tion. The area is a short grass prairie with Yucca glauca Nut
tall.
21. Field No. ALM 1559 (DSF 442); 1974; Point of Rocks,
an escarpment of Ogallala Formation, 3 mi W of Kansas
Hwy 27 on N side of Cimarron River, Morton County, Kan-
sas. Annual precipitation about 16.2". Habitat: most of the
Succinea avara were under a single large stone lying at base
of scarp. Yucca glauca NuJt. and Rhus trilobata Nutt. were
common plants. Grama grass and annual ragweed were
abundant.
The Shell: Shell is conically-ovate, imperfo-
rate, amber, somewhat glossy, translucent, usu-
ally encrusted with grains of sand or soil. Com-
posed of 2V2 to 3% whorls, the shell attains a
height of 12.6 mm and a width of 6.6 mm (Table
1). Whorls inflated, sharply incised, increasing
rapidly in size from the knoblike nuclear whorl
to the large, inflated body whorl. Aperture
ovate, ranging from 47.6% to 77.7% of the
height of the largest shells obtained at the 21
stations, bounded by a sharp peristome which
Vol. 96(2)
April 21, 1982
THE NAUTILUS 85
TABLE 1. DtmermoTis of shells o/Succinea avara Say of selected ten oftli£ tumity-one collecting sites. The nwtisurements are
of the three largest shells of each locality. Ratios of measurements are listed in the last four columns.
■'.ontinues over the body whorl as a thin callus.
Columella is gently curved (Fig. 2). Surface of
the nuclear whorl appears to be, at high magnifi-
cation, malleated. Surface of the remaining
86 THE NAUTILUS
April 21, 1982
Vol. 96(2)
FIG. 2. Shells q/'Succinea avara Say of four- collecting stations: A, Station 19. Marshall County, Oklahoma
(Height 8.5 mm): B, Station 11, Hartley County, Texas (Height 11.1 mm): C, Station 13, Ochiltree County, Texas
(Height 11.2 mm): D, Station 1. Union County. New Mexico (Height 10.5 mm).
whorls are marked with striae, fine on the pe-
nultimate whorl, becoming heavier and coarser
producing a rough appearance on the ultimate
whorl, especially near the aperture (Fig. 2).
Body and Mantle Surfaces: Surface of translu-
cent, gray-white body is smooth; low tubercles
may be observed on head region. On either side
of the lower lateral body wall a suprapedal
groove, paralleled by a shallow pedal groove, ex-
tends from the labial palp to the posterior tip of
the body. Lateral body wall incised by shallow
vertical grooves which extend to the pedal
groove, resulting in a scalloped edge. Genital
aperture elongate-crescent, about 0.7 mm in
length, surrounded by a white, tumid lip, and
situated on the anterior right-hand side of the
body.
The bodies oi Surcinea avara of the geograph-
ical region included in this study are generally
so lightly pigmented that it is difficult to
recognize any distinct pattern. When intense
enough to be discerned, pigmentation is seen to
form a pair of median bands on the anterior-
most portion of the head. Just anterior to the
superior (posterior) tentacles these bands fuse
and expand to form a triangle. From this, at
level of the tentacles, a single band extends to
where the mantle attaches to the body. On the
anterior portion of the head each of the two me-
dian bands is flanked laterally by a not very
distinct band which extends to the base of the
tentacles. Blotches of pigment on the tentacles
form, at the base of each, a band which parallels
the median band to the edge of the mantle. Also
scattered flecks of pigment are to be noted. On
either lateral body wall a faint band of flecks of
pigment may run above and parallel to the
suprapedal groove. The sole of the foot exhibits
faint longitudinal bands of pigment.
Bands of pigment extend from the mantle col-
lar across the mantle surface, coalesce as they
approach the nephridium. Pigmentation in the
form of a fine line outlines the anterior margin
of the nephridium, diffuses over its surface, and,
Vol. 96(2)
April 21, 1982
THE NAUTILUS 87
as a heavier band, outlines its posterior margin.
The nephridium is white.
Reproductive System: The stout penis and
epiphallus fill the thin, translucent, non-pig-
mented or lightly flecked, penial sheath. Junc-
ture of epiphallus and penis is marked by a con-
■;triction (Fig. 3A). Epiphallus and penis may be
contained entirely within the sheath (Fig. 3B) or
:he epiphallus and the distal portion of the penis
•nay extend through the distally open-ended
sheath (Fig. 3B). Because the thin sheath tends
;o cling to the penis, it is difficult to note that it
s open-ended. Such variations occur within any
)f the populations included in this study. The vas
deferens enters the penial sheath near its distal
end, emerges from the sheath as it enters the
epiphallus terminally (Fig. 3A, B). The broad,
stout penial retractor muscle attaches to the
distal end of the epiphallus (Fig. 3A, B).
Prostate gland, globular, composed of small
acini, enclosed within a very thin, finely pep-
pered sheath, is approximately one-third the
size of the albumin gland. Albumin gland, gener-
ally triangular, composed of small acini, is
enclosed within a very thin, finely peppered
sheath. Hermaphroditic duct may be slightly or
moderately pigmented. Lobes of the bilobed
seminal vesicles, unequal in length, are gener-
ally narrow, elongate, and lightly to moderately
pigmented. Juncture of uterus and oviduct is
marked by a slight constriction. Spermathecal
duct is broad at its base where it enters the
uterus (Fig. 3A, B).
Radula and Jaw: Structure of the radula of
Succvnea avara exhibits characteristics of the
genus. Number of rows of teeth range from
about 70 to 90. Formulae of representative rows
of teeth are to be noted in Table 2. Ratio of
laterals to marginals approaches 1:1 as found to
be true of S. ovalis Say (Franzen, 1959, Table H)
and of S. vaginacontorta Lee (Franzen, 1971,
Table H).
Structures of representative teeth are illus-
trated in Fig. 4A. The central tooth has a long,
pointed mesocone which equals or exceeds
TABLE 2. Formulae of representalioe rows of teeth of
radulae o/Suceinea avara Say.
No. of Rows
of Teeth
Row
M
STATION
No. 402
14 8-11-1-10-10
32 10 - 9-1-10-10
60 - 1 - 15 - 6
61 - 1 - 15 - 6
62 - 1 - 13 - 8
8 - 18 - 1 ■ 18 -
'IG. 3. Reproductive organs of Succinea avara Say. PS.
eniai sheath; EP. epiphallus: PRM, penial retrattor mus-
le; VD, vas deferens: VA, vagina: SPD, spermathecal duct:
>D, oviduct: SP, spermatheca: HD, hermaphroditic duct:
iG, albumin gland: GA, genital atrium: PG. prostate gland:
'S. fertilization sac: SV, seyninal vesicle.
No. 428 (Slide 2)
88 THE NAUTILUS
April 21, 1982
Vol. 96(2)
The amber-colored jaw is illustrated in Fig.
4B. Anteriorly the collar has a pointed median
fold and posteriorly a rounded indentation. The
posterior margin of the basal plate has a pointed
median fold flanked on either side by a rounded
boss.
FIG. 4. A, Representative radula teeth of Succinea avara
Say. C, central tooth; 1-L-L, first left lateral; 1-L-M, first left
marginal; 2-L-M, second left marginal; 7-L-M, seventh left
marginal; 8-L-M, eighth left marginal. B, A jaw o/Succinea
avara Say.
length of the basal plate; mesocone is flanked on
either side by a small ectocone. Laterals have a
long, sharply pointed mesocone which, gener-
ally, exceeds length of the basal plate; there is a
single smaller ectocone; endocone is generally
wanting. Differentiation between laterals and
marginals is not always sharply defined; fre-
quently an endocone is present on the outermost
one to three laterals. There may be on either
side of a lateral with a split ectocone a tooth
with an undivided ectocone. Marginals are char-
acterized by a short endocone, a long, sharply
pointed mesocone, and an ectocone which is
divided into two, three or four cusps. In 5. ovalis
and S. vaginacontorta the three small cusps of
the ectocone are short and almost equal in size.
In S. avara the two medial-most cusps of the ec-
tocone are long; the outermost cusps are minute
(Fig. 4A). The basal plates of the marginals are
as in S. ovalis Say (Franzen, 1959, Fig. 3) and as
inS. vaginacontorta Lee {Franzen, 1971, Fig. 3).
They are not long and tapering as in the genus
Oxyloma (Franzen, 1963, Fig. 1) nor as short
and broad as in the genus Catinella (Quick,
1933, Fig. 4); (Franzen, 1979, Fig. 3).
ACKNOWLEDGMENTS
National Science Foundation Grants-in-Aid
No's. NSF G18000 and NSF GB2715 provided
laboratory equipment and supported, in part,
field studies. The Academy of Natural Sciences
of Philadelphia graciously lent shells of the
holotype and paratypes of Succinea avara Say.
Dr. A. Byron Leonard read the manuscript and
offered helpful suggestions.
LITERATURE CITED
Franzen, Dorothea S. 1959. Anatomy of Succinea ovaltK
Say. Proc. Mai. Soc. London 33(5):193-199, Tables MI,
Figs. 1-7.
1963. Variations in the Anatomy of the Succi
neid Gastropod Oxyloma retusa (Lea). The Nautilus
76(3):82-95, Tables MI, Figs. 1-4.
1971. Anatomy and Geographic Distribution of
the Succineid Gastropod Succinea vaginacontorta Lee.
The Nautilus 84(4):131-142, Tables MI, Figs. 1-3.
1979. Catinella parallela. a New Succineidae
(Puimonata) From Midwestern United States. The Nauti-
lus 93(2-3):63-69, Tables 1-2, Figs. 1-3.
Pilsbry, Henry A. 1948. Land Mollusca of North America
(North of Mexico). Acad. Nat. Sci. Philadelphia Mon. No.
3. Vol. II, Ft. 2: xlvii + 521-1113, 585 figs.
Quick, H. E. 1933. The Anatomy of British Succinea. Proc.
Mai Soc. London 20(6):295-318, Tables I-V, PI. 23-25,
Figs. 1-18.
Say, Thomas. 1824. In Appendix to Keating's Narrative
Expedition . . . source of St. Peter's River, etc. (North-
west Territory) 2:260, PI. 15, fig. 6.
Yearbook of Agriculture. 1941. Climate and Man. United
States Department of Agriculture, U.S. Government
Printing Office, Washington, D.C.: v-xii and 1-1248.
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THE
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THE
NAUTILUS
Volume 96, number 3 - July 26, 1982
ISSN 0028-1344
CONTENTS
Eileen H. Jokinen
Cipangopaludina chinensis (Gastropoda: Viviparidae) in North America,
Review and Update 89
Hans Bertsch and Barbara Myers
Comments on the Eastern Pacific Trivia ritteri (Gastropoda: Triviidae) 96
Bretton W. Kent
An Overlooked Busycon Whelk (Melongenidae) from the Eastern United States 99
M. G. Harasewych and Richard E. Petit
Notes on the Morphology ofCancellaria reticulata (Gastropoda: Cancellariidae) 104
William Miller, III and Sheree Kooser
The Distribution of Donax variabilis (Bivalvia) at Ship Island, Mississippi:
I Some Paleomalacological Aspects 113
J. Gibson-Smith and W. Gibson-Smith
Divarilima (Bivalvia: Limidae) and a New Subspecies from the Caribbean 115
J. Gibson-Smith and W. Gibson-Smith
The Subfamily Melampinae (Pulmonata: Basommatophora) in Venezuela,
with Descriptions of Two New Species 116
J. Gibson-Smith and W. Gibson-Smith
An Ancestral Stephopoma (Mollusca: Gastropoda) from the Tertiary
„ of Venezuela 120
K. E. Hoagland and Wesley R. Coe
Larval Development in Orepidula maculosa (Prosobranchia: Crepidulidae),
from Florida 122
Errata 96
COMPENDIUM OF SEASHELLS
An Authoritative Guide to over 4,000 Marine Shells of the World in Color
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Two internationally known experts on mollusks have combined their knowledge and writing
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4.(l()() Species - 4.()()() cnl<.r phitcs
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Vol. 96(3)
July 16, 1982
THE NAUTILUS 89
CIPANGOPALUDINA CHINENSIS (GASTROPODA: VIVIPARIDAE)
IN NORTH AMERICA, REVIEW AND UPDATE
Eileen H. Jokinen
Ecology Section, U-42
The Univeristy of Connecticut
Storrs, CT 06268
ABSTRACT
The Asian freshwater viviparid snail. Cipangopaludina chinensis (Gray), was
introdiwed into North America in the 1890's. The species has spread across the
United States and southern Canada and is well-established in the northeastern
U.S. Connecticut populations are limited to lakes and ponds of medium-hard to
hard waters of calcium levels in excess of 5 ppm. The shell growth ofC. chinensis is
allometric with the young snails having a lower shell height to shell width ratio
than the adults. The growth patterns and radular cusp number of the typical
chinensis and the japonicus morph differ from, each other. A literature review
notes the five-year life span, diatom diet, the importance of quality food sources in
regulating population parameters, and the role ofC. chinensis as a possible host
for Asian helminths.-
The Asian freshwater prosobranch snail
Cipangopaludina chinensis (Gray, 1834)
(Synonym; Viviparus chinensis malleatus
(Reeve, 1863)) was first introduced into North
America in the 1890's (Abbott, 1950). Since
then, malacologists have been documenting the
spread of populations of C. chinensis. This
species has become well-established in parts of
North America and it is time to review the
known North American biogeography, ecology
and natural history of C. chinensis. This paper
will also add information on the snail's en-
vironmental preferences, radular structure, and
shell growth pattern.
Dundee (1974) and Clarke (1978) have syno-
nymized C. japonicws (von Martens, 1861), with
C. chinensis. Clench & Fuller (1965) believed
that the two were different species with in-
dividuals of C. japonicus having more elongate
shells (higher height/width ratios) with smaller
apical angles than C. chinensis. Morphological
intergrades exist (Clench & Fuller, 1965), indi-
cating either hybrid populations of two species,
or different morphological types within one
species. Apparently Clarke (1978) has decided
upon the latter explanation but extensive com-
parative morphological and immunological
studies have not been published. Therefore, this
paper will differentiate, when possible, between
topical C. chinensis and C. japonicus by in-
dicating "japonicus" forms as "japonicus"
morphs, thereby cautiously following a middle
ground that may easily be assimilated into a
final resolution of the problem.
C. chinetisis was first brought to North
America in the early 1890's by sailors returning
from Yokohama, Japan. The sailors sold the
snails to merchandize dealers in San Francisco's
Chinatown (Wood, 1892a, 1892b; Stearns, 1901).
Although Wood called these specimens "japoni-
ca", the snails were actually C. chinensis, the
first introduced japonicus not being recorded
until 1911 (Hannibal, 1911; see discussion in
Clench & Fuller, 1965). A second west coast in-
troduction was reported by Rev. G. W. Taylor
who found "japonica" being sold in a Chinese
market in Victoria, British Columbia (Anony-
mous, 1894). It is not known whether these
snails were of the japo7iic2is or the chinensis
tj'pe (Clench & Fuller, 1965), and there has been
no report of established Asian viviparid popula-
tions in British Columbia. Additional west coast
I
90 THE NAUTILUS
July 16, 1982
Vol. 96(3)
colonies have been reported from California and
Washington (Clench & Fuller, 1965; Hanna,
1966; Branson, 1977).
Individuals of C. chinensis were first found on
the east coast by W. Clench who collected speci-
mens in Massachusetts from the Muddy River, a
stream dividing Boston from Brookline. The
snails may have been introduced when goldfish
were added to the stream for mosquito larvae
control (Johnson, 1915). Additional east coast
colonies have been reported from Quebec,
Maine, Vermont, New Hampshire, Massachu-
setts, Rhode Island, New York, New Jersey,
Pennsylvania, Delaware, Maryland, North
Carolina, and Florida (Johnson, 1916, 1918;
Richards & Adams, 1929; Schmeck, 1942;
Jacobson & Emerson, 1961; Clench & Fuller,
1965; Stanczykowska et aL, 1971; Perron &
Probert, 1973; Bucci, 1974; Dundee, 1974;
Clarke, 1978). Additional populations have
recently been found in Connecticut (see below
for details).
C. chinensis populations have also spread mid-
continentally in Ohio, Michigan, Wisconsin,
Indiana, Minnesota, Arizona, Colorado, Texas,
Iowa, Oklahoma, and Utah (Teskey, 1954; Bran-
son, 1959; Clench & Fuller, 1965; Huehner &
Etges, 1971, 1972; Barnhart, 1978). Figure 1 is
a map of all the recorded references to North
American populations of C. chinensis north of
Mexico (excluding Hawaii). This species is very
well established on the northeast coast where it
should now be considered as a permanent part
of the freshwater molluscan fauna. The species
is also becoming well entrenched in the St.
Lawrence-Great Lakes drainage. Is is also com-
mon on the west coast between San Francisco
and Seattle. Additional colonies are scattered
across the continent. The paucity of mid-
continental colonies may reflect a lack of infor-
mation but it should be noted that some reports
of recent continental malacological surveys
mention no colonies of C. chinensis (Harman &
Berg, 1971; Clarke, 1973).
Connecticut Records
Over the past several summers I surveyed 215
aquatic sites in southern New England, especial-
ly Connecticut, for gastropods. Populations of
typical C. chinensis have been found in seven
FIG. 1. Thu \iirth American 1982 distributiov q/'Cipangopaludina chinensis (Gray). See text for references.
Vol. 96(3)
July 16, 1982
THE NAUTILUS 91
lakes and ponds in Connecticut and one lake in
\'ermont (Lake Fairlee, Thetford Center, pre-
viously reported in Clench & Fuller, 1965). A
population of the japonicus-morph lives in one
lake in Connecticut (Black Pond). Table 1 sum-
marizes the physical/chemical data on the Con-
necticut sites. Methods of water chemical analy-
sis have been described elsewhere (Jokinen,
1978).
Populations of C. chinensis were generally
found in larger lakes or ponds with sandy to
muddy sand substrates. The snails were either
crawling on the substrate or on dock pilings.
Even though several investigators have noted
C. chinensis living in slower waters of streams
(Schmeck, 1942; Stanczykowska et ai. 1971) all
Connecticut sites were lentic.
Due to the fact that most of the bedrock in
Connecticut is of the highly insoluble schist-
gneiss type, the majority of the surface waters
(75% of those sampled) are very soft (calcium
values below 5ppm). Yet, five of the eight C.
chinensis populations were found in harder
waters (Ca*-' > lOppm) and none lived in waters
with Ca < 7ppm. If one statistically compares
expected to actual percent occurrence of C.
chinensis in soft (Ca < 5ppm) waters (56% ex-
pected occurrence, 0% actual) to medium-hard
to hard (Ca > 5ppm) waters (44% expected,
100% actual), using an arcsin transformation
(Sokal & Rohlf, 1969), there is a statistically
significant difference at the t = .02 level. This
indicates that C. chinensis is more likely to be
found in waters of higher calcium values than
Table 1. Physical/chemical data for the habitats of Clpangopaludina chinensis in Connecticut.
Lake or pond
Area CO. Cond. Ca Mg
Type ha S pH mgC/1 ymhos Color ppm ppm
Black Pond, Middlefield,
Middlesex Co.
Bunnell's Pond, Bridgeport,
Fairfield Co.
East Twin Lake, Salisbury,
Litchfield Co.
Goodwin Park Pond, Wethers- NR
field, Hartford Co.
Holbrook Pond, Hebron,
Tolland Co.
North Farms Reservoir,
Wallingford,
New Haven Co.
Tyler Pond, Goshen,
Litchfield Co.
Lake Wononskopomus ,
Salisbury ,
Litchfield Co.
NR 30.6 11 7.3 7.6 194 .024 11.4 4.5
A 16.6 10 7.1 3.5 207 .025 9.9 3.3
N 227.6 15 7.4 33.3 286 .005 35.0 11.6
1 7.0 14.2 280 .222 19.6 4.2
NR
NR
1.8
29.3 8 6.4 4.5
74 .059 7.1 2.0
25.3
73.7
7.5 8.6 158 .041 14.0 3.5
6.9 7.2 112 .030 7.8 4.1
NR 142.7 10 7.5 22.8 217 .010 26.6 8.3
Lake Type: N = natural, NR - natural, water level raised, A = artificial impoundment
S = total number of snail species in lake
-I- -I-
Na K
ppm ppm
8.2 0.5
22.0 2.9
3.9 2.1
11.9 2.0
4.8 0.3
5.5 1.8
3.1 0.5
4.5 1.6
I
92 THE NAUTILUS
July 16, 1982
Vol. 96(3)
lower, and that it may have a physiological need
for dissolved calcium levels above 5ppm.
Boycott (1936) termed mollusks which could not
exist in soft water as "calciphilic". Greater sam-
ple sizes and physiological tolerance testing are
needed for greater resolution of required envi-
ronmental calcium values.
Natural history and Ecology
Data on the life history pattern of C. chinensis
has been published by Stanczykowska et al.
(1971, 1972). They estimated the maximum life
span for female snails as five years, for males,
usually three years, sometimes four. All individ-
uals grew throughout life, with the female's
reaching larger sizes because of their longer life
span. The females may begin to produce em-
bryos by the end of their first year but the four
and five year classes produced the most off-
spring. Each female produced a minimum of 169
embryos during a life time (an estimation based
on embryo counts published by Stanczykowska
et aL, 1971). Crabb (1929) found up to 102 em-
bryos in one female. The embryos develop in the
uterus, and during spring and summer 100% of
the females are carrying embryos. The young
begin to appear in the population by June and
continue to be born through October. The snails
begin a migration into deeper water in October,
the females appearing to migrate first (Stanc-
zykowska et al., 1971).
Quality of food affects the population para-
meters of C chinertsis. Stanczykowska et al.
(1972) and Plinski et al, (1978) compared snail
populations from three different habitats near
Montreal, the Ottawa River, a canal, and a lake.
The snails fed on the bottom material which was
composed of inorganics, organics and algae. The
percent composition of substrate materials was
identical to the percent composition of the gut
contents, indicating that the snails were not
selectively ingesting any specific bottom mate-
rial. Most of the algae ingested were epiphytic
or benthic, indicating that feeding was primarily
radular and not by filtration. The ingested algae
were primarily diatoms, especially species of
Fragilaria, followed by greens, blue-greens,
and flagellates. The percent composition of algal
forms differed between the three habitats. The
Ottawa River snails were larger, heavier, had
higher carbon and nitrogen values, and a
greater population density than snails from the
other two habitats. Sediment and gut analysis
revealed that the Ottawa River sediments had
not only a higher percentage of algae but a
higher diatom content. The lake snails made
some attempt to compensate for poorer quality
and quantity by consuming greater quanitities
of substrate. Increase in ingestion rate with a
decreased food quality has also been noted for
pulmonate snails (Calow, 1975). No studies have
been done to date on why diatoms appear to be
more nutritious to C. chirieyisis than other algae.
The entire area of freshwater gastropod feeding
and nutrition is poorly explored.
Allometric Shell Growth
Shell growth in C. chinensis is allometric, that
is, the proportions of the shell width to the shell
height change throughout development. Conse-
quently, the shell looks different in juvenile and
adult individuals. The subject of allometric
growth has been explored by Gould (1966 &
1971), White & Gould (196.5), and Jokinen (in
review). Allometric growth may be analyzed by
using linear regression and the resultant curves
graphed. Figure 2 illustrates the allometric
growth pattern of "typical" C. chinensis and
compares it to the growth pattern of the japoni-
CTis-morph. Shell measurements were made to
the nearest 0.1 mm with vernier calipers and in-
cluded embryonic shells. The raw data are avail-
able from the author. The data were analyzed
using the computer program SAS (Statistical
Analysis System) (Barr et al., 1979) and both
linear and curvilinear regressions (SAS-General
Linear Models and Non-linear Models) were run
on shell height vs. width and log shell height vs.
log width to determine which model best fit the
data. Analysis proved that shell growth in both
groups is best described by a linear log shell
height vs. log width curve. Log shell height was
used as the independent variable.
The ratio of the shell width to the shell height
(W/H) decreases as the shell increases in size,
the shell becoming relatively more elongate as it
Vol. 96(3)
July 16, 1982
THE NAUTILUS 93
18-
1 6-
X
I-
Q 14
12-
_l
—I
1^10
X
o
6-
C. CHINENSIS
» JAPONICUS-
MORPH
EMBRYO
.4 .6 .8 10 12 14
SHELL HEIGHT
16
OQi
0
FIG. 2. Allometric shell growth o/C. chinensis and the ]a.pomcus-morph. Sketches
illustrate the shape of the shells at various points on the curves. The scale bars
represent 5 mm. The regression equation C. chinensis is logW = 0.81, (±0.00U S.
E.jlogH + 0.17. The regression equation for the ]a.'pomais,-morph is logW = 0.78
(±0.01 S. E.jlogH + 0.23. The standard error values do not overlap, indicating
that the two growth patterns are significantly different. The regression coeffi-
cients (slopes) are less than one. meaning that the shell width increases in size at
a slower rate than the shell height. The shells, therefore, elongate as they grow. If
the slopes equaled unity, both height and width would grow at an equal rate and
the shell shape would not change with increase in size.
grows. The regression equation for the relation-
ship between height and width for "typical" C.
chiyiettms is logW = 0.84 logH + 0.17, r-square
= .998. A value of less than unity for the regres-
sion coefficient (slope), in this case 0.84, indi-
cates negative allometry, the shell width not in-
creasing as fast as shell height. The regression
equation for the japonicus-morph, the popula-
tion from Black Pond, is logW = 0.78 logH -i-
0.23, r-square = .997. The lower slope value,
0.78, indicates that the shell width of the japo-
nicM^-morph increases even less rapidly than C.
chinensis shell width. This is reflected in the
relatively more elongate shells of the japonicws-
morph.
Young individuals of C. chinensis not only
have a different shaped shell from the older
snails but demonstrate marked periostracal
spiral hirsuteness. When embryonic shells are
placed in water or alcohol and examined under a
dissecting microscope, they show a pattern of
three spiral rows of stiff periostracal hairs. The
hairs are distinctly hooked and the longest hairs
are 0.35 mm in length. The hooks face outward
from the shell. Some of the larger shells show
rows of pits in the same position as the em-
bryonic hairs (see Fig. 2). Since the hairs
become obliterated as the snails grow post-
partum, their function, if one exists, is most
likely intra-uterine. The hairs might serve to
hook the embryonic shells together to stabilize
their positions in the uterus, or they might func-
tion during birth.
94 THE NAUTILUS
July 16, 1982
Vol. 96(3)
Radular Structure
Radulae of C. chinensis individuals were ex-
amined for basic structure (Fig. 3). The teeth
were separated from each other and mounted in
Turtox's CMC-9AF mounting medium which
contains acid fuchsin for staining chitinous
material. The stain picked-up certain structural
details of the central tooth where the radular
material is thickened.
C. chinensis has the typical taenioglossid
tooth number of 7 per row. The central, first and
second laterals all have a large central cusp
bounded on either side by four smaller cusps.
The marginal teeth do not have an enlarged cen-
tral cusp but have seven small cusps (this
number appears to be somewhat variable).
Radular structure is similar to that of Viviparus
georgianus Lea (as illustrated in Clench, 1962)
except for the lack of an enlarged central cusp
on the marginals of C. chinensis. An examina-
tion of the radular structure of one individual of
the Black Pond population {japonicus-mov\>\\)
revealed five small cusps on either side of the
central cusp on the first lateral tooth and nine
cusps on the marginal tooth. It is not known if
these differences reflect individual variation (if
the two morphs are of the same species) or
reflect interspecific variation. A much more ex-
tensive examination of interpopulation variation
is needed before real conclusions can be drawn.
Parasites
Information is sparse concerning the role of C
chinensis as the final or intermediate host of hel-
FIG. 3. Thf mthilar teeth o/C. chinensis. C = central tooth.
L-I = first laivnl. LIl = I'eeond lateral. M = marginal
(greatly erdargi'li.
minth parasites. Penner (1942) found Massachu-
setts populations to be negative for schistosome
parasites. The snail may serve as a final host to
the normally clam-inhabiting trematode A spido-
gaster conchicola von Baer. The snails are in-
fected by eating embryonated eggs passed in the
feces of other snails (Michelson, 1970; Huehner
& Etges, 1971, 1972, 1977). The snail also serves
as intermediate host to a number of echino-
stome trematodes (U.S. Dept. Agriculture,
1946), including Echinostoma cinetorchis Ando
& Ozaki, a species which has been reported from
humans in Japan, Taiwan and Java (Schmidt &
Roberts, 1977). Angiostrotigylus cantonensis
(Chen), a nematode which infects vertebrate
nervous systems, may use C. chinensis as an in-
termediate host (Chang et al., 1968). This
parasite has been reported from Hawaii and
Costa Rica (Schmidt & Roberts, 1977).
Summary
The introduced Asian snail, C. chinensis. does
well in cool-temperate to warm-temperate cli-
mates in permanent ponds, lakes and the slow
parts of rivers with mud, silt or sand substrates.
Available data indicate that the snail requires a
minimum of 5ppm calcium in its habitat and is
excluded from very soft waters. This species
should be considered a well-established part of
the North American fauna, especially in the
northeastern U.S.
Some basic studies on the natural history and
ecology of this species have been undertaken in
Canada but more studies should be done to de-
termine what effect populations of C. chinensis
are having on the native fauna.
More studies need to be undertaken on the
parasites carried by C chinensis in North
America to determine its potential as a second-
ary host to both native and introduced Asian
parasites.
Shell growth is allometric, the snails tending
to become relatively more elongate with age.
The embryonic periostracal hairs are stiff and
hooked and may serve to stabilize the young
snails within the uterus. The shell growth pat-
tern as well as details of the radula structure dif-
fer between the "typical" C. chinensis and the
japonicus-morph. Whether or not these should
Vol. 96(3)
July 16, 1982
THE NAUTILUS 95
be considered to be intraspecific individual or in-
terspecific differences awaits more extensive
analysis.
