THE NAUTILUS
Volume 114, Number 1
March 27, 2000
ISSN 0028-1344
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TH E€9NAUTI LUS
CONTENTS
Volume 114, Number 1
March 27, 2000
ISSN 0028-1344
Adriaan Gittenberger Epitoniinii (Gastropoda: Epitoniidae) associated with
Jeroen Goud iinislirooni corals (Scleractinia: Fun<fiidae) from Sulawesi,
Edmund Gittenberger Indonesia, with the description ot four new species 1
Marta J. deMaintenon A new species ot CohtmbcUa (Neogastropoda:
Columbellidae) from the Caribbean Neogene 14
Bruce A. Marshall The New Zealand Recent species of Muricopsis Bucquoy,
Kevin W. Burch Dautzenberg and Dollfus, 1882 (Gastropoda: Muricidae) 18
Notices 3{)
APRl
THE NAUTILUS 114(1):1-13, 2000
Page 1
Epitoniiun (Gastropoda: Epitoniidae) associated with mushroom
corals (Scleractinia: Fungiidae) from Sulawesi, Indonesia, with
the description of four new species
Adriaan Gittenberger
Institute of Evolutionan- and
Ecological Sciences
Universitv of Leiden
P.O. Box'9516
NL 2300 RA Leiden
THE NETHERLANDS
Jeroen Coud
National Museum of Natural Histon'
RO. Box 9.517
NL 2.300 RA Leiden
THE NETHERLANDS
Edmund Gittenberger'
Institute of Evolutionary and
Ecological Sciences
National Museum of Natural Historv
RO. Box 9517
NL 2300 RA Leiden
THE NETHERLANDS
ABSTRACT
At least six species of the genus Epitoniiim scnsii lata are found
associated witli mushroom corals (Fungiidae) off Ujinig Pan-
dang, Sulawesi. Indonesia. Revised descriptions of £. costiila-
tiim (Kiener, 1838) and E. iilu Pilsbry, 1921 based on t\pe
specimens and additional material are given. Four new species
are described: E. hoeksemai. E. ingridae, E. lochi, and E. tivi-
lae. The true identity of £. bullntum (Sowerbw 1844), a species
not associated with corals and not found in Sulawesi and near-
by areas, is clarified. Examination of tyjie sjiecimens made pos-
sible the characterization of nominal species that appear to be
either identical with or closely related to the fungiid-associated
epitoniids found off Sulawesi.
Ki-ij words: Indo-Pacific, parasites, coral reefs, coral/mollusk
association, egg capsules.
INTRODUCTION
Several epitoniid species are known to live in association
with sea anemones (phvluni Cnidaria, order Actiniaria)
(Robertson, 1963; 1983a, b; 1993; Vecchi(j, 1964; Salo,
1977; Perron, 1978; Kay, 1979; Schimek. 1986; Hartog,
1987; Dushane, 1988a-<'; Yamashiro, 1990; Nakayama,
1991; Mienis, 1994). Less commonly, epitoniids are found
associated with stony corals (piiylum Cnidaria, order
Scleractinia), in particular with species of the free-living
Fungiidae or mushroom corals (Robertson, 1963; 1970;
Bosch, 1965; Hadfield, 1976; Kav, 1979; Bratcher, 1982;
Loch, 1982; Sabelh and Taviani, 1984; Bell, 1985; Dusha-
ne, 1988a-c; Loo and Chou, 1988; Page and Willan, 1988;
Hoeksema, 1988; 1989; Yamashiro, 1990; Mienis, 1994;
Oliverio ct ai, 1997). OnK' three Epitoiiitim species are
usualK' mentioned in the literature in association with
fungiids; in one case (Lcjch, 1982) a fourth species is re-
ported but not named. This paper deals mainK' widi die
taxonomy of die surprisingly high number of species of
' Author for correspondence; gittenberger@naturalis.nnni nl
Epitonium found associated widi mushroom corals during
a survey in a relatively restricted area in Indonesia, off
Ujung Pandang (Sulawesi). Four of these species proved
to be new to science, although at least one of them had
frequenth' been cited and illustrated under an incorrect
name. The shells of diese species are ver)' fragile, which
might explain why diey are mosdy poorly represented or
not represented at all in most institutional collections.
These species are only kiiouni from live-collected speci-
mens: it is very unlikely diat emptv shells will be found
washed ashore without being seriously damaged or un-
recognizable. A more elaborate analysis of the ecological
data collected during the project is being prepared (Git-
tenberger, A., unpul)lished data).
The systematic and evolutionary importance of vari-
able characters such as egg capsules (Figures 36-38),
eggs (Figure 41) and mucous threads (Figures 43-47),
which can be either straight or hoisted, is still poorlv
known. We observed, however, that populations of the
different species may differ in these characters. With
exception of one article by Oliverio et al. (1997). the
literature is scantx- in respect to these characters. Oliv-
erio ct nl., while discussing the coral-associated epitoniid
Epitonium billccanuni Dushane and Bratcher, 1965, fig-
ured the egg capsules, eggs, mucous threads (of the
tswsted type) and shells of veliger larvae. We did not
obseiA'c a difference in sculpture or well-defined tran-
sition between the protoconch 1, formed by the shell
gland of the larva inside the egg capsule, and protoconch
2, secreted by the velum of the swimming veliger be-
tween hatching and settling. The protoconchs (Figures
16, 25-29, 42, 48) turned out to be verv uniform among
the various species studied here, all of which apparently
have planktotrophic development. Sclerites of at least
one species of soft coral, probabh' of the genus Sinularia
May, 1898 (subclass Octocorallia, order Alcyonacea, fam-
ily AlcNoniidae) (L. P. van Ofvvegen, NNM) were found
associated with the egg capsules of some species (Fig-
ures 39-40).
Page 2
THE NAUTILUS. Vol. 114. No. 1
Figure 1. Sun'e\ed area off Ujung Paiidang. S. Sulawesi. Indonesia. The coral reefs investigated in particular are: 1. W (Pulau)
Lae-Lae; 2, W Bone Baku; 3, E (Pulau) Samalona; 4, W (Pulau) Samalona; 5, E and ESE (Pulau) Kudingareng Keke; 6. W (Pulau)
Kudingareng Keke: 7. NW Lan[g]kai; 8. Pulau Badi: 9. Bone Lola: 10. (Pulau) Bone Tanibung.
In a monograph on Epitoniidae from southern Africa
and Mozambique, Kilbum (1985: 240) stated that "epi-
toniid taxonomy remains in a chaotic state, particularK^
above the species level." Kilbum observed that the clas-
sification of the genus Epitonium is (p. 280) "vers' ten-
tative and is aimed soieK at grouping together similar
species for convenience sake." Clench and Turner (1951)
and Bouchet and Waren (1986) followed a similar ap-
proach in their revision of eastern Atlantic Epitoniidae.
Because we could not imequivocalK' classify- all Indo-
nesian species within one or more of the 19 subgenera
used by Kilbum (1985) or the 39 subgenera listed bv
Wenz (1940) under "Scala" (= Epitonium). we decided
to refrain from following anv subgeneric classification.
The epitoniid species described in this studv live as-
sociated with mushroom corals and at least some of
them are so similar that they seem to be closelv related
phvlogenedcalK-. Thev point to possible adaptive radia-
tion within a single clade. Adequate ph\logenetic anal-
yses including other species of Epitonium co-occurring
with different hosts in the same general area could help
clarify- whether these species found in association with
fungiid corals form a monophsletic group.
MATERIALS AND METHODS
Samples were collected off the coast of Ujung Pandang,
Sulawesi, Indonesia. The fungiid fauna of the area (Fig-
ure 1) is relatively well known; see Hoeksema (1989) for
details. During the period April-June, 1997, 9 coral reefs
were inspected, to a depth of 18 (rarelv 24) meters. Ap-
proximately 10' mushroom corals, belonging to about 30
species of free-living Fungiidae, were searched for epi-
toniids and their eggs. Beneath these corals, about 10'
specimens of Epitonium. some of which with egg cap-
sules, were collected. The identifications of the coral
species were made or at least checked b)' Dr. B. W.
Hoeksema. The snails were classified into morphological
categories according to characters of shell, egg capsules,
and proboscis. Secondarilv, the species thus disdn-
guished were anaKzed ecologicallv for preferential
depths, hosts, and substrates. The ecologiciU data will be
discussed in a future article (Gittenberger, A., unpub-
lished data).
The various Epitonium species recorded during the
surve\' were identified bv review of the literature, con-
sultation with specialists, and by comparison with ma-
terial deposited in several collections; this includes com-
parison with hpe specimens of conchologicallv similar
taxa. These tvpes are mentioned in the systematic treat-
ment of each species.
From the about 10' specimens collected, only shells
with more than 4 mm length were measured. The num-
ber of specimens (n) measured in the calculation of
mean values is mentioned at the beginning of the de-
scriptions. Means are indicated between the e.xtremes
(minimum-mean-maximum). To allow for better com-
parisons, shell sculpture is described for both the fifth
teleoconch whorl and where the teleoconch is 5 mm in
width, a part of die spire that is in part independent of
Gittenberger et ai, 2000
Page 3
Figure 2. Maps of the Indo-Pacific Region, from the Red Sea to the Hawaiian Archipelago, showing records of the Epitonium
species in this study known from more than tvvo localities: Epitonium costulatum (Kiener, 1838) (stars), E. ingridae new species
(triangles), E. twilae new species (squares) and E. iilu Pilsbry, 1921 (circles).
the actual whorl number. The term protoconch refers to
the protoconchs 1+2. The maximum diameter of pro-
toconch 1 was measured in two shells for each species
(except tor E. lochi because of insufficient material), us-
ing SEM photographs of specimens prepared from egg
capsules (Figures 30-31); because ver\' similar values
were consistently found, no more measurements were
taken. Shells of Epitonium species cannot be recognized
as fulK' grown or not. Comparative informal observations
indicate that when the snails start laving eggs thev have
not yet reached maximum size. No minimum values are
included in the descriptions but only the largest speci-
men and the largest number f)f whorls. After removal
from 70% ethanol, egg capsules without embedded sand
(juicklv collapsed; these could not be photographed. Un-
less stated otherwise, all descriptions refer to material
from off Ujung Pandang.
The following institutional abbreviations are used:
AMS, Australian Museum, Sydney; ANSP, Academy of
Natural Sciences, Philadelphia; BMNH, The Natural
Histon' Museum, London; LACM, Natural Histoiv Mu-
seum of Los Angeles County, Los Angeles; MHNG, Mu-
seum d'Histoire Naturelle, Geneve; MNHN, Museum
national d'Histoire naturelle, Paris; MZB, Museum Zool-
ogicum Bogoriense, Bogor, Indonesia; NNM, National
Museum of Natural Historv, Leiden. Numbers following
a slash sign after collection numbers refer to number of
shells in relevant lots.
SYSTEMATICS
Family Epitoniidae Berrv, 1910
Genus Epitonium Boding, 1798
Epitonium costulatum (Kiener, 1838)
(Figures 2-6, 22, 25, 38-41, 47)
Scalaha costulatum Kiener, 1838: pi. 2, fig. 4; 1838: 5.
Epitonium costulatum. — Robertson, 1963: 57, pi. 5, fig. 4;
1970: 45; Loch. 1982: 4, 1 fig.; Dushane, 1988a; 30, figs.
1, 2.
Description: Shell (Figures 3-6, 22, 25) (n = 7): Frag-
ile (large specimens) to verv fragile, moderately elongate-
Page 4
THE NAUTILUS, Vol. 114, No, 1
Figures 3 — 1. Epitonium costiilatum (Kiener, 1838), holotype
(MHNG 1152/16). Shell length 3.3 cm.
conical, cream\ white, reacliing 32 mm in length, with at
least 1 damaged specimen (from Ambon) measuring 41.2
mm. Lengtli/vvidth 1.6-1.9-2.2. Protoconch whorls 3 .3/8;
maximum protoconch 1 diameter 0.14 mm (n = 2). Pro-
toconch with numerous fine, incised, axial lines. Teleo-
conch whorls up to 10, separated bv vers' deep (fenes-
trate) suture. Successive whorls are almost detached. Te-
leoconch with e\enK- spaced, orthocline, thin costae, dam-
aged in all examined specimens. Over most of their
lengdi, costae appear to be curved abaperturally at outer
margin. Costae adapicallv relativelv high and erect, not
coronate, becoming short toward columella. Costae most-
K' continuous, but touching onK' slightK' diose of adjoining
whorls. Ver\- weak spiral lines present. Fifth teleoconcli
whorl (widtli 4.9 mm) with 16-18.4^26 costae. Five mm
width whorl (whorl 4, 5, or 6) widi 16-17.4-20 costae.
Aperture subcircular. Apertural lengtli/shell length 0.3.
Umbilicus moderately wide.
Egg capsules (Fif^iires 38, 3.9, 40, 47): Embedded with
sand and closel)- connected along a straight, longitudi-
nally striated, mucous diread (Figure 47). Capsules
asymmetrical, somewhat conical with a circular widest
part. Capsules 3. 0-3. .3-3. 5 mm in length and 1.5-1.6-
2.0 mm in width (n = 8). One egg capsule contains 70-
17.5-335 eggs (n = 5).
Proboscis: With some irreguIarK' interrupted, longitvi-
dinal, white zones, which are as wide as transparent in-
terspaces.
Type material (Figures 3-4):
1152/16.
Holotype MHNG
Type locality: Unknown.
Other material examined: NNM, Indonesia, Am-
bon, Hitu, outer part of Ambon Bay, E and W sides of
Laha, A. Fortuin and J. C. den Hartog leg.; LACM
124.505, Thailand. Phuket Island.
Records in the Uterature: Australia: Queensland,
Thetford Reef off Caims (Loch, 1982: 4). Philippines;
Bongao Channel, Sanga Sanga (Robertson, 1963; 57-.58,
pi. 5, fig. 4). Thailand;"Rava Island (Dushane, 1988a; 32).
Maldives, Little Hiva (Dushane, 1988a: 32). Red Sea:
Straits of Tiran (Dushane, 1988a: .30-31); Sinai, Thomas
Reef 27°.59'N, 34°27'E (Dushane, 1988a; .32).
Distribution (Figure 2): Australia (Queensland), In-
donesia (Sulawesi), Philippines, Thailand, and Red Sea.
Habitat: Snails were recorded at 6-12 m depth. Coral
hosts were Ctenactis cchinata (Pallas, 1766), and Her-
poUtlia Umax (Esper, 1797). Groups of one to four snails
were found in the sand (sometimes buried) under a sin-
gle coral; sometimes close to a few hundred egg cap-
sules.
Remarks: The data provided bv Sherbom and Wood-
ward (1901) are insufficient to indicate the exact vear of
publication of the new taxa in Kiener's monograph on
the Genre Scalaire'. We follow Troschel (18.39), who
Listed Kiener's undated work, with the new species in it,
in his 'Report on the achievements in zoology during the
year 1838. V. MoUusca' [in German]. The names are
printed botli on the plates and in the main text of Kie-
ner's work. The severely damaged holotspe of this spe-
cies (Figures .'3-4) is a relatively elongate shell. Shells of
this species are most similar to those of Epitonium pal-
lasii (Kiener, 1838), a species originally described from
an unknown locality, but now known from the Indo-West
Pacific (Kaicher, 1980: 2382; Eisenberg, 1981; pi. 37, fig.
9; Wilson, 1993: 278, pi. 44, fig. 6a-b). According to
Kiener (1838) and in agreement with Wilson's descrip-
tion ("about ten costae on the last whorl") and the fig-
ures in the litterature, E. paUasii differs from E. costii-
latum h\ the stronger shells with thicker costae, which
are more widely spaced. Dushane (19S8a: .'30, fig. 2) fig-
ured very similar egg capsules of this species, reporting
two connecting threads for material from the Red Sea.
Epitonium hoeksemai A. Gittenberger and Goud new species
(Figures 9-10, 18, 20, 26, 43)
Description: Shell (Figures 9-10, 18, 20, 26) (n = 9):
Ven- fragile, elongate-conical, creamy white, reaching
19 mm in length. Length/width 1.6-1.9-2.4. Protoconch
whorls 3. Maximum protoconch 1 diameter 0.13 mm (n
= 2). Protoconch with numerous very fine, incised, axial
lines. Teleoconch whorls up to 9 1/8, separated b)' a
moderately deep suture. Teleoconch sculpture (Figures
IS, 20) of somewhat unevenly spaced, orthocline, rela-
tively low costae, and low spiral threads that become
conspicuously more numerous and variable on the ab-
apical whorls. Costae on entire teleoconch more prom-
inent than spiral sculpture. Third teleoconch whorl has
ca. 12 spiral threads, fifth ca. 25. Costae not alwa\s con-
tinuous, touching the adjoining whorls, where thev are
curved adaperturallv. Fiftli teleoconch whorl (width 2.1
Gittenberger et al, 2000
Page 5
Figures 5-14. Species of Epitonium associated with mushrooni corals off Ujung Pandang. 5-6. E. costulatuin (Kiener, 1838),
length 2.8 cm. 7-8. E. ingridae new species, holotype, NNM 59088, length 2.0 cm. 9-10. £. hoeksemai new species, holotype,
NNM 59074, length 1.3 cm. 11-12. E. tihi Pilsbry, 1921, length 1.6 cm and 1.0 cm, respectively. 13-14. E. lochi new species,
holot>pe, NNM .59094, length 0.9 cm.
mm) with 24—27-29 costae. Five mm width whorl (whorl
8, 9 or 10) with 32-35-38 costae. Aperture subcircular.
Apertural length/shell length 0.28-0.29-0..30. Umbilicus
very narrow.
Egg capsules (Figure 43): Sub-.spherical, white, tran.s-
parent. with protuberances, no noticeable embedded
sand. Capsules closelv connected to each other along a
twisted mucous thread.
Page 6
THE NAUTILUS, Vol. 114, No. 1
Figures 15-21. SEM micrographs of species of Epitonitim associated with uiuslinKim corals off Ujung Pandang. 15-16. E. lochi
new species 15. Shell. Scale line = 1 mm. 16. Protoconch. Scale line = 0.1 mm. 17. £. tihi Pilsbrw 1921, shell. Scale line = 1
mm. 18. E. hock.scmai new species, apical whorls. Scale line = 1 mm. 19. E. twilac new species, teleoconch whorl sculpture. Scale
line = 0.1 mm. 20. E. hoeksemai new species, teleoconch sculpture. Scale line = 0.1 mm. 21. E. iilii Pilsbr\', 1921, teleoconch
whorl sculpture. Scale line = 0.1 mm.
Habitat: This species was recorded between 5-15 me-
ters depth. Coral hosts were Heliofungia actinifonnis
(Quoy and Gaimard, 1833) and Fungia ftiugitcs (Lin-
naeus, 1758). One to 5 specimens were found attached
by mucous threads to the underside of a coral, near a
few hundred egg capsules.
Type material: Holohpe NNM 59074, from t)pe lo-
caliU-. Parat\pes: NNM 59081/1, Indonesia, Sulawesi, off
Ujung Pandang, W. Lae-Lae, 9 m; NNM 59079/1, MZB/
1, W' Bone Baku, 6 m: NNM 59080/1, 59082/1, 9 ni;
NNM 59086/2, t\pe localit\-: NNM 59076/1, 6 m; NNM
59077/5, 12 m: NNM 59083/1, E Kudingareng Keke, 3
Gittenberger et al, 2000
Page 7
m: NNM 59078/1. W. Kudingareng Keke, 12 m; NNM
59075/1, 14 m; NNM 59084/1, NW. Lankai, 6 m; NNM
59087/2, Bone Lola. 15 m; NNM 59085/1. Bone Tam-
biing. 6 ni.
Type locality: Indonesia, Sulawesi, off Ujimg Pan-
dang. W Samalona. 5 m tlepth.
Distribution: Onlv known from Indone.sia, off Sula-
wesi.
Etymology: This species is named after Dr. B. W.
Hoeksema, who supervised the field portion of this pro-
ject.
Remark.s: Shells of this .species resemble those of Ep-
ituniuin iilu, but differ b)- a lengtli/width ratio of ca. 1.9
instead of ca. 2.6. Because most examined specimens are
damaged, the fine structure of the costae could not be
observed. The teleoconch sculpture appears alwavs ob-
solete to the naked eye and the number of spiral threads
increases more evidently in E. huehscmai, with ca. 13
spiral threads added between the third and the whorl.
In £. lochi new species (see below), on the other hand,
there is a more clearly reticulate sculpture on the early
teleoconch whorls.
Epitonium ingridae A. Gittenberger and Govid new species
(Figures 2. 7-8. 23-24. 27. .30. 36. 46)
Description: Shell (Figures 7-8, 23-24, 27, 30) (n =
5): Verv fragile, moderatelv slender conical, creamy
white; reaching 20.8 in length. Lengtli/width 2.0-2.2-
2.3. Protoconch whorls ca. 3. Protoconch with three
whorls, with numerous fine, incised, axial lines. Maxi-
mum diameter of protoconch 1. 0.14-0.15 mm (n = 2)
(Figure 30). Teleoconch whorls up to 10, separated by
deep suture. Teleoconch sculpture of evenly spaced, or-
thocline, thin, lamellate costae, and numerous very fine
spiral threads (>100 on the 9th whorl), superimposed
on somewhat coarser spiral cordlets (ca. 15 on fifth te-
leoconch whorl). Initial whorls with multiple, lamellate
costae, fused together to form thicker ones (Figures 23,
24). Coarser spiral cordlets are most prominent on initial
teleoconch whorls, where thev are superimposed on cos-
tae (Figure 24); coarser cordlets become obsolete on
most abapical whorls. Costae are more or less damaged
in all specimens; better preserved costae coronate. Par-
ticularly below the periphery', costae somewhat curved
abaperturally at their free margins, whereas adapically
more erect and shghtly curved abaperturally or adaper-
turally near suture, depending on position of costa on
adjoining whorl. Costae mostly continuous, but hardly
touching each other. Fifth teleoconch whorl (width 3.8
mm) with 20-24-31 costae. Five mm width whorl (whorl
6 or 7) with 23-30-33 costae. Aperture subcircular. Ap-
ertural lengtli/shell length 0.3. Umbilicus very narrow.
Egg capsules (Figures 36, 46) (n = 8): Oval (Figure
36), embedded with sand and closelv C(jnnected along
straight, longitudinalK striated, mucous thread (Figure
46). Capsules 3,0-3.3-3.5 mm length and 1.5-1.6-2.0
mm in width. Capsules cont;un 93-120-173 white eggs.
ProlM
)scis:
Whitish
Type material: lloiotvpe NNM 59088, from t\pe lo-
calih. Paratopes: NNM 59089/1. Indonesia, Sulawesi, off
Ujung Pandang, W. Kudingareng Keke, 12 m; NNM
59090/2. 59092/1. E Samaknia. 9^m: NNM 59091/1, 24
m; NNM 59093/1, Bone Tambung, 7 m.
Type locality: Indonesia, Sulawesi, off Ujung Pan-
dang, ESE. Kudingareng Keke, 15 m.
Other material examined: AMS 329657, Australia,
Queensland, off Macgillivray Bav, Lizard Island,
14°39'S, 145°29'E. 10 m, I. Loch leg.; NNM unnum-
bered, 1 shell, Indonesia, Ambon, llitu. outer part of
Ambon Bav, eastern Laha, J. C. den Hartog leg.
Distribution (Figure 2): Australia, Queensland; In-
donesia, Ambon, and Sulawesi.
Habitat: Specimens of this species were found be-
tween 7-24 meters depth. Coral hosts were Fungia con-
cinna Verrill, 1864, F fungites, Hcliofungia actinifonnis,
Herpolitha limax and Foh/pht/llia talpina (Lamarck,
1801). Specimens were found attached by mucous
threads to the underside of a coral; one or two speci-
mens were found associated with up to a few hundred
egg capsules.
Etymology: This species is named after Ms. Ingrid
van der Loo. Leiden.
Remarks: Conchologically this species resembles the
■probaiile hoIot)pe" (Kaicher, 1981: 3036) of Epitonium
clubium Sowerby 1844 (BMNH 1981234) from the Phil-
ippines, which is an imperfect shell with a broken ap-
erture and several apical wliorls missing. Its length could
have been ca. 20 mm. Costae of adjacent whorls are
continuous, slightly curved toward aperture adapically
and away from aperture abapically, not projecting over
suture. The holotvpe of Epitonium duhium most clearlv
differs from E. ingridae bv its less prominent teleoconch
sculpture and thicker, not lamellate costae. The speci-
men figured bv De Boury (1912: pi. 7, fig. 4, Scala du-
hia), which might represent E. duhium (of. Kilbum,
1985: 327) has more oblique costae. The identih' of Sca-
laria graiji Nvst. 1871, (nomen novum for Scalaria stri-
ata Gray, 1847, not Defrance, 1827) is unclear; Tryon
(1887: 60, as S. striata) and De Bour\- (1912: 95, as S.
striata and S. graiji) considered this nominal ta.xon a syn-
onym of S. duhia. Kilburn (1985: 327) questioned this
synonym)'. The shell of S. graiji figured by Tryon (1887:
pi. 12, fig. 68, as S. striata) has a more shallow suture
and relatively larger aperture when compared to E. in-
gridae. The new species also resembles Epitonium fria-
hilis (Sowerby 1844) from Western Australia. Swan Riv-
er The holotvpe (BMNH 1966653). figured b\ Kaicher
(1980: 2329).' is 16 mm in length ancf 7 mm in width,
with ten whorls. It differs most conspicuousK' from E.
ingridae bv its closed lunbilicus and absence of spiral
threads. The species described and illustrated from Svd-
ney Harbour as Foliaceiscala barLssa by Iredale (1936:
Page 8
THE NAUTILUS, Vol. 114, No. 1
Figures 22-31. SEM micrographs of species of Epitoniiiin associated with mushroom corals off Ujimg Pandang (unless stated
otherwise). 22. E. costulatum (Kiener, 1838), Indonesia, Ambon, Hitu, outer part of Ambon Bay, W Lalia, apical whorls. Scale line
= 0.5 mm. 23-24. E. in^ridae new species 23. Apical whorls. Scale line = 0.5 mm. 24. Teleoconch whorl sculpture. Scale line =
0.1 mm. 25-29. Protoconch. 25. E. costulatum (Kiener, 1838) (same shells as figure 22). Scale hne = 0.1 mm. 26. E. hoeksemai
new species. 27. £. inffidae new species. 28. E. twilae new species. 29. E. uhi Pilsbr\', 1921. Scale hne = 0.1 mm. 30-31.
Protoconch 1. 30. £ ingridae new species. 31. E. twilae new species. Scale line = 0.02 mm.
Gittenberger el ai. 2()()()
Page 9
Figures 32-35. Species of Epitoniiim often confused in the
literature. 32-33. E. tivilae new species, holotype, NNM
59104, length 1.5 cm. 34-35. £. buUntitm (Sowerby, 1844),
holotype, BMNH 198136, length 2.0 cm.
300, pi. 22, fig. 15) seems to be similar in shape and
size, but the costae are described as "of different
strength, some fine, others large and recurved, while still
others approach varices in size."
Epitoniiim lochi A. Gittenberger and Goud new species
(Figures 13-16, 37, 45)
?Epitonium species 4: Loch, 1982: 4-5, 1 fig. (see remarks
below).
Description: Shell (Fig^urc.s 13-16) (n = 4): Very
fragile, elongate-conical, creamy white, reaching 8.5 mm
in length. Length/width 2. 0-2. .3-2. 7. Protoconch whorls
3.25. Maximum diameter of protoconch 1 diameter 0.12
mm (n = 1). Protoconch with numerous fine, incised,
axial lines. Teleoconch whorls up to 8, separated by a
very deep suture. Teleoconch with evenly spaced, or-
thocline, lamellate costae, crossing low spiral threads
that are approximateK' a half to a fifth as wide as inter-
spaces (Figure 15). Reticulate pattern present on most
adapical whorls, replaced by spiral threads on later
whorls. Third whorl with ca. 13 spiral threads, fifth one
with ca. 15; spiral threads equally prominent throughout
whorl. C^ostae usualK not continuous, lamellar hut rather
low, barely touching preceding whorl. Due to damage in
most specimens, fine structure of costae could not be
examined. Fifth teleoconch whorl (width 1.3 mm) with
24-25-26 costae and 12-13-15 spiral threads. Aperture
subcircular Apertural length/shell length 0.22-0.23.
Umbihcus absent.
Egg capsules {Figures 37, 45): The roundish, white,
egg capsules (Figure 37) are mixed with sand, and close-
ly connected to each other along a straight mucous
thread without well-defined sculpture (Figure 45).
Type material: Holotv'pe NNM 59094, from type lo-
calit)'. Paratopes: NNM 59095/2, 59096/1, Indonesia, Su-
lawesi, off Ujung Pandang, MZB/1, tyi^e locality; 16 m;
NNM 59098/1, 18 m; NNM 59099/1, E Kudingareng
Keke, 3 m; 59100/1, 12 m; 59102/1, 18 m; NNM 59101/
2, ESE Kudingareng Keke, 15 m; 59103/1, Pulau Badi,
24 m. See also Remarks.
Type localitj': Indonesia, Sulawesi, off Ujung Pan-
dang, W Kudingareng Keke, 12 m.
Other material examined: AMS 329687/2, Australia,
Queensland, Lizard Island, Watsons Bav, 14°40'S,
145°27'E, 24 m, I. Loch leg.; AMS 329688/1, 329689/1,
Granite Bluff, 14°39'S, 145°27'E, 23 m, I. Loch leg. (see
Remarks below).
Distribution: Indonesia and probably Australia.
Habitat: The snails were found between 3-24 m.
Fuitgia costulata Ortmann, 1889, and F. tenuis Dana,
1846, were coral hosts. If the Australian record really
proves to be this new species, Fungia ci/clolitcs La-
marck, 1816, should be included as an additional host
(Loch, 1982: 4). One to 4 specimens were found at-
tached by a straight mucous thread (Figure 45) to the
underside of a coral accompanied by up to a few hun-
dred egg capsules.
Etymology: This species is named after Mr Ian Loch,
who described this or a very similar species from Aus-
tralia, without naming it.
Remarks: Loch (1982) referred to and figured an un-
named species 4' from Australia, distinguishing it from
E. ulii. We were able to compare that material with the
specimens collected off Ujung Pandang. In the Austra-
lian specimens, the spiral threads are somewhat more
prominent, which could represent some degree of intra-
specific variation. The limited amount of material does
not allow for conclusions on the identity' of the Austra-
lian specimens; this prevented their inclusion as para-
types.