ACKNOWLEDGMENTS
Data collection was supported by a research
contract from the Department of Environmen-
tal Protection, State of Connecticut. My thanks
to L. Penner for loan of shells from the Muddy
River.
LITERATURE CITED
Abbott, R. T. 19.50. Snail invaders. Ndtiirnl History
59:80-8.5.
Barnhart, M. C. 1978. Three intmiluced gastropods in Iowa.
The Nautilus 92:106-107.
Barr, A. J., J. H. Goodnight, J. P. Sail, W. H. Blair, C. M.
Chilko. 1979. SAS Users Guide. 1979 ed., SAS Institute,
Inc., Raleigh, N.C., 495 p.
Branson, B. A. 1977. The Chinese apple snail, Cipatigopnlu-
dina chinensis. on Orcas Island. Washington. The Nauti-
lus 91:76-77.
Bucci, D. A. 1974. Vivipnrus malleatus in Montreal,
Canada. The Nautilus 88:55.
Calow, P. 1975. The feeding strategies of two freshwater
gastropods, Ancylus fluviatilis Mull, and Planorhis con-
tortus Linn. (Pulmonata), in terms of ingestion rates and
absorption efficiencies. Oecologia (Berl.) 20:33-49.
Chang. P. -K.. J. H. Cross, Jr. & S.S.S. Chen. 1968. Aquatic
snails as intermediate hosts tor Angiostrongylus cantonen-
sis on Taiwan. Jour. Parasitol. 54:182-183.
Clarke, A. H. 1973. The freshwater molluscs of the Canadian
Interior Basin. Malacologia 13:1-509.
Clarke, A. H. 1978. The Asian apple snail, Cipangopaludina
chinensis (Viviparidae) in (.)neida Lake, New York. The
Nautilus 92:134.
Clench, W. J. 1962. A catalogue of the Viviparidae of North
America with notes on the distribution of Vivipariis
georgianus Lea. Occas. Papers on Mollu.tks. Mus. Comp.
Zool., Harvard Univ. 2(27):261-287.
Clench, W. J. & S. L. H. Fuller. 1965. The genus Viviparus
(Viviparidae) in North America. Occas. Papers on Mol-
lusks. Mus. Comp. Zool. Harvard Univ. 2(32):385-412.
Crabb, E. D. 1929. Egg laying and birth of young in three
species of Viviparidae. The Nautilus 42:125-129.
Dundee, D. S. 1974. Catalog of introduced mollusks of East-
ern North America (North of Me.xico). Sterkiana 55:1-36.
Gould, S. J. 1966. Allometry and size in ontogeny and phy-
logeny. Bio. Rev. 41:587-640.
Gould. S. J. 1971. Geometric similarity in allometric growth:
a contribution to the problem of scaling in the evolution of
size. American Naturalist 105:113-136.
Hanna, G. D. 1966. Introduced mollusks of western North
America. Occ. Papers Calif. Acad. Sci. 48:1-108.
Harman, W. N. & C. 0. Berg. 1971. The freshwater snails of
central New York. Neiv York State Agric. Exp. Sta.
Search: Entomology 1(4): 1-68.
Huehner, M. K. & F. S. Etges. 1971. A new gastropod host
(or Aspidogaxter conchicola. Jour. Parasitol. 57:1255.
Huehner, M. K. & F. S. Etges. 1972. Experimental trans-
mission of A.yjidogaster conrhicola von Baer, 1827. Jour.
Parasitol. 58:109.
Huehner, M. K. & F. S. Etges. 1977. The life cycle and devel-
opment ofAspidngaster conchicola in the snails, Viviparus
malleatus and Goniobasis livescens. Jour. Parasitol.
63:669-674.
.lohnson, C. W, 1915. Viviparus malleatus Reeve in Massa-
chusetts. The Nautilus 19:35.
Johnson, C. W. 1916. Viviparus malleatus Reeve. The
Nautilus 30:48.
.lohnson, C. W. 1918. Viviparus malleatus and contectoides
in Massachusetts. The Nautilus 31:107-108.
Jokinen, E. 1978. Habitats of two freshwater limpets {Fer-
ri.<:sia: Ancylidae) from New England. The Nautilus
92:156-160.
Jokinen, E. H. (In review). Allometric growth of planorbid
snails.
Michelson, E. H. 1970. Aspidogaster conchicola from fresh-
water gastropods in the United States. Jour. Parasitol.
56:709-712.
Penner. L. R. 1942. Studies on dermatitis-producing shisto-
somes in eastern Massachusetts, with emphasis on the
status oi Scihistosojnatium pathloc.opticum Tanabe, 1923.
Jour. Parasitol. 28:103-116.
Perron, F. and T. Probert. 1973. Viviparus malleatus in
New Hampshire. The Nautilus 87:90.
Plinski, M.. W. Lawacz, A. Stanczykowska & E. Magnin.
1978. Etude quantitative et qualitative de la nourriture
des Viviparus ?NaWea/Ms (Reeve) (Gastropoda, Prosobran-
chia) dans deux lacs de la region de Montreal. Canadian
Jour Zool. 56:272-279.
Schmeck, E. H. 1942. Viviparus malleatus in Niagara River.
The Nautilus 55:102-103.
Schmidt, G. D. and L. S. Roberts. 1977. Foundations of
Parasitology. C. V. Mosby Co., St. Louis., 604 pp.
Sokal, R. R. and F. J. Rohlf. 1969. Biometry. W. H. Freeman
& Co.. San Francisco, 776 pp.
Stanczykowska, A., E. Magnin and A. Dumouchel. 1971.
Etude de trois populations de Viviparus malleatus (Reeve)
(Gastropoda. Prosobranchia) de la region de Montreal. I.
Croissance, fecondite, biomasse et production annuelle.
Canadian Jour. Zool. 49:1431-1441.
Stanczykowska, A. M., M. Plinski and E. Magnin. 1972.
Etude de trois populations de Viviparus malleatus (Reeve)
(Gastropoda, Prosobranchia) de la region de Montreal. II.
Etude qualitative et quantitative de la nourriture. Cana-
dian Jour Zool. 50:1617-1624.
Stearns, R. E. C. 1901. Japanese Vivipara in California. Thv
Nautilus 15:91.
Teskey, M. C. 1954. The mollusks of Brown County. Wiscon-
sin. The Nautilus 68:24-28.
U.S. Department of Agriculture. 1946. Index-Catalogue of
Medical and Veterinary Zoology. Part 7. Hosts.
White. J. F. and S. J. Gould. 1965. Interpretation of the coef-
ficient in the allometric equation. American Naturalist
99:5-18.
96 THE NAUTILUS
July 16, 1982
Vol. 96(3)
FOR SALE
A matched pair of blond wood shell cabinets, each
42" wide, 25" deep, and 40" high, with a 3'/z" deep
display case on top, covered by 'A" plate glass.
Each cabinet contains 24 drawers .3" deep. Price
for pair $9.SO.OO F.O.B. Mobile.
One shell dredge, 12" wide, 7" high (with sloped lip
at mouth), 18" long; complete with break-aloose
steel rod bridle and 1" galvanized steel lead chain,
also equipped with trailing float. Steel bar frame
hot-dipped galvanized after fabrication, covered
with 'A" galvanized hardware cloth. Total weight
20 lbs. Price $125.00 F.O.B. Mobile. Contact H. I.
Johnstone, 2209 River Forest Rd.. Mobile, Ala.
3(5fi05. I'hone (205) 471-1219.
ERRATA
Nautilus, vol. 94 (1) J. K. Buttner and R. C.
Heidinger, "Seasonal Variations - Corbi-
cula - Illinois Fish Pond." Page 9, Table 2,
bottom line, for 10"" read 10-\ Page 10, left
column near bottom, for P>0.01, read
P<0.01. The authors express their regrets.
COMMENTS ON THE EASTERN PACIFIC TRIVIA RITTERI
(GASTROPODA: TRIVIIDAE)
Hans Bertsch
Instituto de Investigaciones Oceanologicas
Universidad Autonoma de Baja California
Ensenada, B.C., Mexico
Barbara Myers
and Department of Marine Invertebrates,
Natural History Museum
P.O. Box 1390
San Diego, California 92112
Although Cate (1979) recently surveyed all
known species of Triviidae the information he
presented on Trivia ritteri Raymond, 1903, was
only a condensation of the original description.
Not only were no new data presented, but one of
the original collecting sites of T. ritteri (Cortez
Bank, west of San Diego) was omitted. The find-
ing of two specimens of T. ritteri from deep
water off San Diego, California, occasioned a
search for additional information.
References, Synonymy and Published Records:
Triiw ritteri Raymond, 1903: 85-86; Catalina Island
(60 fms); Monterey; Cortez Bank (54 fms); Catalina Island
near Avalon (40 fms); off San Pedro (50 fms); Lowe, 1904:
18-20; C:i(alina Island; Dall, 1921: 140; Oldroyd, 1927:
238-239; Grant & Gale, 1931; 44, 754; Upper Pliocene,
Los AiiKfl's; Keen, 1937: 47; Smith & Emer.son, 1955:
99, 101; Ficny, 1956: 151, 154; Anacapa Passage, ,34°00'
38-20" N; ll;»'30' 35-1.3" W (26-27 fms); Anacapa Pas-
sage, 34°00' IC" N; W.i'^-zr :j5-05" W (29-31.5 fms); 2 1/2
miles N. of W. end of Anacapa Island, 34°03' 05-45" N;
119°26' 02" to 25' 28" W (46-58 fms); Abbott, 1974: 149.
fig. 1637
Puiiula ritteri (Raymond). Burch, 1945: 27-29; 42; off
Redondo Beach (25 fms), White's Landing, Catalina
Island (40 fms); Pleistocene of Timm's Point, San Pedro.
Decoriatrivin ritteri (Raymond). Cate, 1979: 11, 98; figs.
94 and 94a.
Geographic and. Bathyynetric Distributions:
Trivia ritteri has been recorded from the
upper Pliocene and the Pleistocene of Los
Angeles, and in the Recent from Monterey to
San Pedro, Catalina Island, Anacapa Passage
and Island, and Cortez Bank. Our knowledge of
the distribution of Trivia ritteri has been based
on just a few specimens.
In the collections of California Academy of
Sciences (CAS), Los Angeles County Natural
History Museum (LACM), and San Diego Nat-
ural History Museum (SDNHM) are numerous
Vol. 96(3)
July 16, 1982
THE NAUTILUS 97
lots of Trivia ritteri. An analysis of the accom-
panying data of those specimens gives a better
understanding of the distribution of T. ritteri
(Table 1). Specimens in the LACM collection ex-
tend the range of T. ritteri southward more
than 400 miles (over 650 km) to midway down
the Baja California peninsula (27° N). Trivia
ritteri is endemic to the California Province
(sensu Valentine, 1966), with a few northern
records to Monterey (36° N).
Trivia ritteri is usually found deeper than 50
m (Figure 1). More than two-thirds of the 113
specimens analyzed for bathymetric occurrence
were found between 51-90 meters deep. Trivia
ritteri has a predominantly insular distribution:
the majority of specimens have been collected
from the offshore islands of southern California
and northern Baja California. Mainland collect-
ing records are either from several miles off-
shore or from deep trenches (such as La Jolla)
which rapidly drop off close to the shoreline.
TABLE 1. Recent records o/ Trivia ritteri with their depth
ranges.
Location Specimens Depth Range
Central California
Monterey Bay area
Southern California, mainland
Los Angeles area, offshore «12 mi.)
San Diego, La Jolla trench
Southern California , Channel Islands
San Miguel, Santa Rosa, Santa Cruz
and Ana cap a Islands
San Nicholas, Santa Barbara and
Santa Catalina Islands
San Clement e Island
Baja California. Mexico
West of Isla Cedros
South of Isla Cedros
Off Thurloe Head (27° 36" 50" N;
lU* 50' 50" W)
Off San Pablo Pt . (27° 12' 45" N;
114° 31' 45" W)
FIG. 1. Bathymetric distribution o/Trivia ritteri, bitsed on
113 spechnens. Vertical numbers are alternating 10 m
depths. The mid-point oftlie collection information was used
for specimen, lots with a range of depth.
TABLE 2. Shell size and teeth counts o/Trivia ritteri. Shells
in collection of the San Diego Museum of Natural History.
Number of Apertural Denticles
Inner Lip Outer Lip
98 THE NAUTILUS
July 16, 1982
Vol. 96(3)
Shell Maiyhology:
Raymond (1903) described the shell characters
of Trivia ritteri fairly comprehensively; the
first published illustration of the species appears
to be Abbott, 1974: fig. 1637. Among the mate-
rial we examined (Table 2) were several imma-
ture specimens, a bulloid juvenile form com-
pletely lacking apertural denticles and dorsal
ribbing (Figs. 2 and 3) and a subadult (Figs. 4
and 5) with teeth, the outer lip still thin but hav-
ing begun folding over the aperture, and the
dorsal surface nearly smooth. The animal begins
to develop the adult shell morphology (Figs. 6
and 7) when it reaches 6-8 mm. The British
Trivia arctica reaches the adult stage in 6-8
months (Lebour, 1933).
Radula:
The radula of Trivia ritteri is illustrated here
for the first time (Fig. 8). The radula we exa-
mined has 22 rows of fully formed teeth, with 2
scythe-shaped marginal teeth and a single large
admedian tooth on each side of the median tooth
(cf. Schilder, 1936, for terminology). The adme-
dian tooth has a single denticle on the inner side
of the erect shaft, and 3 or 4 small denticles on
its outer side. The median tooth has a major
cusp with 6-8 small accessory denticles on each
side.
ACKNOWLEDGMENTS
We are grateful to those who graciously
loaned us specimens or gave us data from collec-
tions in their care: Mr. Loyal J. Bibbey; Dr.
Barry Roth, California Academy of Sciences;
and especially Mr. Gale Sphon and Dr. James H.
McLean, Los Angeles County Natural History
Museum. We thank Anthony D'Attilio, San
Diego Natiiral History Museum, for the draw-
ings.
LITERATURE CITED
Abbott, R. T. 1974, American SciishMa. Second Edition.
Van Nostrand Reinhold Company, New York. 663 pp.;
24 pis.; numerous text figs.
FIGS. 2-7, Sh:lt <;/'Tri\na ritteri, dm-xat mid venlrai vinrs.
Photo(/rnj,hs hy B. Myers. 2-3, Juvenile hulla-form; . 4-5,
SuhrtdnlU<: 6-7. Ad^ill.-i.
FIG. 8, Radula of Trivia ritteri. Drawimj hy Anthony
D'Attilio.
Vol. 96(3)
July 16, 1982
THE NAUTILUS 99
Berry. S. S. 19,56. Mollusca dredged by the Orea off the
Santa Barbara Islands, California, in 1951. Jirur. Wash-
uigtoH Acml. Sri. 46(5):150-15T; 9 text figs. (5 June 1956).
Burch, J. Q. 1945. Distributional list of the west American
marine mollusks from San Diego to the Polar Sea. Pror.
Conchohyical Club So. California 53:27-29; 42 pis.
(October 1945).
Gate, C. N. 1979. A review of the Triviidae (Mollusca:
Gastropoda). San Diego Soc. Nal. Hi.-it. Mem. 10:1-126;
41 pis. (20 June 1979).
Dall, W. H. 1921. Summary of the marine shellbearing
mollusks of the northwest coast of America, from San
Diego, California, to the Polar Sea, mostly contained in
the collection of the United States National Museum,
with illustrations of hitherto unfigured species. Bull. U.S.
Nat. Mus. 112:1-217; 22 pis. (24 February 1921).
Grant, S., IV and H. R. Gale. 1931. Catalogue of the marine
Pliocene and Pleistocene Mollusca of California and adja-
cent regions. San Diego Soc. Nat. Hist. Mem. 1:1-1036;
32 pis. (3 November 1931).
Keen, A. M. 1937. An abridged check list and bibliography
of West North American Mollusca. Stanford Univ. Press.
Stanford, California. 87 pp.
Lebour, M. V. 1933. The British species of Triina: T. artica
and T. monacha. Jour. Marine Biol. Assoc. U.K. 18(2):
477-484; 1 pi. (January 1933).
Lowe, H. N. 1904. k dredging trip to Santa Catalina I.sland.
The Nautilus 18(2):18-20. (June 1904).
t)ldroyd, I. S. 1927. The marine shells of the west coos* of
North America. Stanford Univ. Press, Stanford, Cali-
fornia, Vol. II (2);l-304; pis. 30-72.
Riiymond, W. J. 1903. A new Californian Trivia. The
Nautilus 17(8):85-86. (December 1903).
Schilder. F. A. 1936. Anatomical characters of the Cypraea-
cea which confirm the conchological classification. Pruc.
Malar. Soc. London 22(2):75-112; pis. 11 & 12. (15 July
1936).
Smith, A. G. and W. K. Emerson. 1955. William James
Raymond, 1865-1947. The Nautilus 68(3):98-102.
(January 1955).
Valentine, J. W. 1966. Numerical analysis of marine mollus-
can ranges on the e.xtratropical northeastern Pacific
shelf. Limnology and Oceanography 11(2):198-211; 7 text
figs. (April 1966).
AN OVERLOOKED BUSYCON WHELK (MELONGENIDAE)
FROM THE EASTERN UNITED STATES
Bretton W. Kent
Department of Zoology
University of Maryland
College Park, MD 20742
ABSTRACT
Busycon laeostomum new species, a large living sinistral Busycon u>helk is
described from the eastern United States. This new species is compared with B.
carica (Gmelin, 1 791) and B. contrarium (Conrad, 18U0) and its subgeneric affini-
ties are discussed.
A large, sinistral Busycon is occasionally col-
lected offshore along the Atlantic coast of the
United States between southern New Jersey
and northern Virginia. This whelk frequently
has a pure white shell and has been referred to
as either a sinistral form of B. carica (Gmelin,
1791) or as B. contrarium (Conrad, 1840)
(Abbott, 1974, p. 222). Here I show that this
whelk is distinct from sympatric B. carica and
B. contrarium, and describe this new species.
100 THE NAUTILUS
July 16, 1982
Vol. 96(3)
FIGS. 1-.5. Busycon laeostomum tl sp. 1, 258 mm (Pope coUeclion); 2, 213 mm (USNM no. 679720), 3, 222 mm (with soft tissues
and operculum; Harasewych collection), 4, 221, mm (USNM no. 806850). and 5, 221 mm (siphonal canal broken; USNM wo.
806850).
Vol. 96(3)
July 16, 1982
THE NAUTILUS 101
Busycon laeostomum, new species
Figs. 1-5, 7, 10
Shell Description - Shell sinistral, solid, sub-
pyriform, inflated; shoulder rounded, tubercu-
late; spire low, subconical; spiral cords on spire
weak or absent; aperture broad, elliptical,
longer than siphonal canal; anal ridge on
parietal wall narrow, weak; siphonal canal open,
somewhat flaring; columella broad, strongly
bowed; spiral cords on body whorl restricted to
dorsum of siphonal canal, weak; shell exterior
usually chalky, white or pale pinkish-orange, oc-
casionally with indistinct slightly darker suffu-
sions; periostracum minutely ciliated; aperture
white or light pinkish-orange; apertural lirae ab-
sent or rarely weak.
Description of Animal - Head and foot black;
operculum corneus, elliptical, lingulate, nucleus
apical; radula with 3 teeth per row, 5-6 cusps on
central teeth.
Material Examined - Holotype - Length =
245 mm (U.S. National Museum no. 806849);
trapped in 10-15 m of water off Stone Harbor,
New Jersey, January 1979. Paratypes - Length
= 184 mm (USNM no. 678850); dredged 8-10 km
off Avalon, New Jersey, July 1967. Length =
213, 176 and 138 mm (USNM no. 679720);
dredged off Ocean City, Maryland, 1969.
Length = 224 and 221 mm (USNM no. 806850)
and 222 and 220 mm (M. G. Harasewych collec-
tion); trapped off Stone Harbor, New Jersey in
10-15 m of water, January 1979. Length = 220
mm (USNM no. 806851); off Avalon, New
Jersey, 1968. Length = 258 mm (Theresa R.
Pope collection) and 83 mm (author's collection);
collected as beach shells at Tom's Cove,
Assateague Island, Virginia, April 1977. Length
= 163 mm (Geerat J. Vermeij collection); off
Ocean City, Maryland, 1977.
Type Locality - Stone Harbor, New Jersey;
in 10-15 m of water.
Range - Southern New Jersey to northern
Virginia; offshore.
Etymology - laios (Gk.) = left, stoma (Gk.) =
mouth.
Remarks - B. laeostomum is sinistral and has
a ciliated periostracum hke B. contrarium. but
otherwise more closelv resembles B. carica in
general shell shape (Figs. 6-11, Table 1). B. con-
trarium is more slender and has a more angular
shoulder than B. laeostomum, although tuber-
cles along the shoulder make the latter differ-
ence somewhat difficult to observe in photo-
graphs (e.g. - Figs. 4 and 10). B. contrarium and
B. laeostomum also differ with respect to the
development of these tubercles, the nature of
the external spiral cords and apertural lirae, the
shape of the columella, and the color of the shell.
■WliileS. laeostomum has only rounded tubercles
along the shoulder, in B. contrarium these
tubercles are frequently elongated into promi-
nent spines. B. contrarium also has well-
developed spiral cords and apertural lirae which
become obsolete in later whorls. In B. laeosto-
mum these cords and lirae are very weakly
developed or more commonly completely ab-
sent, even in the early whorls (e.g. -compare
Figs. 9 and 10). The columella of 5. contrarium.
is slender and relatively straight compared to
broad, strongly bowed columella of B. laeo-
stomum. Finally, the dark brown axial streaks
that usually occur on the early whorls of B. con-
trarium (Fig. 9) do not occur in B. laeostomum.
In B. laeostomum 62% of the types (8 of 13) had
a pure white shell; the remaining shells were a
TABLE 1. Comparison of northern Busycon contrarium
and B. carica with B. laeostomum, with respect to spire
angle, the ratio of siphonal canal length to aperture length,
aperture shape ( = aperture uidth divided by aperture length)
and canal shape (= canal uridth halfway along canal divided
by canal length). The values listed are means with ranges in-
dicated in parentheses. Shells with badly broken lips or
siphonal canals were not measured. Differences were tested
for signif>.cance with a one-tailed Mann-Whitney U test and
the level of significance is indicated by asterisks (i.e.-' in-
dicates p <0.05. ** indicates p <0.01. and **' indicates p
<ri.ooii.
contrarium laeostomum carica
."^pire
Angle
Canal: Aperture
Ratio
Aperture
Shape
Canal
Shape
N
.Size Range
94°** 105° 81°"*
(85-121°) (92-126°) (75-90°)
1.10*** 0.77 0.82
(0.87-1.48) (0.66-0.93) (0.72-0.93)
0.60 0.60 0.58
(0.57-0.64) (0.57-0.64) (0.51-0.63)
0.19*" 0.33 0.29
(0.14-0.26) (0.24-0.41) (0.19-0.35)
15 10 12
75-224 mm 83-258 mm 93-219 mm
102 THE NAUTILUS
July 16, 1982
Vol. 96(3)
I
7
\
«<
I
I
0
FIGS. 6-11. Comparison of typical adults (upper row) and juveniles (lower row) o/Busycon contrarium (Fig. 6 and 91, B.
laeostomum (Fig. 7 and 10) and B. carica (Fig. 8 and 11). 6, 22J, mm, 7, 2^5 mm (holotype; USNM no. SOtiHi'J). 8, 191 mm, 9, 88
mm, 10, S3 mm (author's collection), and 11, 93 mm.
pale pinkish-orange with slightly darker suffu-
sions. Pure white shells (i.e. -no axial streaks
even on the early whorls) are known to occur in
B. contrarium, but are very rare (HoUister
1958). I have examined four white B. con-
trarium (USNM nos. 36298. 414722. 609947.
Vol. 96(3)
July 16, 1982
THE NAUTILUS 103
and 631770). Except for the white shells these
B. contrarium are indistingiiishable from other
B. contrarium. This suggests that B. laeosto-
mum is not merely a white-shelled morph of B.
contrarium. Further, B. laeostom,um is probably
not just a northern form of B. contrarium. The
two species are sympatric throughout the range
of B. laeostomum. rather than having con-
tiguous or disjunct ranges as would be expected
of geographic morphs.
Although B. laeostomum and B. carica are
similar in shape (Figs. 7, 8, 10 and 11, Table 1),
several lines of evidence suggest that they are
not merely sinistral and dextral morphs of the
same species. B. laeostomum and B. carica dif-
fer, not only with respect to handedness and the
nature of the periostracum, but also in spire
angle (compare spires in figs. 7, 8, 10 and 11;
Table 1), the shape of the anal ridge, and shell
color. The anal ridge in B. carica is a swollen
prominance (Hollister 1958) that is very dif-
ferent from the weak ridge in B. laeostomum. B.
carica also frequently has a bright reddish-
orange aperture (Hollister 1958), but this has
not been observed in B. laeostomum. The white
shells which commonly occur in B. laeostomum
have not been reported in B. carica.
If B. laeostomum, and B. carica were sinistral
and dextral morphs of the same species they
should have similar geographic and bathymetric
ranges. The geographic ranges of the two
species are very different; B. carica occurs from
Massachusetts to northern Florida (Abbott
1974), while B. laeostomum has a restricted
range between southern New Jersey and north-
ern Virginia. The bathymetric ranges are also
different. B. carica occurs both intertidally and
subtidally in areas where it is sympatric with B.
laeostomum (pers. observ., M. G. Harasewych,
pers. comm.), while all of the live-collected B.
laeostomum were subtidal.
Finally, differences in handedness may pre-
clude copulation between B. laeostomum and B.
carica. There is no direct evidence that sinistral
and dextral morphs are unable to copulate, but
as Pulley (1959) has argued, even slight diffi-
culty in copulation would reduce gene flow be-
tween the two forms. If copulation between the
two morphs were possible, egg capsules should
occasionally be found containing both sinistral
and dextral individuals. Gill (1867) examined
over 500 B. carica egg capsules, but found only
dextral individuals.
The presence of sinistral coiling and a ciliated
periostracum strongly suggests that B. laeo-
stomum is much more closely allied to B. con-
trarium than to B. carica. Consequently, B.
laeostoynum should be placed in the subgenus
Sinistrofulgur Hollister 1958 with B. con-
trarium and B. perversum Linne 1758.
B. laeostomum is also distinct from fossil
sinistral Busycon, which have either prominant
shoulder spines, such as B. adversarium Conrad
1862 and B. obfilosum (Grabau 1903), or strong
external spiral cords, such as B. obrapum
(Grabau 1903) and B. perversum robosonense
Gardner 1948. In B. laeostomum the shoulder is
tuberculate, but not spiny, and the spiral cords
are absent qr only very weakly developed even
in small individuals. The absence of fossil forms
similar to B. laeostomum suggests that this
species is relatively recent, possibly a northern.
Pleistocene offshoot of B. contrarium.
Conclusions - Hollister (1958) reviewed the
extant species of Busycon, but made no mention
of a form resembling B. laeostomum. This omis-
sion appears to be due to a lack of well-pre-
served specimens. Except for a few heavily
beachworn specimens in the Academy of
Natural Sciences in Philadelphia, which may be
referable to B. laeostomum. no specimens of B.
laeostomum appear to have been in museums
prior to 1967. Beachworn B. laeostomum are dif-
ficult to separate from B. contrarium and B.
carica, so in the absence of live-collected
specimens confusion between the three species
was not surprising. Only in the past few years as
live-collected B. laeostomum became available
for study has it been possible to differentiate
these three species.
ACKNOWLEDGMENTS
I would like to express my deepest thanks to
M. G. Harasewych and E. J. Petuch for their
numerous contributions. I would also like to
thank R. S. Houbrick and G. M. Davis for allow-
104 THE NAUTILUS
July 16, 1982
Vol. 96(3)
ing me to examine specimens in the U.S. Na-
tional Museum and the Academy of Natural
Sciences, to T. R. Pope for allowing me to ex-
amine the specimen in her collection, and to G.
J. Vermeij for his encouragement and helpful
discussions. Support was provided by a grant
from the National Science Foundation (number
OCE-7901806) to the author and G. J. Vermeij.
LITERATURE CITED
Abbott, R. T. 1974. Aynerican Seashells. Van Nostrand/
Reinhold Co., New York. N.Y. 66.3 p.
Gill, T. 1867. On the genus Fulgur and its allies. Amer. Jour.
Conch. 3:141-152.
Hollister, S. C. 1958. A review of the genus Busycon and its
allies. Part I. Paleontographica Amer. 4(28):59-126.
Pulley, T. E. 1959. Busycon -perversum (Linne) and some
related species. Rice Inst. Pamphlet 46:70-89.
NOTES ON THE MORPHOLOGY OF CANCELLARIA RETICULATA
(GASTROPODA: CANCELLARHDAE)
M. G. Harasewych
College of Marine Studies
University of Delaware
Newark, Delaware 19711
and
Richard E. Petit
P.O. Box 30
North Myrtle Beach,
South Carolina 29582
ABSTRACT
Cancellaria reticulata (Linne, 1 767), the type species of the type genus ofCancel-
lariacea, inhabits subtidal sandy bottoms of the temperate and tropical western
Atlantic. Externally, the cancellate shell is smooth and well adapted for burrow-
ing. Internally, it has periodic reinforcing structures analogous to muricid
varices. With the exception of an enlarged, bilohed left, cephalic tentacle, external
features, as well as those of the pallial complex and reproductive systems are not
unlike those of other Neogastropods. The nervou^s system differs from the usual
rachiglossan arrangement only in the extreme anterior placement of bvx;cal
ganglia and the resulting length of cerebro-buccal connectives. The cuticularized
lining of the buccal cavity, highly specialized radula, lack of anterior oesophagus,
anterior placement of buccal ganglia and simplified alimentary system posterior
to the valve ofLeiblein are features that distinguish this superfamily from other
Neogastropods. Although the food and feeding mechanisms remain unknown, the
functional morphology of the alimentary system suggests a diet of soft tissue or
fluid. Scanning electron micrographs reveal the complex structure of the radular
tip, which raises the possibility that the cancellariid radula was formed by fusion
of central and lateral teeth, rattier than by the loss of lateral teeth, as previously
believed.