Conchologically this species is most similar to Epiton-
ium zat rephes MeUiW. 1910 (holotype BMNH
191281683), from the Mekran coast. This shell is figured
by Kaicher (1980; 2377); it differs bv having continuous
Paee 10
THE NAUTILUS, Vol. 114, No. 1
Figures 36 — 48. .Spt'cii-N ol Epiloniiim associated with imislirooiu corals oii L'luiig Pandang. 36-38. Egg capsules. 36. E. ingridae.
Scale line = 1 mm. 37. E. lochi new species. Scale line = 1 mm. 38. E. costiilatum (Kiener. LS38). Scale line = 1 mm. 39. Sclerite
of alcvoniid octocoral found in association with egg capsules ot E. costiilatiim. Scale line = 0.1 mm. 40. Detail of figure 39. Scale
hue = 0.1 mm. 41. E costiilatum. Eggs within a capsule. 42. E iilii Egg capsule with protoconchs 1. Scale line = 0.1 mm. 43-
47. Mucous threads. Scale line, with figure 43, = 0.01 mm. 43. E. hoekscinai. 44. E iilii. 45. E. lochi. 46. E. ingridac. 47. £.
costulatiiin. 48. E. twilac, lar\'al shells (= protoconchs 1). Scale line = 0.1 mm.
costae and b\- the more narro\\l\ spaced spiral threads,
which are about as wide as their interspaces.
The holotv'pe of Epitoniuin obliqita (Sowerbw 1844)
[Scalaria] (BMNH 19812.31) also resembles E. lochi. but
differs in having a clearh' open, though narrow, umbili-
cus, and continuous costae.
The holotvpe of Epitoniuin dcficrsi (Jousseaume,
1911) [Tenuiscala] (MNHN De Bou'r\-2706) from Aden,
which has a broken aperture and missing apical whorls,
can notwithstanding be distinguished from £. loclii bv
the relatively small shell lengtli/width ratio (only ca. 1.9)
and the presence of some varices. This holot\pe is also
figured by Kaicher (1981: 3116).
Epitoniuin twilae A. Gittenberger and Goud new species
(Figures 2, 19, 28, 32-33, 48)
Epitonium bullatum (Sowerbv, 1S44): Dushane. 1988; .30, figs.
5, 6. Yamashiro, 1990: 299, figs. 1-6. Not Scahiha hulla-
tum Sowerby, 1844.
Epitonium species 2: Loch, 1982: 3^, 1 fig.
Epitonium sp.: Bratcher, 1982: 3, fig. 1.
DescripHon: Slull (Fifiures 19, 28, 31, 32^3, 48) (n
= 20): Very fragile, broad-conical, creamy white,
reaching 17 mm in length. Lengtli/width 1.2-1.-1-1.6.
Protoconch whorls 3. Protoconch widi numerous verv
fine, incised, axial lines. Ma.\imum protoconch 1 diam-
eter 0.12-0.13 mm (n = 2). Teleoconch whorls up to 9,
straight-sided, separated h\ a shallow suture. Teleoconch
sculpture (Figure 19) of unevenly spaced, fine, ortho-
cline, more or less obsolete costae, not or onK' in part
lamellate, and numerous low spiral threads that are sep-
arated bv interspaces that varv from as wide as the spiral
threads to three times as wide. Costae not continuous,
not curved, barely touching adjacent whorls. Fifth teleo-
conch whorl (width = 2. .5 mm) with 19-24.4-30 costae.
Five mm width whorl (whorl 6 or 7) widi 24-31-36 cos-
Gittenberger et ai, 2()()()
Page 11
tae. Aperture subcircular. Apertural length/shell lengtli
0.37-0.44-{).52. Umbilicus ven uanou.
E<i^ capsules (ti = 10): Egg capsules roundisli, white,
transparent, with protuberances, without embedded
sand, closely connected along straiglit mucous thread.
Egg capsules 1.2-1.4—1.6 mm diameter with 342^25-
532 white eggs per capsule.
Type material: Holotvpe NNM 59104, from type lo-
calit\. Paratopes: NNM 59149/1, Indonesia, Sulawesi, off
Ujung Pandang: W Lae-Lae, 7 m: NNM 59148/2, 9 m;
NNM 59145/L t^pe !ocalit^■, 3 m; NNM 59105/1. 591.38/
3, 6 m: NNM '59127/1, 59129/1, .59141/10, 59147/1,
59150/2, 9 m; NNM 59126/1, 59142/1, 59143/1, 12 m;
NNM 59146, 15 ni; NNM .59139, ESE Samalona, 5 m;
NNM 59131/4, 12 ni; NNM 59140/5, 13 ni; NNM
59116/1, 59117/1, 591.32/3, 591.3.3/2, 59134/1, .591.35/1,
W Samalona, 9 m; NNM .59121/1, 59122/1, 12 m: NNM
59118/1, 15 m; NNM .59151/1, E Kudingareng Keke, 9
m: NNM 59106/1, .59107/1, W Kudingareng Keke, 9 ni;
NNM .5911.5/3, 10 m; NNM .5911.3/1, .59114/1, 12 ni;
NNM 59108/1, .59109/1, .59110/1, .59111/2, .59112/1, 15
m: NNM .5912.3/1, .59124/1, 18 m; NNM .591.52/1,
.591.5.3/1, 24 m; NNM .591.37/1, NW Lankai. 12 ni; NNM
.59159/5, Pulau Badi, 25 m; NNM 59161/2, Bone Lola,
8 m: NNM 5959160/1, 9 m; NNM 59154/2, 591.5.5/2,
.59156/2, 5916,3/1, Bone Tambung, 5 m; NNM 59157/1,
22 m. Onh' the specimens from off Ujung Pandang are
considered the t\pe series (see Distribution below).
Type locality: Indonesia, Sulawesi, off Ujung Pan-
dang, W. Bone Baku, 6 m.
Other material examined: AMS 3296.5.3/1, Austraha,
Queensland (see also Loch, 1982: 3, 4, 1 fig.): No. 5
Sandbank Reef, 1.3°45'S, 144°16'E, 9 m, I. Loch leg.;
AMS 09980.3/2, 0998041, 09980.5/1, 099806/1, 100188/
14, .329680/1, .32968.3/2, off Lizard Island, 14°39'-
14°42'S, 14,5°23'-145°28'E, 2-11 m, P H. Colman, 1.
Loch and W. F. Ponder leg.; AMS 329672/1, Opal Reef,
N. of Cairns, 16°15'S, 14.5°.50'E, 9 m, I. Loch leg.; AMS
09657.5/2, 101238/2, 147334/2, 329676/4, 329679/3,
329670/1, E-NE of Townsville. 18°46'-18°57'S,
147°31'-147°44'E, 9-18 m, I. Loch leg. NNM unnum-
bered, Indonesia, Ambon, Hitu, outer part of Ambon
Bay, W Laha, J. C. den Hartog leg.; NNM unnumbered,
Sulawesi, off Ujung Pandang.
Records in the literature: Papua New Guinea, Na-
gada (16 km N of Madang) (Bratcher, 1982: 3, 1 fig.).
Japan: Sesoko Island, Okinawa (Yamashiro, 1990; 299-
305, figs. 1-6). Red Sea, Sinai, Thomas Reef, 27°59'N,
.34°27'E (Dushane, 19SSa: 31, figs. 5, 6).
Distribution (Figure 2): Australia (Queensland),
Papua New Guinea, Indonesia, Japan, and Red Sea.
Habitat: This species was found from 3 m to the max-
imum diving depth of 24 meters. In the literature that
might refer to this species a depth of 45 meters was
mentioned (Loch, 19S2). The following coral host spe-
cies were recorded: Ctcnactis echinata, Heiyolillui li-
max, Sandtilolitlui dcntata Quelch, 1884, S'. rolnista
(Quelch, 1886) and Zoopiltis echinatus Dana, 1846.
Clung with mucous threads to the underside of a coral,
one to fourteen specimens were found accompanied by
up to a few hundreds of egg capsules.
Etymology: This species is named after Mrs. Twila
Bratcher, of Los Angeles, California, USA, vylio first dif-
ferentiated the new taxon from E. Imllotiint.
Remarks: This species has been misidentified by var-
ious authors (Dushane, 1988a; Yamashiro, 1990; Mienis,
1994, conditionally) as Epitonium hullatum (Sowerbv,
1844), a species associated with sea anemones (Kilburn
and Rippey, 1982; Kilbum. 1985; Mienis, 1994). The
badly damaged holot)pe of E. buHaturn (Figtires 34, .35)
has a more globular, far less fragile shell with convex
whorls, costae occasionally forming a varix, and only
about 5 teleoconch whorls at a length of 19 mm (several
apical whorls are missing). The specimens illustrated by
Jousseaume (1921: pi. 3, fig. 2), Azuma (1962: fig. 2, as
Globiscala koshiwajimcnsis), Kilbum and Rippev- (1982;
pi. 11, fig. 15), Kilbum (1985: .3.30, figures 160-163) and
Wilson (1993: pi. 44, fig. 9) exemplifs- the variability- of
E. hiillnfiiin. Although £. tuihic differs conspicuousK- in
shape from the other Epitonium species in this studv; its
protoconch (Figures 28, 31, 48) cannot be distinguished
from that of these other species.
Yamashiro (1990) published various data on the life
history of £. twilac (as E. huUatum). That author de-
scribed the egg capsules as elliptical, 0.88 mm in length
and 0.75 mm in width, containing 38-98 eggs each.
These data chffer from our results. Based on very similar
shell morphologies, however, we consider his specimens
and the ones examined in this section to be conspecific.
Despite the fact that E. twilac differs markedly in
shell morphology from E ulu, the protoconchs of these
species are yer\' similar
Epitonium uhi Pilsbrv, 1921
(Figures 2, 11-12, 17, 21, 29, 44)
Epitonium ulu Pilsbiy, 1921: 376, fig. llc; Bosch, 196.5; 267,
fig. 1: Robertson, 1970: 4.5; Hadfield, 1976: 1.35, Table 1;
Tavlor, 1977: 253, 2.58, fig. 7; Kav, 1979: 1.56, fig. 5.3a, b;
Loch, 1982: 3, 1 fig.; Bell, 1985: '1.59, figs. 1-6; Dushane,
1988a: 31, figs. 3, 4; 1988c: 9, 1 fig.; Wilson, 1993: 273.
Description: Shell (Fipircs 11-12, 17, 21, 29) (n =
20): Very fragile, elongate-conical, creamy white;
reaching 16 mm in length. Lengtli/width 2. .3-2. 6-3. 6.
Protoconch whorls 3. Maximiun protoconch 1 diameter
0.13 mm (n = 2). Protoconch with numerous, ver\- fine,
incised, axial lines. Teleoconch whorls up to 12, sepa-
rated by moderately deep suture. Teleoconch sculpture
varxing in intensit)' from well-defined to obsolete. Cos-
tae unevenly spaced, orthocline, more or less lamellate
or obsolete, not continuous, relatively prominent adapi-
cally and clearK' encroaching on adjacent whorl, curxed
in adapertural direction (Figure 21). Spiral threads vary
in strength on a single whorl; spiral threads only slightly
Page 12
THE NAUTILUS, Vol. 114, No. 1
increasing in number on later whorls. Fifth teleoconch
whorl (width 2.0 mm) with 15-23-28 costae and 9-11-
15 spiral threads. Five mm width whorl (between whorl
8 and 11) with 19-28-33 costae and 10-14-25 spiral
direads. Aperture circular to somewhat oval. Apertural
length/shell length 0.20-0.26-0.29. Umbilicus very nar-
row to closed.
Egg capsules (Figure 44): Egg capsules roundish to
oval, white, granulated, sometimes embedded with sand.
Egg capsules closely connected along a twisted mucous
diread (Figure 44)'; Dushane (19S8a; 32) reported 3
t\\isted threads. Capsule diameter 0.8-1.3-1.7 mm (n =
5). One capsule contains 67-225-405 eggs. Dushane
(1988a: 32) reported 400-600 eggs within a capsule,
which she described as papillose, with softly rounded
papillae. Kay (1979: fig. 53B) figures the egg capsules as
elliptical, 1.1 mm in width and ca. 1.6 mm in length. See
Bell (1982; 1985) and Dushane (1988a) for further data
on egg capsules, lite history and other relevant data.
Proboscis: Whitish, with some transversal, transparent
bands.
Type material: Holotype ANSP 127818, from t\pe lo-
caliU'.
Type locality: USA, Hawaii, Hilo.
Other material examined: ANSP 127818. USA, Ha-
waii, Big Island, Hilo; AMS 138321/1, Australia, Queens-
land (see also Loch, 1982: 3, 1 fig.). Eel Reef, 12°24'S,
143°22'E, 4-8 m, I. Loch leg.; AMS 329660/1, Long
Sandy Reef 12°29'S, 143°46'E, 10 m, I. L<xh, leg.; AMS
099801/3, 099802/2, 100821/1, 329656/3, near Lizard Is-
land, 14°40'-14°42'S, 145°23'-145°28'E, 1.5-14 m, P
H. Colman and I. Loch leg.; AMS 138320/1, S Escape
Reef 15°53'S, 145°49'E, 18 m. I. Loch, leg.; AMS
096573/7, 329649/2, 329650/1, 329651/1, 329652/1,
329655/2, 329658/7, E-NE of Townsville, 18°46'-
18°57'S, 147°31'-147°44'E, 6-15 m, I. Loch leg.; NNM
unnumbered, Indonesia: Ambon, Hitu, outer part of
Ambon Bay, E and W Laha, A. Fortuin and J. C. den
Hartog leg.; LACM 86-163. Java, off Jakarta, Kepulauan
Seribu (= Thousand Islands), Pulau Pelangi and Pulau
Putri; AMS 138318/1, Malaysia: Pulau Singa Besar Pu-
lau Langkawi, 6°14'S, 99°44'E, I m, I. Loch, leg.
Records in the literature: USA, Hawaii, Oaliu, Ka-
neoke Bay (Bell 1985: 159-164, figs. 1-6); Papua New
Guinea (Dushane. 1988a: 32; Maldives (Dushane,
1988a: 32); Red Sea, Straits of Tiran, Tiran Island and
Sinafir Island (Dushane, 1988a: 31, 32, figs. 3, 4); Sinai,
Thomas Reef 27°59'N, 34°27'E (Dushane, 1988a: 31,
figs. 5, 6).
Distribution (Figure 2): Hawaii, Australia (Queens-
land), Indonesia, Malaysia, Maldives, and Red Sea.
Habitat: Tliis species was recorded between 3-24 me-
ters depth. Coral hosts were Fungia spinifcr Claere-
boudt and Hoeksema, 1987, F. scabra Doderlein, 1901,
F. concinna, F. horrkla Dana, 1846, F. scniposa Klun-
zinger, 1879, F fungites, F granulosa Klunzinger, 1879,
F. scutaria Lamarck, 1801, F. moluccensis Van der Horst,
1919, F. gravis Nemenzo, 1955, and F. paumotensis
Stutchbury, 1833. One to 11 specimens, free or accom-
panied by up to a few hundreds of egg capsules, were
observed on the individual corals, attached witli mucous
threads to the underside or on the substrate of these
hosts.
Remarks: Shells of this species yar\' considerably in
lengtli/width ratio, intensit\' of teleoconch sculpture and
number of costae. They differ from E. hoeksemai b)' a
lengtli/width ratio of ca. 2.6 instead of ca. 1.9 and b\- the
presence of less than 20 spiral threads on the fifth te-
leoconch whorl. It is the most common epitoniid species
associated with Fungiidae in the study area.
ACKNOWLEDGMENTS
We are particularK- grateful to Dr B. W. Hoeksema for
his most valuable assistance in collecting and identifying
the fungiid corals examined in this article and for con-
tributing his expertise on corals. We thank all who al-
lowed us to examine material in the molluscan collec-
tions under their care; Dr P. Bouchet (MNHN), Mr I.
Loch (AMS), Dr Y. Finet (MHNG), Dr J. H. McLean
(LACM), Dr G. Rosenberg (ANSP). and Mrs. K. Way
(BMNH). We also thank' Mr A. Weil and Mrs. L.
Brown, who contributed expertise on epitoniids, and Dr
L. P. van ORvegen (NNM), who identified the sclerites
associated with some egg capsules. Some photographs
were taken b\- A "t Hooft (Universitv- of Leiden Institute
of Evolutionary and Ecological Sciences, Leiden). This
project was subsidized h\ the Royal Dutch Academ\' of
Sciences, the SHchting Jan Joost ter Pelkwijk-fonds and
the Leiden Universits Foundation.
LITERATURE CITED
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Bell, J. L. 1982. Larval development and metamorphosis of die
prosobranch mollusc Epitonium ulii. associated v\ith a sol-
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Bell, J. L. 1985. Larval growth and metamoqshosis of a pros-
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Bosch, H. F. 1965. \ gastropod parasite of solitan' corals in
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Bouchet, P. and A. Waren. 1986. Revision of the Nordieast
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Clench, W. J. and R. D. Tvmier 1951. The genus Epiionium
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Dushane, H. 1988a. Geographical distribution of some Epito-
Gittenherger et «/., 2000
Page 13
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Dushane, H. 1988b. Hawaiian Ejiitoiiiidac. Hawaiian .Shell
News 36(4):6-7.
Dushane, H. 1988c. Hawaiian Epitoniidae (continued). Ha-
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Eisenberg, J. M. 1981. \ collector's guide to sea shells of the
world. Bloonisburv, Books, London. 2.39 pp.
Hadfield, M. G. 1976. .Vlolhi.scs as.sociated with li\ing tropical
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(Scleractinia), a dispersion mechanism and sui"viv;J strat-
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At the time the manuscript was being sent for tvpesetting, the
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This work apparently does not contain data that could substan-
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THE NAUTILUS 114(1):14-17, 2000
Page 14
A new species of Columhella (Neogastropoda: Columbellidae)
from the Caribbean Neogene
Maria J. deMaintenon
Department of Marine Science
Universitv of Hawaii at Hilo
200 W. Kawili Street
Hilo. HI 96720 USA
deniainte@ha\vaii.edu
ABSTRACT
A new species of CohimbeUa is described from the Neogene
of the southwestern Caribbean and compared widi other Ca-
ribbean CohimhcUa species. The new species is a member of
a species pair diitering primarily in inferred lar^'al ecolog\-. Pro-
toconch morphology suggests that the new species had planktic
development, whereas its extant analogue. Columhella mcrca-
toria (Linnaeus, 1758), has nonplanktic development. Though
tlie 2 species were contemporaneous. the\' do not appear to
have been svmpatric.
Kcif words: Colombia. Costa Rica, lanal ecolog\'. protoconch.
INTRODUCTION
Evolutionary divergence in larval ecology between
planktic and nonplanktic modes i.s a common pattern in
marine molluscs. Many gastropod genera in several fam-
ilies display both reproductive modes. Recent evolution-
arv divergence may result in pairs of .species differing
primariK- in lar\al shell moq^hologx-. Traditionally such
variation was considered as evidence for poecilogony in-
traspecific variation in larval developmental modes. Re-
cent reviews of poecilogony in marine invertebrates
(Hoagland and Robertson, 1988; Bouchet. 1989; Knowl-
ton, 1993; Oli\erio, 1996) however, ha\e found httle ev-
idence to definitiveK' support that poecilogony occurs.
Hoagland and Robertson (I98S) reviewed reported cases
of poecilogon\' in marine gastropods, and concluded that
the pattern of larval development is generalK informa-
Hve in species-level invertebrate swstematics. The pur-
pose of this paper is to describe a new species of col-
umbellid gastropod, CohimhcUa mohiciisis, that differs
from another Caribbean CohimhcUo species in its in-
ferred developmental mode. AdditionalK. the 2 species
appear to be allopatric, lending further support to their
taxonomic distinction.
CohimhcUa Lamarck, 1799 is primariK- a tropical
American taxon, consisting of 15 Neogene and Recent
American species and 2 species in the eastern Atlantic.
Phylogenetic analyses of representative columbellid ta.\a
(deMaintenon. 1999) supports the monoph\K of Col-
umhcUa. based on 8 characters of anatom\-, radular mor-
phology' and shell morpholog)-. Recent species of Col-
iimhcUa are differentiated primarily on the basis of con-
chological characters. The extant species comprise 2
morphological groups, one of which occurs in the Atlan-
tic. The Atlantic CohimhcUa species are very similar, and
are characterized by having shells with spiral cords over
die entire shell surface. The\' differ primariK' in shell
coloration and in the number and strength of spiral
cords. Jung (1994) recently reviewed the fossil species
of the Atlantic group in a discussion of the CohimhcUa
species from the Neogene of the Dominican Republic.
The extant members of the Atlantic group include 2 spe-
cies in the eastern Atlantic and 2 in die western Atlantic.
The known fossil record of the group extends back to
the late Miocene. Of the living and fossil species of Col-
iimhcUa in the Atlantic, the new species is the onK' one
considered to have planktic development.
The second group comprises the 10 extant Panamic
CohimhcUa species. These differ from the Atlantic group
by lacking spiral cords on the shell except as juveniles.
All members of the Pacific group have multiwhorled
protoconchs, and are inferred to have planktic devel-
opment. The fossil record of this group is unk-nown be-
fore the Pliocene, when the extant species appear Al-
lopatric species pairs differing in developmental mode
alread\' have been reported in the group of Atlantic Col-
umhella species. Moolenbeek and Hoenselaar (I99I) dif-
ferentiated 2 species in the eastern Atlantic: CohimhcUa
nistica (Linnaeus. 1758) with nonplanktic development,
in the Mediterranean and eastern Atlantic coast, and
CohimhcUa adansoni (Menke, 1853) with planktic de-
velopment, endemic to the offshore islands of the east-
em Atlantic. Stud\' of alloz\me data from these 2 species
(Oliverio, 1995, 1996) indicates that they thverged about
2 million years ago. The new species described herein
has a similar relationship with one of the western Atlan-
tic species, Columhella mcrcatoria (Linnaeus, 1758).
The following institutional abbrexiations are used: UF,
Universit\' of Florida, Florida Museum of Natural His-
M. J. deMaintenon, 2000
Page 15
torv'; SBMNH, Santa Barbara Museum of Natural His-
tor\-: UCMP, Unhersih' of California Museiun of Pale-
ontologN ; uses, United States (Geological Survev;
USNM, National Museum of Natural History-, Smithson-
ian Institution.
The micrographs in figures 1 and 2 were taken using
the Elettroscan Environmental Scanning Electron Mi-
croscope at the Universit)' of California Museum ot Pa-
leontology. Specimens were scanned uncoated, at 15 k\'
and between 2 and 3 Torr water vapor.
SYSTEMATICS
Famil\- Columbellidae Swainson, 1840
Genus ColumheUa Lamarck, 1799
Columbclla luoincnsis new species
(Figures 2, 4-8, Table 1)
Description: Shell small, stronibiform, up to 19 mm
shell length. Aperture length slightK' more than half
shell length. Protoconch conical, multiwhorled, smooth,
widi 3 whorls. Teleoconch with 6-7.5 whorls, with spiral
cords over all whorls. Bodv whorl with 12-18 cords
counted at the aperture edge, continuing anteriorlv to a
few finer cords at the base of the shell. Each spire whorl
with 4-6 cords visible. Usually vvith a prominent, slighth-
nodulose cord at the shoulder, which is most often the
second cord below the suture. First 2-3 teleoconch
whorls with nodules at the periphers' and weak axial
ridges, which fade out on subsequent whorls. Aperture
constricted by inrolled labial edge, thickest in the center.
Labial edge with 10-12 denticles, facing inward. Colu-
mella with 2 weak folds. Anterior parietal wall with 5-
10 denticles in an axial row. Short posterior parietal cal-
lus, continuous with aperture edge.
Type material: Holot>pe, UCMP 39918, 12.8 mm
long, 7.5 mm wide, Uq^e iocalit>'. Para^pe UCMP 39919,
t\-pe localit)'; Paratopes UCMP 39920 and 39921, Upper
Tubara Group, below type localit\', Punta Pua, Bolivar,
Colombia; Paratype USNM 501150, Moi'n Fm. 2 km
west of Puerto Limon, Costa Rica; Paratvpe USNM
501151, Mofn Formation, between Puerto Limon and
Pueblo Nuevo, Costa Rica.
Type locality: Upper Tubara Group, Punta Pua, about
15 miles northeast of Cartagena, Bolivar, Colombia
(UCMP S-66).
Other material examined: USGS localit\' 21037, 1
specimen, Moi'n Formation, outskirts of Puerto Limon,
Costa Rica; UCMP S-66, 11 .specimens; UCMP S-65, 2
specimens; TU 954, 1 specimen; TU 956, 1 specimen.
Distribution: The k-nown lots of Coliimbella moinen-
sis are from the Pliocene to Pleistocene (?) of Costa Rica
and Colombia. The material from Colombia lacks pre-
cise stratigraphic data but is thought to be from the Mio-
cene to Pliocene Tubara Group (Yokes, 1990). Yokes
(1990) reported that the muricid species she studied
from these 2 (^oloniiiian localities are tspical of the
Pleistocene Moi'n fauna from Costa Rica. .Although the
Moi'n Formation has better stratigraphic definition than
the above mentioned units, some controversy exists
about the age of the formation. Coates et al. (1993) state
that the Moi'n Formation is Late Pliocene in age, how-
ever its fainias are more usuallv considered to be Pleis-
tocene in age (Robinson, 1993, and references therein).
Thus the stratigraphic range of this species is currently
imprecise.
Etymology: Columbclla itwiucitsis is named after the
Moi'n Formation of Costa Rica.
Discussion: Columbclla uioincusis is verv' similar to
Columbclla mercatoiia (Linnaeus, 1758) (Figure 3). a
common western Atlantic species k-nown from the Pli-
ocene to the Recent. The new species can be differen-
tiated from C. mercatoiia by its multiwhorled proto-
conch. Columbclla mercatoria has 1.5 to 2 bulbous pro-
toconch whorls (Figure 1), with at least one specimen
having 2.25 whorls. The new species has a conical pro-
toconch with 3 whorls (Figure 2), and its nuclear whorl
is smaller than that of C. mercatoria. This latter species
has nonplanktic development; its eggs hatch as crawling
juveniles after about 33 days, during which the larvae
feed on nurse eggs in the capsules (Bandel, 1974). The
multiwhorled protoconch of C. moinensis, in contrast, is
indicative of plank-tic development.
Columbclla mercatoria varies greatly in adult size and
strength of sculpturing, as do many other Columbclla
species. In the case of C mercatoria, this variation may
be a function of environment. In southern Florida, the
species is commonlv associated with both reef rock and
seagrass habitats, and specimens found in seagrasses
tend to be smaller and less brightK patterned than reef
specimens. The k-nown specimens of C. moinensis come
from only 6 lots, and most of the material is similar in
size. The single specimen from LISGS localit\' 21037
(USNM 501152, Figure 8) is inarkedK' larger than other
specimens (Table 1), and has a weaker shoulder. It does
have a multiwhorled protoconch (broken off though still
with the shell) consistent with that of C. moinensis, so
will be referred to the new species in spite of the dif-
ferences between it and odier specimens.
Many of the specimens that are considered to repre-
sent C moinensis have eroded protoconchs and thus
cannot be diagnosed with certaintv. However, the\- are
comparable in shape and size to specimens of C mo-
inensis from the same localities.
Columbclla tnercatoria was contemporaneous with C.
nwinensis. However, the 2 species have not so far been
found svmpatricallv. Columbclla mercatoiia has been
collected in the Pliocene and Pleistocene Mare and Abi-
sinia Formations of Yenezuela (Weisbord, 1962) and in
the Pliocene Bowden Formation of |amaica (a worn and
damaged .specimen incorrectK' identified as Columbclla
submercatoiia is illustrated by Woodring, 1928).
Columbclla submercatoria Olsson, 1922 occurs in the
Late Miocene of the Dominican Republic (Jung, 1994)
Page 16
THE NAUTILUS, Vol. 114, No. 1
Figure 1. Recent CoIuml>elln mercntoria. protoeonch. UF 126820. Colon Iskuid. Bocas del Tom Province, Panama. Scale line = 2(X)
jxni. Figure 2. Coliimhdln moineim.s new species. Protoconch of paratvpe, UCMP .39919. Sc;ilc line = 2(X) ]xm. Figure 3. Recent
Columbdla inercntuiia (SBMNH 144H5I, Los Totiinios, Venezuela). Scale line = 5 mm. Figures 4—5. Colunibclla iitoinciisLs new
species. Holohpe, UCMP 39918. Scale line = 5 mm. Figures 6-7. Columbdla inoinensi.s new species. Paratvpe, UCMP 39919. Scale
line = 5 mm. Figure 8. Larsje specimen itf (^ohnnlirlla niciiiirii'ii-s now species. USNM .5011.52. Sc;Je line = 5 mm.
M. J. deMaintenon, 2000
Page 17
Table 1. Lengths and widths in mm, and number of cords on
the bodv whorl of t\pes and figured specimens
Spe
Max.
length
(mm)
Ma\. width No. of
(mm) spiral cords
Holotvpe, UCMP 39918
Paratype, UCMP .39919
Paratvpe, UCMP 39920
Paratvpe, UCMP .39921
Parat\pe, USNM .5011.50
Paratvpe, USNM 501151
USNM .5011.52
12.8
7.5
14
11.4
6.3
14
15.3
8.7
12
15.8
9.1
17
10.1
5.5
15
12.5
7.2
16
18.6
10.4
17
and in the Neogene of Costa Rica. Whether this is a
distinct species or a form of C. mcrcatoiia lias been de-
bated and should still be regarded as uncertain. The pri-
marv' difference between them is the greater number of
spiral cords on C. submcrcatoiia (22 to 25 per whorl
rather than 15 to 20), but large specimens of e.xtant C.
mcrcatoiia from some areas of the Caribbean also have
a greater number of spiral cords than usual. The type
locahty for C. submcrcatoria is Red Cliff Creek, Costa
Rica, a locality- that is presentK' imlocated but thought
to correspond to late Miocene or earl\ Pliocene beds in
the Limon Basin (Jung, 1994). Coliiinhclhi submcrcato-
ria has a paucispiral protoconch of about 1.5 whorls
(Jung, 1994), similar to that of C. rnercatoria.
LITERATURE CITED
Bandel, K. 1974. Spawning and development of some Col-
umbellidae from the Caribbean Sea of Colombia (South
America). The Veliger 16:271-282,
Bouchet, P. 1989. A review of poecilogonv in gastropods. Jour-
nal of Molluscan Studies 55:67-78.
Coates, A. C, J. B. C. Jackson, L. S. Collins, T. M. Cronin, H.
J. Dowsett, L. M. Bybell, P Jung, and J. A. Obando. 1992.
Closure of the Isthmus of Panama: the near-shore marine
record of Costa Rica and western Panama. Bulletin of the
Geological SocieU- of America 104:814-828.