The cancellariaceans comprise a small, mono-
phyietic and morphologically compact group of
marine neogastropods that inhabit subtidal to
bathyal sand and mud bottoms of tropical and
temperate regions. The earliest known fossil
record is from the Lower Cretaceous (Upper
Albian) of Austria, while the greatest diversity
in the Recent fauna occurs along the eastern
Pacific coast and in the central Indo-Pacific
area. The relationship between numerous can-
cellariids from various Cretaceous deposits has
not been investigated. Several genera based on
Cretaceous species have been placed in Cancel-
lariidae by some authors, and elsewhere by
others.
The taxonomic position of this group has, until
Vol. 96(3)
July 16, 1982
THE NAUTILUS 105
recently, been uncertain. Troschel (1866) placed
the family Cancellariidae in Toxoglossa, based
largely on radular characteristics. Thiele (1929)
and Wenz (1938-1944) included it in the rachi-
glossan superfamily Volutacea. Olsson (1970),
also on radular characteristics, erected the
order Nematoglossa for the grouJD. Ponder
(1973) showed that this lineage diverged from
early neogastropod stock with unique modifica-
tions of. the anterior alimentary system, and
erected the superfamily Cancellariacea to in-
clude the families Cancellariidae and the extinct
Paladmetidae.
Investigations into the anatomy of cancel-
lariids have been limited, concentrating mostly
on radular morphology (Troschel, 1865; Barn-
ard, 1958; Olsson, 1970) and on the fore-gut
(Graham, 1966; Ponder, 1973).
The following is an account of the morphology
of the shell and soft parts of CanceUaria reticu-
lata (Linne, 1767), the type species of Cancel-
laria, the type genus of the superfamily. No
previous description of its anatomy has ap-
peared, other than several comparative remarks
by Graham (1966).
Materials and Methods
We were fortunate in obtaining a number of
preserved specimens from the following locali-
ties:
19 and 20", pumped ashore from approxi-
mately 20 meters depth during a beach nourish-
ment project, Atlantic Beach, Duval Co.,
Florida.
19 and 40* dredged in 6 meters, W to SW from
the southern end of Egmont Key, Florida.
In addition, a number of shells from the fol-
lowing localities were used to investigate shell
structure: 4 specimens dredged in 38 meters, S
of Sombrero Light, Marathon, Florida. 3 speci-
mens collected on sand, minus tide, Mangue da
Olaria, Guarapari, Espirito Santo, Brasil. 2
specimens from St. Lucie Inlet, Martin Co.,
Florida.
For anatomical studies, preserved specimens
were immersed in 10% hydrochloric acid (HCL)
until shells were dissolved. Soft parts were then
rinsed and returned to 70% ethanol for dissec-
tion. Internal shell structure was investigated
by sectioning dry shells on a diamond saw and
by fracturing them in a vise.
Radulae and shell ultrastructure were ex-
amined on a Novascan 30 Scanning Electron
Microscope.
KEY TO ABBREVIATIONS ON FIGURES
a - anus
ag - albumen gland
asg - accessory salivary gland
au - auricle
ba - bulbus aorta
be - bursa copulatrix
bg - buccal ganglion
cbc - cerebro-buccal connective
eg - capsule gland
ct - ctenidium
cut - cuticularized tube
dasg - duct accessory salivary gland
dg - digestive gland
e - eye
fo - female opening
gpd - gonopericardial duct
hg - hypobranchial gland
ig - ingesting gland
k - kidney
ko - kidney opening
let - left cephalic tentacle
m - mouth
me - mantle edge
moe - mid-oesophagus
oaoe - opening of anterior oesophagus
od - oviduct
opm - opening of prostrate gland to mantle cavity
OS - osphradium
ot - oral tube
ov - ovary
p - periostracum
pc - pericardium
pd - penial duct
pen - penis
pr - prostate gland
];iro - propodium
r - rectum
rme - rear of mantle cavity
rs - radular sac
rt -radular teeth
s - siphon
sg - salivary gland
srm - subradular membrane
sto - stomach
sv - seminal vesicle
td - testicular duct
te - testis
vd - vas deferens
ve - ventricle
vl - valve of Leiblein
XLC - crossed lamellar aragonite collabral
XLT - crossed lamellar aragonite transverse
106 THE NAUTILUS
July 16, 1982
Vol. 96(3)
Shell Morphology
External: Shell fairly large for genus (to 50
mm), heavy, biconic, and may be pseudo-umbili-
cate (Fig. 1). Spire sharply conical (spire angle
56-65°), comprising about 2/5 of total shell
length. Protoconch paucispiral, of 2 glassy,
slightly bulbous, amber-colored whorls, unorna-
mented except by fine pits (Fig. 2). Coiling axis
of protoconch deviated from that of teleoconch
by 10-20°. Teleoconch, with up to 7 2/3 convex
whorls, bears prominent collabral and spiral or-
nament that intersect to produce the cancellate
scupture that gives the superfamily its name.
Suture deeply impressed. Spiral sculpture con-
sists of 12-16 major cords on body whorl and
4-6 on penultimate whorl, with 0-2 fine striae
between major cords. Collabral sculpture of
markedly prosocline ribs var3ang in number
from 12-14 on the first post-nuclear whorl to
28-33 on the sixth post-nuclear whorl. Ribs
strong and evenly spaced, except for areas
roughly every 1/3 whorl where they are weak
and more numerous. Aperture large, hemi-ellip-
tical, deflected from coiling axis by 22-27°.
Outer lip with shallow indentation posterior to
juncture with siphonal canal and 9-13 strong,
slightly recessed lirae that diminish rapidly. In-
FK.
side I
reticulata ^Z,iK?i<5| A pert )i ml and right
sp,. cuium dredged in 6 meters of water, W toSW
from the xouthem end of Eginnnt Key, Florida. (USNM
806999). 1 1/2 X.
ner lip with 2 pronounced columellar folds and a
distinct siphonal fold. Posterior fold, much the
largest, distinctly bifurcate. Anterior fold some-
times subdivided by a shallow furrow, but to a
much lesser degree. The posterior fold overlies
the siphonal fasciole. Siphonal canal short
(about 1/5 aperture length), slightly recurved
dorsally and to the right. Base color is white,
with patches of light ginger to chocolate brown
that are sharply limited by both collabral and
spiral bands of white. The collabral bands
overlie areas of weak ribbing and areas midway
between them. Spiral white bands are situated
medially and near the siphonal margin. The
aperture is white.
Internal: Examination of shells sectioned
through planes normal to the coiling axis and
transverse to growth lines revealed that aper-
tural lirae and columellar folds are not spirally
continuous, but are prominent only every 1/3
whorl, and disappear or are greatly reduced be-
tween (Fig. 3). The spiral lirae of the outer lip
are produced intermittently, and do not extend
to the outer lip. The area between the lirae and
the edge of the outer lip is thin and corresponds
to the areas of weak collabral ribbing noted pre-
viously. The columellar folds reach maximum
extension into the aperture in direct opposition
to maximum Ural extension, and are reduced
and appressed to the columella between.
Ultrastructure: The yellow, unornamented
periostracum reaches a thickness of 4-6 ^m
(Figs. 6, 7 P), and overlies a layer of crossed-
lamellar aragonite (Figs. 4-7, XLC) in which the
lamellar planes are collabral. As the axial ribs,
spiral cords and lirae are composed of this layer,
its thickness is quite variable (from 1 to 3 mm in
mature specimens). A second crossed-lamellar
shell layer (Figs. 4-6, XLT), in which the lamel-
lar planes are roughly perpendicular to those of
the preceding layer (XLC) as well as to the coil-
ing axis, lines the inner edge of the shell, and is
more uniform in thickness (450 to 750 \xm).
The general form and diversity of sculpturing
among 73 living species of Cancellariidae have
been illustrated in color in the forthcoming
book, the Compendium of Seashells (pp.
225-231) by Abbott and Dance (1982). Speci-
mens figured are from the collection of the
Vol. 96(3)
July 16, 1982
THE NAUTILUS 107
FIGS. 2-7. Details of shell structure -j? L ancellana reticulata iLinmi. 2, i ,._,(.,...,„/,. Scak bar = WO tirn. 3, Anterior view of
shell in which 112 whorl of the outer lip was removed along its midline to show internal structure. Scale bar =5 mm. 4, Fracture
surface. Plane of fracture parallel to outer lip and passing through apertural lirae. Scale bar =400 tim. 5. Fracture surface.
Plane of fracture perpendicular to outer lip. Scale bar = UOO urn, 6. Partial fracture through outer, collabral layer but not
through inner, transverse layer. Scale bar = 100 lAm. 7, Outer edge of fracture surface in a plane parallel to the auier lip. Scale
bar=i ijm.
108 THE NAUTILUS
July 16, 1982
Vol. 96(3)
junior author and from the type collection at the
U.S. National Museum.
Soft-parts Morphology
External features: The shell-less animal con-
sists of about 5 whorls, of which the mantle cav-
ity occupies approximately 2/3 whorl, the volu-
minous kidney (Fig. 8, k) 1/3 whorl, and the
large digestive gland (Fig. 8, dg) about 4 whorls.
Animals were able to retract about 1/2 whorl in-
side the aperture. The broad attachment area of
the columellar muscle is situated below the rear
of the mantle cavity when the animal is with-
drawn. Preserved animals are uniformly pale
orange in color, lacking a discernable pattern.
The mantle edge (Fig. 8, me) is thin and finely
papillose. The long, narrow, posteriorly taper-
ing foot has a pronounced propodium (Fig. 8,
pro) and lacks an operculum. Of the cephalic ten-
tacles, the left (Fig. 8, let) is longer and broader
than the right, and bears 2 papillae above the
eye (Fig. 8, e). The siphon (Fig. 8, s) extends
slightly beyond the mantle edge and lies over
the left tentacle.
Mantle cavity: The mantle cavity is narrow
and deep, with pallial organs situated as in other
Neogastropods. The osphradium (Fig. 8, os) is
short (7 mm) and broad (L/W = 3), bearing about
70 leaflets per side. There is an unusually large
space between the osphradium and the cteni-
dium (Fig. 8, ct) (about 1.5 times the width of
either organ), so that the ctenidium, which is
long, slightly narrower than the osphradium and
consists of about 250 leaflets, is suspended from
the top of the mantle cavity. On the right side of
the ctenidium lies the transversely pleated hypo-
branchial gland (Fig. 8, hg), and to the right of
it, the rectum (Fig. 8, r) and genital ducts. The
kidney forms the right rear wall of the mantle
cavity, and opens into it by a single, vertical slit
(Fig. 8, ko). The large pericardium (Fig. 8, pc) is
embedded in the left side of the kidney, and
forms the left rear wall of the mantle cavity.
Alimentary system: When fully extended, the
narrow, pleurombolic proboscis can be pro-
truded through the rhyncostome to a length
equal to 1 1/2 times the shell length. It is of the
same color as the foot, and twice as broad as
high, being smooth along its curved dorsal sur-
face and papillose along the entire length of its
flat ventral surface (Fig. 9). When retracted, the
proboscis is folded within the proboscis sheath.
The retractor muscles originate from the body
wall as well as from the columellar muscle.
From the mouth (Fig. 9, m) situated terminally
on the curved anterior of the proboscis, a short
(750 f^m) oral tube (Fig. 9, ot) leads to a
cuticularized, ventrally overlapping tube-like
structure (Fig. 9, cut) [Upper Shield or Mandible
of Olsson, 1970], which is narrow anteriorly and
expands posteriorly to enclose the buccal mass.
The floor of the buccal mass is lined by a broad,
cuticularized sub-radular membrane (Fig. 9,
srm) [Inner Shield of Olsson, 1970] which sup-
ports the radula in a narrow groove. The radula
(Fig. 12) consists of a ribbon supporting 73-109
rows of single teeth, of which slightly less than
half are directed anteriorly, the balance posteri-
orly. The anteriorly directed teeth may be pro-
truded slightly beyond the end of the cuticula-
rized tube. The posteriormost teeth are poorly
formed, and lie in the radular sac (Fig. 9, rs)
which extends slightly below the buccal mass.
The division between the anteriorly and posteri-
orly directed teeth is slightly anterior to the
oesophageal opening (Fig. 9, oaoe). Several
specimens were observed with groups of teeth
(4-9) coiled in a loop under the oesophagus, indi-
cating the mechanism by which they are redi-
rected. Individual teeth are long (1.2-1.9 mm)
(Fig. 12), narrow (25 ^m at the base) (Fig. 13)
and extremely flexible. Toward the tip (Figs. 14,
15), they constrict (20 ^<m) and bear 3 highly
modified cusps, each with secondary, anteriorly
directed cusps. The 2 lateral cusps are directed
inward, and interlock medially with the up-
wardly directed central cusp. The oesophagus
opens along the roof of the buccal cavity, where
it appears to be cuticularized. At the rear of the
buccal mass is the valve of Leiblein (Fig. 9, vl),
and beyond it the long, narrow mid-oesophagus
(Fig. 9, moe) winds backward to the stomach
(Fig. 8, sto). Just behind the buccal mass lie two
pairs of salivary glands. One pair (Fig. 9, sg) is
narrow and long, entering the buccal mass just
anterior to the oesophageal opening. These are
homologous to the normal salivary glands of
other prosobranchs. The second pair (Fig. 9,
Vol. 96(3)
July 16, 1982
THE NAUTILUS 109
dasg
'IGS. 8-11. Anatomical features o/Cancellaria reticulata (Linne). 8, Mate specimen removedfrom shell, uncoiled and mnntle
[Tvity opened mid-darsally to display contents. 9, Dissection of proboscis tip, viewed from left side. 10, Diagrammatic
Wepresentation of the female genital ducts. 11, Diagrammatic rejjresentation of the male genital diicts.
no THE NAUTILUS
July 16, 1982
Vol. 96(3)
FIGS. 12-15. Scanning electron micrograpks of raduia o/ Cancellaria reticulata (Linne). 12, Entire radular ribbon with
suhradular membrane. Scale bar = i.00 \im.. 13, Attachment of basal ends of teeth to radular ribbon. Scale bar=10 nm. 14, Ter-
minal ends of radular teeth. Scale bar = 10 (j?n. 15, Terminal ends of radular teeth. Scale bar = J, ^im.
asg) are smaller and sausage-shaped, giving rise
to ducts (Fig. 9, dasg) that lead anteriorly,
becoming convoluted and fusing just prior to
entering the oral tube near the mouth. These ap-
pear to be homologous to the accessory salivary
glands of muricids and volutids. At the ventral
posterior ends of the buccal mass lie the buccal
ganglia (Fig. 9, bg), and from them the cerebro-
buc( ' -I'nnectives (Fig. 9, cbc), bound together
with I ■ poboscis nerves, run medially down
the len;. ' ^r i!,,i probo.scis. The oesophagus
passes through il;c )iy^h\y concentrated nerve
ring and becomes highly convoluted before
entering the stomach. There is no separate
gland of Leiblein, but rather a narrow glandular
strip runs along the mid-oesophagus. The
stomach (Fig. 8, sto), small, narrow and tube-
like, runs across the anterior face of the diges-
tive gland (Fig. 8, dg). The narrow oesophagus
(1/3 the diameter of the bulbus aortae. Fig. 8,
ba) enters on the left, near the opening of the
duct to the digestive gland. Longitudinal folds
run the length of the stomach into the intestine,
which continues as the rectum (Fig. 9, r) along
Vol. 96(3)
July 16, 1982
THE NAUTILUS 111
the right side of the roof of the mantle cavity,
but detaches from it 1-2 mm before ending in
the anus (Fig. 8, a). There appears to be no anal
gland.
Female reproductive system: The light-yellow
ovary (Fig. 10, ov) lies at the apex of the diges-
tive gland, forming the terminal 1 1/2 whorls. It
is composed of numerous thin ascini that con-
verge to form the oviduct (Fig. 10, od) that runs
anteriorly along the right ventral side of the
visceral mass. The oviduct is joined by the gono-
pericardial duct (Fig. 10, gpd) just before enter-
ing the rear of the mantle cavity and joining the
large, arched albumen gland (Fig. 10, ag). Be-
tween the albumen gland and the large, rectan-
gular capsule gland (Fig. 10, eg) is the ingesting
gland (Fig. 10, ig) that appears as a small mass
of dark-brown ridged tubules. Its duct serves as
the seminal receptacle. At the anterior end of
the capsule gland is the large, squarish bursa
copulatrix (Fig. 10, be). Cutting through the
muscular wall reveals an arched, rapidly elarg-
ing tube with the female opening (Fig. 10, fo) at
its end. The ventral pedal gland, a 2-3 mm deep
invagination lined with glandular folds, is situ-
ated along the midline of the sole of the foot,
about 1/4 of its length from the anterior edge.
Male reproductive system: The dark-brown
testis (Fig. 11, te) consists of a mass of ascinous
tubules imbedded in the columellar side of the
digestive gland. These tubules join together to
form a common testicular duct (Fig. 11, td)
which runs anteriorly along the right ventral
side of the visceral mass. When next to the pos-
terior portion of the kidney, it becomes con-
voluted, acting as a seminal vesicle (Fig. 11, sv),
then straightens and enters the rear of the man-
.tle cavity ventral to the rectum, where it
enlarges in diameter and again becomes con-
voluted. These convolutions act as a prostate
gland (Fig. 11, pr), and have an opening to the
mantle cavity (Fig. 11, opm). The vas deferens
(Figs. 8, 11, vd) winds along the base of the man-
tle cavity from the prostate gland to the base of
the penis (Figs. 8, 11, pen). The penis is long
(18-20 mm), narrow (1 1/2-2 mm) and flat, bear-
ing a terminal papilla (2-2 1/2 mm). Judging by
the highly coiled penial duct (Fig. 11, pd), the
penis is capable of considerable extension.
Nervous system: The cerebral, pleural, pedal
and suboesophageal ganglia are fused into a
concentrated nerve ring through which pass the
oesophagus and the anterior aorta. The buccal
ganglia are at the base of the buccal mass at the
tip of the long proboscis, with the cerebro-buccal
connectives reaching 50 mm in length. The su-
praoesophageal ganglion lies over the oesopha-
gus on the right side of the cephalic hemocoel,
just behind the proboscis sheath, and gives rise
to the osphradial nerve. The visceral ganglion
lies in its usual position at the innermost end of
the floor of the mantle cavity.
Discussion
The anteriorly rounded, posteriorly tapering
shell, short siphonal canal, lack of pronounced
ornament and smooth surface identify Cancel-
laria reticulata as a frontally burrowing, in-
faunal neogastropod. The majority of specimens
examined (27 of 32) had 1 or more crab breaks
on the last whorl. These breaks, however, failed
to penetrate beyond the penultimate apertural
lirae, suggesting that these serve as shell rein-
forcements or internal varices. The periodic in-
crease in the size of the columellar folds in op-
position to the lirae of the outer lip decreases
the size of the aperture and serves, at least in
part, an antipredatory function. This periodicity
of shell structure indicates that growth is
episodic and rapid, occurring in increments of
approximately 1/3 whorl.
Knight, et al. (1954) suggested that cancel-
lariids (included in their Volutacea) evolved
from the Mesozoic Nerineacea, which, along
with some of the Soleniscinae (Subulitacea), had
internal folds of considerable complexity. A re-
examination of these groups for periodicity of
internal structure may shed light on the origins
of Cancellariacea.
Ultrastructural studies reveal that the shell
consists of a thin periostraclim overlying 2
orthogonal layers of crossed-lamellar aragonite.
In the outer layer, which comprises the bulk of
the shell, the crystal planes are oriented parallel
to the outer lip, while in the thinner, inner layer,
which lines the inner surface of the shell, the
crystal planes are perpendicular to those of the
outer layer.
112 THE NAUTILUS
July 16, 1982
Vol. 96(3)
The fracture plane of the thicker outer layer
would cause breaks in the shell to run parallel
to the outer lip, while the orthogonal inner layer
greatly increases the mechanical strength of
the shell. In studies of shell crystallography,
Boggild (1930) reported that "Different Tertiary
and Quaternary species of Cancellaria . . . were
all quite alike and built up of the ordinary three
layers." [transverse, collabral, transverse], but
did not indicate where in the shell the sections
were taken. Along the inner lip, a layer of trans-
verse crystals is deposited over the outer layer
of shell, possibly accounting for the discrepancy.
Cancellaria reticulata is similar to other
neogastropods in the morphology of its head-
foot, pallial complex, reproductive and nervous
systems, with the following noteworthy excep-
tions. The enlarged and bilobed left cephalic ten-
tacle was found, in all the preserved specimens
examined (n = 8), to run along the base of the
siphon, with the two papillae extending over and
beyond the opening. It is not known if it func-
tions together with the siphon, forming a tube,
or is simply oriented in the anteriormost direc-
tion. Several other cancellariid species have
similar, and, in some cases, more elaborate ar-
rangements (unpublished observations). Of the
pallial organs, the position of the ctenidium is
unusual, in that it is displayed to the top of the
roof of the mantle cavity. The morphology of
both male and female reproductive systems is
typically neogastropod (as exemplified by Nu-
cella lapillus, see Fretter, 1941), with minor
modifications only in the anteriormost portion
of each system [bursa copulatrix- female; penial
papillae -male]. The nervous system differs
from that of other neogastropods chiefly in the
location of the buccal ganglia and the extreme
length of the cerebro-buccal connectives.
The unique and highly specialized alimentary
system is the basis for the superfamilial status
of this group, yet the food and feeding mecha-
nisms remain unknown for all cancellariids.
Both Graham (1966) and Olsson (1970) have
speculated that these animals feed on soft-
bodied micrncrganisms which are "brushed" into
the gut by the radular teeth. Like Graham
(1966), we wt-re unable to find any traces of solid
food in the alimentary systems of the specimens
we examined.
The extreme length of the ventraliy papillose
proboscis suggests that cancellariids feed at a
distance on animals or tissues they cannot reach
directly. The presence of well developed acces-
sory salivary glands is generally associated with
a carnivorous rather than a scavanger diet.
It is currently believed that cancellariid radu-
lae consist of rows of rachidia, the lateral teeth
having been lost (Ponder, 1973). Scanning elec-
tron micrographs of the distal tips of radular
teeth reveal an elaborate cusp structure, which
can be interpreted as being a tri-cusped rachi-
dian in which each of the primary cusps have
developed secondary cusps. As the lateral cusps
bear a strong resemblance to rachiglossate
lateral teeth, we feel an alternative interpreta-
tion may be that lateral teeth fused with the
rachidian prior to elongation in the ancestral
cancellariid.
Viewed functionally, the extreme anterior
placement of the valve of Leiblein would serve
to minimize the volume of food anterior to it,
permitting rapid interaction with salivary gland
secretions, and, perhaps more importantly, to
prevent the backflow of liquified food posterior
to it. The lack of a gland of Leiblein, the long,
thin oesophagus and simple tubular stomach
suggest that little further treatment of food is
required prior to digestion.
Based on certain general similarities between
the cancellariid alimentary system and those of
pyramidellids and melanellids, we suggest that
cancellariids are piercing, fluid feeders rather
than microphagous grazers.
ACKNOWLEDGMENTS
We wish to thank William G. Lyons of the
Department of Natural Resources, State of
Florida, as well as Dr. Harry G. Lee, Mr. Allan
Walker and Mrs. Jane Dawley, all of Jackson-
ville, Florida, for making available the pre-
served material used in this study. Special
thanks are due to Mr. L. C. Bailey of the Engi-
neering Test Center, E. I. du Pont de Nemours
Co. for his help with scanning electron micro-
scopy. Critical review of the manuscript by Dr.
M. R. Carriker, College of Marine Studies,
Vol. 96(3)
July 16, 1982
THE NAUTILUS 113
University of Delaware, is gratefully acknow-
ledged.
LITERATURE CITED
Abbott, R. Tucker and S. Peter Dance. 1982. Compendium
ofSeashelh. E. P. Dutton, N.Y. 400 pp., 4,300 color plates.
Barnard, K. H. 1958. The radula of Cancellaria. Jour.
Confhology 24(7):243-244.
Boggild, U. B. 1930. The sheU structure of mollusks. Acad.
Roy. Sci. Lettres Danemark. Mem. ser. 9, 2:230-325,
pi. 1-15.-
Fretter, V. 1941. The genital ducts of some British steno-
glossan prosobranchs. Jour. Mar. Biol. Assoc. U.K.
25:173-211.
Graham, A. 1966. The fore-gut of some marginellid and
cancellariid prosobranchs. Stud, Trop. Oceanog. Miami
4(1):1.34-151.
Knight, J. B., Bratten, R. L. and Yochelson, E.L. 1954.
Status of Invertebrate Paleontology, 1953. V. Mollusca:
Gastropoda. Bull Mus. comp. Zool. Hare. 112(3):173-179.
Olsson, A. A. 1970. The cancellariid radula and its interpre-
tation. Palaeontogr. Amer. 7(43):19-27.
Ponder, W. F. 1973. The origin and evolution of the Neo-
gastropoda. Malamlogia 12(2):295-338.
Thiele, J. 1929. Handhuch der systetnatischen Weichtier-
kunde. (Jena, Gustav Fischer, 1929-1935):1154 p.
Troschel, F. H. 1856-1893. Das Gebiss der Schnecken zur
Begriindung einer natiirlichen Classification. 2. Berlin.
Wenz, W. 1938-1943. Handbuch der Paldozoologie (0. H.
Schindewolf, ed.). Berlin.
THE DISTRIBUTION OF DONAX VARIABILIS (BIVALVIA) AT SHIP
ISLAND, MISSISSIPPI: SOME PALEOMALACOLOGICAL ASPECTS
William Miller, III
Earth Sciences Dept., Tulane University
New Orleans, LA 70118
Donax variabilis is the easily recognized
tellinacean bivalve that inhabits the high energy
foreshore zone of ocean beaches from Virginia
to Texas (Abbott, 1968). This clam is remarkable
for its abilities as a rapid burrower, for its tidal
migrations on the beachface, and for its occur-
rence in densely packed "colonies" in an en-
vironment from which typically little else is col-
lected alive (Stanley, 1970). The purpose of this
note is to describe the distribution of D.
variabilis, both living populations and dead
shells, along a section of moderate energy ocean
beach at Ship Island, Mississippi, a barrier
island separating Mississippi Sound from the
Gulf of Mexico. This section of beach was (in
May, 1980) composed of fine quartz sand with a
trace of shell fragments, showed no signs of
pollution, and featured a foreshore slope of only
a few degrees. Other than infrequent churning
of the substrate by swimmers using a beach just
to the west of the study area, the beachface is
undisturbed by man.
and
Sheree Kooser
148320 Hartwell Terrace
Novelty, OH 44072
Beginning 90 m east of the swimming area on
the western end of Ship Island, 11 samples were
collected from the middle beachface at 90 m in-
tervals proceeding east along the beach. At each
sample station one litre of sand was scooped
from the beach and wet sieved using nested
screens having openings of 4.0 and 2.4 mm to
recover all shells contained in the samples. Live
individuals, as well as articulated and disarticu-
lated dead shells, were counted and returned to
the beachface. The results of the survey are
summarized in Table 1.
Nearly all living Z). variabilis recovered were
about 2 cm in length (adults); only a few in-
dividuals were larger or smaller. The majority of
the specimens were alive (86%), and the dead
shells were mostly disarticulated and abraded
(84%). The survey appears to have encountered
at least two "regional aggregations" of living D.
variabilis in the beachface: one at sample sta-
tions 3 and 4, and another at stations 7, 8, and 9.
All sample stations except 2 and 6 encountered
114 THE NAUTILUS
July 16, 1982
Vol. 96(3)
TABLE 1. Distribution o/Donax variabilis at Ship Island.
Misfdssippi: May 20, 1980.
at least local aggregations. The smaller, local
aggregations appeared to be clumped together
forming the larger, regional aggregations. Well-
defined aggregations were not preserved
among the dead shells. The largest local aggre-
gations of living clams occurred near the end of
the transect farthest from the public swimming
beach.
The distribution of Donax is of interest to
paleontologists because of its use as an indicator
of proximity to ancient shorelines in paleoenvi-
ronmentai reconstructions (for example, see
Mixon and Pilkey, 1976). However, as shown in
this study, relatively few dead shells of D.
variabilis were found in situ in the beachface at
Ship Island. It seems that after individuals die
their shells are temporarily concentrated at the
plunge step just offshore from the beachface
(see Davis, 1978). Tides and currents probably
redistribute the dead shells to various areas in
the nearshore zone and other parts of the inner
shelf. This transport of D. variabilis shells out
onto the adjacent shelf explains the admixture
of small numbers of these swash zone inhabi-
tants in Pleistocene fossil assemblages of sub-
tidal marine origin with which we are familiar,
and argues against the use of Donax as an une-
quivocal indicator of proximity to ancient shore-
lines. Moreover, tropical storm overwash and
the migration of tidal inlets tend to recycle
Donax shells into backshore, interdune, and
even backbarrier environments. Shells re-
worked from relict sediments compound the
problem (see Pilkey et al.. 1969). In conclusion,
paleoenvironmental interpretations involving
Donax always should take into account the
taphonomic history and paleosynecologic prop-
erties of fossil deposits, and not focus on a few
selected taxa as "reliable" indicators of environ-
ment.