Jung, P. 1994. Neogene paleontolog\- in the Northern Domin-
ican Republic 15. The genera Coluinbdla. Eiin/pi/rciie,
Panniictdrin. Coiwlla, Nitidella, and Mctulella (Gastro-
poda: Columbellidae). Bulletin of American Paleontology
106(. 344): 1-45.
deMaintenon, M. 1999. The phylogenetic relationships of mod-
em columbellid taxa (Neogastropoda: Columbellidae), and
the evolution of herbivorv from camivorv. Invertebrate Bi-
ologv' 118:2.58-288.
Hoagland. K. E. and R. Robertson. 1988. An assessment of
poecilogonv in marine invertebrates: phenomenon or fan-
tasy? Biolo'gical Bulletin 174:109-125.
Knowlton, N. 1993. Sibling species in the .sea. Annual Review
of Ecology' and Systematics 24:189-216.
Moolenbeek, R. G. and H. J. Hoenselaar. 1991. On the identity
of 'Coliiinbi'llti nistica' from West Africa and the Maca-
ronesian Islands. Bulletin Zoologisch Museum 1.3:6.5-70.
Oliverio, M. 1995. Larval development and allozyme variation
in East Atlantic Columhella (Gastropoda: Prosobranchia:
Columbellidae). Scientia Marina .52:77-86.
Oliverio, M. 1996. Life-histories, speciation, and biodiversih" in
Mediterranean prosobranch gastropods. Vie et Milieu 46:
16.3-169.
Robinson, D. G. 1993. The zoogeographic implications of the
prosobranch gastropods ot the Moi'n Formation of Costa
Rica. American Malacological Bulletin 10:251-255.
Weisbord, N. E. 1962. Late Cenozoie gastropods from North-
ern Venezuela. Bulletin of American Paleontology
42(193): 1-672.
Woodring, W. P. 1928. Miocene mollusks from Bowden, Ja-
maica. Part 2: gastropods and discussion of results. Car-
negie Institute of Wasliington. 564 pp., 40 pis.
Vokes, E. 1990. Cenozoie Muricidae of the West Atlantic re-
gion Pt. VIII — Miircx S.S., Haiistclliim. Cliicorciis and
Hcxnplcx, additions and corrections. Tulane Studies in Ge-
ology and Paleontolog}' 23:1-96.
THE NAUTILUS 114(l):18-29, 2000
Page 18
The New Zealand Recent species oi Muricopsis Bucquoy,
Dautzenberg and Dollfus, 1882 (Gastropoda: Muricidae)
Bruce A. Marshall
Museum of New Zealand Te Papa
Tongarewa
PO. Box 467
Wellington
NEW ZEALAND
bnieeni@tepapa.govt.nz
Kevin W. Burch
6 Oakland Avenue
Whangarei
NEW ZEALAND
ABSTRACT
Four New Zealand Recent Miiricopsis species are recognized:
M. octogonus (Quoy and Gainiard, 1833), M. mariae (Finlay,
1930) and M. profunda new species, which belong in subgenus
Murcxsul Iredale, 1915, and M. scotti new species, which is
referred to Rolandiclla new subgenus together with the south-
em Australian species A/, umhilicatus (Tenison Woods, 1876).
Their shells and radulae are illustrated and distributions plot-
ted. Mtiiicopsis mariae is interpreted as a species rather than
a chronosubspecies of Af. espinosiis (Hutton, 1886) as has been
traditional.
Key words: New Zealand, Muricidae, Muiicopsis, Murcxsul,
new taxa.
INTRODUCTION
For a number of vears a lar2e, locall\' common, sublit-
tcjral form of Muricopsis from rockv ground off northern
New Zealand was suspected to be an imnamed species
distinct from M. octogonus (Quoy and Gaimard, 1833).
Extensive collecting and field observ-ations led Scott
(1989) to conclude that distinct species were indeed in-
volved, and he reported differences in shell morphologv
operculum colour and habitat. On areas of rock\' ground
at 12-15 m depth, cut by channels with sand floors, Scott
found that whereas M. octogonus t\picalh' lives both on
horizontal rockv surfaces with dominant kelp (Eklonia
radiata) and on sand at the channel floors, the undes-
cribed species typically lives on the channel walls
amongst abundant sponges and brachiopods. The pref-
erence for vertical sublittoral rock surfaces would ac-
count for its extreme raritv- on beaches and in dredge
and trawl samples. The following revision was initiated
after recent discovery of well preserved juvenile speci-
mens (hitherto unavailable or unrecognised) of the un-
described species, which show additional differences
from M. octogonus that in turn suggest a closer relation-
ship with the southern Australian species M. umbilicatus
(Tenison Woods, 1876). Abbreviations and text conven-
tions are: AIM, Auckland Institute and Museum;
BMNH, The Natural History Museum, London; CM,
Canterbury^ Museum, Christchurch; IS, Ian Scott collec-
tion, Auckland: K\VB, Kevin W. Burch collection, Whan-
garei (includes the outstanding collection formed bv our
late friend Dave Gibbs); NMNZ, Museum of New Zea-
land Te Papa Tongarewa, Weflington; NZGS, Institute
of Geological and Nuclear Sciences, Lower Hutt. Unless
specified, all material is at NMNZ (registration numbers
preceded bv "M."). Length dimension precedes width in
all cited measurements.
SYSTEMATICS
Superfamilv Muricoidea Rafinesque, 1815
Familv Muricidae Rafinesque, 1815
SubfamiK Muricidae Rafinesque, 1815
Genus Muricopsis Bucquoy, Dautzenberg and Dollfus,
1882
Muricopsis Bucquoy, Dautzenberg and Dollfus, 1882: 19. Type
species (by original designation): Murcx hlainviUii Pa\Tau-
deau, 1826: Recent, Mediterranean.
Subgenus Murcxsul Iredale, 1915
Murcxsul Iredale, 1915: 471. Tvpe species (by original desig-
nation): Murex octogonus Quoy and Gainiard, 1833; Re-
cent, New Zealand.
Remarks: Ponder (1972) considered Murcxsul to be a
s\iion\Tn of Muricopsis. though Radwin and D'Attilio
(1976), Yokes (1970, 1988) and Beu and Max-wefl (1990)
have treated them as cbstinct genera. We agree with Vo-
kes (1988) that they are closelv related, but Uke Houart
(1988, 1991, 1993), prefer to interpret Murcxsul as a
subgenus oi Muricopsis.
Muricopsis (Murcxsul) octogonus (Quov and Gainiard, 1833)
(Figures 1-15, 24, 25, .33, .37)
Murcx octogonus Quov and Giiiniard, 1833: 531, pi. 36, fig. 8,
9; Kiener, 1843: 64, pi. 15, fig. 2; Grav, 1843: 229; Reeve,
1845, pi. 29, fig. 1.34; Kiister and Kobelt, 1869: 79, pi. 28,
B. A. Marshall and K. \X. Burch, 2000
Page 19
fig. 23; Hutton, 1880: 47; Poirk-r, 1883; 112; Snter. 1901:
61.
Mnrex penividiius Sowerln, 1841a: 8, lit;. 103; Sovverhw 1841b:
147; \bkes, 1970; .327. Not Miinx pinniiiuiis Lamarck.
1816 (preoccupied).
Miircx (Phi/Uonotus) octo^i^oiiiis. — Tr\on. 1880; 110, pi. .30. fig.
272. 273 onK' I, in purt — fig. 274 = Muricop.si.s aispidatiis
(Sowerbv, 1879)); Hutton, 1884; 218.
Miirex clipsactis. —Tnon. 1880; 110, pi. .30, fig. 281 onl\-. Not
Broderip, 18.33. '
Miirex octogoniis var iimhilicata. — Suter 1901; 61. Not Tcni-
son Woods, 1876.
Murex {Miirii-antlui) octofionii.s. — Suter, 1913: 400. pi, 48, fig.
1.
Murc'x (Miiricantha) octog,oiiu.s var iiiiihilirdtii.s. — Suter 1913:
401. Not Tenison Woods, 1876.
Hcxiifilcx (Miircxsul) octogonii.s. — Iredale, 1915; 471; Wenz,
1941; 1090, text fig. 3096.
Hexaplcx (Murexsul) octogonus var umbilicntns. — Iredale,
191.5; 471. Not Tenison Woods, 1876.
Murexsul octogonus. — Finlav, 1926; 419; Yokes, 1964; 13, fig.
20, .50, 61; Ponder 1968; 31. fig. 1, 37-41; Yokes, 1970;
327; Fiiir 1976; 63, pi, 17. fig. 239; Radwin and DAttilio.
1976; 163, text fig. 104, pi. 26, fig, 6, 7; Abbott and Dance,
1983; 143, te.xt fig.; Scott. 1989; 6, text figs.; Ben and Max-
well. 1990: .359, pi. 481.
Murexsul cuvierensis Finlav, 1926; 419 = noiiun nudum.
Murexsul cuvierensis Finlav, 1927: 487, pi. 24, fig. 2.
Murex (Murex.'iul) octogonus. — Thiele, 1929; 290; Shikama and
Horikoshi, 1963; 69, te.xt fig. 104.
Murex {Murex.sul) ednae Smitli,"l940; 43, pi. 2, fig. 10.
Muricopsis octogonus octogonus. — Ponder 1972: 237, te.xt fig.
.3/24.
Murcx.sut octagunus [sic]. — Kaicher 1978, card 1608.
Muricopsis octogonus. — Powell, 1979; 170, pi. .35, fig. 1; Scott,
1989; 6, text figs.; Hart, 1993; 44, text fig. (in part— far
right figure = holotvpe of Af . scotti new species).
Type material: M. octogonus: syntypes (2), including
the originally figured specimen (Figure 15) MNHN, Bay
of Islands, New Zealand; M. pcniiianus: repositors' of
txpe material unknown (not located at BMNH. K.M.
Way, pers. comm.), "Pacosma\o, Peru" = New Zealand;
M. cuvierensis: holotxpe AIM 70500, off Cuvier Island,
73 m; M. ednae: repositorx- of txpe material unhiown,
"Japan" = New Zealand.
Other material e.xamined: About 1000 specimens in
NMNZ (152 lots) and K.W. Burch (24 lots) collections.
Di.stribution (Figure 37): Pleist(K'ene (Castlecliffian)
to Recent. Three Kings Islands and North Island, New
Zealand, as far south as Kapiti Island (west coast) and
Mahia Peninsula (east coast), 0-508 m; taken alive at low
tide to 121 m.
Remark.s: Muricopsis octogoitus is exceptionally vari-
able in teleoconch moq'jhologx', and there is complete
intergradation between the most extreme of the forms
illustrated here (Figures 1-15). Despite great variation
in sculpture of the last few whorls in adults, all of the
specimens are identical in protoconch and earlv teleo-
conch morphologx'. Moreover, we could detect no cbf-
ferences between the most extreme forms in radular
morphology or e.xternal anatomy. It thus seems ilear that
all specimens under consideration here represent a sin-
gle higliK variable .species.
Mature specimens range from 29 to 92 (est.) mm in
length. Spines may be entirely absent, or short to long.
The secondary- spiral cords ma\- remain weaker than the
primaries and spineless throughout, or the% ma\- enlarge
to resemble the primaries before the last adult whorl,
and some or all may develop spines that may be as long
as those on the primaries. The siphonal canal may be
short and broad and the fasciole rounded with low ridg-
es, or the canal ma\' be long and narrow, and the fasciole
set with canals from earlier stages of growth that encircle
a narrow to rather large false umbilicus. The teleoconch
may be reddisli brown with black spiral cords, or white
or cream with vellovvish or (txpicalK ) reddish brown spi-
ral cords. Shells with dark, extensive pigmentation pre-
dominate in the littoral and locally to about 12 m. Spec-
imens with short spines, and with secondary' spirals that
enlarge to resemble the primaries predominate in the
littoral and localK' to about 50 m, whereas long-spined
shells on which the secondarv spirals remain weaker
than the primaries txpically occur deeper than about 30
m, thfjugh localK- as shallow as about 20 m. The outer
lip of mature specimens ma\' be smooth or (hpicalK )
dentate, and the inner lip rim ma\' be free and projecting
below a narrow parietal area, or almost fully adlierent.
Unusually large, entirely spineless shells occur off Spirits
Bax', where thev' intergrade with short-spined specimens
(Figures 9, II).
Muricopsis octogonus has been observed on a number
of occasions on sandy substrata, boring holes in and
feeding upon the shallowK'-burrowing bivalve Tawera
spissa (Desha\es, 18.35) (I. Scott, pers. comm.; K.W.B.,
pers. obs.). What it eats on rock-\- ground remains to be
established. The radula is illustrated (Figure 33) for
comparison with those of M. mariac, M. scotti and M.
unibilicatus (Figures 34-36).
There are no records of M. octogonus from the west
coast of the North Island between Cape Maria van Die-
men and Cape Egmont, or from the east coast south of
Mahia Peninsula (Figure 37), and it would seem that the
present distribution off the northeastern and southwest-
em North Island is relictual, perhaps dating from prior
to the last glacial maximum.
How far back this .species extends in the fossil record
is unclear. Specimens from a Late Pliocene (Nukuma-
ruan) horizon near Waipukurau (GS 10858, former cut-
ting on disused section of Ashcott Road, coll. A.C. Beu,
NZGS) appear to be indistinguishable from Recent spec-
imens in teleoconch moqihology but differ in having
smoothly rountleil instead of angulate protoconchs as in
Recent material (Figure 30) (see below). If it proves to
be specifically distinct from M. octogonus, it mav- be as-
signable to M. dihtcidus Marwick, 1931 (Early Pliocene,
Gisborne District). Some of the New Zealand Cenozoic
ta.xa are scarceK' distinguishable from M. octogonus or
from each other, and it is likely diat M. octogonus is a
direct descendent of one or other of them, such as M.
Page 20
THE NAUTILUS. Vol. 114, No. 1
B. A. Marshall and K. W. Burch, 2000
Pa^e 21
proavitiis (Laws, 1935), M. proi^enitor (Laws, 1935), or
M. manvicki (Max^A'ell, 1971), all from Middle Miocene
(Lilbumian) beds.
Muricopsis (Murexsul) mariae (Finlav, 1930)
(Figures 17, 19, 27, 28, 34, 38)
Murexsul inariac Finlay, 1930: 237; Kaiclicr, 197S, card 1639;
Ben and Maxwell,' 1990: 359.
Murexsul cspinosus mariae. — Ponder, 1968: 32, fig. 2, 32, 33,
.34.
Muricopsis espinosus marine. — Powell, 1979: 170, pi. 37. fig.
5; Scott, 1989: 6, text figs.
Ty-pe material: HolotApe AIM 70502, Cape Maria van
Dienien, northern New Zealand.
Other material examined: Several hundred speci-
mens in NMNZ (66 lots) and K.W. Burch (13 lots) col-
lections.
Distribution (Figure 38): Three Kings Islands and
northeastern North Island, New Zealand, as far south as
Anaura Bav, 0-233 m; taken living under rocks at low
tide to 40 ni.
Remarks: Muricopsis mariae differs principally from
M. octogonus in consistentK- lacking spines, in being
smaller relative to the number of whorls, in having stron-
ger denticles within the adult outer lip, in attaining
smaller size (ma.\imum length 29 mm as against ca. 9.3
mm), in being bluish white instead of tvpicalh' white
within the aperture, and in tvpicalh' lacking a distinct
shoulder angulation, at least on the early teleoconch
whorls (some specimens have a distinct shoulder angu-
lation on later whorls). In a sample of both species taken
living together at 25 m in Whangaroa Harbour entrance
(M. 1:37244, M. 74899), the protoconch ranges from 800-
1000 |j.m wide (mean = 900 ixnx SD = 6.053, n = 21)
in M. inariac, and 650-1050 |jLm wide (mean = 930 |jLm,
SD = 0.097, n = 17) in M. octogonus. The largest M.
mariae protoconch seen is 1250 |jLni wide (M. 133712).