LITERATURE CITED
Abbott, R. T. 1968. Seashells of North America. Golden
Press, New York, 280 pp.
Davis, R. A. 1978. Beach and nearshore zone. In. R. k. Davis
(ed.), Coastal Sedimentary Environments: Springer-
Verlag, New York, pp. 237-285.
Mixon, R. B. and 0. H. Pilkey. 1976. Reconnaissance geo-
logy of the submerged and emerged Coastal Plain Prov-
ince, Cape Lookout area, North Carolina. U. S. Geol.
Survey, Pi-oJ. Paper 859, 45 pp.
Pilkey, 0. H.,'b. W. Blackwelder, L. J. Doyle. E. Estes and
P. M. Terlecky. 1969. Aspects of carbonate sedimentation
on the Atlantic continental Shelf off the southern United
States. Jour. Sed. Petrology 39:744-768.
Stanley, S. M. 1970. Relation of shell form to life habits of
the Bivalvia (Mollusca). Geol. Soc. Am. Memoir 125.
296 pp.
PHILLIP W. CLOVER
COLLECTOR & DEALER IN
WORLD WIDE SPECIMEN
SEA SHELLS P. Q. Box 83
Glen Ellen, CA 95442
FREE SHELL
BOOK LIS is
AND
SPECIALISTS IN RARE
CV'PRAEA, CONUS. VOLUTA
MAKGINELLA, MITRA, MUREX
Specmen Shells
Offering microscopic and miniature (to '/. inch) shells
from the Florida Keys, vrith accurate locality data Also
unsorted grunge; u/rite for list.
Margaret Teskey
P.O. Box 273
Big Pine Key. Fl. SSOiS
Vol. 96(3)
July 16, 1982
THE NAUTILUS 115
DIVARILIMA (BIVALVIA: LIMIDAE) AND A NEW SUBSPECIES
FROM THE CARIBBEAN
J. Gibson-Smith and W. Gibson-Smith
Escuela de Geologia, Minas y Geofisica, Universidad Central de Venezuela,
Apartado 47.351, Caracas 1041 A, Venezuela
ABSTRACT
Lima albicoma Dall. 1886. from the Caribbean Recent. i,s reassigned to
Divarilima Powell. 1958. a Recent taxon from the Western Pacific, the ancestor
probably being the genus Badiotella Bittner. 1890. known only from the middle
Trias of Europe. The new subspecies D. albicoma handini, is described from the
Venezuelan Recent.
Lima albicola Dall, 1886, was found off Cuba
(type locality) and off Barbados at a depth of
about 200 m; it has been re-figxired by Abbott
(1974:454:5249). This small shell (8 mm') with its
long, straight, anterodorsal margin is similar in
outline to the large, coarsely sculptured Lima
S.S., but resembles Ctenoides Morch, 1853, in
possessing a divaricate sculpture. It differs from
all Western Atlantic limids in having a very
deeply excavated lunule, or "truncature", as Dall
(1886:225) called it. A similar Recent species
from off eastern Australia and Kermadec
Island, Lima sidneyensis Hedley, 1904, was
made the type of Divarilima Powell, 1958 (Cox
& Hertlein, in Moore 1969:N389), thus drawing
attention to the divaricate sculpture, a feature
of Ctenoides, rather than to the characteristic
lunule. Lima albicola can be assigned to
Divarilima. The same lunule is present in
another small genus, Badiotella Bittner, 1890
(Cox & Hertlein, in Moore 1969:N386), known
only from the middle Trias of Europe which,
although lacking the divaricate sculpture, can
probably be considered ancestral to the present
day forms of Divarilima from the Western
Pacific and Western Atlantic, forms to be
regarded as Tethyan relicts.
From the north coast of Venezuela comes a
second Caribbean form, here named: Divari-
lima albicola handini, n. subsp.
Divarilima albicola handini
Gibson-Smith & Gibson-Smith, n. subsp.
Figures 1,2.
Description - Shell small, trigonally ovate.
Anterodorsal margin nearly straight, extended,
coinciding with a strong umbonal ridge along
which runs a fine keel. Posterior margin almost
straight above, these two margins subtending
an acute angle at the umbo. Ventral margin
deeply rounded. Shell almost equilateral. Poste-
FIGS. 1-3. 1 and 2, Divarilima albicoma handini n. subsp.
Holotype, external and internal views, right valve, height
10.0 mm, length 8.2 mm. Recent of Venezuela. USNM no.
784699. 3, Divarilima albicoma Dall. 1886. Paratype. inter-
nal view, left valve, height .V.S mm. length 3.S mm. Caribbean
Recent. MCZ 7829.
116 THE NAUTILUS
July 16, 1982
Vol. 96(3)
rior auricle moderate, anterior absent. Cardinal
area triangular with a narrow ligament pit over-
hung slightly by the small sharp umbo; hinge
edentulous. Lunule triangular, concave, both
borders angulate (90°), sculptured with a weak
radial riblet and weaker, irregular, radial wrin-
kles. Ornament of fine, close, punctate grooves,
divaricate along the median line from to umbo to
ventral margin; angle of divarication very acute
and hardly to be seen. Several strongly marked
growth stages stepping down across the disc.
Color a very pale brown, translucent; growth
stages marked by narrow, opaque white, con-
centric bands. Remnant of pale brown perio-
stracum within the lunule.
Holotype - USNM No. 784699. A right valve,
height 10.0 mm, length 8.2 mm, semi-diameter
2.5 mm.
Type locality - Recent, Chichiriviche de la
Costa, Federal District, Venezuela.
Remarks - Apart from the holotype there are
two, small paratypes each measuring approx-
imately: height 3.0 mm, length 2.75 mm. All are
right valves and came from a sand sample col-
lected at 30 m by SCUBA-diver Alan Handin. A
figure of a paratype of D. albicoma (courtesy Dr.
Kenneth J. Boss, MCZ) is shown for comparison
(Fig. 3).
Comparisons - Divarilima albicoma handini
n. subsp. differs from D. albicoma Dall in being
less produced anteriorily and posteriorily, re-
sulting in a narrower, more equilateral shell. In
handini the anterodorsal and posterior margins
subtend an acute angle at the umbo; in albicoma
the angle is obtuse. The narrowness of handini
is reflected in the much more acute angle of
divarication along the median line. Further-
more, albicomn is described as having two lines
of divarication (the figure even shows three), in
handini there is only one. Whether the depth
ranges of the two forms overlap remains to be
seen; it may be significant that neither taxon
was found in seafloor samples from nine off-
shore drilling locations, in water depths from 55
to 150 m.
LITERATURE CITED
Abbott, R. T. 1974. Armrican Seashells. 2nd ed. Van
Nostrand Reinhold Co., New York; 663 pp., 4000+ text
figs.; 24 pis. (in color).
Dall, W. H. 1886. Reports on the results of dredging, under
the supervision of Alexander Agassiz, in the Gulf of
Mexico (1877-78) and in the Caribbean Sea (1879-80)
by the U.S. Coast Survey Steamer "Blake" Bull. Mus.
Comp, Zool., Vol. 12, pp. 153-318, 9 pis. Harvard Univ.,
Cambridge, Massachusetts, U.S.A.
Moore, R. C. 1969. Treatise on Invertebrate Paleontology,
Part N, vol. 1, Mollusca 6, Bivalvia, pp. i-xxxviii +
N1-N489, text figs. Geol. Soc. Amer. Inc. & Univ. Kansas.
THE SUBFAMILY MELAMPINAE (PULMONATA: BASOMMATOPHORA)
IN VENEZUELA, WITH DESCRIPTIONS OF TWO NEW SPECIES
J. Gibson-Smith and W. Gibson-Smith
Escuela de Geologia, Minas y Geofisica, Universidad Central de Venezuela
Apartado 47.351, Caracas 1041 A, Venezuela
ABSTRACT
The presence of two, new melampid species in the Venezv£lan Recent i§ re-
ported: Detracia roquesana n. sp. and Tralia venezUelana n. sp., the latter occur-
ring also in the early Miocene Cantaure Formation, Paraguand Peninsula, and
the late Pliocene Mare Formation, Cabo Blanco. T. venezuelana is only the second
species o/ Tralia to be recorded from the Western Atlantic.
The pulmonate genus Melampus is repre-
sented in the Venezuelan Recent by Melampus
(Melampus) coffea (Linnaeus, 1758) (Fig. 1) and
Melampus (Pira) monilis (Bruguiere, 1789)
Vol. 96(3)
July 16, 1982
THE NAUTILUS 117
Figs. 2, 3). These two taxa range from Florida
ind Bermuda to Brazil (Abbott 1974:331). The
former is generally known as cojfeus, but it has
Deen pointed out by Altena (1975:86) that being
1 noun, it is correctly, coffea. Two other
aulmonate genera present in the Recent of
Venezuela are Detracia Gray in Turton, 1840,
ind Tralia Gray in Turton, 1840. The former is
-epresented in Florida and the northern Carib-
bean by the type-species D. bullaeoides
Montagu, 1808), D. floridana (Pfeiffer, 1856)
md D. clarki Morrison, 1951, but in Suriname
Altena, 1975:86) and Brazil (Marcus & Marcus,
1965:42) the representative is D. parana
Viorrison, 1951, the type locality being Para
= Belem), Brazil. In Venezuela, Detracia has
lot been found on the mainland but is present on
;he islands of Los Roques where it is repre-
sented by a new species here identified as
letracia roquesana n. sp. The genus Tralia is
cnown in the Recent of the Western Atlantic by
I single species, T. ovula (Bruguiere, 1789),
vhich ranges from southeast Florida and Ber-
nuda to Barbados (Abbott 1974:33). It has been
■eported also from the Caribbean coast of
^anama (Olsson & McGinty 1958:19) and from
];uracao (Coomans 1958:103), in both instances
IS Tralia pusilla (Gmelin, 1791), a synonym. It
)ccurs also in Venezuela (Figs. 4, 5) where,
lowever, a second, more common form is pre-
sent which is identified here as, Tralia
jenezuelayia n. sp. The ancestor of the latter is
)resent in the early Miocene (Burdigalian) Can-
a.ure Formation of the Paraguana Peninsula; it
vas referred to, Tralia cf. oimla, by Gibson-
Smith & Gibson-Smith (1979:22), but is now
bund to be identical with T. venezuelana n. sp.;
■t occurs also in the late Pliocene Mare Forma-
tion, Cabo Blanco. The Melampinae are hardly
mown as fossils in the region, one other record
)eing of Tralia vetula Woodring, 1928, from the
^liocene Bowden Formation, Jamaica.
Detracia roquesana
Gibson-Smith & Gibson-Smith, n. sp.
Fig. 6
Description - Shell small, about 10 mm in
height, obovate, widest at the middle. Whorls
adpressed, about 11 in all, the bodywhorl about
two-thirds of the shell height. Protoconch at
right angles to shell axis, one-half turn only visi-
ble, brown. The shell lacks sculpture and is
spirally banded in shades of brown. Aperture
narrow, the outer lip not flared. Inner lip with
heavy callus, a strong fold at the base of the col-
umella and a weak fold, well within the aper-
ture, at the middle of the parietal area. Above
the latter the parietal area is weakly excavated
and lacks callus, with the result that the lower
edge of the area becomes a broad, low fold, or
pseudo-fold. Within the outer lip are 3 to 8 lirae,
the lowest and largest projects towards the col-
umella fold, leaving only a narrow gap between.
Opposite the parietal fold and pseudo-fold, the
gap is again narrowed by two strengthened lirae
lying opposite within the outer lip.
Holotype - USNM 784718. Height 10.6 mm,
diameter 5.8 mm.
Locality - Recent, Islas Los Roques, Vene-
zuela.
Paratypes - British Museum (Natural His-
tory) and the Natural History Museum Basel.
Remainder in the collections of the authors.
Remarks - The 6 specimens were collected in
beach drift and the exact ecological niche is
unknown, but is, presumably, above high tide
level as for other members of the family. The
islands are fringed by coral reefs and man-
groves abound. There is no obvious variation in
shell morphology.
Comparisons - Detracia roquesana n. sp. dif-
fers from all the four known Western Atlantic
species; D. bullaeoides is more elongate, lacks a
parietal fold and lirae within the outer lip, and
the protoconch -is white; D.floridana is smaller,
more globose and the lirae within the outer lip
are not enlarged opposite the columella and
parietal folds; D. clarki has 2 lower columella
folds and is sculptured with spiral, incised lines
above the shoulder and around the base and,
lastly, D. parana is smaller, more rotund and
normally possesses only a single, outer lip lira,
many shells lacking even that.
118 THE NAUTILUS
July 16, 1982
Vol. 96(3)
FIGS 1-9. The subfamily Melampinae {n Venezuela (for explanations, see opposite).
Vol. 96(3)
July 16, 1982
THE NAUTILUS 119
Tralia venezuelana
Gibson-Smith & Gibsoyi-Stiiith, n. sp.
Figs. 7, 8 9
Tralia cf. otmla (Bruguiere, 1789), Gibson-Smith & Gibson-
Smith, 1979, GEOS No. 24, p. 22.
Description - Shell small up to about 15 mm
in height, obovate, greatest diameter about the
middle. Protoconch small, pimple-like, at right
angles to shell axis, about one-half turn only visi-
ble. Teleoconch of 8 whorls, the weakly shoul-
dered bodywhorl comprising three-quarters of
the shell. Shell glossy, color dark brown with
faint spiral and axial banding in shades of
brown. Sculpture of up to 9, spiral, pitted
grooves above the shoulder, marking the rows
of setae of the periostracum; remainder of
surface covered with crowded, microscopic
scratches, stronger around the base. Shell sur-
face interrupted by growth incrementals. Aper-
ture wider and flaring below, restricted at the
middle by a heavy spiral thickening within the
outer lip. Columella with a strong basal fold and
a stronger one above at the base of the parietal
area with, on the parietal area proper, weaker
third and fourth folds, the uppermost the weak-
est, lying well inside the aperture and more
easily seen in juvenile specimens.
Holotype - USNM 784719. Height 12.7 mm,
diameter 7.2 mm.
Locality - Recent, Borburata, Falcon State,
Venezuela. Living also at other north coast lo-
;alities from the Paraguana Peninsula to
Carenero, Miranda State, and on the islands of
Los Roques, Tortuga and Margarita. As a fossil
it occurs in the early Miocene Cantaure Forma-
tion, Paraguana Peninsula, and in the late Plio-
cene Mare Formation, Cabo Blanco.
Paratypes - British Museum (Natural His-
l;ory) and the Natural History Museum Basel.
Remainder in the collections of the authors.
Remarks - The material available consists of
87 specimens from the various localities; it is
from beach drift only, the animal living, pre-
sumably, just above high tide level as do other
members of the family. There is some variation
in globosity. In Venezuela, Tralia ovula is large-
ly replaced by T. venezuelana n. sp. only 3
specimens of the former having been found, two
at Borburata, Carababo State and one from
Islas Los Roques (Figs. 4, 5), two localities
where T. venezuelana also occurs. From the
Cantaure Formation one juvenile (Fig. 9) and
one spire have been recovered and from the
Mare Formation a spire only with pitted
grooves. T. venezuelana is only the second Re-
cent species to be reported from the region. Its
presence at Cantaure and Mare helps to confirm
the shallow water nature of those faunas.
Comparisons - The fourth inner lip fold dis-
tinguishes T. venezuelana from T. ovula and
from the west coast forms T. payiamensis (C. B.
Adams, 1852) and T. vanderbilti Schwengel,
1938. T. ovula, furthermore, lacks the pitted
spiral grooves of T. venezuelana. The only other
fossil from the region is T. vetula Woodring,
1928, from the Pliocene Bowden Formation,
Jamaica; it also has pitted spiral grooves at the
top of the whorl, but lacks the fourth, inner lip
fold and it is smaller and slimmer.
LITERATURE CITED
Abbott, R. T. 1974. American Seashells. Second Edition.
Van Nostrand Reinhold Company, New York, 663 pages.
Altena, C. 0. van Regteren. 1975. The marine Mollusca of
Suriname (Dutch Guiana) Holocene and Recent, Part 3:
Gastropoda and Cephalopoda. Zoo/. Verhand. No. 139,
104 pp., 43 Text figs., 11 pis.
Coomans, H. E. 1958. A survey of the littoral Gastropoda of
the Netherlands Antilles and other Caribbean Islands.
Studs. Fauna Curacao, No. 31, pp. 42-111, 16 pis.
^IG. 1. Melampus (Melampus) coffea (Linnaeus, 1758). Re-
■ent, Carenero, Miranda State, Venezuela. Height 9.5 mm.
iiameter 6.0 mm.
^'IGS. 2-3. Melampus (Pira) monilis (Bruguiere. 1789). Re-
■ent. Borburata, Carabobo State, Venezuela. 2, height 12.1
nm. diameter 7.9 mm. 3, whitened, height 8.9 mm, diameter
).l mm.
""IGS. 4-5. Tralia ovula (Bruguiere, 1789). 4, Recent.
uvenile. Borburata, Carabobo State. Venezuela, whitened.
wight U.6 mm, diameter 2.J, mm. 5, Recent, Islas Los Roques,
Venezuela, height 10.1 mm., diameter 5.0 mm.
FIG. 6. Detracia roquesana n. sp., holotype, USNM 781,718,
height 10.6 mm. diameter 5.8 mm. Recent, Islas Los Roques,
Venezuela.
FIGS. 7-9. Tralia venezuelana n. sp. 7, holotype, USNM
784719, height 12.7 mm, diameter 7.2 mm. Recent, Bor-
burata, Carabobo State, Venezuela. 8, paratype, whitened,
height 7.8 mm, diameter J,.6 mm, ibid. 9, Cantaure Forma-
tion, Paraguana Peninsula, Venezuela, height .3.8 mm.
diameter 2.2 mm.
120 THE NAUTILUS
July 16, 1982
Vol. 96(3)
Gibson-Smith, J. and W. Gibson-Smith. 1979. The genus
Ardnella (Moilusca: Bivalvia) in Venezuela and some
associated faunas. GEOS No. 24, pp. 11-32, 3 pis.
Marcus E. and E. Marcus. 1965. On BraziHan supratidal and
estuarine snails. Bol. Fax:. Fit Cien. Letr. Univ. S. Paulo
No. 287, Zoologia No. 25, pp. 19-82, 10 pis.
Olsson, A. A. and T. McGinty. 1958. Recent marine mol-
lusks from the Caribbean coast of Panama with the de-
scription of some new genera and species. Bull. Amer.
Paleont. 39(177):58, 5 pis.
AN ANCESTRAL STEPHOPOMA (MOLLUSC A: GASTROPODA) FROM
THE TERTIARY OF VENEZUELA
J. Gibson-Smith and W. Gibson-Smith
Escuela de Geologia, Minas y Geofisica, Universidad Central de Venezuela,
Apartado 47.351, Caracas 1041 A, Venezuela
ABSTRACT
Stephopoma pennatum Morch, I860, from the Panamic Province and not pre-
viously knovm as a fossil, has been found in the early Miocene Cantaure Forma-
tion, Venezuela. The only other species in the region is S. myrakeenae Olsson &
McGinty, 1958, from the Caribbean adjacent to the exit of the Panama canal. S.
myrakeenae has not been shovm to differ from S. pennatum and this raises the
question of whether the former is a Miocene relict, or whether the sessile pennatum
has reached the Caribbean shore via the canal, attached to the hulls of ships.
Stephopoma pennatum Morch, 1860, lives in
shallow water in the Eastern Pacific from
Nicaragua to Peru. Keen (1971:396:450) places
the genus in the Vermiculariinae, probably
because of its turretellid operculum edged with
bristles. On the other hand, Abbott (1974:101)
assigns it to the Vermetidae. The most striking
feature is the protoconch which is neither tur-
ritellid nor vermetid. It is described by Keen
(loc. cit.) as follows: "The initial whorls are flat,
resembling a small Heliacus, lighter-colored
than the adult shell, studded with radial rows of
pustules". Olsson & McGinty (1958:35) identified
a second species, but from the Caribbean coast
of Panama: Stephopoma myrakeenae. They
assigned it also to the Vermetidae.
Stephopoma Morch, 1860, the type of which is
Vermetu.s roseum Quoy & Gaimard, 1832, from
the Recent of New Zealand, is not known as a
fossil. However, from the early Miocene (Burdi-
galian) Cantaure Formation, Paraguana Penin-
sula, Venezuela, twelve protoconchs have been
collected with short lengths of the disjunctly-
coiled shell attached (Fig. 1). The specimen
micrographed (SEM) was inadvertently in-
verted when mounted; but no matter. The
planorbid protoconch consists of 1 1/4 rapidly
expanding whorls, the first half-turn smooth,
followed by the pustulose decoration. The ir-
regular adult tube, subquadrate to subcircular in
section, is smooth and glossy within; externally,
it is closely, longitudinally ribbed, the surface
roughened by sinuous growth incrementals,
some of which are scaly, and the longest tube
measures about 15 mm with a diameter of 2 mm.
All this is much as in S. pennatum, to which the
shell is referred.
The Caribbean 5. myrakeenae was not dif-
ferentiated from S. pennatum and although it
was not described as being ribbed, it was said
that most of the adult tubes were very worn.
Otherwise, it is indistinguishable and should,
perhaps, be added to the short list of species oc-
curring on either side of the Isthmus of Panama
(Radwin 1969:234, 235; Vermeij 1978:213, 269).
S. myrakeenae was found at Colon and Bocas del
Toro Island, some 250 km to the west. The ques-
tion has to be asked, therefore, whether it is
pure coincidence that this Miocene relict found
refuge adjacent to the exit of the Panama canal.
Vol. 96(3)
July 16, 1982
THE NAUTILUS 121
FIG. 1. Stephupoma pennatum Miij-r/i. ISHO. Entiy Miocene
Cantaure Formation, Venezuela. SEM mirnigrnph (x 55).
Ventral view of protoconck.
There is the possibility that it is a case of
recolonization by pennatum, this sessile animal
navigating the canal attached to the hulls of
ships. The collecting dates were 1917, 1920 and
1953; the canal opening was in 1914, but it is not
known whether tuyrukeenae was present at
Bocas del Tore Island on the earlier visits. If
present only in 1953, just to reach the island
would require a migration rate of some 6 km per
annum, assisted by the prevailing currents. It
might be significant if it were to be found that to
the east of Colon, against the prevailing cur-
rents, there was a not too distant limit to the oc-
currence of rnyrakeenae. It has been reported
from Payardi Island (Radwin 1969:230), but that
lies very close to Colon.
If it is a case of re-colonization, then Sfepho-
poma joins the list of "paciphile" genera (Wood-
ring 1966:426). In that case, its extinction in the
Caribbean could not have been due to the
change in environment induced by the severing
of the Atlantic-Pacific connection, an event
believed to have resulted in many extinctions
(Woodring loc. cit.). Had it been so, it could not
have re-colonized. If extinction occurred, there-
fore, it was more likely due to the drop in sea-
level and temperature during the Pleistocene
glaciations (Olsson 1961:7).
LITERATURE CITED
Abbott. R. T. 1974. Ameriran Sea-shells. 2nd ed., Van
Nostrand Reinhold Co., New York; 663 pp., 4000 -^ text
figs. 24 pis.
Keen, A. M. 1971. Sea shells of tropical West Amei-ica:
marine mollusks from Baja California to Peru, 2nd ed.,
Stanford Univ. Press, Stanford, Calif, i-xiv + 1064 pp.,
ca. 4000 text figs., 22 col. pis.
Olsson, A. A. 1961. Mollusks of the tropical Eastern Pacific:
Panamie- Pacific Pelecypoda. PRI, Ithaca, N.Y., 574 pp.,
86 pis.
Olsson, A. A. and T. L. McGint.v. 1958. Recent marine mol-
lusks from the Caribbean coast of Panama with the de-
scription of some new genera and species. Bull. Amer.
Paleont. 39(177):52, 5 pis.
Riidwin, G. E. 1969. A Recent molluscan fauna from the
Caribl>ean coast of Panama. Trans. San Diego Soc. Nat.
Hist. 15(14):229-236, 1 fig.
Vermeij, G. .J. 1978. Biogeograpliy and adaptation: patterns
of life. Harvard Univ. Press, Cambridge, Massachusetts
and London, England, i-xi -i- 332 pp., 50 text figs.
Woodring, W. P. 1966. The Panama land bridge as a sea
barrier. Pine. Amer. Phil Soc. 110(6):425-433, 3 figs.
Rare and Exotic Spex:imen Shells
for the discriminating collector
Free price list
Janowsky's
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946 Ralph Avenue
Brooklyn, New York 11236 USA
(212) i85-S550
122 THE NAUTILUS
July 16, 1982
Vol. 96(3)
LARVAL DEVELOPMENT IN CREPIDULA MACULOSA
(PROSOBRANCHIA: CREPIDULIDAE) FROM FLORIDA'
K. E. Hoagland and
Lehigh University
Bethlehem, PA
and
Academy of Natural Sciences
Philadelphia, PA 19103
Mr. Dale Stingley recently forwarded to The
Nautilus a letter he found in his files dated
October 14, 1952, from Wesley R. Coe, now
deceased. The letter contained unpublished
information on the type of eggs produced by
Crepidula maculosa Conrad, 1846. Stingley had
sent two or three specimens of C. maculosa^ col-
lected at Sanibel Island in May 1952 to Dr. Coe,
who had already published several papers on
developmental mode and size of eggs in species
of the genus Crepidula (Coe, 1949). It was
Stingley (1952) who recognized that C. maculosa
was, indeed, a valid species distinct from C. for-
nicata with which it had been synonymized.
Coe's remarks to Stingley are quoted below.
They are significant because of renewed interest
in the evolutionary ecology of egg type and lar-
val development in mollusks (Pechenik, 1979;
Caswell, 1981). The verification of complete
brooding in Crepidula maculosa compared with
mixed development (brooding followed by plank-
totrophy) in C. fomicata, a larger but similar
species, provides another case of divergent
modes of egg development in two similar con-
geners. As found by Gallardo (1977, 1979) for C.
dilatata and C.fecunda in Chile and as discussed
by Hoagland (1975, 1977, p. 403) for the genus
as a whole, the smaller species of Crepidula tend
to have direct development of a few yolky eggs
while the larger species release numerous plank-
totrophic veligers that develop from small eggs.
Caswell (1981), uninformed of Gallardo (1979),
erroneously stated that individuals of Crepidula
dilatata could produce one of two types of eggs:
those that metamorphose within egg capsules
and those that hatch into planktonic larvae. No
known species of Crepidula can produce both
Wesley R. Coe
(posthumous)
'The name Calyptraeidae Blainville, 1824, is also used for
Crepidulidae Fleming, 1 S22, but would need to be made a
nomen conservandum -bd\tor.
types of eggs. The works of Stingley and Coe on
C. maculosa confirm this fact and add to the
foundation of systematics and life history re-
quired for incorporating Crepidula into models
of evolutionary ecology.
Remarks on the Eggs of Crepidula maculosa
by W. R. Coe, 1952 were: ". . . you may add that
a superficial examination of the egg cluster will
show a marked distinction from C fomicata.
Your collection shows that C. maculosa pro-
duces at each ovulation about 10 to 12 gelatin-
ous capsules each containing 8 to 10 large ova
(0.44 mm in diameter) or about 100 in all. C.for-
nicata on the contrary deposits 40 to 70 capsules
each with 120 to 150 small ova (0.17 mm dia-
meter) or 10,000 to 13,000 at one ovulation. The
ova of C. maculosa (we now know) are com-
pletely incubated beneath the parent's foot,
while those of C. fomicata hatch early into free-
swimming veligers."
LITERATURE CITED
Caswell, H. 1981. The evolution of "mixed" life histories in
marine invertebrates and elsewhere. Amcr. Naturalist
117(4):529-536.
Coe, W. R. 1949. Divergent methods of development in
morphologically similar species of prosobranch gastro-
pods. Joun. ofMorphoL 84:383-400.
Gallardo, C. S. 1977. Two modes of development in the
morphospecies Crepidula dilatata (Gastropoda: Calyp-
traeidae) from Southern Chile. Marine Biol. 39:241-251.
1979. Especies gemelas del genero Crepidula
en la costa de Chile; una redescripcion de C dilatata
Lamarck y descripcion de C fecunda n. sp. Studies on
Neotropical Fauna and Environment 14(4):216-227.
Hoagland, K. E. 1975. Reproductive strategies and evolu-
tion in the genus Crepidula (Gastropoda: Calyptraeidae).
PhD. Diss., Harvard University. 360 pp.
1977. Systematic review of fossil and recent
Crepidula and discussion of evolution of the Calyptraei-
dae. Malacologia 16(2):353-420.
Pechenik, J. A. 1979. Role of encapsulation in invertebrate
life histories. Amer. Naturalist 114(6):859-870.
Stingley, D. V. 1952. Crepidula maculosa Conrad. The
Nautihis 65:83-85. pi. 2.
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Volume 96, number 4
THE
NAUTILUS
October 29, 1982
ISSN 0028-1344
CONTENTS
Jules R. DuBar and Susan S. DuBar
A Sinistral Specimen of Scaphella from the
Waccamaw Formation (Early Pleistocene), South Carolina.
Michael A. Zeto
Notes on the Freshwater Mussels (Unionidae) of the
Upper Monongahela River Basin, West Virginia
.125
.127
Edward M. Stern and Cheryl A. Vander Weit
Helix aspersa and Polygyra cereolus. Two Gastropods Introduced into Wisconsin .
Russell J. Barber
The Indigenous Distribution of Elliptio complanata
in Ohio: Archaeological Evidence
.129
,130
C. John Finlay and Danker L. N. Vink
New Records of Cymatiidae (Gastropoda) in the Western Atlantic .
,132
Robert F. McMahon
The Occurrence and Spread of the Introduced Asiatic Freshwater Clam,
Corbicula fluminea (Miiller), in North America: 1924-1982
.134
John W. Ropes
Hermaphroditism, Sexuality and Sex Ratio in the Surf Clam,
Spisula solidissima, and the Soft-shell Clam, Mya arenaria . . .
,141
Billy G. Isom and Robert G. Hudson
In Vitro Culture of Parasitic Freshwater Mussell Glochidia.
147
Becky A. Houck
Temporal Spacing in the Activity Patterns of Three Hawaiian Shallow- water Octopods.
Barry Roth and William K. Emerson
Rediscovery of the Marginellid Gastropod Persicula
tessellata (Lamarck, 1822) on the Pacific Coast of Panama
Notices 161
Recent Deaths.
,152
,156
,151
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124 THE NAUTILUS
October 29, 1982
Vol. 96(4)
Freshwater Snails of Africa and their Medical Importance
by David S. Brown
hor the first time:
A comprehensive account of freshwater snails
in Africa and neighbouring islands.
An exhaustive guide to species
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Published by TAYLOR & FRANCIS LTD, LONDON.
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Vol. 96(4)
October 29, 1982
THE NAUTILUS 125
A SINISTRAL SPECIMEN OF SCAPHELLA
FROM THE WACCAMAW FORMATION (EARLY PLEISTOCENE),
SOUTH CAROLINA
Jules R. DuBar' and Susan S. DuBar
Geoscience Department
Morehead State University
Morehead, Kentucky
ABSTRACT
A sinistral specimen of the volut id gastropod Scaphella floridana brennmortoni
Olsson and Petit was collected from the Waccamaw Formation (Early
Pleistocene) of northeastern South Carolina. This appears to be the first sinistral
specimen of the genus to be recorded froyn the Neogene of Southeastern United
States. The associated shallow water marine faunal assetnblage includes
numerous semi-tropical and tropical species rare elsewhere in the Waccamaw, or
previously knoum only from late Neogene deposits of southern Florida.
A sinistral specimen of the gastropod
Scaphella floridana brennmortoni Olsson and
Petit was collected from the Waccamaw Forma-
tion (Early Pleistocene) of Horry County, South
Carolina (Plate 1, Figures 1, 2). This is the first
recorded occurrence of a sinistral specimen of
the genus Scaphella from the Waccamaw, and to
the authors' knowledge, the first recorded from
the Neogene (post-Oligocene) of eastern United
States. At least three sinistral specimens of the
closely related Scaphella junonia (Lamarck,
1844) are known from the Recent (Abbott, p.
244, 1974).
The sinistral specimen was found in place in
the basal one foot of the Waccamaw where the
formation is exposed along the right bank of the
Intracoastal Waterway, approximately 14.0
miles northeast of Myrtle Beach, South Carolina
(Fig. 1). The enclosing sediment is a slightly in-
durated admixture of very fine to fine quartz
sand (17% by weight), silt and clay (3% by
weight), and calcareous shells (80% by weight).
The lower part of the Waccamaw at this locali-
FIGS. 1-4. Scaphella floridana brennmortoni Olsson and
Petit. 196J,. locality WA 56A--2. Waccamaw Formation (Ear-
ly Pleistocene), Horry County, South Carolina. 1 and 2,
sinistral specimen (height restored: 69.2 mm): 3 and 4, dex-
tral specimen (height 91.2 mm).
\-aj|r •' .
'New address: Bureau of Economic Geology, University Sta-
tion, Box X, Austin, TX 78712.
126 THE NAUTILUS
October 29, 1982
Vol. 96(4)
^ SCAPHELLA LOCALI
'6 ' r-iT
10 Mile
ii-33
FIG. 1. Map showing locality from which sinistral Scaphella
specimen was collected.
ty was deposited below wave base, several miles
offshore. The sedimentation rate was relatively
slow, and turbidity was generally very low.
SaHnity was normal for the open ocean and bot-
tom water temperatures were in the range of
those prevailing today off Southern Florida.
The associated faunal assemblage yielded 30
dextral specimens oi Scaphella (Aurinia) obttisa
(Emmons) and 49 dextral specimens of
Scaphella Jloridana brennmortoni Olsson and
Petit (Plate 1, figures 3, 4). In addition, the
assemblage included numerous semi-tropical
and tropical species rare elsewhere in the Wac-
camaw or previously known only from late
Neogene deposits of southern Florida (Table 1).
The total macrofauna exceeds 250 species
(DuBar, 1965, 1971).
Generally the morphological features of the
sinistral specimen lie well within the observed
range of variation for the species. It is noted,
however, that the sutural slope angle is slightly
greater than that of any associated dextral
specimens.
The height of the sinistral specimen is 62.6
mm, however, approximately 7.0 mm of the
anterior extremity of the columella has been
broken away. The original height of 69.2 mm
places it near the median for all associated
specimens (15.5 mm to 138.9 mm) from the
same locality.
TABLE 1. Invertebrate species associated with sinistral
speciriieii of Scaphella floridana brenmorloni Olsson and
Petit.
Bivalvia
Anadara rustica (Tuomey and Holmes)
Anadara scalarina (Heilprin)
Antigona rugatina (Heilprin)
Area wagneriana Dall
Chama. (Psev-dochama) caloosana Dall
Glycymeris americana (DeFrance)
Laevicardium laevigatum wagnerianum
Olsson and Harbison
Semele leayia (Dall)
Gastropoda
Aesopns slearnsi (Tyron)
Callio.stoma willcoxiayium Dall
Cancellaria venusta Tuomey and Holmes
Diodora caloosaensis (Dall)
Diodora carditella Dall
Fngciolaria cronleyensis Gardner
Fusinus caloosaensis carolinensis Dall
Murex (Chicoreus) floridanus (E. Yokes)
Marex {Facartia) macgintyi (M. Smith)
Murex (Phyllonotus) globosu.s (Emmons)
Plerorhytis conradi Dall
Scaphella floridana brennmortoni
Olsson and Petit (dextral specimens)
Scaphella (Aurinia) obtiisa (Emmons)
Anthozoa
Septastraea crassa (Holmes)
P>hinoidea
Arbiiciii wacca/naw Cooke
I'lypeaster crassus Kier
Encope michelini imperforata Kier
Rhyricholampus sp. cf. R. ayresi Kier
LITERATURE CITED
Abbott, R. T. 1974. American SeaJiells. 2n(l Ed.. Van
Nostrand Reinbold Co., N.Y., 663 p.
DuBar, J. R. 1971. Neogene stratigraphy of the lower
Coastal Plain of the Carolinas. Atlantic Coastal Plain
Geo!. Assoc, 13th Ann, Field Conf., Guidebook: 1-128.
and H. W. C. Furbunch, 1965. The Waccamaw
Formation (Pliocene?) and its macrofauna, Intracoastal
Waterway, Horry County, South Carolina. Geologic Notes.
Div. Geol., South Carolina Development Board, (^ilumbia.
S. C. 9(l):l-24.
Olsson, A. A., and Petit, R. E.. 1964. Some Neogene
Mollusca from Florida and the Carolinas, Bull. Am.
Paleoiit. 47 (217);.i09-.574; 7 pis.
Vol. 96(4)
Oct(.l>er 29, 1982
THE NAUTILUS 127
NOTES ON THE FRESHWATER MUSSELS (UNI()NH)AE)
OF THE UPPER MONONGAHELA RIVER BASIN,
WEST VIRGINIA
Michael A. Zeto
West Virginia Department of Natural Resources
Division of Water Resources
350 North Vance Drive
Beckley, WV 25801
ABSTRACT
During the spring and summer months of 1980, a preliminary survey of the
freshwater mussels of the Upper Monongahela River Basin was conducted. A total
of fifteen species of the family Uyiionidae were found in various tributaries of the
Monongahela River, with only the Asiatic clam, Corbicula fluminea being found
in the mainstem. of the river. Many of the species recorded represent new records
for this watershed.
Information on the extant mussel populations
in West Virginia is extremely limited at this
time. Recent studies in the state were done by
Taylor and Hughart (1981), Morris and Taylor
(1978), and Taylor (1980). These studies were
conducted on the Elk, Kanawha, and Ohio
Rivers, respectively. Bates (1971) attempted a
statewide survey, which represents the only re-
cent study performed on the upper Mononga-
hela River Basin. Earlier studies were per-
formed on the Monongahela River by Rhoads
(1899) and Ortmann (1909). However, these
earlier works were concerned with mussel
populations of the Monongahela River and
tributaries in Pennsylvania.
Study Area
The Monongahela River is formed by the con-
fluence of the West Fork and Tygart Valley
Rivers at Fairmont in Marion County, in north
central West Virginia. The river meanders
northward through Marion and Monongalia
counties over a course of 60.5 kilometers before
exiting the state into Pennsylvania.
Site 1 is located on the West Fork River off
county route 25/3 approximately 1.60 kilo-
meters northeast of West Milford in Harrison
County. The river originates in southwestern
Upshur County and flows in a generally norther-
ly course through Lewis, Harrison, and Marion
counties. The river is 166 kilometers long and
falls at an average of 2.13 meters per kilometer.
Site 2 is situated near the mouth of Hackers
Creek at U.S. route 19 bridge approximately
3.20 kilometers southeast of Goodhope in the
southern portion of Harrison County. Hackers
Creek is a tributary of the West Fork River and
is 37.19 kilometers long. The stream has a
drainage area of 150 square kilometers over its
course through Upshur, Lewis, and Harrison
counties.
Site 3 is located on Buffalo Creek off county
route 1 near Mannington in western Marion
County. Buffalo Creek is 48.90 kilometers long
and has a drainage area of 323.75 square
kilometers. The entire drainage is located within
Marion County and falls at an average of 7.30
meters per kilometer. The stream is the largest
tributary of the Monongahela River in West
Virginia, with the confluence located in North
Fairmont.
Site 4 is situated on Dunkard Creek off county
route 7/28, approximately 1.70 kilometers
northeast of Fentress in northern Monongalia
County. The stream is nearly 56.45 kilometers
in length as it meanders and crosses the state
line six times before it joins the Monongahela
River in Pennsylvania. The stream has a total
drainage area of 588 square kilometers of which
272 are located in West Virginia.
128 THE NAUTILUS
October 29, 1982
Vol. 96(4)
All stream descriptions are taken from the
West Virginia Department of Natural Re-
sources Monongahela River Basin Plan (1981).
Methods
The specimens used in this study were col-
lected by wading the shallow riffles and pools
and hand picking. Empty mussel shells were
also collected in this fashion from sand bars and
the banks of the streams. The shells collected
appeared to have been recently discarded. Each
site was visited at least twice during the study
period in the spring and summer months of
1980. The Monongahela River was brailed in the
fall of 1981 at several locations. No Unionid
mussels were obtained nor were there any signs
of shells along the river banks. Identification of
the specimens collected was aided by the use of
Burch (1975) and were verified by Dr. David
Stansbery, The Ohio State University.
Results
A total of fifteen Unionid species were col-
lected during this study (Table 1). The greatest
diversity was found in Dunkard Creek (site 4)
which supports twelve species. The West Fork
River (site 1) and Hackers Creek (site 2) also had
TABLE 1. MusseLs of the Upper Monongahela Rii'er Basin,
1980.
a fairly diverse population. Freshly discarded
shells oi Corbicula Jlurninea were noted below
the locks and dam at Morgan town. This species
was also flourishing in the West Fork River.
Fusconaia flava represents a new record from
the West Fork River, as it was not reported by
Bates (1971) and there are no records at the ma-
jor museums in the eastern United States (pers.
comm. Taylor, 1981).
All of the mussels collected on Hackers Creek
represent first records, as there are no records
of collection on this watershed nor were any of
the species reported by Bates (1971). This state-
ment would also apply to the three species col-
lected on Buffalo Creek (site 3).
Many of the species taken from Dunkard
Creek are also new records for this watershed in
West Virginia. The following species were not
reported by Ortmann (1909) nor Bates (1971):
Amblema. p. plicata, Simpsonaias ambigua,
Epioblasma triquetra, Fusconaia flava, Pleuro-
bema sintoxia. Elliptio dilatata, and Tritogonia
verrucosa. Other species collected at this site
had been recorded by Ortmann (1909).
It should be noted that two of the species col-
lected appear on the list of Rare and En-
dangered Mollusks of the United States (USFW,
1971). These species are Pleurobema clava from
site 2 and Simpsonaias (formerly Simpsonicon-
cha) ambigua from site 4.
Representatives of the mussels collected in
this survey have been accessioned in The Ohio
State University Museum of Zoology as voucher
specimens.
ACKNOWLEDGMENTS
I would like to extend my great appreciation
to Dr. David Stansbery and Dr. Ralph Taylor for
their valuable time and assistance in identifica-
tion. I would also like to thank the following in-
dividuals for their assistance in collecting:
Denzil Courtney, Sheila Kelley, Jack Mumaw,
Judy Milne Ricketts, and Sheila Zeto.
LITERATURE CITED
Bates, ,1. M. 1971. Mussel Investigations State of West
Virginia, Part I -Section I. U.S. Bureau of Commercial
Fisheries, 91 pp.
Burch, .J. B. 197.5. Freshwater Unionacean C7am,< of North
Vol. 96(4)
October 29, 1982
THE NAUTILUS 129
America. Malacologica! Publications, Hamburg, Michigan.
l:()4 pp.
■Morris, J. S., and R. W. Taylor 1978. A survey of the fresh-
water mussels of the Kanawha River of West Virginia. The
.VaH(i7«s92(4):153-1.5.5.
(.)rtmann, A. E. 1909. Unionidae from an Indian garbage
heap. The Nautiluf: 23(l):ll-l.o.
Rhoads, S. N. 1899. On a recent collection of Pennsylvanian
mollusks from the Ohio River system below Pittsburg. The
Nautilus 12(12):133-137.
Taylor, R. W. 1980. A Survey of the Freshwater Mussels of
the Ohio River from Greenup Locks and Dam to Pitts-
burgh, Pa. L'.S. Army C'orjis of Engineers, Huntington/
Pittsburgh Districts. 71 pp.
Taylor, R. W.. and R. C. llughart 19X1. The freshwater
naia<ls of Elk River, West Virginia with a comparison of
earlier collections. The Ndutihia 95(l):21-25.
llnited States Fish and Wildlife Service, Department of the
Interior 1971. Proceedings of a Symposium on Rare and
Endangered Mollusks (Naiads) of the U.S. 79 pp.
West Virginia Department of Natural Resources, Water
Resources Division 1981. Monongahela River Basin Plan.
414 pp.
HELIX ASPERSA A}^D POLYGYRA CEREOLUS, TWO GASTROPODS
INTRODUCED INTO WISCONSIN
Edward M. Stern and Cheryl A. Vandei Weit
Department of Biolog'y
University of Wisconsin
Stevens Point, Wisconsin 54481
ABSTRACT
Two species of land snails. Helix aspersa and Polygyra cereolus, are reported
for the first time from Wisconsin. Both species were introduced through the com-
■mercial shipment of plants.
Numerous individuals have reported the
spread of both native and exotic mollusks to new
localities throughout the United States via com-
mercially shipped plants. Hanna (1966) summa-
rized molluscan introductions into western
North America while more recently Dundee
(1974) catalogued introduced mollusks of east-
ern North America. Abbott (1950) gave distribu-
tional maps of introduced land and freshwater
mollusks, including Helix aspersa.
During August, 1980, while examining plants
at a local grocery store, the junior author
observed a single subadult Helix aspersa Miiller
crawling on the foliage of the creeping fig, Ficus
pumila. The store manager indicated that all of
their plants were purchased from a single sup-
plier located in Wausau, Wisconsin. It was not
possible to verify conclusively that the snail had
been transported on the fig plant and the owner
of the involved nursery firm noted that occa-
sionally snails and slugs were observed on
plants shipped from California, Texas, and
Florida. Helix aspersa is established and/or has
been intercepted in the latter two states
(Dundee, 1974) and a similar introduction of H.
a.spersa with container grown nursery stock was
reported in neighboring Michigan (Hanna,
1969). With the cooperation of the wholesaler,
the senior author examined the warehouse for
additional specimens. No H. aspersa were
found. Unlike H. pomatia Linnaeus, which at
last report (McClary, 1965) was still established
near Milwaukee, Wisconsin some 25 years after
its introduction (Washburn, 1941), there is no
indication that H. a.'ipersa has become estab-
lished as a breeding population within central
Wisconsin.
However, several individuals of a second
species, Polygyra cereolus (Muhlfeld), were col-
lected within the greenhouse. Unlike//, aspersa.
130 THE NAUTILUS
October 29, 1982
Vol. 96(4)
the natural distribution of P. cereolus is rather
restricted geographically. It inhabits the Florida
Keys and the rim of the peninsula (Pilsbry,
1940). Although the spread of P. cereolus may
not be of economic or regulatory concern and no
established colonies of H. aspersa are known to
occur in Wisconsin, they well illustrate the
dispersal of mollusks is a continuing problem.
Voucher specimens of both species are de-
posited in the University of Wisconsin-Stevens
Point Museum of Natural History.
LITERATURE CITED
Abbott, R. Tucker 1950. Snail Invaders. Natural History
59(2):80-85.
Dundee, D. S. 1974. Catalog of introduced molluscs of east-
ern North America (North of Mexico). Sterkiana 55:1-37.
Hanna, G. D. 1966. Introduced mollusks of western North
America. Occ. Papers Calif. Acad. Sci. 48:1-108.
Hanna, M. 1969. Dispersal of Helix aspersa with container
grown nursery stock. The Nautilus 82:145.
McClary, A. 1965. Helix pomatia in Wisconsin. The Nautilus
79:3,5-,36.
Pilsbry, H. A. 1940. Land Molluscaof North America (North
of Mexico). Acad. Nat. Sci. Phila. Monog. 3. Vol. 1, Pt. 2,
pp. 575-994.
Washburn, R. G. 1941. A Wisconsin colony oi Helix pomatia.
The Nautilus 5i:145.
THE INDIGENOUS DISTRIBUTION OF ELLIPTIO COMPLANATA
IN OHIO: ARCHAEOLOGICAL EVIDENCE
Russell J. Barber
Institute for Conservation Archaeology
Peabody Museum, Harvard University
Cambridge, MA 02138
ABSTRACT
It generally has been concluded that extra-limital records of the freshwater
mussel, Elliptio complanata, in Ohio resulted from species dispersal allowed by
the nineteenth century construction of canals. Faunal remains from a prehistoric
archaeological site suggest that an earlier mechanism of dispersal was in opera-
tion. The potential valv£ of archaeological evidence for zoogeographical studies is
stressed.
The freshwater mussel Elliptio complanata
(Solander in Lightfoot) is distributed widely in
the rivers of the Atlantic Seaboard of North
America, in the rivers and lakes of the Great
Lakes basin, and in a few rivers flowing into the
extreme eastern portion of the Gulf of Mexico.
It generally is excluded, however, from the In-
terior Basin of the Ohio and Mississippi Valleys
(Matteson 1948; LaRocque 1967: 171-172).
In Ohio, Elliptio complanata has been
reported from two localities: Grand River,
Ashtabula County (Ortmann 1919: 103) and
Tuscarawas River, Tuscarawas County (Sterki
1907: 393). The Grand River is part of the Great
Lakes drainage system; the Tuscarawas River is
part of the Ohio River drainage system. The oc-
currence of the species in the Tuscarawas River,
presently unconnected with other rivers from
which Elliptio complanata is known, requires
explanation.
Sterki (1907: 393) suggested that the species
migrated to the Tuscarawas River from Lake
Erie via the Ohio Canal. While recognizing the
possibility of "a very complex and rather un-
Vol. 96(4)
October 29. 1982
THE NAl'TI I. rs 131
likely introduction through drainage changes in
the river system," LaR<icque(1967: 172) favored
the explanation of introduction through nine-
teenth century canals.
These interpretations of the meager evidence
lare hampered by limited time depth for distribu-
tional data. Molluscan remains from prehistoric
archaeological sites, tyj^ically collected and iden-
tified during the course of archaeological
research, can extend that time depth backward
considerably.
The Anderson Village site {33-Wa-4) is located
in Warren County, Ohio, on the banks of the Lit-
tle Miami River, a tributary of the Ohio River.
During the years around 1350 A.D., it was oc-
cupied by Indians of the Fort Ancient Culture.
Excavation at the site by Patricia S. Essenpreis
in 1976 disclosed a series of refuse pits
;"features"), some of which contained several
hundred freshwater bivalve shells, apparently
the refuse remaining from human meals. These
remains subsequently were analyzed and
reported by Barber (1978).
The Anderson Village site produced 10 valves
of Ell iptio complanata, 2 from Feature 10 and 8
from Feature 11. Seven of the 10 valves were
whole or nearly so and all included both hinge
and umbo portions. Preservation of shell was
good and the identifications were routine and
certain.
These remains of ElUptio complanata might
be explained in two ways. First, they might be
claimed to have been imported from the Great
Lakes drainage basin. The distance involved,
however, is one of over 100 kilometers and suc-
cessfully transporting a perishable foodstuff
such a distance would have been impossible. The
shells were found with domestic refuse in-
dicating simple cooking; there was no evidence
of the use of shells for industrial or otlu'r pur-
poses.
Second, the ElUptio complataita might have
been living in the Little Miami River during the
fourteenth century and might have been
gathered locally. This explanation is consistent
with present knowledge of human resource ex-
ploitation and is favored here.
The Anderson Village site remains, thei'el'ore,
suggest that the Euro-American canals might
not have been the mechanism of introduction of
ElUptio complanata to the Ohio Valley, or at
least not the earliest mechanism. Complex river
system changes or even fortuitous transporta-
tion by mobile animals indeed may have been
responsible.
Archaeologists long have sought the advice of
zoologists in the interpretation of the faunal re-
mains they encounter. Though largely untap-
ped, archaeological remains form a data base
which zoologists profitably could use, especially
in zoogeographical studies. Hopefully the future
will demonstrate the mutual benefit of increased
information exchange between the disciplines.
Identification of the mussel was confirmed by
Richard I. Johnson.
LITERATURE CITED
Barl)er, K. J. 197S. Kep<jrt iin iho molluscan fauna from the
Anderson Village site(33-Wa-4). Report on file, Ohio State
Historical Society.
LaKocijue. A. 1967. Pleistocene Mollusca of Ohio. Bulletin.
Ohio Gi'otoyicat Surety. 62(2).
Matteson, M. K. 1948. The taxonomic and distril)Utional
history of the fresh-water mussel Elliptio complanatu.s
(Dillwyn, 1817). The Nautilus ^l(A):\21-\Z2, 62(1):13-17.
Ortman, A. E. 1919. A monograph of the Najades of Penn-
sylvania. Part III: Systematic account of the genera and
species. Carnegie Museum Mevwirx 8(1).
Sterki, V. 1907. A preliminary catalogue of the land and
fresh-water Mollusca of Oliio. Prdceedim/s of the Ohio
State Academy of Science 4(8):3()7-402.
PHILLIP W. CLOVER
IN
O
:OLLECTOR & DEALER
♦fORLD WIDE SPECIMEN
5EA SHELLS p. O. Box 83
Glen Ellen, CA 95442
SPECIALISTS IN RARE
CYPRAEA, CONCS, VOLUTA
MARGINELLA, MITRA. MUREX
REE SHELL AND
!()()K LISTS
Specimen Shells
Offering microscopic and miniature (to '/» inch) shells
from the Florida Keys, unlh accurate locality data. Also
unsorted grunge: urrite for list.
Margaret Teskey
P.O.Bnx273
Big Pme Key. Fl. SSOUS
132 THE NAUTILUS
October 29, 1982
Vol. 96(4)
NEW RECORDS OF CYMATIIDAE (GASTROPODA)
IN THE WESTERN ATLANTIC
C. John Finlay
116 Tanglewood Lane
Newark, Delaware 19711
U.S.A.
and
Danker L. N. Vink
Prinsenweg 73
2242 EC Wassenaar
Holland
ABSTRACT
Since the coverage of the family Cymatiidae /or the Western Atlantic by Clench
and Turner in 1957, and subsequently by Abbott in 197^. a number of new records
in the genera Argobuccinum, Ranella, Charonia, Sassia and Cymatium have
turned up in the Caribbean marine province.
Argobuccinum gemmiferum (Euthyme, 1889)
Cuba- An immature worn specimen was
taken by Jose Fernandez Milera after a severe
winter storm in 1952, washed up on a rocky
shoreline, approximately one mile west of the
fishing village of Camarioca, Matanzas, not far
from Varadero Beach, Cuba.
Brazil-Dr. Luiz Roberto Tostes kindly sent
us an adult specimen taken by a diver alive on
sand, near rocks, at a depth of 40-50 metres,
near Cabo Frio, Ilha dos Pagagaios, State of Rio
de Janeiro. A total of four specimens were taken
near Cabo Frio, the largest measuring 126.5
mm in length, and the smallest 101.4 mm. Two
of these shells are in the collection of Dr. Tostes,
one in the collection of the Museu Oceanografico
de Rio Grande, and the other in the Vink collec-
FIGS. 3 and 4. Argobuccinum gemmiferum (Euthyme, 1889).
Jeffrey's Bay. South Africa, Length: 123 mm.
FIGS. 1 and 2. Argobuccinum gemmiferum (Euthyme, 1889).
Avar Camarioca., Matanzas Prov., Cuba. Length: 62 mm.
F'IGS. h anil ti. Argoliuccinum genunifei-um /£."w//iy///< . ISSU).
Near Cabo Frio. Ilha dos Pagagaios, R. J.. Brazil. Length:
101 mm.
Vol. 96(4)
October 29, 1982
THE NAUTILUS 133
tion. A fifth specimen from Marica, State of Rio
de Janeiro, measuring 1 10.0 mm, was tal<en by a
fisherman in 70-80 metres, and is also in the col-
lection of Dr. Tostes.
Ranella olearium (Linne, 1758)
Brazil-ln June 1973, Matthews, Rios and
Coelho, described a new Brazilian species of
Bur^ifi as 5. harcellosi. The new species was con-
sidered by the authors to be closely related to B.
multinodosa Bucknill, 1927, found in New Zea-
land waters. Certain differing characteristics
however were cited to support the new species,
the most important of which was the lack of nod-
ules on the early post nuclear whorls of B. multi-
nodosa. From a recent examination of the New
Zealand taxon in the collection of the Delaware
Museum of Natural History, co-author Finlay
has been able to determine that the four ex-
amples at the museum revealed nodules on all of
the early post nuclear whorls. As only one
specimen of B. multinodosa was apparently ex-
amined, it could be assumed that that specimen
was worn and the nodules eroded. Later, Rios,
in 1975, considered B. barcellosi as a synonym of
Ranella olearium. Although not so stated by
Rios, it would seem that B. multinodosa must
also appear in the synonomy of olearium..
Eight type specimens of B. barcellosi (i.e.,
Ranella olearium) were dredged in depths from
100 to 280 metres, by the vessels "Mestre
Jeronimo" and "Kosei Maru" from a muddy sand
substrate, at stations off Torres, Solidao, Con-
ceigao and Albardao, all in the State of Rio
Grande do Sul. One of the paratypes was do-
nated to the United States National Museum,
Smithsonian Institution, Washington, D.C.
Bermuda -In recent years. Jack Lightbourn
and Arthur Guest of Bermuda, have taken
several specimens of this species in specially de-
vised deep water traps, set in depths of 120 to
140 fathoms (219-256 metres), VU miles off Cas-
tle Roads, S. E. Bermuda (all shells were dead,
occupied by hermit crabs.) A specimen of the
species has been deposited in the collection of
the Delaware Museum of Natural History. This
species has a worldwide distribution, occurring
in the Mediterranean, West Africa, South
Africa, Australia and New Zealand.
Charonia rubicunda (Perry, 1811)
Brazil -In 1981, Rios and Tostes reported the
presence of Charonia. rubicunda in Brazilian
waters. A total of 18 records were cited, from
Itajai, State of Santa Catarina, to Sao Mateus,
State of Espirito Santo, between 8 and 50 m in
depth. The majority of the specimens, collected
in 1976 and 1977, occurred off Cabo Frio, State
of Rio de Janeiro. Divers reported that the spec-
imens were taken on a sandy bottom near rocks.
This species occurs commonly in Australian
waters.
Cymatium pharcidum (Dall, 1889)
Surinam and Bermuda -DaW described this
species as new in the "Blake Report" from a
specimen dredged off Barbados in 82 fathoms
(150 metres) on a sandy bottom. Clench and
Turner, 1957, considered the species as a syno-
nym of Cymatium krebsi Morch, 1877. Abbott,
1974, suggested that the species might be a
"high spired, finely beaded form of Cymatium
vespaceum (Lamarck, 1822) or may be a valid
species". It is the considered opinion of the
writers that the species is valid. Dr. E. Gitten-
berger of the Rijksmuseum van Natuurlijke
Historie, Leiden, Holland, and D. W. van Veen,
presently have a publication in press redescrib-
ing and reporting this species from 104 to 130 m
off Surinam, some 100 miles north of the
Marowijne river. They compared their speci-
mens with the holotype of C. pharcidum. The
type is illustrated in the forthcoming Compen-
dium ofSeashells by Abbott and Dance (E. P.
DuttonCo., 1982).
Specimens from Bermuda, recently trapped in
120-140 fathoms (219-256 m) I'A miles off Castle
Roads have been taken by Jack Lightbourn.
Specimens from this same source are also in the
Delaware Museum of Natural History and
Finlay collections.