The first whorl of the protoconch has a distinct angula-
tion and the summit is more or less flattened in both
species. Juveniles of A/, mariae and M, octogonus mav
be difficult to distinguish, but in M mariae the primarv-
spiral cords are stronger after the second teleoconch
whorl, the secondary spirals enlarge more rapidly to re-
semble the primaries, and the Secondaries on the sutural
ramp become pigmented early on the third whorl in-
stead of after the third or fourth whorl (compare Figures
24, 25 with 27, 28). Specimens from Cape Maria van
Diemen to North Cape and off the Three Kings Islands
are more broadly conical than most specimens from fur-
ther south (Figures 17, 19) but are otherwise indistin-
guishable.
The diet of this species is unknown. The distinctive
radiila is illustrated (Figure 34) for comparison with that
of A/, octogonus, M. scotti and M. timhilicatus (F'igures
.33, 35, .36).
Ponder (1968) interpreted M. mariae as a chronosub-
species of A/, espinosus (Hutton, 1886), though Beu and
Maxwell (1990) suggested that they might well be dis-
tinct species. Compared with 15 well preserved .speci-
mens of M. espinosus obtained near Waipukurau
(GS10858, map ref. U22/085.308, former cutting on dis-
used section of Ashcott Road, WNW of Waipukurau,
A.G. Beu, NZCS — lowest Nukumaruan, Late Pliocene),
which are indistinguishable from the hpe material ob-
tained nearln', M. mariae differs in having a protoconch
that is shorter relative to its width with a shouldered
(rarely rounded) instead of rounded, more or less bul-
bous first whorl (Figure 27), and in having narrower spi-
ral interspaces, especially on the first three or four te-
leoconch whorls. In most specimens of M. mariae the
secondary spiral cords enlarge to resemble the primaries
more rapidlv than in M. espinosus. InterestingK- enough,
the sample includes well-preserved specimens of a larger
species that also lacks a shoulder angulation on the pro-
toconch (Figure 30). The status of this larger fossil spe-
cies is unclear, but it is certainly more closely related to
M. octogonus than to M. espinosus. Muricopsis espinosus
or a very similar species occurs in the bath\a! "coral
thicket". Lake Ferry, Palliser Bay (Mangapanian: Late
Phocene) (Figure 31). The protoconch has thus inde-
pendently become angulate in the M. octogonus and M.
mariae lineages since the Pliocene. The differences be-
tween M. espinosus and M. mariae in protoconch mor-
phology and similarities in teleoconch morphology sug-
gest that thev are distinct species.
The original description o( Murcx espinosus (Hutton,
1886) is based on more than one specimen, the larger
of which provided the cited dimensions (30.0 X 14.5 mm,
CM3294), the smaller of which was subsecjuently illus-
trated bv- Hutton (1893) (28.0X13.3 mm, CM3295). Al-
though these specimens each have two labels (none orig-
inal) staring that they are "holotype ' and "paratype" re-
spectively, they are in fact synt\pes because Hutton did
not use these unecjuivocal terms. Ponder (1968, figs 35,
36) effectively designated the larger specimen as lecto-
type by stating that it was the "holotype". Incidentally,
Figures 1-12. Shells of adult Muricopsis (Murexsul) octogonus (Quoy and Gainiard). 1. Off Thompson Point, Wailieke Island,
22 m, KWB (length .54 mm). 2. Off Cuvier Island, 70 m, M..5911 (length 78.5 mm). 3. Off Motiikalian Island, W of Paparoha,
Coramandel, 18-20 m, KWB (length 45.5 mm). 4. Scallop bed near Matiatia Bav entrance, Waiheke Island, 13 m, K\^'B (length
48 mm). 5. Off Three Kings Islands, craxpot, KWB (length 90 mm, est. 93 mm). 6. Raiifurlv Bank. East Cape, 31-47 m, M. 75079
(length 46 mm). 7. Off Mavor Island, .59-74 m, M.64825 (length 63.5 mm). 8. Off Motnhoropapa Island, The Noises, 25 m, K'WB
(length 42.5 mm). 9. Off Spirits Bav, 48 m, M. 137051 (length 54 mm). 10. Hooper Point, Spirits Bav 12 m, M. 1.346.30 (length 29
mm). 11. Off Tom Bowling Bay, 49 m, M. 137090 (length 64 mm). 12. Reotalii, Whangarei, low tide, KWB (length 45.5 mm).
Page 22
THE NAUTILUS, Vol. 114, No. 1
Figures 13-23. Shells of Muricopsis species {all specimens adult except IS). 13-15. Muricopsis (Murexsul) octogonits (Quoy and
Gaimard). 13. Ranfurlv Bank. Ea.st Cape, 89-94 m, M.64812 (length 46 mm). 14. Whangaroa Harbour entrance^ 2,5 m, M. 74899
(length .38 mm). 15. originallv figured s\iit\pe, MNHN (length .3.5. .5 mm). 16, 23. Murexsul (Muricop.sis) profunda new species,
holohpe, off Three Kings Islands, 91 m, M. 70356. 17, 19. Muricopsis (Murexsul) marine (Finlav). 17. Archvvav Island. Three Kings
Islands, 15 m. M. 117096 (22.3X12.3 mm). 19. Whangaroa Harbour entrance. 25 m. M. 137244 (26x13 mm). 18, 20. Murexsul
(Rolniicliella) umhilicatus (Tenison Woods), Gulf St. Vincent, South Australia, South Australian Museiun (Figure 20, length .32 mm).
21, 22. Murexsul (Rolandiella) scotti new species. 21. Holotvpe, Mathesons Bay, Leigh, 6-9 m, M. 138186 (length 44 mm). 22.
Paratype, Southeast Bay, Great Island, Three Kings Islands, 18 m, KWB (length 53.5 mm). Scale Una = 1 mm.
B. A. Marshall and K. W. Burcli, 2()()()
Page 23
Figures 24-32. Early whorls of Miiiicopsi.s species. 24, 25. Muiicop.sK {Miircxsiil) ociof^oiius (Qiio\' aiid Gainiard), VVhangaroa
Harlioiir entrance, 25 m, M. 74899 (shell length 7.05 mm). 26. Miiirx.stil (Roland icllti) scotti new species, submarine cave S side of
Ro.seman' Rock, Princes Islands, Three Kings Islands, 20 m, M. 117084 (length 6 nnn). 27, 28. Muricopsi.s (Murcx.sul) niariac (Finlay),
Whangaroa Harbour entrance, 25 m, M. 1.37244 (shell length 4.75 mm). 29, 32. A/i/rico/i.v/.v (Miircx.wl) profunda new species, early
whorls (29) and teleoconch (left) and protoconcli (right) microsculpture (32), NW ol Great Island, Three Kings Islands, 310 m,
M. 93876. 30. Mttricopsis (Mtirexsul) sp. aff octogonu.s (Quoy and Gaimard), GSI0858, Ashcott Road, VVaipuknrau, shallow water.
Late Pliocene (lowest Nukvnnanian), NZGS TM8078. 31. Muricopsi.s (Murexsul) sp. cf espinosus (Hutton), "coral thicket". Lake Ferry,
Palliser Bay, bathyal. Late Pliocene (Mangapanian), M. 40408. Scale line for figure 32 = 50 |xm, other scale lines = 500 |jini.
Page 24
THE NAUTILUS, Vol. 114, No. 1
Figures 33-36. Radulae of Muricopsis species. 33. Muricopsis (Murexsul) octogonus (Quoy and Gaimard), off Te Arai Point,
Northland, 41 ni, M. 137251 (shell length 65 mm). 34. Muricopsis (Murexsul) mariae (Finlay), Governors Pass, Great Barrier Island,
11-29 m, M. 21784 (shell length 22 mm). 35. Muricopsis (Rolandiella) scotti new species, off Cape Rodney, 11-13 m, M. 137416
(shell length 40 mm). 36. Muricopsis (Rolandiella) umbilicatus (Tenison Woods), Edithburgh, South Australia: South Australian
Museum, Adelaide, unregistered (shell length 28 mm). Scale lines = 50 jxm.
this t)-pe material was mislaid imdl recentK', and omitted
from the catalogue of tspe and figured fossils in the Ge-
ology Department of the Canterbury Museum (Brad-
shaw et al, 1992).
Muricopsis (Murexsul) profunda new species
(Figures 16, 23, 29, 39)
Description: Shell up to 10.5 mm high (holotype
adult?), fusiform, of moderate thickness; protoconch and
teleoconch pale orange, adapical 4 primary spirals and
secondary spirals between them reddish brown on last
whorl. Protoconch 830-870 |xm wide excluding flared
rim, of 1.5 convex whorls, covered with minute hemi-
spherical granules, summit of first whorl angulate, last
half whorl rather e\enly convex. Teleoconch of 4.5 reg-
ularly expanding whorls; first whorl broadly convex; sub-
sequent whorls with pronounced supramedian angula-
tion, sutural ramp broad and flat, side broadl\' convex,
smoothly confluent with siphonal canal. Sculpture con-
sisting of axial varices, and rounded primarv' and sec-
ondary spiral cords. Axial varices strongly retracted from
adapical insertion throughout, 12 on last whorl (holo-
tspe), narrow on 1st whorl, sloping adaxialh so that bases
are overhung, blade like and strongly adapicalK- pro-
duced above protoconcli/teleoconch suture and cement-
ed to side of last whorl of protoconch, e.xtending beyond
adapical extremitv of last protoconch whorl or to about
mid whorl length. .Axial varices on subsecjuent whorls
becoming diicker and rounded, each sumiounted by 4
or 5 fine, collabral, ada.xially sloping, axial lamellae. Axial
interspaces with fine collabral growth lines and a few
lamellar growth lines. Primarv spiral cords numbering 3
on spire and 3 on base; spire spirals commencing ini-
niediatelw similar throughout, adapical spiral at shoulder
angulation, abapical spiral bordering suture; adapical 2
basal spirals similar to spire spirals, abapical spiral stron-
ger, widely separated. Secondary spirals numbering com-
mencing on 3rd whorl, remaining weaker than primaries,
2 on ramp, 1 between each priniar\- spiral, 3 between
abapical basal primaries, and 1 between abapical basal
primarv and tip of canal. Siphonal canal of moderate
B. A. Marshall and K. W. Burch, 2000
Page 25
Figures 37. Distributions of New Zealand Recent Muricop-
sis {Miircxstd) octogonus (Quov and Gaimard) (500 and 1000
m isobaths indicated).
Figure 38. Distributions of New Zealand Recent Muricopsis
(Miircxsiil) marine (Finlay) (500 and 1000 m isobaths indicat-
ed).
length, gently flexed, partly enclosed by thin extension
of inner lip. Aperture p\riform; outer lip rather thin at
rim, weakly thickened within, simple; inner lip fully ad-
herent adapically, rim free at abapical extremity and ex-
tending almost to canal tip. Animal unktiown.
Type material: Holotype NMNZ M. 70356, 34°11'S,
172°10'E, off Three Kings Islands, northern New Zea-
land, 91 m, 19 Februar\' 1974, r.v. Acheron. Paratx^jes:
33°59.2'S, 172°13.6'E, 18 km N of Great Island, Three
Kings Islands, 155 m, 23 June 1978, r.y. Tangaroa (1
juvenile, M. 137247); 34°06.5'S, 172°04.7'E, llkm NW
of Great Island, 310 m, 30 June 1978, r.v. Tam^awa (1
juvenile, M.93876).
Other material examined: 34°009'S, 171°44 7'E,
Middlesex Bank, NW of Three Kings Islands, 201-216
m, 31 January 1981, r.v. Tan^aroa (2 juveniles,
M.93302); 34°02.0'S, 171°44.0'E, Middlesex Bank, 246-
291 m, 31 January 1981, r.v. Tan^aroa (3 juveniles,
M. 137245); .34°05.9'S, 171°55.1'E, 24 km NW of Great
Island, Three Kings Islands, 710 m, 27 June 1978, r.v.
Tangaroa (4 juveniles, M. 137246); 34°17.6'S,
17r45.3'E, 39 km SW of Great Island, 427 m, 21 June
1978, r.v Tangaroa (3 juveniles, M. 94338).
Distribution: Off Three Kings Islands, northern New
Zealand, 91-710 m (shells only).
Remarks: Muricopsis profunda differs from M. octo-
goniis and M. mariac principalK' in having ;Lxial varices
that ride up onto the protoconch from the next whorl,
in that the outer lip is much more strongly retracted
from the suture, and in that the spiral cords are stronger
at equivalent stages of growth and become pigmented
at a later stage of growth. The size attained by this spe-
cies is unclear, though it may not grow much larger than
the holotvj^e (length 10.5 mm).
Etymology: Deep (Latin).
Rolandiella new subgenus (of Muricopsis)
Type species: Muricopsis (Rolandiella) scotti new
species; Recent, northern New Zealand.
Diagnosis: Sliell similar to those of species of Muri-
copsis (Murexsul), but with median shoulder angulation
and weak abapical 2 primary spiral cords on first 1.5
teleoconch whorls. Inner Lip of most specimens upstand-
ing over most of its length.
Description: Shell 21-62 mm high at maturity, spire
about as high as last adult whorl or slightly shorter, stout,
of moderate thickness. Protoconch of 1.5-2.0 rovmded
whorls. Teleoconch of mature specimens widi 5.5-7.0
convex, shouldered whorls, shoulder median on first 2
whorls, ascending to adapical third or slightly higher on
subsequent whorls; sutural ramp shallowly concave; side
broadly convex, smoothly confluent with siphonal canal.
Primary- sculpture consisting of strong, axial varices and
spiral cords with spines at intersections. Varices travers-
ing all whorls, angulate in section, numbering 8-11 (7
or 12 in occasional specimens) on adult penultimate
whorl. Primary spiral cords rounded, numbering 3 on
spire and 3 on base in adults. Adapical primary spiral at
Page 26
THE NAUTILUS, Vol. 114, No. 1
shoulder angulation, peripheral; abapical primary bor-
dering suture throughout, or separating as insertion of
last few whorls descends to ne.xt priniarv spiral: adapical
and abapical primaries commencing immediately; inter-
mediate primary* commencing at about mid first whorl,
gradually enlarging to resemble other primaries. Abapi-
cal basal primary spiral wideK' separated from adjacent
primary, interspaces ot other primar)' spirals closer and
of similar width to each other. Secondary' spirals pro-
gressively developing, 1-5 on sutural ramp, 1 each in
some or all interspaces of primaiT spirals, 0-.3 betyveen
abapical basal priman' spiral and tip of canal, others on
summits of some or all primary- spirals, 1 or more en-
larging to resemble primaries on last adult whorl. Pri-
mar\' and 1 (abapical shoulder spiral) or more secondarv
spirals procKiced as short to moderate-length spines at
varices, spines on primar\' spirals of similar length or
shoulder spiral longest. Secondary axial sculpture com-
prising fine collabral growdi lines that are raised as thin,
fragile lamellae on ramp against suture and where in-
tersecting spiral sculpture. Aperture pvriform. Outer lip
thickened within at maturity, strongh' so in particularly
large specimens, which may also develop spirally elon-
gate denticles. Inner lip thin, fulK* adherent over adap-
ical third or quarter, abapical part typically free, flared
and strongK' projecting, ajjapical extremity e.xtenchng
well beyond flexure of siphonal canal. Siphonal canal of
moderate length, almost enclosed by infolding: siphonal
fasciole strong, forming an umbilicus in some ver\' large
specimens. Radula and operculum similar to those in
Miiricop.sis (s. str) and Murcxsul.
Remarks: Rolandiclla is introduced for Muiicopsis
scotti new species from northern New Zealand, and M.
umbilicatiis (Tenison Woods, 1876) from southern Aus-
tralia, both of which resemble typical Murcxsul species
in gross facies, but differ in that the shoulder spiral is
situated medially on the early spire whorls then ascends
adapicalK', and the intermediate primary spiral on the
spire commences later than the others and develops
slowly. By contrast, in Muiicopsis species, all three pri-
maries are strong and commence immediately on die
first teleoconch whorl, and the shoulder spiral borders
the suture then descends abapically over subsequent
whorls.
None of the named New Zealand Cenozoic species
referred to Murcxsul by Beu and Maxwell (1990) seem
to belong in Muiicopsis (Rolandiclla). though the rela-
tionships of the Early Miocene species Muiicopsis cchin-
ophorus (Powell and Bartrum, 1929) are unclear be-
cause the early teleoconch morphology is unknown.
Both M. (Rolaiuliclla) scotti and M. (R.) uinbilicatus
have large, rounded, paucispiral protoconchs indicating
non-planktotrophic development, and suggesting that
they have either crawl-away larvae or drifting larval stag-
es of short duration. We suppose that the\' are derived
from a common ancestor with planktotrophic larval de-
velopment that had a trans-Tasman distribution. How far
back in time diis putative common ancestor may have
@ .
Figure 39. Distributions of New Zealand Recent Muricopsis
(MtirexstiJ) profunda new species (circle) and Muricopsis {Ro-
landicUa) scotti new species (squares) (500 and 1000 m iso-
baths indicated).
lived is impossible to estimate without fossil records or
Tiiolecular data.
Etymology: After Roland Houart, Belgium, in appre-
ciation of his outstanding contribution to world muricid
systematics.
Muricopsis (Rolandiclla) scotti new species
(Figures 21, 22, 26, 35. 39)
Muricopsis species Scott, 1989: 6, text figs.
Muricopsis octogonus. — Hart, 1993: 4.5, right text fig. onlv
( = holotype). Not Qnov and Gainiard, 18.3.3.
Description: Shell up to 62 mm high, fusiform, spire
about as high as last adult whorl or slightK' shorter, stout,
of moderate diickness. Protoconch and first 1 or 2 te-
leoconch whorls white, subsequent whorls white or pale
buff, primary, secondary and some finer spiral cords red-
dish brown, aperture porcellaneous white. Protoconch
sharply delineated b\' low varix, of 1.5-2.0 smooth, con-
vex whorls. Teleoconch of up to 7 convex, shouldered
whorls, shoulder median on first 2 whorls, ascending to
adapical third or slightly higher on subsequent whorls;
sutural ramp shallowK' conca\e: side broadk' convex,
smoothly confluent with siphonal canal. Primary sculp-
ture consisting of strong, axial varices and spiral cords
with spines at intersections. Varices traversing all whorls,
angulate in section, numbering 8-11 (7 or 12 in occa-
sional specimens) on adult penultimate whorl. Primary
spiral cords rounded, numbering 3 on spire and 3 on
base in adults. Adapical primary spiral at shoulder an-
B. A. Marshall and K. W. Burch, 2000
Page 27
gulatioii, peripheral; ahapical spire spiral bordering su-
ture at first, separating as insertion oi last few whorls
descends to next (iornierK' adapieal basal) priinar\' spiral;
adapical and abapical spire spirals commencing imme-
diatek": intermediate spire spiriil commencing at about
mid first whorl, slowlv enlarging to resemble abapical
spire spiral and basal primary- spirals. Abapical basal pri-
mar\ spiral wideK separated from adjacent primarw in-
terspaces of other primars' spirals closer and of similar
width to each other. Secondar\' spirals appearing pro-
gressively, numbering 3-5 on sutural ramp, 5-7 in zone
comprising summit of shoulder spiral space behveen it
and adjacent primars, usualK 3 or 4 on sununits of other
primary spire spirals, 3 or 4 between abapical 2 basal
primaries, 3 between abapical basal priman* spiral and
tip of canal, and generally 1 each in some or all inter-
spaces of primar\' spirals, most or all secondaries re-
maining weaker than primaries throughout, or some en-
larging to resemble primaries on last adult whorl. Pri-
man and some secondars' spirals produced as short to
moderate-length spines at varices, shoulder spines lon-
ger than others on spire, spines on larger spirals tspicalK
of similar length on last adult whorl. Secondar\' axial
sculpture comprising fine collabral growth lines that are
raised as thin, fragile lamellae on ramp against suture
and where intersecting spiral sculpture. Aperture p\Ti-
form. Outer lip thickened within at maturity, strongly so
in particularK' large specimens, which ma\' also develop
spiralK' elongate denticles. Inner lip thin, fidh" adherent
over adapical third or quarter, abapical part hpicalK'
free, flared and strongly projecting, abapical extremits*
extending well beyond flexure of siphonal canal. Siphon-
al canal of moderate length, almost enclosed bv infold-
ing; siphonal fasciole strong, forming an umbilicus in
some vers' large specimens. Operculum with terminal
nucleus, yellowish brown. Radula (figure 35): Central
teeth each with strong, conical central cusp; smaller,
conical lateral and marginal cusps, and 2 \er\' small inner
lateral denticles that are well separated from lateral
cusp. Lateral teeth narrow.
Type material: Holotype NMNZ M. 138186, Mathe-
sons Bay, Leigh, northern New Zealand, 6-9 m, Feb-
niar\-March 1992, D.W. Gibbs (ex D.W. Gibbs and
K.W. Burch collections). Paratvpes: 34°09.5'S,
172°08.8'E, Southeast Bay, Great Island, Three Kings
Islands, 20-22 m, 4 March 1997, K.W. Burch and D.D.
Crosby (2 juveniles, M. 134760); Southeast Bay, alive, 18
m, ISMay 1982, K.W. Burch (6, KWB); Princes Islands,
Three Kings Islands, 15 m, 29 November 1983, G.S.
Hardy and A.L. Stewart (1, M. 75135); S side of South-
west Island, Three Kings Islands, ;ilive, 27 m, 12 Feb-
nian' 1986, G.S. Hardv (2, M.84267): off Cape Maria
van Dienien, craypot. May 1991 (1, KWB); Whangaroa
Harbour entrance, alive, 18 m, November 1995, K.W.
Burch and D.W Gibbs (2, KWB); Rikoriko Cave, Poor
Knights Islands, alive, 30-40 m, 1982, M.II.B. ONeill
(1, 'm.75181); Poor Knights Islands, alive. May 1979,
A.S.W. Penniket (1, M. 133691); Poor Knights Islands,
December 1980, K.W. Burch (1, M. 133692); Poor
Knights Islands, alive, 15-20 m, 1983, K.W. Burch (4,
KWB); Poor Knights Islands, alive, 1970, 1972, W. Doak
(5, M. 133690); South Cave, Poor Knights Islands, alive,
17 m, 21 May 1969, A.N. Baker (1,' M.23617); South
Harbour, Poor Knights Islands, tilive, 25 Mav 1969, A.N.
Baker (3, M.23618); off Cape Karikari, 30m, 20 June
1981 (1, M. 133694); Urtjuarts Bav Whangarei Heads,
alive, March 1965 (1, M. 133695); "The Canyon", N side
of Burgess Island, Mokohinau Islands, alive, 15-21 m,
Januari- 1985, D.W. Gibbs (3, KWB); Maori Island,
Leigh,' 22 Mav 1975, A.S.W. Penniket (1, M. 133695);
NE of Mathesons Bay, Leigh, alive, 18 m, Mav 1995,
D.W. Gibbs (1, M.127040);'Mathesons Bay, alive, 6-10
m, Februars-March 1992, D.W. Gibbs (6,' KWB); S of
entrance to Omaha Cove, Leigh, 20 ni, December 1967,
I. Scott (2, IS); off Little Barrier Island, alive, craypot,
T. Riley (2, M. 133693); Cape Rodney alive, 15 m,'june
1987, D.W. Gibbs (7, M.90125); Cape Rodney, alive, 15
m, 4 March 1989, I. Scott (12, M. 117277); Cape Rodnev,
alive, 11-13 m, I. Scott, Mav 1989 (53, M. 137416); Cape
Rodney alive, 18 m, June 1977 (1, M. 133698); Waika-
wau Bay, Coramandel, alive, 16 m, April 1989, D.W.
Gibbs (2, KWB); off Needle Island, Mercury Bay, alive,
16 m, January 1985, D.W. Gibbs (3, KWB).'
Other material examined: S side of Rosemar\- Rock,
Princes Islands, Three Kings Islands, 20 ni, 18 January
1985, FJ. Brook (5, M. 117084); off West Island, Three
Kings Islands, Elinfiamitc wreck, alive, W Doak (1,
M. 133696); .34°2().0'S, 173°06.6'E, N of North Cape,
163-168 m, 27 Januar\' 1981, r.v. Tonj^aroa (1,
M. 137225); Rarawa Reef' Great E.xliibition Bay crav-
pots, alive, 40 ni, August 1989, I. McMillan (2,
M. 100382); Rarawa Reef cra\pots, alive, 73 m, 28 Sep-
tember 1988, I. McMillan (6, M.95234); Rarawa Reef
cra\pots, alive. 40 m, 16 December 1987, I. McMillan
(3, M. 95315); off Cape Karikari, alive, cra\pots, 1988, I.
McMillan (1, M.95322); Henr\- Island, ' Whangaruni,
alive, 13 m, 5 December 1971, \.N. Baker (1, M.2592());
off Hen and Chickens Islands, alive (1, M.2686; 1,
M.83882); Mathesons Bay, Leigh, alive, 15-20 m, 26
March 1995, A. Spurgeon (2, MT26998).
Distribution (Figure 39): Three Kings Islands and
northeastern North Island, New Zealand as far south as
Little Barrier Island, 13-168 m; taken alive at 13-40 m
from rocky groirnd.
Remarks: Miiricopsis ■•icotti is most similar to the
southern Australian species M. nmbilicatus (Figures 18,
20, 26) in early shell ontogeny and gross adult shell fa-
cies than to any New Zealand Recent Murcxsiil species.
Muricopsis scotfi differs from M. nmbilicatus in a num-
ber of details including larger adult size (shell length 34—
62 mm versus 21-30 mm), stronger and more numerous
secondary- spirals, insertion point of the last few whorls
desceruling froirr the abapical spire spiral to the next
(formerly adapical basal) primary spiral, and abapical
secondary spiral on the sutural ramp never becoming as
Page 28
THE NAUTILUS, Vol. 114, No. 1
large as tlie shoulder spiral. The radula of M. scotti is
similar to those of M. umhihcatus and M. octogomis
(Figures 3, 35, 36).
Muricopsis scotti resembles M. octof^onus in size, but
is readily distinguishable bv the following characteristics:
orange brown instead of dark reddish brown operculum,
rounded instead of angulate protoconch, generally larger
aperture, shorter siphonal canal, and much stronger sec-
ondary spiral sculpture on the primary spiral cords, es-
pecially on the shoulder spiral and between it and the
adjacent primary. Unlike M. octogonus, which has ex-
tremeK' variable sculpture, M. scotti consistently has a
distinct shoulder angulation, angular yarices and short
spines that are not curved backwards, or at most only
slightK' so. In M. scotti the shoulder spiral (adapical pri-
man) is much stronger than the others on the first two
teleoconch whorls and occupies a median position, then
gradualK' ascends to about the adapical third on subse-
quent whorls (Figure 26). By contrast, on the first 1.5
teleoconch whorls in M. ocfogoiius, the three primary'
spire spirals are all strong and similar, and the shoulder
spiral commences beside the suture and descends to
about the adapical third, remaining there or at the adap-
ical quarter on subsequent whorls (Figure 24). Although
the rim of the inner lip may be upstanding or more or
less fulK' adherent in both species, that in M. scotti is
typically free and more strongly upstanding abapically,
and extends abapicallv further beyond the angulation at
the top of the siphonal canal.
Shells of living M. scotti are invariably more or less
covered widi living Br\'ozoa, barnacles and other epi-
bionts, often with the addition of Waltonia inconspiciia
(Sowerb\', 1846) (Brachiopoda), upon which it has been
observed to feed (Scott, 1989 and pers. comm; K.W.B.,
pers. obs.).
Etjinology: After Ian Scott, Auckland.
ACKNOWLEDGMENTS
For the loan of type material, other specimens, and in-
formation, we are grateful to P. Bouchet and V. Heros
(Museum National d'Histoire Naturelle, Paris), N. Hiller
(Canterburv' Museum, Christchurch), I. Loch (Austra-
han Museum, Sydney), I. Scott (Auckland), A. Spurgeon
(Hamilton), FG. Thompson (Florida Museum of Natu-
ral Historv', Gainesville), and K.M. Way (The Natural
History Museum, London). We also record our indebt-
edness to our late friends D.W. Gibbs, PR. Jamieson,
and J.R. Penniket, who supplied some of die finest ma-
terial used in this study; and Wellington Shell Club
members, who provided Mahia Peninsula records of M.
octogomis. Thanks also to A.G. Beu (Institute of Geo-
logical and Nuclear Sciences, Lower Hutt), I. Scott
(Auckland), and anonymous referees for comments on
the manuscript, N. Heke and M. Hall (Museum of New
Zealand) for pliotography and photographic printing re-
spectively, and to W'. St. George (Institute of Geological
and Nuclear Sciences, Lower Hutt) for scanning elec-
tron microscope facilities.