Cymatium trigonum (Gmelin. 1791)
Venezuela -Th\s species had heretofore been
known only from the Eastern Atlantic (Cape
Verde and Senegal, to Benguela (Angola)). J. W.
and F. Gibson-Smith (1970) reported this species
washed ashore after a storm in 1967 near
134 THE NAUTILUS
October 29, 1982
Vol. 96(4)
Caniuri Grande, Federal District, on the north
coast of Venezuela.
Sassia lewisi Harasewych and Petuch, 1980
Mexico and Barbados -Specimens of this
recentl}' described species, were originally
dredged off Contoy Island, Quintana Roo, Mex-
ico, in 60-80 metres, and off St. James, Bar-
bados in 140 metres.
LITERATURE CITED
Abbott, R. Tucker, 1974. American Seashells. 2nd edition.
Van Nostrand Reinhold, N.Y.
Clench, William J. and Turner, Ruth D., 1957. The family
Cvmatiidae in the Western Atlantic. Johnsonia 3(36):
189-244.
Finlay, C. John 1978. Review of the genus Bursa in the
Western Atlantic. The Nautilus 92(4), 147-150.
Gibson-Smith. J. W. and F. Another species of the genus
Cymatium swims the Atlantic. Boletin Informativo. Asoc.
Venezolana de Geologia. Minera y Petroleo. Sept. 1970,
Vol. 13 No. 9.
Harasewych, M. G. and Petuch, E. J. Sassia leufisi. a new
Cymatiid gastropod from the Caribbean Sea. The Nautilus
94(3):121-122.
Matthews, H. R., Rios, E. C. and Coelho, A. C, 1973. Super-
familia Tonnacea do Brasil. V-Nova especie de genero
Bursa Roding, 1798 (Mollusca: Gastropoda) Arq. Cien.
Mar. 13(l):51-56, Junho 1973, Fortaleza, Ceara, Brasil.
Rios, E. C. and Tostes, L. R. Nota sobre a presenija de
Charonia rubicunda em aguas brasileiras (Mollusca,
Gastropoda, Cymatiidae) Lab. de Biologia Marinha, Acad.
Brasileira Ciencia, Rio de Janeiro, 1981.
THE OCCURRENCE AND SPREAD OF THE INTRODUCED
ASIATIC FRESHV^ATER CLAM, CORBICULA FLUMINEA
(MULLER), IN NORTH AMERICA: 1924-1982
Robert F. McMahon
Department of Biology
The University of Texas at Arlington
University Box 19498
Arlington, Texas 76019
ABSTRACT
The distribution and dispersal of Corbicula fluminea (MiUler) in North
America were examined on the basis of all available published reports of new
populations from 192Jt through 1982. The dispersal of C. fluminea in North
America has proceeded from two epicenters of artificial introduction, the first a
result of an introduction from southeast Asia into the no7-thwestern United
States, and the second from a population in the Ohio River (probably a result of
introduction of specimens from populations earlier established in western United
States). The dispersal from these two sites of introduction has been marked by a
progressive invasion of adjacent drainage systems, high downstream rates of
dispersal and inability to breach barriers to dispersal such as mountain ranges.
The very high natural dispersal powers of C. fluminea appear to be associated
with its invasive nature and have been previously overlooked as the basis for this
species' extraordinarily rapid invasion of North American fresh waters.
Corbicula fluminea (Miiller) is a freshwater
clam (Family Corbiculidae) (Newell, 1969)
endemic to southeast Asia (Morton, 1979). This
species was introduced to North America near
the end of the 19th century. It was first re-
corded from the northwest corner of the United
Vol. 96(4)
October 29, 1982
THE NAUTILUS 135
States and has since spread rapidly over many
parts of the United States (Cherry, et nl. 1980a,
1980b). C. fluminea has now been reported in 35
of the continental states, the exceptions being
Montana, Wyoming, North Dakota, South
Dakota, Nebraska, Kansas, New York, Connec-
ticut, Rhode Island, New Hampshire, Maine,
Massachusetts, and Vermont (Cherry, et ai.
1980a, 1980b). It has also been reported from
fresh waters in northern Mexico (Taylor, 1981;
B. Morton, personal communication).
C. fluminea has become an important member
of many benthic communities in North Ameri-
can fresh waters. Its high growth rates and ex-
traordinary reproductive capacity (Aldridge and
McMahon, 1978) allow it to reach very high den-
sities soon after establishment of a new popula-
tion (McMahon, 1983).
By sheer weight of numbers C. fluminea has
become one of the most important aquatic pest
species in the United States. Its shells accumu-
late in and obstruct irrigation canals and under-
ground pipes (Eng, 1979; Fitch, 1953; Ingram,
1959; Prokopovich, 1969; Prokopovich and
Hebert, 1965). It enters and fouls municipal
water treatment facilities (Ingram, 1959;
Sinclair, 1974; Smith, et ai. 1979). C. fluminea
also renders dredged river sand and gravel unfit
for use as aggregation material in cement
(Sinclair and Isom, 1961, 1963). This species has
also been reported to outcompete native unionid
and sphaeriid bivalves, many of which are
presently endangered (Boozer and Mirkes, 1979;
Cooper and Johnson, 1980; Fuller and Imlay,
1976; Gardner, et ai. 1976; van der Schalie.
1973; Sickel, 1973; Taylor and Hughart, 1981).
The most serious aspect of C. fluminea as a pest
species is its ability to foul the service water
systems and steam condensers of electrical
generating stations, causing extensive damage
to equipment and expensive shut-downs for
manual removal of shells (Boozer and Mirkes,
1979; Cherry, et a/., 1980a, 1980b; Diaz, 1974;
Goss and Cain, 1977; Goss, et a/., 1979; Harvey,
1981; Ingram, 1959; McMahon, 1977; Mattice,
1979; Sinclair and Isom, 1961, 1963; Smith, et
'//.. 1979; Thomas and MacKenthum, 1964;
Thomerson and Myer, 1970). Perhaps of even
greater concern, C. fluminea has not only been
reported to foul the steam condensers of nuclear
power stations, but, also, to enter and obstruct
the emergency reactor cooling systems of these
facilities (Parsons, 1980).
While there have been several recently pub-
lished accounts of the distribution of C. fluminea
in the United States (Britton and Morton, 1982;
Cherry, et a/.. 1980a, 1980b), there is little
published information regarding the actual pat-
tern and pace of the spread of this important
pest species in North American fresh waters.
Since its probable introduction by Chinese im-
migrants who may have carried it to North
America as a conveniently transported food
item (Britton and Morton, i979; Counts, 1981),
it has been presumed by the majority of investi-
gators that the spectacularly rapid spread of
this species through North American fresh
waters has been the result of human activities
including; its use as fish bait (Ingram, 1959);
utilization by tropical fish hobbyists as an
aquarium specimen (Abbott. 1975); transport of
juveniles in the bilge water of pleasure craft or
as a tourist curiosity (Britton and Morton,
1979); and, perhaps, unknowingly by fish stock-
ing programs and with transported river sand
and gravel used as cement aggregation material
(Britton and Morton, 1979; Sinclair and Isom,
1961, 1963).
While human mediated dispersal of C. flu-
minea certainly has occurred, investigators ap-
peared to have generally overlooked this
species' great inherent natural powers of disper-
sal which are associated with its invasive habit
and are an apparent adaptation to its preferred
disturbed, highly variable, temporally unstable,
lotic habitats, from which most unionids and
sphaeriids are excluded (Kraemer, 1979;
McMahon, 1983). Indeed, the high dispersal
powers of the genus, Corbicula, are illustrated
by the fact that it has a recent fossil history in
North America and by fossil record and amino-
stratigraphic shell dating evidence that indicate
that a species of Corbicula has reinvaded the
fresh waters of southeastern England during
each of the last three or four interglacial periods
(Miller, et ai. 1978).
If the spread of C. fluminea in North America
was primarily the result of human activity one
136 THE NAUTILUS
October 29, 1982
Vol. 96(4)
would expect that the appearance of new popu-
lations would have a largely random component,
with upstream invasion rates being equal to or
greater than downstream rates, with reports of
new populations occurring in habitats great dis-
tances outside the previously known species'
range and with a marked dispersal of new popu-
lations across natural barriers, as mountain
ranges, that bisect drainage systems. On the
other hand, if the majority of dispersal in this
species was by natural means then dispersal
would be characterized by a steady, progressive
expansion of its range from one closely adjacent
drainage system to the next, with no anomalous
reports of high upstream invasion rates or the
breaching by new populations of natural bar-
riers to dispersal.
In order to better understand the pace, pat-
tern and modes of dispersal of C. fluminea in
North America all available literature on this
species was surveyed for reports of new popula-
tions (primarily in The Nautilus) as part of a
more extensive review of the biology of this
species in North America (McMahon, 1983). The
location of each new population and the date on
which it was first observed were recorded on an
outline map of the United States (Fig. 1). This
information was then utilized in the following
analysis of the distribution and spread of C.
fluminea in North American fresh waters.
The first specimens of C. fluminea found in
North America were recorded as empty shells in
Namaino, Vancouver Island, British Columbia
in 1924 (Counts, 1981). The first living popula-
tion was discovered near the mouth of the Co-
lumbia River separating Washington and
Oregon in 1938 (Burch, 1944) (Fig. 1). From this
apparent point of original introduction, C.
FIG. 1. Occurrence and spread o/Corbicula fluminea in North America from 1924 to 1982. Published population records for C.
fluminea ore indicated by the stars and dates on which they were first obsemed. Probable patterns of dispersal by natural
rneanx are indicated by solid arrows while those pattenm of dispersal axsociated unth human activity and vectors are indicated
hy dashed arrows.
,/ol. 96(4)
October 29, 1982
THE NAUTILUS 137
luminea dispersed throughout North American
fresh waters at an extraordinary rate, primarily
oy successive invasion of adjacent drainage
ystems (a pattern characteristic of dispersal by
aatural means).
C.fluminea spread southwards in West Coast
drainage systems from the Columbia River,
•eaching the San Joaquin River Drainage
System near San Francisco, California, by 1946
Ingram, 1948). By 1952 it was recorded from
Irainage systems in extreme southern Califor-
lia (Fitch, 1953) (Fig. 1). During this period of
southward expansion on the West Coast no C.
luminea populations were reported from east of
,he Rocky Mountains, which formed an effective
larrier to its dispersal (Fig. 1). Only after
•eaching the southern portions of California, did
l.fluminea spread to the east, probably through
i network of interconnecting irrigation canals
nto the Colorado River Drainage System where
t was first recorded in irrigation canals near
Phoenix, Arizona, as early as 1956 (Dundee and
Dundee, 1958). From the Colorado Drainage
System Corhicula spread to the adjacent
irainage system of the Rio Grande River, the
most likely mode of dispersal again being
through irrigation canal systems, where it was
first observed in the Rio Grande River near El
Paso, Texas, in 1964 (Metcalf, 1966) (Fig. 1). C.
tluminea quickly extended its range to the
downstream portions of the Rio Grande, being
reported near the mouth of the river at
Brownsville, Texas, in 1969 (Murray, 1971).
From the Rio Grande the range of C. fluminea
expanded rapidly northwards through several
closely adjacent Texan river drainage systems
reaching northeastern Texas by 1972 (Britton
and Murphy, 1977; Aldridge and McMahon,
1978; Pool and McCullough, 1979) (Fig. 1).
While the range of C. fluminea was expanding
into southern California on the West Coast of
the United States, a second, unexpected infesta-
tion of this species was recorded in 1957 in the
Ohio River, near Paducah, Kentucky (Sinclair
and Isom, 1961, 1963). This anomalous popula-
tion was recorded at a time when the range of C.
fluminea in the western United States had ap-
parently, extended no further east than the Col-
orado Drainage System in Arizona, 3100 km
southwest of Paducah (Fig. 1). As such, it
almost certainly represents an unnatural exten-
sion of the range of C. fluminea in North
America, associated with an, as yet, uniden-
tified human vect(M-. It is highly unlikely that
this new infestation was the result of specimens
being carried to the Ohio River from western
populations by migratory waterfowl as C.
fluminea cannot survive in their digestive tracts
(Dreier, 1977; Thompson and Sparks, 1977).
This artificially introduced population of C.
fluminea in the Ohio River formed the epicenter
of a second major expansion of this species'
range in the eastern half of the United States
(Fig. 1). From Paducah it spread rapidly down-
stream in the Mississippi River, reaching the
lower portions of the river itself and adjacent
Gulf Coastal drainage systems extending into
western Florida as early as 1960 (Dundee and
Harman, 1963; Schneider, 1967) (Fig. 1). The
rapid downstream advance oi C. fluminea in the
Ohio and Mississippi Rivers was almost certain-
ly associated with the ability of its small juvenile
stage (~ 0.2 mm in shell length, Aldridge and
McMahon, 1978) to be passively transported by
water currents (Goss and Cain, 1977; Goss, et
al.. 1979; Sickel, 1979; Sinclair, 1964; Sinclair
and Isom, 1961, 1963; Smith, et al, 1979). As
did the Rocky Mountains on the West Coast, the
Appalachian Mountains seemed to have formed
an effective barrier to the expansion of C. flu-
minea into the drainage systems of the Atlantic
seaboard (Fig. 1). Instead, only after it reached
the lower portions of the Mississippi River, did
the range of C. fluminea expand greatly in an
easterly direction, progressing successively
across the closely adjacent drainage systems of
the lower elevations of the Southern Coastal
Plain, extending into extreme southern Florida,
by 1969 (Clench, 1970). During this period of
range expansion across the Gulf Coastal States,
a second anomalous range extension of C.
tluminea was reported in Lake Overholser,
Oklahoma, in 1969 (Clench, 1972) (Fig. 1). Speci-
mens were taken from this lake long before C.
fluminea had extended into north central Texas
and either represent an incredibly rapid up-
stream expansion in the Arkansas River Drain-
age System, or, as appears more likely, an artifi-
138 THENAl'TIUIS
October 29, 1982
Vol. 96(4)
cial introduction by a liuman vector (Fig. 1).
From the drainage systems of the eastern
Gulf Coastal Plain, C. Jluminea extended into
the adjacent fresh waters of the Atlantic
Coastal States, being reported from the Atlantic
drainage system of Georgia by 1971 (Fuller and
Powell, 1973) and reaching as far north as
Virginia and New Jersey by 1972 (Diaz, 1974;
Fuller and Powell, 1973). Thereafter, the north-
ern expansion of C. Jluminea slowed greatly
with the species still reported to be slowly ex-
tending its range in New Jersey (Trama, 1982).
The present northern limit of C. jluminea in the
eastern United States is marked by a marginal
population in Lake Erie, Michigan, first re-
corded in 1980 (Clarke, 1981) (Fig. 1).
C Jluminea has now probably reached the ex-
tent of its northern distribution in North
America. It is apparently excluded from more
northern fresh waters by its intolerance of low
winter temperatures. Laboratory studies have
shown the absolute lower thermal limit of C.
Jluminea to be 2°C (Mattice and Dye, 1976), a
minimum temperature exceeded by most bodies
of water in the higher latitudes of North
America for several months during the winter.
Indeed, massive mid-winter mortalities induced
by unusually cold ambient water temperatures
(< 2°C) have been reported for a C. Jluminea
population in the Ohio River near Cincinnati
(Horning and Keup, 1964). In this regard, it is
highly significant that populations on the north-
ern edge of the range of C. Jluminea in the
eastern United States appear to be restricted to
and to only survive in areas receiving thermal
discharges from power stations during winter
months (Dreier and Tranquilli, 1981; Eckbald,
1975; Rodgers, et al, 1979; Thomas and
MacKenthum, 1964).
The upstream invasion rate of C. Jluminea ap-
pears to be far slower than downstream rates in
the major drainage systems in which it has
become established (Fig. 1). Of particular in-
terest is the slow upstream expansion of C.
Jluminea in the Ohio River from its point of
probable origin near Paducah, Kentucky,
around 1957, from which it reached the up-
stream limit of its range in the Ohio River
Drainage System in the Kanawha River, West
Virginia, by 1963 (Thomas and MacKenthum,
1964) (Fig. 1). During the same period this
species spread downstream a much greater
distance into Louisiana, Mississippi and
Alabama (Fig. 1). The upstream dispersal of C.
Jluminea in the Mississippi River was similarly
slow, with populations reaching Allamakee
County, Iowa, in the river proper by 1974
(Eckbald, 1975) and Lake Sangchris, Illinois, by
1973 (Dreier and Tranquilli, 1981) (Fig. 1).
If the majority of dispersal of C. Jluminea in
the United States was mediated by human vec-
tors the upstream dispersal rate should be
similar to the downstream rate. Instead, the
downstream rate is many times that of the
upstream rate in most drainage systems,
presumally the result of passive downstream
transport of newly released juveniles over
relatively large distances on water currents.
However, rapid upstream invasion has been
recorded for C. Jluminea in the Tennessee
River, where it was found in the river's upper
reaches by 1959, only two years after it was
recorded at the river's mouth in the Ohio River
in 1957 (Sinclair and Isom, 1961, 1963), in-
dicating that human activity may have been im-
plicated in its dispersal in this drainage system.
It appears that much of the dispersal of C.
Jluminea in North America has occurred by
natural means. It can be demonstrated that
mountain ranges appear to form effective bar-
riers to the extension of the range of C. flu-
minea, and that downstream dispersal rates are
generally much more rapid than upstream rates,
two factors that would not be characteristic of
the more random dispersal patterns that should
be associated with human vectors. Upstream
dispersal may be the result of transport of speci-
mens in fish digestive tracts as many species are
known to feed on smaller (shell length <5.0 mm)
individuals of C. Jluminea (Britton and Murphy,
1977; Dreier, 1977; Grantham, 1967; Ingram,
1959; Rinne, 1974; Sinclair and Isom, 1961,
1963). A more likely vector for the transport of
C. Jluminea are wading shore birds and water-
fowl. Juveniles of C. Jluminea (<5.0 mm shell
length) have been observed to produce a muci-
lagenous byssal thread with which they attach
themselves to sand grains (Kraemer, 1979) and
Vol. 96(4)
October 29. ]!t,S2
THE NAUTILUS 139
particularly to filamentous green algae
(McMahon. unpulilished observations). Such
sand grains and especially filamentous green
algae could easily become attached to or en-
tangled in the feet of wading birds or ducks
(many species of which feed on C. fluminea.
Dreier, 1977; Thompson and Sparks, 1977,
1978) and be subsecjuently transported into
upstream habitats. Obviously, it is also highly
likely that such transport by bird vectors may be
the major mode of dispersal between closely ad-
jacent drainage systems and could, therefore,
along with passive dispersal of juveniles by
water currents, account for most of the rapid
range expansion of this species in North
American freshwaters. In contrast, longer-term
migratory flights would expose juveniles to
lethal levels of desiccation and would, therefore,
prevent transportation across mountain ranges.
Consequently, it appears that while there have
been several obvious instances of human
mediated introductions of C. fluminea into
, North American freshwater habitats, the ma-
jority of the dispersal of this species appears to
have been by natural means from perhaps two
major epicenters of artificial introduction, one
in the Northwest corner of the United States
and a second in the Ohio River. The dispersal of
C. fluminea from these two sites of introduction
has been marked by a steady progression of its
range through adjacent drainage systems,
higher downstream than upstream invasion
rates and the obstruction of its dispersal by
mountain ranges, a pattern of range expansion
generally associated with natural modes of
dispersal.
Of apparent high importance in the rapid ex-
pansion of the range of C. fluminea in North
America is the passive transport of its juvenile
stage over large distances on water currents. In
this regard, human activities in the navigable
waterways of the United States as dredging and
canalization not only appear to jeopardize native
unionid and sphaeriid species (Kraemer, 1979;
McMahon, 1983) but, also, to optimize condi-
tions for passive dispersal of C. fluminea on
water currents.
Certainly, the extraordinary rate at which C.
fluminea has spread through North American
fresh waters (Fig. 1) no longer requires explana-
tions based solely on human vectors. Rather, it
may have occurred primarily by natural means
that are clearly associated with the highly inva-
sive nature of this species and with the remark-
able capacities for dispersal, as evidenced in the
fossil record (Miller, et al. 1979), of freshwater
members of the genus, Corhicida. as a whole.
ACKNOWLEDGMENTS
I wish to express my gratitude to Lori
McDowell and Colette (J'Byrne-McMahon for
their assistance with the preparation of this
manuscript. This research was supported by
grants from the Texas Electric Service Com-
pany and Organized Research Funds of The
University of Texas at Arlington to R. F.
McMahon.
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HERMAPHRODITISM, SEXUALITY AND SEX RATIO IN THE SURF CLAM,
SPISULA SOLIDISSIMA, AND THE SOFT-SHELL CLAM, MYA ARENARIA
John W. Ropes
National Marine F'isheries Service
Northeast Fisheries Center
Woods Hole Laboratory
Woods Hole, Massachusetts 02543
ABSTRACT
In the surf clam, Spisula solidissima and soft-ahMl clam. Mya arenaria, herma-
phroditism is an anomalous condition of eery loiv prevalence (ea. 0.13% for surf
clams and 0.35% for soft-shell clams). No conclusive evidence was found that en-
xnronmental stress caused the condition or influenced the sex ratio, which inis ap-
proximately equal for both .^fiecies.
Accidental functional hermaphroditism in the
dioecious surf clam, Spisula solidissima
Dillwyn, was reported l)y Ropes (1968a) from a
single individual taken from off P'alse Cape,
North Carolina. He pointed out that this anom-
aly is rare, in part because the ^tmadal tissues
142 THE NAUTILUS
October 29, 1982
Vol. 96(4)
must be prepared histologically and examined
microscopically to detect the condition, but
more importantly because the condition is an
unusual deviation from normal gametogenesis
in pelecypods(Pelseneer, 1894; Coe, 1943, 1944;
Galtsoff, 1961). Its rarity suggests that two
additional specimens found recently be docu-
mented.
The discovery of accidental functional herma-
phrodites in species thought to be normally of
separate sexes (unisexual, dioecious, or gono-
choristic) has resulted in speculation about its
cause. A discussion of the condition in surf
clams and soft-shell clams (My a arenaria) is in-
cluded relating possible causes to sexuality and
the sex ratio of the two species.
Methods
The preparation of gonadal tissues for micro-
scopic examination was by standard histological
methods outlined in Ropes and Stickney (1965).
Results
The first hermaphrodite was among 14 dredge
samples and 132 clams collected from off Point
Pleasant, New Jersey, during January to
November 1968 (Fig. 1 A-B). It was found with
four females and five males sampled on August
7 from a 68 ft (ca. 20.7 m) depth about 10 n mi
(ca. 18.5 km) east-southeast of the Manasquan
Inlet entrance (40°00'N Lat., 73°53'W Long.).
The second hermaphrodite was among nine
dredge samples and 87 clams collected during a
June 20 to July 2, 1969 assessment survey (Fig.
1 C-F). It was found with nine females and one
male sampled on June 22 at a 76 ft (ca. 23.2 m)
depth about 24 n mi (ca. 44.5 km) east of Little
Egg Inlet (39°35'N Lat., 73°47'W Long.).
Both specimens were bilateral hermaphro-
dites, as was the earlier example, and gameto-
genesis in testicular and ovarian alveoli was
much like that described for the earlier speci-
men (Ropes, 1968a). A major difference in the
clams reported herein is that the gonads also
contained a trematode parasite of uncertain
identity (Yancey and Welch, 1968). The parasite
can effectively castrate infected clams by in-
filtrating the alveoli. In the hermaphrodites
uninfected alveoli undergoing apparently nor-
mal gametogenesis comprised about 20% of the
gonad; the parasites filled the lumina of remain-
ing alveoli.
DISCUSSION
Hermaphroditism may be a positive evolu-
tionary response by some bivalve species, per-
mitting survival under unfavorable environmen-
tal stress, such as low salinity or fresh water
conditions (Fretter and Graham, 1964). Purchon
(1968) postulated that a delicate balance exists
for the expression of the gonochoristic or her-
maphroditic state in mollusks, and considered
the former a more primitive condition. Further,
he felt that young mollusks have a latent capa-
city to develop in either state; the transition
possibly effected by genetic or environmental
changes.
Direct causality between specific intrinsic or
extrinsic factors and the expression of her-
maphroditism has not been found. Castration
from parasites invading the gonad may upset
the balance between male and female poten-
tialities, but the mechanism is not understood
(Noble and Noble, 1961). Malek and Cheng
(1974) noted that the evidence for true sex
reversal in mollusks suffering from parasitic
castration was inconclusive, because the gonia
for one sex may not be completely destroyed by
parasitic infection. This was the case in the two
infected hermaphroditic surf clams from New
Jersey; cells denoting male and female sex were
observed in development (Figure 1). The
parasite was found in other surf clams that
showed no apparent signs of bisexuality.
Environmental stress has recently been cited
as the possible cause of accidental functional
bisexuality in the soft-shell clam, Mya arenaria
(Otto, 1973). Ten hermaphroditic clams were
found in 1,311 examined from low salinity
(3.0-13.8''/oo) areas of Chesapeake Bay, a
prevalence rate of 0.76% (Otto, 1973). The
Chesapeake clams which are near the southern
limit of their geographic range (Hanks, 1963),
were seriously affected by dilution of the Bay
water after a 1972 hurricane (Shaw and
Hamons, 1974). The hermaphroditic soft-shell
clams studied by Otto (1973) ranged from 50 to
70 mm in shell length and were considered
v'ol. 96(4)
A
October 29, 1982
THE NAUTILUS 143
. 100 ^m
c
D
cf
am
]0 ^m
' *
to tj.f"
FIG 1 SecUon. of the gonad, ofhennaph nMl<lir .urf clams, Spisula solidissima. M Trst^cular (a) and ova-nan
(9) alveoli and duct coviairwm, parasites (p); and (B) parasite tissues and spermatogeritc cells m the darn col-
lected on August 7. 1968. (C) Testicular (^1 and ovarian (9) alveoli and duct contaming parasites (p: (D)
parasite tissues and spermatogenic cells: (E) oogenic cells; and (F) spermatogemc cells in the rl,u„ collected on
June 22. 1969. A scale of magnification is in the left hand comer of each photograph.
144 THE NAUTILUS
October 29, 1982
Vol. 96(4)
adults (Otto, personal communication). Coe and
Turner (1938) found "no evidence of protandry
or change of sex" in the species, but did find
three hermaphrodites in over 1,000 examined
from New Haven, Connecticut, and reported a
prevalence value of less than 0.5% (Table 1);
Shaw (1970) found one in 36 from Umpqua Bay,
Oregon, a prevalence of 2.8%; and Porter (1974)
found one in 1,785 from Skagit Bay, Washing-
ton, a prevalence of 0.00056%. Other investiga-
tors have examined many (ca. 5,600) soft-shell
clam gonads without finding any hermaphro-
dites (Ropes and Stickney, 1965; Pfitzenmeyer,
1965; Shaw, 1962, 1965; Brousseau, 1978; Table
1). The prevalence of hermaphroditism from all
these observations is 0.35%.
Although soft-shell clams are generally con-
sidered to be a gonochoristic species, Coe and
Turner (1938) observed that "the differentiated
young gonad shows some indications of bisex-
uality" and their figure 17 includes "ovocyte-
like" cells in the spermary of a young clam. If, in
fact, the potentialities for both sexes exist in the
gonads of young soft-shell clams and extrinsic
conditions cause hermaphroditism, then it can
be theorized that the population sex ratio might
also be affected. The sex ratios of gonochoristic
species are generally thought to approximate
equality and, thus, the observed frequency in
samples can be subjected to goodness of fit
tests.
The highest per-sample prevalence (4-8%) oj
hermaphroditic soft-shell clams was reported bj
Otto (1973); a sex ratio of 1:0.82 males tc
females was noted in these samples. No signifi-
cant differences (P>0.05) in the sex ratio,
however, were detected in any of the sets ol
samples. Thus, an imbalance in the sexuality ol
these clams was not observed.
The hermaphroditic surf clam found in 196J
and 1969 were from the environmentallj
stressed New York Bight area, which has and i;
being intensively studied to identify th«
ecological effects of waste disposal practices
(Gross et al., 1976). Although the impact o:
these spoils on the surf clam resource in this
region is not well understood, sublethal effects
are suspected to have important impact on som(
or all life stages of marine animals, possibly in
fluencing survival, normal growth, and othei
physiological processes related to disease anc
parasitism (Sindermann, 1976). High incidences
of chromosome or mitotic irregularities hav(
been found in developing mackerel eggs fron
the area (Longwell, 1976). Surf clams are non
migratory, sedentary, and infaunal creatures
They cannot avoid the impact of contaminants
Environmental stress has occurred in th(
TABLE 1. Observations of henna pli >•< ifli f ism in tht> soJl-shi'lJ clum. Mya arenaria.
Location
No. clams
examined
No. hermaphro-
dites
Reference
New Haven, Conn.
Tred Avon R. , Md.
Patuxent R. , Md.
Maine to Mass .
Umpqua Bay, Oreg.
ChQ,sapeake Bay
Skagit Bay, Wash.
W. Gloucester, Mass.
3l. 96(4)
October 29, 1982
THE NAUTILUS
ea. Anoxic conditions off the New Jersey
ast in 1976 resulted in the loss of a larjje por-
)n (144,672 metric tons of meats and 61.5%) of
e surf clam biomass (Ropes et al. 1979). Ogreii
d Chess (1969) observed mortalities of surf
ims and other marine animals related to anox-
around wrecks and reefs off New Jersey in
68.
Environmental stress affecting the survival of
rf clams in the New York Bight might cause
jtagenesis and sex ratio imbalances. Data
)m observations on 2,307 gonadal tissues of
rf clams were available from several sources:
samples taken during 1962-1965 to study the
reproductive cycle of the clam in offshore New
Jersey waters (Ropes, 1968b); and from loca-
tions off Long Island, NY, to off Virginia, 42
samples taken during surveys in the spring and
fall of 1965; 35 samples taken in 1968; and 9
samjiles taken in 1969 (Table 2). In general, the
hyjHithesis of an equality in the .sex ratio of surf
clams can be accepted, based on the combined
totals and chi-square test results of all but three
1969 samples. These latter, taken off I'oint
Pleasant, NJ, are an exception, since the dif-
ferences in sex were highly significant
(X^= 10.36; df=2; P>.01)-78.6%' of the clams
were females; 17.9% were males; and 3.6% her-
TABLE 2. The sex ratio ofsurfrliniis (Spi.sula S(]li(li.ssiiiia).
1/ Includes a hermaphrodite in the total.
146 THE NAUTILUS
October 29, 1982
Vol. 96(4)
niaplirodites. However, the sample size may
have been too small to make the test statistically
conclusive (Dixon and Massey, 1957). The
prevalence of hermaphroditism in all of the
samples was a low 0.13%; the sex ratio was
1:1.0645 males to females.
ACKNOWLEDGMENTS
I wish to thank Drs. Diane J. Brousseau of
Fairfield University, Fairfield, Connecticut,
Saul B. Saila of the University of Rhode Island,
KinjTston, Rhode Island, and Fredric M. Ser-
chuk of the National Marine Fisheries Service,
Northeast Fisheries Center, Woods Hole, Mass-
achusetts, for their critical reviews and helpful
comments.
LITERATURE CITED
Brousseau, D. J. 1978. Spawning cycle, fecundity and
recruitment in a population of Mya arenaria (soft-shell
clam) from Cape Ann, Massachusetts. U.S. Fish. Bull.
76:1.5,V166.
Coe, W. R., and H. J. Turner, Jr. 1938. Development of the
gonads and gametes in the soft-shell chim (Mya iirenariiil.
Jour. Morjih. 62:91-111.
Coe, W. R. 1943. Se.xual differentiation in mollusks. I. Pole-
cypods. Quart. Rev. Biol. 18:1.54-l(i4.
1944. Sexual differentiation in mollusks. II. Gas-
tropods, Amphineurans, Scaphopods, and Cephalopods.
Qtiart. Rn: Biol. 19:8r)-97.
Dixon, W. J., and F. .1. Massey, .Jr. UI.ST. Iiilroi/iirlinn hi
Statistical Amily.'<is. McGraw-Hill [?ook Co.. Inc., N.Y.
488 p.
Fretter, V., and A. (Jraham 1964. Reproduction. In: Wilbur.
K. M. and C. M. Yonge (eds.) Physiology of Mollusca.
Academic Press, N. Y. Vol. 1, p. 127-164.
Galtsoff, P. S. 1961. Physiology' of reproduction in molluscs.
Amer. Zool. 1:273-289.
Gross, M. G., R. L. Swan.son, and H. M. Stanford. 1976.
Man's impact on the middle Atlantic continental shelf and
the New York Bight- Symposium summary. In: (iross, M.
G. (ed.) Middle Atlantic Continental Shelf and the New
YiTk Bight. Amer. Soc. Limnol. Ocfanogr.. Inc.. Spec.
Symp. Vol. 2, p. 1-13.
Hanks, R. W. 1963. The soft-shell clam. r..S. Fish and Wihll.
ScTiK. Circ. 162, 16 p.
Longwell, A. C. 1976. C'hroniosome mutagenesis in develop-
ing mackerel eggs sampled from the New York Bight. In:
Gross, M. G. (ed.). Middle Atlantic Continental Shelf and
the New York Bight. Amer. Sue. Limnol. Oceanoyr.. Inc..
Spec. Symp.. Vol. 2, p. 337-339 (Abstract).
Maiek, E. A., and T. C. Cheng. 1974. Medical and Economic
Malacology. Academic Press, N.Y. 398 p.
Nohle, E. R., and G. A. Noble. 1961. Parasitology. The
Biology of Animal Parasites. Lea and Febiger, Phila.
767 p.
Ogren, L., and ,J. Chess. 1969. A marine kill on New Jersey
wrecks. Underwater Naturalist. 6(2):4-12.
Otto, S. V. 1973. Hermaphroditism in two species of
pelecypod mollusks. Proc. Natl. Shellfish. Assoc.
63:96-98.
Pelseneer. P. 1894. Hermaphroditism in molluscs. Quurl.
.lour. Micros. Soc. 37:19-46.
Pfitzenmeyer, H. T. 1965. Annual cycle of gametogenesi.^ ■ ;
the soft-shell c\am,Mya arenaria. at Solomons. Maryland.
Chesapeake Sci. 6:.52-.59.
Porter, R. G. 1974. Reproductive cycle of the soft-shell clam,
Mya arenaria. at Skagit Bay, Washington. F(sA. Bull. 72:
648-656.
Purchon, R. D. 1968. The Biology of the Mollusca. Pergamon
Press, Oxford. 560 p.
Ropes, J. W., and A. P. Stickney. 1965. Reproductive cycle
of Mya arenaria in New England. Biol. Bull.
128:315-327.
Ropes, J. W. 1968a. Hermaphroditism in the surf clam,
Spisula solidissinia. Proc. Natl. Shellfi.'<h. Assih-.
58:63-65.
1968b. Reproductive cycle of the surf clam.
Spisula solidissinia. in offshore New Jersey. Biol. Bull.
135:349-365.
Ropes, J. W., A. S. Merrill, S. A. Murawski, S. Chang, and
C. L. MacKenzie, Jr. 1979. Chap. 11. Impact on clams and
scallops. Part 1. Field survey assessments. In: Swanson,
R. L., and C. J. Sindermann (eds.) Oxygen depletion and
associated mass mortalities in the New York Bight.
A'0.4.4. Prof Paper 11, p. 263-275.
Sindermann, C. J. 1976. Effects of coastal pollution on fish
and fisheries- with particular reference to the Middle
Atlantic Bight. In: Gross, M. G. (ed.). Middle Atlantic Con
tinental Shelf and the New York Bight, Amer. Soc. Lim-
nol. Oceanogr.. Inc.. Spec. Symp.. \'ol. 2. p. 281-301.
Shaw. W. N. 1962. Seasonal gonadal changes in female sol't-
shell clams, Mya arenaria. in the Tred Avon Ri\i-i-,
Maryland. Proc. Natl. Shcllfi.'^h. .4.s.soc. 53:121-132.
1965. Seasonal gonadal cycle of the male soft-
shell clam, Mya arenaria, in M,-u-yland. L'.S. Fish Wildl.
Serv., Spec. Sci. Rep. Fish. 508, 5 p.
1970. A hermaphroditic soft-shell clam. .Mn"
arenaria. from IJmpqua Bay. Oregon. Res. Rcpts.. Fi.^h.
Comm. Oregon. 2:100-102.
Shaw. W. N. and F. Hamons 1974. The present status of tlic
soft-shell clam in Maryland. Proc. Natl. Shellfish. Asso,:
64:38-44.
Yancey. R. M.. and W. K. Welch 19(;s. Tlu' Atlantic coasi
surf clam- with ,a partial liililiivgra|)hy. r..S. Fish Wihll.
Sere. Circ. 288, 14 pp.
Vol. 96(4)
October 29, 1982
THE NAUTILUS 147
IN VITRO CULTURE OF PARASITIC
FRESHWATER MUSSEL GLOCHIDIA
Billy G. Isom
Division of Water Resources
Office of Natural Resources
Tennessee Valley Authority
Muscle Shoals, AL 3566o"
and
Robert G. Hudson
Associate Professor of Biology
Department of Biology
Presbyterian College
Clinton, SC 29325
ABSTRACT
Ellis and Ellis (1926 and 1930) reported fnnusformation of fresh water mussel
glochidia in vitro culture. However, their methodology was never published. This
report gives a new method for the in vitro culture of mussel glochidia to juveniles
rather than by their natural fish host encystmmt. The medium consists of
physiological salts, amino acids, glucose, vitamins, antibiotics, and a nonspecific
component offish blood plasma. The relative concentration offish plasma re-
quired for optimum, results was S3 percent. In vitro culture may prove very
beneficial in reestablishing the populations of endangered mussels, management
of species used by the pearl culture industry, and culturing of stocks for bioassays,
genetic studies, or other uses.
Application of in vitro culture for the purpose
3f sustaining endangered mussels of commercial
mportance is obvious, since usually an unknown
'ish host is required for larval development in
lature. The female mussel has her eggs fertil-
zed by sperm cells which are released into the
vater by a male mussel and travel into the
'emale with water taken in during filter feeding.
The fertilized eggs, contained in the female's
jills, develop into simple glochidia, or larvae,
■onsisting primarily of two shells, mantle cells,
ind one adductor muscle. The glochidia are
•eleased and encyst in a specific fish tissue,
isually the gills. Development of glochidia into
uveniles (transformation) in an artificial
nedium would help endangered mussels, since
he fish host required for most of these species is
mknown and would be difficult to determine,
^he fish host of some species may even be extir-
lated. Use of in vitro culture could sustain a
pecies until its fish host could be found or the
tbsence of a host availability determined. Even
nussels with a known fish host could be reared
or commercial or scientific purposes.
Freshwater mussels have been used commer-
ially for manufacturing buttons and presently
is nuclei for cultured marine pearls. J'hey are
also currently being used for the culture of
freshwater pearls in the United States. Over-
harvesting as a result of demand for shells has
contributed significantly to the decline of
freshwater mussel resources in the United
States over the past three decades. Historically,
over 500 of the more than 1000 world species of
freshwater mussels occurred in the United
8n-211-200X LIGUHIA RECTA
FK;. 1. Cliii-lniliiil n}icU of tkrj're.'ih water miissti l.iuuniia
recta (Iciiijtii JfiO \ini).
148 THE NAUTILUS
October 29, 1982
Vol. 96(4)
States. Many species are now thought to be ex-
tinct; others are listed as threatened or en-
dangered by individual states or the United
States Government.
Ellis and Ellis reported in 1926 that they had
successfully obtained transformation of parasi-
tic glochidia of freshwater mussels in physio-
logical nutrient solutions. However, neither the
composition of the media nor the process used
was ever published. In addition, unlike the pre-
sent study, Ellis and Ellis excised the glochidia
they used from a known fish host, an action
which undoubtedly contributed to their reported
success.
Composition of our artificial medium include
salts which are modified from the "unionid
Ringers" solution proposed by Ellis et al. (1930)
and are shown in Table 1. The essential modifi-
cation of the solution includes the deletion of
K^HPO. and the addition of 2.2 gm NaHCOj per
1000 milliliters of solution. The NaHCOj was re-
quired in order to regulate the pH with varying
atmospheric CO2 concentrations.
TABLE 1. Sdlt.'i contained in stock artificial glochidial
medium.
Compound
CaCU
MgCli.eH.O
NaCl
KCl
NaHCO,
Concentration
(mg/L)
1200
1000
1530
99
2200
The amino acids in the artificial medium are
the same as those used by Eagle (1959) for cell
and tissue cultures with the exception of the ad-
dition of taurine and ornithine which are consti-
tuents of fish blood. The essential amino acids
are shown in Table 2, the nonessential amino
acids in Table 3.
The vitamins present in the complex artificial
growth medium, the same as those used by
Eagle (1959) for cell and tissue cultures, are
shown below in Table 4. The antibiotics and
antimycotic used in the artificial medium are
listed in Table 5; other compounds are shown in
Table 6.
Plasma was obtained from fish blood which
TABLE 2. Essential amino acids contained in stock artifi-
cial gluchiiiial medium.
Concentration
ImgIL)
105
24
31
52
52
58
15
32
48
10
36
46
TABLE 3. Nonessential amino acids contained in stock ar-
tificial glochidial medium.
Compound
L - alanine
L - aspara^ne
L - aspartic acid
glycine
L - glutamic acid
L ■ proline
L - serine
taurine
L - ornithine
Concentration
(mg/L I
8.9
13.2
13.3
7.5
14.7
11.5
10.5
31.0
10.0
TABLE 4. Vitamins contained in stock artificial glochidial
medium.
Compound
choline chloride
folic acid
inositol
nicotinamide
calcium pantohthenate
pyridoxal
riboflavin
thiamine
Concentration
(mg/L)
1.0
1.0
2.0.
1.0
1.0
1.0
0.1
1.0
was removed from the fish by heart puncture
with a sterile heparinized syringe (the syringe
chamber was coated with a sodium heparin solu-
Vol. 96(4)
October 29, 1982
TABLE 5. The antibiotics and antimycotic contained in
stock artificial glochidial medium.
Compound
Antibiotics
Carbenicillin
Gentamicin sulfate
Rifampin
Antimycotic
Amphotericin B
Concentration
100 uglml
100 f/g/ml
100 i^glm]
5 ng/ml
TABLE 6. Other compounds contained in stork artificial
glochidial medium.
Compound
Glucose
Phenol red (optional)
Concentration
(mg/L)
1000.0
10.0
tion of 1000 U/ml) having an 18 gauge needle.
The blood was centrifuged at 1000 rpm in a
refrigerated centrifuge for 10 minutes followed
by 3000 rpm for 10 minutes, decanted into
sterile centrifuge tubes, and centrifuged for
another 10 minutes. The plasma was removed
by aspiration, then frozen and subsequently
sterile filtered. The antibiotics and antimycotic
were added to the plasma in the same concen-
tration as shown in Table 5, at time of use.
Glochidia from gravid female mussels were
obtained by utilizing sterile surgical instruments
to remove the gills containing glochidia, then
the gills were placed in sterile deionized water.
rhe glochidia were excised from the gills by sec-
tioning and then swirling the gills in the deio-
aized water.
The glochidia were washed several times with
ieionized water by decanting or aspirating the
A'ater following swirling of the beaker contents.
The healthy glochidia settled, allowing the
-emoval of tissue debris, dead glochidia,
jacteria, and protozoa. The glochidia were left
n the last rinse water until they were removed
vith a Pasteur pipette and placed in the growth
nedium. A representative scanning electron
photomicrograph of a glochidium of Ligumia
•ecta (Lamarck, 1819) is shown in Figure 1.
Different components and concentrations of
he growth medium were tested to determine
vhich combination would stimulate and best
THE NAUTILUS 149
1
FIG. 2. Transformed juvenile of the freshwater mussel
Ligumia recta, 39 days old, in lake water. Note the pro-
truding ciliated foot.
FIG. 3. Growth of juvenile Ligumia recta, 75 days in
culture, 13 days in water (dark field), a total of 28 days. End
view showing protruding foot in center.
FIG. 4. Growth of juvenile Lampsilis ovata, 22 days culture,
9 days in lake water (dark field), a total of 31 days old.
150 THE NAUTILUS
October 29, 1982
Vol. 96(4)
support glochidial transformation. Nuniorical
comparisons of different cultures were difficult
to evaluate because the varying stages of devel-
opment in, as well as the number of, glochidia.
The presence of bacteria in initial cultures in
1981 further confounded the accuracy of numer-
ical culture evaluations. Many cultures failed to
yield fully transformed glochidia because of
bacterial infections, even though most glochidia
had good initial development prior to their con-
tamination. Experiments in 1982 with the new-
antibiotics shown in Table 5 have been much
more successful.
Only two different salt solutions, unionid
Ringers (Table 1) and Earles' balanced salt solu-
tion (Earle, 1943), were compared in experi-
ments. Glochidia transformed in both salts, even
though the amino acids used in conjunction w ith
each varied slightly. Because parasitic glochidia
are surrounded by fish cells, and since Earles' is
the salt solution most commonly used in fish cell
culture medium (Wolf and Quimby, 1969), glo-
chidal adaptation for life in Earles' salt concen-
trations as well as in unionid Ringers would be
expected.
Different groups of amino acids were tested in
cultures to get transformation, but elimination
of nonessential, single, amino acids has not been
attempted to date. In earlier experiments with
the medium being 20 percent artificial, the
amino acid content seemed less important, prob-
ably because the 80 percent plasma had the nec-
essary concentrations of amino acids. The artifi-
cial growth medium was formulated to include
all free amino acids which had been found in
three species of catfish (Iddlurus furcates, I.
punctatus. and Pylodictis olivaris) (Johnson,
1971). All of the amino acids which had been
found in fish blood could also be found in equal
or higher concentrations in Eagles' essential
and nonessential amino acids if taurine and
L-ornithine were added. The only amino acid
found in Eagles' amino acid group which was
not found in the catfish blood was L-trypto-
phane. Since Eagles' amino acids could be pur-
chased premixed, this combination was used
along with taurine and L-ornithine in the suc-
cessful in vitro medium. Medium 199, which also
has 21 amino acids (Morgan et al., 1950), was
sufficient for glochidial transformation. Medium
199 has the same 12 essential amino acids as
Eagles' medium; however, medium 199 is lack-
ing 4 of the 9 nonessential amino acids which
had been used. This would indicate that these
four (L-alanine, L-asparagine, L-ornithine, and
taurine) were not necessary for glochidial
development. Even though development occur-
red in both media, the development rate was
faster in Eagles' amino acids with taurine and
L-ornithine than in medium 199.
Fish blood plasma was found to be necessary
to stimulate development in all mussel species
tested. Other massive protein components,
specifically fetal bovine serum, bovine serum,
and lobster hemolymph, were tested and found
unsuccessful. Although earlier tests indicated a
positive correlation between percent transfor-
mation and percent fish blood plasma in the
medium, 33-1/3 percent blood plasma was
adopted in our standard medium as producing
satisfactory yields at a more economical level.
Earlier cultures of Legumia recta were placed
in unfiltered plasma which contained several
blood cells. First observations seemed to in-
dicate that development was enhanced by the
presence of these cells. The glochidia were held
in a matrix of cells and fibrin on the dish and
developed rapidly. Subsequent media changes
were made using filtered plasma to prevent a
buildup of cells in the culture. Conversely, later
cultures with Fusconaia ebena (Lea, 1831) did
not show any indication of enhancement by the
presence of these cells. In fact, cultures with un-
filtered plasma suffered a higher rate of con-
tamination which resulted in a lower yield. More
work is needed in this area, but the presence of
the fish cells does not appear to be necessary for
glochidial development.
The pH of the medium varied from ca. 7.3 to
8. 1; however, the lower pH promoted best trans-
formation in at least one species. Cultures of
Fui^conaia ebena developed much better in a pH
range of 7.3 to 7.4 rather than 7.8 to 8.0. For ex-
ample, in eight different cultures of F. ebena. 16
of 26 culture dishes contained transformed
juveniles after 18 days at a pH of ca. 7.3, where-
as none of an identical set of 26 cultures were
alive at 11 days when cultured at a pH of ca. 7.9.
V()l.%(4)
(MoIht 29, 1982
THE NAUTILUS 151
Bacterial infection was present in cultuix's at
both pH levels and was responsible for much vi'
this loss; however, many of the higher pH
cultures died even when bacterial action was
minimal, while infections in the lower pH
cultures did not result in death of the entire
culture. The lower pH level appeared to either
make it easier to control bacterial contamina-
tion or minimize the detrimental effects of the
bacteria. Subsequent experiments have corro-
borated that a pH of 7.3 is optimum.
The use of antibiotics and their concentrations
varied with the presence or absence of bacteria
in the medium. €arbenicillin, usually added to
yield lOU i^glm\, can be increased to as high as
500 ^iglm\ without apparent inhibition to the
glochidial development. Gentamicin sulfate and
Rifampin can also be increased from lOU f.ig/ml
to 500 figlml safely, and the antimycotic, Am-
photericin B (Fungizone) from 5 to 25 Mg/'ii'-
These antibiotics and antimycotic, along with
rinsing and changing infected glochidia to new
media and dishes, usually would control con-
tamination successfully. Older glochidia could
withstand infection much longer than younger
glochidia.
The medium was kept at 23°C but cultures
were successful, to a lesser extent, even at
28°C. Higher temperature did reduce the yield,
as shown by the comparison of glochidia of
Ligurnia recta which developed in 23°C and
28°C. Using six culture dishes grown in 60 per-
cent plasma, three grown in 23°C had an
average yield of advanced glochidial develop-
ment equal to 48.8 percent (Sx = 8.7), while
those grown at 28°C averaged 18.8 percent
(Sx = 3.3). A transformed glochidium of Ligurnia
recta is shown in Figure 2.
During the spawning season of 1982, these
variables have been refined to a greater degree,
resulting in successful mass culturing of
glochidia (some cultures averaging as high as 80
percent transformation). These successes will
provide opportunity for conservation of many
mussel species including endangered species,
and the management of others. Kfficacy of the
process to date includes transformation of
glochidia of six genera and species representing
two subfamilies of Unionidae, the Unioninae
and Lampsilinae.
A growth stage of a juvenile Ligmia recta is
shown in Figure 3 and that of a Lampsilis ovata
in Figure 4.
LITERATURE CITED
Eagle, H. 1959. Amino acid metabolism in mammalian coll
cultures. Science 130:432-437.
Earle, W. R. 1943. Production of malignancy in vitro. IV.
The mouse fibroblast cultures and changes seen in the liv-
ing cells. Jour. National Cancer Institute 4:165-212.
Ellis. M. M. and M. D. Ellis. 1926. Growth and transforma-
tion of parasitic glochidia in physiological nutrient solu-
tions. Science 54(1667):579-58(l.
Ellis, M. M., A. D. Merrick and M. 1). f:ilis. 1930. The blood
of North American freshwater mussels under normal and
adverse conditions. Bulletin of the Bureau of Fisheries
56, Bur, of Fisheries Doc. No. 1097:509-.542.
.Icihnson, C. L. Unpublished. U.S. Dept. of the Interior,
Bureau of Sport Fisheries and Wildlife, Cook, Wash.,
1971. In: Biology Data Book. P. L. Altman and D. S.
Dittmer (eds.). Federation of American Societies for
Experimental Biology. Bethesda, Maryland, 1974.
Morgan, J. F., H. J. Morton and R. C. Parker. 1950. Nutri-
tion of animal cells in tissue culture. I. Initial studies on
a synthetic medium. Proc. Soc. Exper. Biol. Medicine
73:1-8.
Wfilf. K. and M. C. Quimby. 1969. Fish cells in tissue culture.
//(. Fish Physiology. W. S. Hoar and D. J. Randall (eds.).
\(il. Ill, Academic Press. New York. pp. 253-301.
Recent Deaths
We regret to announce the death of our dear
friend, Katherine Van Winkle Palmer, former
Director of the Paleontological Research Insti-
tution, of Sept. 12, 1982. at the age of 87. Con-
tributions to her memorial fund for P.R.I, may
be sent to Dr. Raymond Van Houtte, Tompkins
County Trust Co., Ithaca, NY 14850. An
obituary is in prepartion.
Meeting
The Eighth International Malacological Con-
gress, sponsored by the Unitas Malacologica,
will be held in Budapest, Hungary, in 1983, from
August 29 - September 3. Further information
may be obtained by writing Dr. Laszlo Pinter,
Natural History Museum, Baross u. 13, H-1088
Budapest, Hungary.
152 THE NAUTILUS
October 29, 1982
Vol. 96(4)
TEMPORAL SPACING IN THE ACTIVITY PATTERNS OF
THREE HAWAIIAN SHALLOW-WATER OCTOPODS
Becky A. Houck
Dept. of Physical and Life Sciences
University of Portland
5000 N. Willamette Boulevard
Portland, OR 97203
ABSTRACT
Th-ee species of Haw ana h, octopods show distinct iocoinotor activity rhythms in
the laboratory and in the field. The periods of peak activity are species-specific
even in isolation. This temporal spacing ayid differences in preferred
microhabitats during periods of inactivity ynay limit interspecific competition
for food and home sites and reduce the incidence of predation. Inactive Octopus
ornatus superficially behave like vertebrates in sleep.
Animals occupying similar niches in the same
geographical area may reduce competition by a
variety of spacing mechanisms. Three species of
shallow-water octopods can be collected on the
same fringing reef flats off the south shore of
Oahu, Hawaii, throughout the year. Data are
presented indicating that these three species
show temporal spacing in locomotor activity
patterns. Observations in the field and in
aquaria also suggest utilization of different
microhabitats on the reef flat for use as refuges
during periods of inactivity.
Methods
Animals were collected by netting during low
tides on shallow reef flats off the south shore of
Oahu, Hawaii. 0. cyanea Gray was collected
before dusk and transported to the Hawaii In-
stitute of Marine Biology, Kaneohe Bay, Oahu.
Specimens of 0. ornatus Gould and the "cres-
cent octopus," a small undescribed Hawaiian
octopod (Houck, 1977; reference specimens:
Department of Invertebrate Zoology, Santa
Barbara Museum of Natural History) were col-
lected at night and maintained at the Bekesy
Laboratory of Neurobiology, University of
Hawaii.
Locomotor activity rhythms of four (). orna-
tus and twelve crescent otopuses were moni-
tored in isolation under controlled laboratory
conditions for periods of one to six months per
animal. Locomotor acitivity rhythms of each
animal were recorded under a variety of light-
dark regimes. Only typical activity patterns
under light-dark conditions similar to timing of
field illumination are reported here. An
ultrasonic activity monitor allowed continuous
recording of all movement of an animal within a
light-tight aquarium. Data were read by a DEC
PDP 11/10 computer and stored on cassette
tape for later analysis. A complete description
of the monitoring system is provided elsewhere
(Akaka and Houck, 1980). The animal within the
aquarium was exposed to an artifical light il-
lumination with light intensity of 7.5 watts/m^
an average value at 0630 hours in a typical oc-
topus habitat (Franzisket, 1969). Hourly activity
values were computed as a percentage of the
mean hourly activity for a monitoring run.
The larger size of specimens of 0. cyanea did
not permit use of the ultrasonic monitoring
system since the animals were too large for the
aquaria. Activity of 0. cyanea was recorded by
providing the animal with a single cinderblock
"refuge" within a 6 foot trough functioning as
part of an open sea water system at the Hawaii
Institute of Marine Biology. The cinderblock
"refuge" was equipped with a trap door bottom
that was activated when the animal retreated in-
to the depression of the block. A multichannel
event recorder documented time spent inactive
within the refuge. Hourly activity values were
Vol. 96(4)
Ort()l)er 29, 1982
THENAl'TIU'S 153
calculated as a percentage of the mean hdurly
activity, with time spent out of the refuge con-
sidered activity. Specimens of 0. cyanea were
exposed to a diffused natural light regime.
Results
0. cyanea is reported to be active during the
day and inactive at night (Van Heukelem, 1966;
Yarnall, 1969) while 0. omatus is considered by
local fisherman to be night active. No previous
data on locomotor activity or behavior of the
crescent octopus have been published. The loco-
motor activity rhythms demonstrated in this
study were species-specific in pattern, and peak
activity of each species was distinct from {)eak
activity of the other two.
In this as in previously published studies, O.
cyanea showed diurnal activity. Maximum loco-
motor activity, as measured by time spent out of
the prepared "refuge", occurred just after dawn
at 7 am (activity from 0600 to 0700 hours) and in
a broad peak between 1300 and 1800 hours. Ac-
tivity was maintained throughout daylight
hours. Van Heukelem (1966) and Yarnall (1969)
reported 0. cyanea to be diurnally active, with
crepuscular peaks in activity. This diurnal pat-
c
500
400
>
U
<
3
O
300 1 T
200
100
0. cyanea
0. ornatus
crescent octopus
1200
Time (Hrs.)
FIG. 1. Locomotor activity patterns for three species of shallow water Hawaiian octopods. Octopus ornatus
record is based on. 6i continuous hourly values. 0. cyanea record is based on 21, continuous hourly values, and
the "crescent octopus" record is based on 91 continuous hourly values.
154 THE NAUTILUS
October 29, 1982
Vol. 96(4)
tern is confirmed in tiie record of locomotor ac-
tivity seen in Fig. 1.
0. oniatu.'^ demonstrated a nocturnal pattern
of overall activity in the aquarium as recorded
by the ultrasonic monitoring system. With a
light regime of twelve hours of light and twelve
hours of darkness, peak activity occurred in the
middle of the lights off period. A dark period
from 6 pm (1800 hours) to 6 am corresponded to
natural conditions on the reefs in Hawaii (US
Department of Commerce, 1944); under this
light regime, 0. ornatus was maximally active
from 2100 hours to 0200 hours.
The crescent octopus also demonstrated noc-
turnal activity in the aquarium as recorded by
the ultrasonic monitor, but maximum activity of
the crescent octopus occurred during those
hours of darkness when 0. ornatu>^ showed
reduced locomotor activity. Under the light
regime in which the lights off period extended
from 1800 hours to 0600 hours, the crescent oc-
topus was most active in the hour immediately
after artifical dusk (1800 to 1900 hours) and im-
mediately before dawn (0500 to 0600 hour-s).
Periods of inactivity in all three species were
characterized by an almost complete lack of
movement, other than regular mantle respira-
tory movements. The ultrasonic monitor was es-
pecially useful for examination of these periods
of inactivity, since it recorded even small twitch-
ing of a single arm. Numerous observations
were made of 0. or-ymtus in the aquarium during
the inactive period. During these periods, the
octopus was found at the bottom of the tank
with its eyelids closed, its arm wrapped about its
head and mantle, a white translucent color to its
skin that was quite distinct from the bright red
and white banded appearance of an active ani-
mal of this species. Respiratory movements
were regular, and sensory perception was suffi-
ciently suppressed for the author to be able to
move a small net about the tank vigorously with-
out the animal responding in any way. When the
animal was touched, it reacted violently with
what could be called a startled reaction. It
opened the eyelids, rapidly spread its arms and
frequently expelled water through its funnel at
the source of the intrusion. This behavior super-
ficially resembles sleep in vertebrates during
periods of inactivity. Other marine inverte-
brates show periods of heightened and reduced
locomotor activity (DeCoursey, 1976) but no
other marine invertebrate has been reported to
exhibit such pronounced sleeplike behavior.
The patterns of locomotor activity demon-
strated in aquaria by the three species were
reflected in observations in the field. When div-
ing on the reefs of Oahu during the day, 0.
cyanea was the only species commonly sited. At
night it was unusual to find this species on the
reef. Yarnall (1969) and Van Heukelem (1966)
report that 0. cyanea retreats to its den at
night, often blocking the entrance with stones.
0. oniutua was never observed by the author on
the reef during the day, and the crescent octo-
pus was rarely seen. 0. ornatus was most easily
collected after 9 pm (2100 hours); when low
tides occurred in the middle the night, 0. or-
nntu^ was frequently seen fully exposed and
moving freely across the reef flat or on sand and
gravel substrates. The crescent octopus was
routinely collected after dusk in shallow tide
pools where the animals positioned themselves
under rock ledges at or near the air-water inter-
face.
Although all three species of octopods can be
found within 100 feet of each other on a shallow
reef flat, there are differences in the substrates
of the inicroenvironments favored by each
species. 0. ornatus cannot be observed on the
reef during inactive periods. When provided
with a gravel or coral substrate in an aquarium,
0. 07~n.a,tus will burrow under the gravel and
disappear from sight during the lights on period.
The crescent octopus, as mentioned above, fre-
quents the undersurface of ledges at the aii--
water interface in tidepools. In an aquarium, the
crescent octopus assumes a position at this in-
terface, often with several arms extended over
its head, the suckers resting at the water sui--
face. 0. cyanea has been located in sites under
large coral boulders or holes at the base of con-
crete walls (Van Heukelem, 1966; Yarnall,
1969). Yarnall reports use of the same "refuge"
by several 0. cyanea in succession. In an
aciuarium, (). cyanea will readily inhabit a ccm-
Crete block or a length of PVC tubing.
Vol. !)fi(4)
October 2i). 1982
THE NAUTILUS 155
DISCUSSION
Octopods demonstrate a variety of locomotor
activity rhythms in the aquarium and in the field
(Woods, i965; Van Heukelem, 1966, 1976;
Altman, 1967; Yarnall, 1969; Kayes, 1974;
Houck, 1977). The three species of Hawaiian oc-
topods in this study show species-specific tem-
poral spacing in locomotor activity rhythms.
This s])acing may influence the diet of each
species. In the laboratory, all three species will
readily accept much the same variety of grapsid
crabs and shrimp species as food. Crustaceans
show locomotor activity patterns of their own,
often entrained by photoperiod and tidal
rhythms (DeCoursey, 1976). In the field, hunt-
ing activity by an octopus at a specific time of
day may restrict the types of crustaceans eaten,
reducing interspecific competition for food.
The distinct locomotor activity rhythms of the
three species of octopods, coupled with the dif-
ferences in habitat and substrate preference,
minimize interspecific contact in the field. Com-
petition for food may not be the only factor im-
pacted. Octopods are predators on other mem-
bers of the genus (Van Heukelem, 1976); larger
animals will readily feed upon small individuals.
The three species of this study vary dramatically
in size. 0. cyanea is the largest, with maximum
weight over 5 kilograms. 0. ornatui< has a mid-
dle size range, with mature individuals of 500
grams common. The crescent octopus is the
smallest species. Maximum size of any in-
dividual collected by the author was 90 grams.
The vast size difference may encourage the
smaller species, especially the crescent octopus,
to limit activity to periods when contact with the
larger individuals of other species is unlikely. It
should be noted, however, that activity rhythms
were recorded and maintained in the laboratory
in isolation, so visual observation of individuals
of the same or other species is not required for
demonstration of locomotor patterns. Boyle
(1980) indicates that a larger octopus may take
food forcefully from a smaller octopus, so tem-
poral spacing may be especially beneficial to
smaller species.
Competition for home sites in the aquarium
has been documented in OcfopM.s vulgaris Cuvier
(Boyle, 1980). On the reef flats on the south
shore of Oahu, tide pools, coral heads and coral
rubble are found near each other. By inhabiting
one of these microhabitats over others, the
three species of Hawaiian octopods in this study
may minimize interspecific contact and reduce
competition for home sites. When this habitat
selection is coupled with the temporal spacing
evident in activity periods, contact between
species may be effectively reduced.
Thus, Octopus cyanea. 0. ornatus and the
"crescent octopus" show distinct species-specific
patterns of locomotor activity in the laboratory
under light regimes similar to those in the field.
The three species are active on the same reefs
on the south shore of Oahu at different times of
the day. These times correspond to the periods
of maximum activity recorded in the laboratory.
ACKNOWLEDGMENTS
The author thanks A. N. Popper, I. M. Cooke
and R. E. Young for their advice and encourage-
ment; W. H. A.kaka, R. Shoemaker and M.
Valdez for help in design and construction of the
acoustic monitor, and W. van Heukelem for
sharing his extensive knowledge of cephalopod
biology. She is also appreciative of editorial
assistance from F. G. Hochberg and R. T.
Abbott. The research was supported in part by
an NIH predoctoral fellowship granted the
author.
LITERATURE CITED
Akaka, W. H. and Houck, B. A. 1980. The use of an
ultrasonic monitor for recording locomotor activity.
Eehnv. Ret^. Methods and Infttr. 12:514-516.
Altman, J. S. 1967. The behavior of Octopus vulgaris Lam.
in its natural habitat: a pilot study. Undenvater Ass. Rep.
1966-67:77-83.
Boyle. P. R. 1980. Home occupancy by male Octopus cul-
garis in a large seawater tank. Animal Behavior
'28:1123-1126.
UeCoursey, P. J. 1976. Builogiral Rtiylhmx in the Marine
Enviromnent. Columbia: Univ. of South Carolina Press.
Franzisket, L. 1969. The ratio of photosynthesis to respira-
tion of reef building corals during a 24 hour period. Forma
et Functio 1:153-158.
Houck, B. A. 1977. A morphological and behavioral study of
an extra-ocular photoreceptor in octopods. Ph.D. disser-
tation. University of Hawaii.
Kayes, R. J. 1974. The daily activity pattern of Octopus
vulgaris in a natural habitat. Marine Behac. Physiol.
2:337-343.
156 THE NAUTILUS
October 2y, 1982
Vol. 96(4)
U.S. Dt'partmenl of ('omnierce 1944. Sunshine tables. (npuf: cyaiipa and Octopnn 111111/11. I'h.l). tlissiTlal imi.
Weather Bur. No. 805. Washington, D.C. University of Hawaii.
Van Heukelem, W. F. 1966. Some aspects of the ecologi,' and Woods, J. 1965. Octopus-watching off Capri. Aninidls
ethology of Octopus cyanea Gray. M. S. thesis. University 7:324-327.
of Hawaii. Yarnall, J. L. 1969. Aspects of the behavior of thinijus
1976. Growth, bioenergetics and life-span of Or- ciiancd Gray. Ariiiiidl Behariar 17:747-754.
REDISCOVERY OF THE MARGINELLID GASTROPOD
PERSICULA TESSELLATA (LAMARCK, 1822)
ON THE PACIFIC COAST OF PANAMA
Barry Roth
California Academy of Sciences
San Francisco, California 94118
William K. Emerson
and American Museum of Natural History
New York, New York 10U24
ABSTRACT
Specimens of Persicula tessellata (Lamarck, 1822), a species originally de-
scribed from an unknoum province, are here recorded from the Pacific coast of
Panama and are compared with Persicula accola (Roth and Coan, 1968) from the
same area. The identity of Persicula porcellana (Gmelin, 1791), a Caribbean
species that ha.s been confused with P. tessellata, is reevaluated.
Live-collected specimens of a Persicula from
Pacific Panamic waters submitted to the Ameri-
can Museum of Natural History by James
Ernest agree well with the holotype of Mar-
(jincllii fessellata Lamarck, 1822, described from
an unknown locality. These specimens permit a
reevaluation of the synonymy oi Marginella tes-
sellaia with Voluta porcellana Gmelin, 1791,
first advanced by Reeve (1846) and perpetuated
in the west American literature (Keen, 1958;
Coan and Roth, 1966; Roth and Coan, 1968).
Persicula tessellata (Lamarck) is here removed
from the synonymy of P. porcellana (Gmelin,
1791) and is recognized as an inhabitant of
tropical west American waters. The Pacific
\'-diYc\m\c Persirula areola Roth and Coan, 1968
is compared with Lamarck's P. tessellata, and
the identity of Gnu'lin's P. porcellana from the
trojiical western .'\tlantic is reconsidered.
Institutional Abbreviation.s
AMNH = American Museum of Natural History
ANSP = Academy of Natural Sciences of
Philadelphia
CAS = California Academy of Sciences
MCZ = Museum of Comparative Zoology,
Harvard University
USNM = National Museum of Natural History.
Smithsonian I nstitutic )n
Family Marginellidae Fleming, 1828
Genus Persicula Schumacher, 1817
Type species by monotypy: Persicula vari-
abilis Schumacher, 1817 {= Voluta persicula
Linnaeus, 1758), Recent, west Africa. Medium-
sized to small marginellids with flat spire usually
concealed l:)y callus; aperture narrow through-
out its length; anterior end strongly notched;
most species strikingly marked or colored.
Eocene to Recent, Old and New World tropics.
Persicula tessellata (Lamarck, 1822)
(Figs. 1-6)
MiirijiiwUd lessctlala Lamarck, 1822:361-362. Kiener.
1834:24, pi. 5, fig. 20.
Maryinetla parri'ltrina (Gmelin), Reeve, 1864:pl. 13, figs.
53a, 53b.
Vol. 96(4)
October 2[). 1982
THENAlTlLrS 157
"IGS. 1-6. Persicula tessellatafLar/iarcA:, 18-J'^). 1-4, specimens from Lm Zurrones, Isia Cehaeo, Panama, ex Ernest C.ullec-
'11)11. 1. 2. (AMNH 208760). S. U. (AMNH 208761); x2. 5, 6. holotype o/Marginella tessellata, Lamarck Collection. Mus. Hist.
Vat. Geneva, courtesy of Dr. E. Binder; x2.1. 7, 8. Persicula accola Roth and Coan (1968). Isla Perida. Panama. (AMNH
102770); X 2. 9-16. Persicula porcellana fGme/in, 1791). 9, 10. reproduttion of Chemnitz (1788) figures 11,19 and U20. Spe^igler
)iUt-ction; x i. 11, 12, heach specimen from "Venezuela" (AMNH 4961,3. ex Constable Collection, received in 1901); x2. 13, 14,
Specimen, from Puerto La Cruz. Venezuela (AMNH 20301,5), x 2. 15, 16, specimen from "St. Martha, " Colombia in the Redfield
Collection (ANSP 29116). labeled typological lot o/Marginella obesa Redfield; x2.
'-'i rsicula porcellana (Gmelin), Jousseaume, 1875:260. Keen,
1958:436, fig. 680. Coan and Roth, 1966:282-283 (m
part), pi. 48, figs. 14, 15 (non figs. 16, 17, which = Persi-
i-iila accola Roth and Coan, 1968). Roth and Coan,
1968:63, pi. 7, figs. 5, 6,
\nn Valuta porcellana Gmelin, 1791:3449.
\on Marginella tessellata Wood, 1828:42. pi. 3, fig. 31
I =P. areola Roth and Coan. 1968].
Original description - "24. Marginelle par-
quetee. Marginella tessellata. M. testa obovatd,
apice retusa, albidd, punctis rufis quadratis
transversim seriatis tessellata: seriis cofertis;
columella plicis praecipuis quinis instructd:
supra aliis duohus seu tribus minimis; labro in-
tus crenulato. An valuta porcellana? Chemn.
158 THE NAUTILUS
October 29. 1982
Vol. 96(4)
Conch. 10. t. 150. f. 1419, 1420. C.mel. p. 3449.
no. 139." (Lamarck, 1822, p. 3(il).
Tyijc locality - Unknown. Here de-sij^nated,
off Isla Cebaco, west Panama.
Supplementary deseription - The following-
description is based on seven specimens dredged
in about 30 meters at Los Zurrones, Isla Cebaco,
Panama (7°40'10"N. 81°30'10"W) by James
Ernest, 1982 (6 specimens, AMNH 208761; 1
specimen CAS 032387). Shell large for the
genus, solid, ovate, diameter 0.61-0.67 times
length; narrower anteriorly, greatest width at
60-64 percent of distance from anterior end;
surface polished, unscuptured e.xcept for a few
raised incremental lines. Color white with 9-11
spiral rows of grayish brown, subrectangular
spots covering 60-80 percent of shell surface;
most posterior row just below suture; most
anterior row running along margin of anterior
canal; spots irregularly spaced, not tending to
align longitudinally, mostly wider than interven-
ing spaces in a row; spiral rows added by fission
of an existing row; incompletely split spots
usually present. Spots well defined or slightly
blurred (particularly on trailing edge) by overly-
ing clear to translucent whitish callus. Spire
covered by a Hat or slightly projecting apical
pad of white callus, circled by a ring of more or
less fused reddish brown blotches; spacing of
these blotches independent of pattern on body
whorl. Outer lip strongly thickened by callus,
not extending beyond apex, white, tinged along
outer margin with reddish brown, finely denti-
culate on apertural edge. Urate within. Aperture
narrow, almost even but slightly wider anterior-
ly, white inside, with acute posterior sulcus and
deep, narrow, oblique anterior canal. Canal set
off from body whorl by raised fasciolar Hange;
columellar side produced dorsally into a rounded
spur, ticked posteriorly with reddish brown.
Parietal wall moderately convex, shallowly ex-
cavated anterior to center; with thick white
callus along its length, merging posteriorly with
apical callus; left edge of callus a raised rim
paralleling aperture. Columella with 8 folds in-
cluding one at base of columella, decreasing in
strength posteriorly; posterior fold sometimes
barely perceptible; second fold from anterior
end large, bifid.
Dimension.^ a/the seven specimens examined-
Largest specimen: length 18.4 mm, diameter
12.3 mm; smallest specimen: length 16.1 mm,
diameter 10.6 mm; average for length: 17.5 mm;
average for diameter: 11.1 mm.
DISCUSSION
Comparison of the seven specimens from
James Ernest with the holotype of Persicula
lessellata (Figures 5, 6) leaves little doubt that
they are conspecific. The holotype is 16.5 mm in
length and 10 mm in diameter. It has 9 subequal
rows of spots on the back of the body whorl; fis-
sion increases these to 12 by the last quarter of
the whorl. The apical callus pad projects slight-
ly. Interspaces in a row of spots are somewhat
variable, particularly around the middle of the
whorl. The thick parietal callus pad and shallow
excavation of the parietal wall are exactly like
those of the Ernest specimens (Figures 1-4).
The holotype is a slightly worn specimen. Its
pattern is warm brownish orange. The super-
ficial wash of milky callus that covers the shell in
many Persicula species (e.g. P. bandera Coan
and Roth, 1966; P. hilli (Smith, 1950); P. accola
Roth and Coan, 1968; and the present species)
imparts a grayish cast to the dark patterning
underneath. When this layer is removed by ero-
sion, the remaining pattern shows as a warm
brownish red or orange, as in the holotype of P.
tessellata. In the Ernest sjiecimens, the differ-
ence in hue between the hody-whoi'l pattern and
the brown tinting on spire, outer liji, and canal is
probably not the ]:>roduct of separate pigments,
but the result of the body-whorl patterns being-
seen through the translucent wash of callus.
The Ernest specimens of P. tessellata differ in
several ways from Persicula accola Roth and
Coan (1968, pi. 7, figs. 7, 8). P. accola is smaller
(range of 20 adult specimens examined: lenglli
11.2-14.6 mm, diameter 7.0-9.1 mm). The rows
of brown spots cover about 90 percent of the
shell surface, the interspaces between them be-
ing narrow and uniform (Figures 7, 8); as in P.
tessellata, the basic number of rows seems to be
nine, with higher nimibers always the result i)t'
fission of one or more rows. The sfiire is tiat to
very low, not projecting as in somi' /'. ttsscllnln.
Vol. 96(4)
October 29, 1982
THE NAUTILUS 159
and the apical callus is ringed by a dense, solid
brown band or else (less commonly) entirely
brown. The brown ticking on the anterior
fasciolar flange is darker and more extensive
than on P. tessellata; the brown patch on the
outer margin of the thickened outer lip darker,
longer, and more distinct. Most P. accola have
seven columellar folds; occasionally a faint
eighth fold is perceptible posteriorly. Specimens
with five and six columellar folds occur.
All known occurrences of Persicula accola are
on the Pacific coast of Panama between Punta
Burica (8°02'N, 82°52'W) and Punta Mariato
(7°12'N, 80°53'W), intertidally (Coan and Roth
in Keen, 1971) to nine meters (AMNH 202770,
AMNH 208759). Isla Cebaco, the source of the
P. tessellata specimens, is also in this area.
James Ernest (m litt. to Emerson, 18 May 1982)
reports that P. accola is collected intertidally in
sand mixed with mud, while P. tessellata is
found in "deeper water [to about 30 meters] and
white sand, with very clear water."
Gmelin (1791) described Valuta porcellana
with reference to two figures in Chemnitz (1788)
(Figures 9, 10) depicting a broadly ovate Persi-
cula with 16 rows of small, irregularly shaped
spots. The locality was cited as Indian Ocean,
undoubtedly speculative since Gmelin probably
had no firsthand knowledge of the source of the
Chemnitz specimen. No occurrence of any Per-
sicula resembling P. porcellana in the Indian
Ocean has been confirmed in the many interven-
ing years. (Nevertheless, a few poorly grounded
citations in the later literature still place P.
porcellana in the Indian Ocean; cf. Dodge's
[1955, p. 85-86] speculative remarks.)
In describing Marginella tessellata, Lamarck
(1822, p. 361-362) "cited the same figure in
Chemnitz with an interrogation mark, then
went on to comment, about the specimen in his
own collection ("Mon cab."), "Ses points ne sont
pas sagittes comme dans le figure citee de
Chemniz, mais carres." Most later authors,
beginning with Reeve (1864) have interpreted
Lamarck's species and Gmelin's as synonymous,
perhaps mainly because both authors cited the
same Chemnitz figure. Dodge (1955, p. 86) inter-
preted Lamarck's comment about the shape of
the spots as a criticism of the fidelity of Chem-
nitz's illustration. It can equally well be seen as a
statement of contrast between the Chemnitz
specimen and Lamarck's own, which we accept
as the holotypic specimen (Figures 5, 6).
Kiener (1834, pi. 5, fig. 20) illustrated as Mar-
ginella tessellata a specimen with eleven rows of
subrectangular, brownish orange spots and a
moderately projecting apical callus. At 26.5 mm
in length, the figure is certainly enlarged; but
with the allowance for a little bit of artistic
license, it could practically be Lamarck's
holotype.
Under the name Marginella tessellata, Sower-
by (1846) illustrated three different specimens.
His figure 195 is evidently Persicula chryso-
melina (Redfield, 1848). Figure 194 shows the
dorsal view of a Persicula 11.1 mm in length
with nine spiral rows of variously sagittate,
subrectangular and irregular spots. Figures
196 and 197 show dorsal and ventral views of a
similar Persicula 14.8 mm in length with 13
rows of irregular to sagittate spots and a
maculated outer lip. Sowerby's (1846, p. 395)
description of the species characterizes the col-
umella as white, swollen in the middle, and
elevated into a swollen varix anteriorly. Sower-
by was also the first to associate a locality with
the name M. tessellata, stating that it was a
common species from Venezuela.
The lack of precision in the Sowerby illustra-
tions makes them somewhat difficult to inter-
pret. However, the characters of maculation on
the outer lip (visible in ventral view) and a tumid
parietal callus rising to a ridge or varix anterior
to the middle are strongly suggestive of an At-
lantic species variously identified in museum
collections as Persicula obesa (Redfield, 1846)
and P. porcellana (Gmelin. 1791). Most of these
specimens are from older collections and the lo-
calities are indefinite: Venezuela (AMNH 49643,
ex James Arnold Constable collection; CAS
030298, ex Ruth Coats collection), Honduras
(USNM 19617), "West Indies" (MCZ 265502).
They have 14-16 spiral rows of spots. The spots
are usually punctate, sagittate, or dash-shaped
rather than rectangular; there is typically a zone
of larger spots over the broadest part of the
body whorl, and another, less pronounced, about
one-fourth of the distance posterior to the
160 THE NAUTILUS
October 29, 1982
Vol. 96(4)
anterior end. The apical callus is flat or slightly
projecting and strongly tinged with brown. The
callus thickening of the outer lip is whitish, often
with brown dashes echoing the color pattern of
the body whorl. None of these specimens show
the longitudinal brown patch of P. tessellata and
P. accola. Authenticated modern records of this
species in the western Atlantic are: Puerto La
Cruz, Anzoategui, Venezuela, three specimens
(AMNH 203045, ex F. J. Fernandez H. collec-
tion, 1976) (Figures 13, 14), Tobago, West In-
dies, two specimens (AMNH 141495, ex Mrs.
Stuart Brown collection, 1967). Rios (1970,
1975) records this species (as P. obesa) from
Brazil, but the cited specimens are actually from
Venezuela {teste Rios, 1982).
The hoiotype of Valuta porcellana Gmelin,
formerly in the Lorenz Spengler (1720-1807)
collection of the University of Copenhagen, is
lost (Coan and Roth, 1966). The Chemnitz draw-
ings (cf. Figures 9, 10 with 11, 12) cited by
Gmelin for his species agree more closely with
the Caribbean species than with the Pacific Per-
sicula tessellata. Voluta porcellana is the oldest
name for the Caribbean species, with Voluta
albida Bosc, 1801 (cites Chemn. figs. 1419 and
1420) and Margimlla obesa Redfield, 1846 (not
Sowerby, 1846) both junior synonyms. Redfield's
taxon was based on specimens provided by W.
W. Whitney from the "Caribbean Sea at Cartha-
gena, SA" [Colombia] that were deposited in the
"Cabinet of the Lyceum" [of Natural History,
New York City]. The collection of the Lyceum
was destroyed by a fire in 1866, (Fairchild,
1887). There are, however, four specimens
(ANSP 29116) from the collection of John H.
Redfield (1815-1895) labeled as "types". None of
these specimens match the measurements or
figures cited in the original description (Red-
field, 1846, p. 164, 165, pi. 10, figs. 5a, b). Fur-
thermore, the locality for this lot is given as "St.
Martha, S.A." [ = Santa Marta, Colombia]. Al-
though this may not represent the type lot, the
specimens agree well with Redfield's description
and illustration (see figures 15, 16). Three topo-
typical specimens of this taxon (ANSP 29386)
are in the Robert Swift collection (1796-1872).
Marginella similis Sowerby, 1846, from
"Brazil", is a possible additional junior synonym
of P. porcellana. Redfield (1848) and others have
referred Sowerby's taxon to the synonymy of
Marginella obesa Redfield, but we have not ex-
amined the types of M. similis. which we
presume are in the British Museum (Natural
History).
Coan and Roth (1966) designated the hoiotype
(which they called a lectotype) of Marginella
tessellata to be a neotype for Voluta porcellana.
Their aim was to cement the synonymy, gener-
ally accepted up to that time, of M. tessellata
and V. porcellana. In light of the foregoing
demonstration that Persicula tessellata is a
Pacific species, and Persicula porcellana is a
consistently differing Atlantic species, the Coan
and Roth neotype designation fails to meet the
provisions of ICZN Article 75 (c) (4), which
states that to be validly designated a neotype
must be published with "evidence that the
neotype is consistent with what is known of the
original type-material, from its description and
from other sources." Coan and Roth (1966, p.
283) actually commented that the Chemnitz
figures differed in pattern and proportions from
any "P. porcellana" that they had examined at
the time. We suggest that the neotype designa-
tion is invalid.
Coan and Roth (1966) first regarded Persicula
porcellana as an eastern Pacific species and il-
lustrated (1966, figs. 16-17) a specimen from
Isla Coiba, Panama, under that name. Later, the
same authors (Roth and Coan, 1968) distin-
guished P. accola as an eastern Pacific species
(including the specimen they had figured in
1966), and allocated P. porcellana to the west-
ern Atlantic, stating that they had examined
"from the Caribbean, specimens that look like
Lamarck's type [i.e., of P. tessellata] and still
others which closely resemble the original
Chemnitz figures" (Roth and Coan, 1968, p. 63).
Such specimens include MCZ 265501 (no locali-
ty; four P. porcellana and four P. a-ccola), USNM
90175 ("Venezuela," ex Wesleyan University col-
lection; two, probably P. accola), and USNM
413838 ("Brazil," ex Ford collection; one P. ac-
cola). It seems most probable that, with the ex-
ception of the four true P. porcellana in MCZ
265501, these all represent misallocations of
eastern Pacific shells.
Vol. 96(4)
October 29, 1982
THE NAUTILUS 161
In summary, Persicula tessellata (Lamarck,
1822) and Persicula accola Roth and Coan, 1968,
ire similar eastern Pacific species occurring in
;he same part of western Panama. Persicula
oorcellana (Gmelin, 1791) is the valid name for a
Caribbean species with more rows of finer spots;
Marginella obesa Redfield, 1846, is synonymous.
ACKNOWLEDGMENTS
We are grateful to Mr. James Ernest of
Balboa, Republic of Panama, for calling our at-
:ention to his findings of Panamanian Persicula
md generously providing us with specimens.
Drs. Pablo E. Penchaszadeh, Instituto de Tec-
nologia y Ciencias Marinas, Universidad Simon
Bolivar, Venezuela, and Eliezer de Carvalho
Rios, Museu Oceanografico de FURG, Rio
jrande, Brazil, generously supplied information
ind/or specimens. Dr. Robert Robertson
ANSP) kindly arranged for the loan of speci-
mens. Mr. William E. Old, Jr. (AMNH) gave his
idvice and provided technical assistance. Mrs.
\my Hkimi (AMNH) typed the manuscript.
"^Jina Root and Karl F. Koopman (both AMNH)
jave bibliographic assistance.
LITERATURE CITED
3osc, L. A. G. 1801. Histoire Naturelle des Coqiiilles . . .
Paris, vol. 5, 255 p.
Ilhemnitz, J. H. 1788. Neues systematisches Conchylien-
Cabin^t. 10. Niirnberg, xxiv + 376 p.
Z;oan, E. V. and B. Roth. 1966. The west American Mar-
ginellidae. The Veliger 8(4):276-299.
Dodge, H. 1955. A historical review of the mollusks of
Linnaeus. Part; 3, the genera Bulla and Valuta of the
class Gastropoda. Bull. Amer. Mus. Nat. Hist.
107(1):1-158.
Fairc-hild, H. L. 1887. A history of the New York Academy
of Sciences, formerly the Lyceum of Natural History.
New York, published by the author, xii + 190 p.
Gmelin, J. F. 1791. Syslema naturae per regna tria naturae
. . . , ed. 13, Leipzig, 1(6):3021-3910.
.lousseaume, F. P. 1875. Coquilles de la famille des mar-
ginelles flpc. Mag. ZiioL. ser. 3, 3:164-271, 429-435.
Keen, A. M. 1958. Sea shells of tropical west America;
marine mollusks from Lower California to Colombia.
Stanford, Calif, xi + 624 p.
1971. Sea shells of tropical west America;
marine mollusks from Baja California to Peru, ed. 2.
Stanford, Calif, xiv + 1064 p.
Kiener, L. C. 1834-1841. Species general et iconographie
des coquilles vivantes. Genre marginelle. Paris, 44 p.
Lamarck, J. B. P. A. de M. de. 1822. Histoire naturelle
des aiiimtmx sans vertebres, 7. Paris, 711 p.
Redfield, J. H. 1846. Description of some new species of
shells. Ann. Lye. Nat. Hist. New York. 4(5):163-168
[Feb., 1846].
1848. Descriptions of new species of Bulla and
Marginella. with notes upon G. B. Sowerby, Jr's. mono-
graph of the latter genus. Ibid., 4(12):491-495 [Sept.,
1848].
Reeve, L. A. 1864-1865. Conchologia iconica; or illustra-
tions of molluscous aniynals. 15. Monograph of the genus
Marginella. London, 27 pis. with text.
Rios, E. C. 1970. Coastal Brazilian seashelU. Rio Grande,
255 p.
1975. Brazilian marine mollusks iconography.
Rio Grande, 331 p.
Roth, B. and E. V. Coan. 1968. Further observations on the
west American Marginellidae with the descriptions of two
new species. The Veliger ll(l):62-69.
Smith, M. 1950. New Mexican and Panamic shells. The
Nautilu.9. 64(2):60, 61.
Sowerby, G. B. IL, 1846. Monograph of the genus Mar-
ginella. Thesaurus Conchyliorum. or figures and descrip-
tions of shells. l(7):373-406, [27 Nov., 1846].
Wood, W. 1828. Supplement of the Index testaceologicus;
or a catalogue of shells, British and Foreign. London,
vi + 59 p.
Notices
A grant of $400 will be awarded by the Ameri-
can Malacological Union to a graduate student
'or the purpose of conducting field studies of
and or freshwater mollusks. Grant proposals
should include: (1) A brief description of the pro-
oosed project, (2) an estimated budget of antici-
Dated expenditures, and (3) a statement from
;he student's supervising professor that the pro-
ect is an appropriate part of the student's re-
search. Proposals must be submitted in quadru-
plicate by January 1, 1983 to Dr. Alan J. Kohn,
President A.M.U., Dept. Zoology, University of
Washington, Seattle, Washington 98195. The
announcement of the award will be made by
April 1, 1983.
This award has been made possible by the
many friends of Dr. Joseph C. Bequaert who
died on January 19, 1982 at the age of 95. Dr.
Bequaert, known as Uncle Joe to his students
and friends, spent a lifetime in the field studying
land and freshwater mollusks, and this award is
a tribute to his memory.
162 THE NAUTILUS
October 29, 1982
Vol. 96(4)
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