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THE NAUTILUS 114(1):30, 2000
Page 30
Notices
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Dr. James H. McLean
Department of Malacology
Los Angeles County Museum of
Natural Histoiy
900 Exposition Boulevard
Los Angeles, CA 90007
Dr. Arthur S. Merrill
% Department of Mollusks
Museum of Comparative Zoology
Harvard Universit)'
Cambridge, MA 02138
Dr. Paula M. Mikkelsen
Department of Li\dng Invertebrates
The American Museum of Natural
History'
New York, NY 10024
Dr. Gustav Paulay
Marine Laboratory
University of Guam
Mangilao, Guam 96923
Mr. Richard E. Petit
PO.Box30
North Myrtle Beach, SC 29582
Dr. Edward J. Petuch
Department of Geology-
Florida Atlantic University
Boca Raton, FL 33431
Dr. Gai-y Rosenberg
Department of Mollusks
The Academy of Natural Sciences
1900 Benjamin Franklin Parkway
Philadelphia, PA 19103
Dr. Ruth D. Turner
Department of Mollusks
Museiun of Comparative Zoolog)-
Harvard University
Cambridge, MA 02138
Dr. Geerat J. Vermeij
Department of Geology
University of California at Davis
Davis, CA 95616
Dr. G. Thomas Watters
Aquatic Ecology Laboratory
1314 Kinnear Road
Columbus, OH 43212-1194
Dr. John B. Wise
Houston Museum of Natural Science
Houston, TX 77030-1799
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TH EfyNAUTI LUS
CONTENTS
Valium' 114. Number 2
June 6, 2000
ISSN 0028-1344
Douglas G. Smith Notes on the ta\onoiny of introduced Bcllainija
(Gastropoda: Viviparidae) species in northeastern North
America 31
Guido Pastorino A revision of the Patagonian genus Xijmeiiopsis Powell,
M. G. Harasewych 1951 (Gastropoda: Muricidae) 38
Jose H. Leal Copiilabi/ssia riosi, a new deep-sea limpet (Gastropoda:
Luiz Rieardo L. Simone Pseudococculinidae) from the continental slope off Brazil
with comments on the svstematics of the genus 59
G. Darrigran Invasion of the exotic freshwater mussel Limnopcnw
I. Ezcurra de Drago fortunei (Dunker, 1857) (Bivalvia: Mytilidae) in South
America 69
Warton Monteiro Location of allospermatozoa in the freshwater gastropod
Toshie Kawano Bioiuphalaiia tcna^iophila (d'Orbigny, 1835) (Pulmonata:
Planorbidae) 74
Jay Cordeiro Status of the tidewater mucket, Lcptodca ochracea (Say,
1817) (Bivalvia: Unionidae), in Halfway Pond,
Massachusetts. USA .' 80
Notices 84
THE NAUTILUS 114(2):31-37, 2000
Page 31
Notes on the tcixonomy of introduced BeUaniya (Gastropoda:
Viviparidae) species in northeastern North America
Douglas G. Smith
Department i)t Biologv' and
Graduate Program in Organismic anti
E\olntionar\ BiologN
Uni\ersit\' ot Massachusetts
Amherst,' MA 01003-5810 USA
dgsmith@bio.uaniss.edu
ABSTRACT
The genus BeUnmi/a has become well established in Nortli
America since its first introduction arovmd the turn ot the 20"'
centurv. Some malacologists have recognized two species, usu-
alK' placed in the genus Cipaiigopahidina. C. chinen.sis. and C.
japonica. Other investigators, however, have questioned a two
species concept or simply considered all populations to be xar-
iants of a single species, C. chinensis. Differences observed in
the juvenile shell and male reproductive anatomy, along with
size-specific features of adult shells, enable easv separation of
the hvo taxa and support the two species concept. Characters
of female and male reproductive anatomv confirms the place-
nient ot the species in the subfamik' Bellanninae. Anatomical
features which ha\e been used to substantiate Cipanaopahi-
dina are proposed to be of subgeneric value only.
Kei/ words: Introduced snails, Cipangopaludina, Idiopoma. Vi-
vipams. Lecijthoconcha.
INTRODUCTION
Among the more conspicuous members of the North
American freshwater gastropod fauna are the large ex-
otic viviparid snails customarily placed in the genus Ci-
pan^opaJiidina. The North American history of Cipaii-
gopahidina and its distribution was discussed and re-
viewed by Clench and Fuller (1965) (as a subgenus of
Vivipanis), Dundee (1974), and Joldnen (1982). The
majority of North American populations are confined to
the coasts, with scattered records from the interior At
present, the east coast appears to comprise the greatest
number of occurrences (Joldnen, 1982).
Since the earliest reports of Cipangopaludina popu-
lations in North America around 1900 there has been
much debate regarding the identification and \ali(lit\' oi
the various species and subspecies reptjrted and, to a
lesser extent, the status and position of the taxon Cipan-
gopaludina in the Vixaparidae. Hannibal (1912) proposed
the subgenus Cipangopaludina to accomodate Idiopoma
niallcata (Reeve, 1863), leaving /. japonica (von Mar-
tens, 1861) in Idiopoma s. s. Subsequent authors (e.g..
Annandale, 1920; Prashad, 1928) regarded Idiopoma
Pilsbrv', 1901, recognized primarily on features of the
operculum, as a synonym of Vivipanis. Annandale
( 1920) used anatomical characters to propose a new ge-
nus Lecijthoconcha to include L. cJiincncsis and, in a
later paper (Annandale, 1921), to include L. japonica as
well. Rao (1925) maintained use oi Lcci/thoconcha and
expanded the number of anatomical characters that de-
fine the genus, most notablv a folded and thickened gill
filament, a thickened muscular mantle edge, and the
"strongly developed brain". Prashad (1928) subsequently
synonymized Lecijthoconcha with Cipangopahidina but
retained Lecijthoconcha as a subgenus. Furthermore, he
reduced Idiopoma maUeata to a subspecies of V chinen-
sis (Gray, 1817). Kuroda (1929) adopted all of Prashads
(1928) revisions. Rohrbach (1937) primarily used char-
acters of the reproductive anatomv to divide the vivi-
parids into two subfamilies, the Vi\iparinae and a new
subfamily Bellamyinae. Under the Bellamyinae he listed
a single large genus, Bcllamija Jousseaume. Although
considered to be a genus largelv limited to tropical spe-
cies, Rohrbach (1937) was able to examine specimens of
a race of non-tropical V. chinensis that displa\ed anatom-
ical features of BcUaintja. Yen (1943) extended Rohr-
bach s (1937) classification to Chinese species and sub-
species, restateil the close relationship between Bella-
mija and Cipangopahidina, but retiuned Cipangopahi-
dina at the genus level.
The first major work on North American \i\iparids
following this period is Clench and Fuller's (1965) study
in which, for unkTiown reasons, they treat Cipangopa-
hidina as a subgenus of Vivipanis. These authors res-
urrected the trinomen V chinensis malleatus for all
North American populations of this species and listed it
as a species separated from V' (Cipangopahidina) japon-
iciis. Most subsequent studies on viviparid faunas (eg.
Pace, 1973: Taylor, 1981; Rao, 1989) have considered
Cipangopahidina a genus of the Bellamyinae.
North American opinion has been di\aded concerning
the \'alidit\' of the two introduced species (see Jokinen,
Page 32
THE NAUTILUS. Vol. 114. No. 2
1991, for review). Many North American faunal studies
including these viviparids have listed all large introduced
\iviparid populations with unhanded shells as Cipango-
pahidina chincnsis (eg. Robertson and Blakeslee, 1948;
Jacobson and Emerson, 1961; Dundee, 1974; Clarke,
197S). Other reports have recognized the two species C
chincnsis and C. japonica (eg. Wolfert and HUtunen,
1968; Burch, 1982; Tavlor, 1981; Jokinen, 1983, 1991;
Smith, 1995).
Certainly one of the problems affecting the species
issue is the apparent rant)- of the ta.\on C. japonica.
Clench and Fuller (1965) gave only four North Ameri-
can records, and Taylor (1981) listed only one in Cali-
fornia. Wolfert and Hiltunen (1968) listed an Ohio re-
cord and Jokinen (1984) provided an additional record
in Connecticut, but has before and since considered the
population C. chincnsis or doubtfully C. Japonica (Joki-
nen, 1983, pers. comm.). Jokinen (1991) subsequently
added a New York record that would be the eighth pub-
hshed North American record for C. japonica.
The impetus for the present study came from the dis-
covery of two wild, previously unreported populations of
C. japonica-morph sn;iils in Connecticut from which se\'-
eral variously aged specimens and reproductively active
females were collected. The present study provides com-
parative data on a number of characters of each species
in an attempt to determine whether two species or a
single variable species occurs in North America. Addi-
tionally, using data from reproductive organs and other
anatomical characters plus observations by previous au-
thors on viviparid subgroups, a proposal to reduce Ci-
pangopahidina to a subgenus ot BeUanu/a is presented.
Hereafter in this study these two species will be referred
to as Bellamija spp.
MATERIALS AND METHODS
Specimens from 12 extant or extirpated BcIIamt/a pop-
ulations were examined. The original assignment ot
specimens to either specific taxon was by use of adult
shell characters. The distribution of specimens is listed
below. All were fixed in 10% formalin, relaxed or unre-
laxed, and stored intact in 50-60% isopropyl alcohol. In-
tact shells of deceased animals were also collected. Each
collection has been catalogued in the Invertebrate Di-
vision, Museum of Zoology, University of Massachusetts,
Amherst (UMA). Collection numbers and other details
regarding the collections can be furnished upon request.
BcUami/a chincnsis s.l: UMA 0668, University Pond,
University of Massachusetts Campus, Amherst, Hamp-
shire County; UMA 0885, unnamed pond in Medford,
and UMA 1705, Lake Winthrop, Holhston, both Mid-
dlesex County; UMA 1635, Forest Park Ponds, Spring-
field, Hampden County; UMA 1663, Wachusett Reser-
voir Outlet, Worcester County; UMA 1094, Purchase
Louisiana Brook, Northfield, Frankhn County; UMA
1330, Pine Tree Brook, Milton, Norfolk County; UMA
1805, Snake River, Norton, Bristol Count>- (all Massa-
chusetts); UMA 1755, Black Pond, Middlefield, Middle-
sex County, Connecticut.
BcIIamija japonica: UMA 1754, Lake Mohegan,
Fairfield, F;iirfield County; UMA 1816, Connecticut Riv-
er, Lviue, New London County; UMA 1755a, Black
Pond, Middlefield, Middlesex County, all Connecticut.
Also examined were specimens (UMA 1700) purchased
from a pet store in Hadley, Hampshire County, Massa-
chusetts.
Samples ol intra-uterine juveniles were removed from
females. The animal was removed from the shell of each
juvenOe and the shell iiir dried. Radulae were also re-
moved from adult specimens, cleaned in 10% potassium
hydroxide, subsequently washed, and air dried. All dried
material was mounted on individual Cambridge stubs
with Duco cement and sputter-coated with gold. All pre-
pared specimens were then examined with a JEOL
Model JSM-5200 scanning electron microscope (SEM).
For anatomiciil study, at least five specimens of each
sex were dissected from the two largest collections of
each species as determined by shell characters. There-
after, dissections were made on at least one adult spec-
imen of each sex (if available) from each remaining lo-
cation. A total of 44 specimens divided almost evenly
among both species were analyzed. Dissections were
performed with the aid of a Wild M5 dissecting micro-
scope.
RESULTS
The principal conchological characters distinguishing the
tsvo taxa are the shape of the spire and the presence of
carination; to quote from Clench and Fuller (1965) re-
garding B. japonica: ". . .can be distinguished from V
mallcatiis (= C. chinen.sis) by having a more acute spire
and by having fine carina or carinae." An examination of
animals from presumed B. japonica populations reveal
that these characteristics are most evident in shells 35-
45 mm shell length (Figure 1). At this size, the species
can be separated using the diagnosis of Clench and Ful-
ler (1965). Below 35 mm shell length both species have
a carina on the body whorl. Above 45 mm, the carina of
B. japonica becomes nearly obsolete, and only a sfightly
more acute spire in B. japonica enables identification.
The source of differentiation in shell characters in
these two species is in part derived from an allometric
growth pattern first described by Jokinen (1982), who
showed that shell width in B. japonica increases at a
slower rate than in B. chincnsis. This phenomenon
would account for the more "acute spire" in B. japonica
described by Clench and Fuller (1965). The regression
slopes for each species, however, are only slightly differ-
ent (see Jokinen, 1982, fig. 2). Therefore, adult shell
moi-phology has its limitations in the distinction of these
two species.
A characteristic that appears to be reliable in separat-
ing B. japonica from B. chincnsis is the morphology of
the intra-uterine juvenile shell. The juveniles occurring
in the uteiTis or brood chamber, considered a functional
D. G. Smith, 2()()()
Page 3.3
Figure 1. Comparison of similar sized shells of Bdlamija.
Upper and lower left, B. japonica from Lake Mohegan, Con-
necticut. Upper right, B. chinensis from Medford, Mussachn-
sets, and lower right, B chinensis from Black Pond, Connect-
icut. Arrow denotes carina. Scale line = 10 mm.
modification of what is otherwise called the pallial ovi-
duct, demonstrate clear differences in the position of the
embryonic whorl (protoconch) and in surface sculpture.
Most viviparid snails in their juvenile stages have specific
features of the periostracum, including the presence of
periostracal hairs encircling the shell v\'horls, and surface
sculpture (Fretter and Griiliam, 1962; Joldnen, 19(S4).
In the juvenile shell of B. chinensis, the spire com-
prises only two elevated whorls (Figures 2-A). The em-
bryonic whorl is depressed in frontal view below the suc-
cessive whorl (first teloconch whorl), characterized by
two fines ot periostracal hairs, <3ne clearly evident on the
whorl, the other along the upper border (Figure 2, ar-
row). Such was observed in all examined populations. In
contrast, the embryonic whorl of B. japonica (Figure 5)
is somewhat elevated above the first teloconch whorl,
indicated by two spiral fines of periostracal hairs, which
in frontal view gives the shell the appearance of having
four whorls.
Differences in periostracum are even more eNddent
than those in whorl development. The periostracum of
the body whorl of juvenile B. chinensis (Figures 6, 7) is
finely sculptured with a series of closely set striae, about
20/mm near the midpoint of the body whorl, interrupted
by peqiencficular shallow grooves more widelv spaced
than tlie striae. The spiral lines bearing the fine hairs are
not raised as spiral carinae. In B. japonica (Figure 8),
the surface of the periostracum is strongly marked by
raised carinae, each having a series of periostracal hairs.
Between the carinae are widely spaced spiral striae,
about 8/mm near the middle of the whorl. Although oc-
casional interiTiptions occur, there is no pattern of dis-
tinct grooves as found in and characteristic of B. chinen-
sis.
Regarding anatomical characters, the radula provides
no specific or cfistinctive characters for interspecific dif-
ferentiation. Veiy subtle cfifferences (Figures 9, 10) oc-
cur in the spacing of denticles of the lateral teeth for
example, but these differences are probablv subject to
variation and should not be considered as refiable taxo-
nomic characters. The gill filament of each species con-
sists of an elongate structure, measuring up to 5 mm
length in the largest (>50 mm shell length) individuals.
The filament is broadest at its base where it is attached
to the mantle, narrowing in depth cfistally. A cfistinct
blood vessel courses its length just below the thickened
superior margin. The "fokfing" of the filament described
by Rao (192.5) in a few species, and used subsequently
as a character of Cipangopahulina. was not observed in
material of either species.
Major features of both the male and female repro-
ducti\'e svstems demonstrate an overall conservative
structural plan clearly characteristic of the Bellamyinae
as defined by Rohrbach (1937). Dissection of the female
reproductive system revealed no consistent differences
between B. chinensis and B. japonica. Within the male
reproductive system, the \'as deferens of each species
shows distinct differences in its cfimensions and its re-
lationship with both the columellar muscle and the tes-
tes. In B. chinensis (Figure 11), the vas deferens arises
from the testes as an unbranched tube. All further
branching of the vas deferens occurs internally within
the testes. Occasionally, a single large anterior branch
merging with the vas deferens is partially visible. The
emerged vas deferens widens considerablv as a complex
duct and proceeds a short cfistance, suspended by mes-
enteries, until it reaches the columellar muscle. At this
point, the remaining portion of the vas deferens bends
shaqiely downwards. It then abruptly and without en-
largement enters the prostate. The downwardlv cfirected
portion of the vas deferens remains free of the colu-
mellar muscle although it is supported throughout by
mesentaiy tissue.
The vas deferens of B, japonica departs from the tes-
tes multibranched, with at least three and usually four
visible branches converging to a single duct (Figure 12).
The duct then enlarges, but not to the degree seen in
B. chincn.'iis, and extends a greater distance, suspended
by mesentery tissue, until meeting with the columellar
muscle where, as in B. chinensis, it bends downward
and, without enlargement, joins the prostate gland. Un-
Page 34
THE NAUTILUS, Vol. 114. No. 2
ij^gaiit«^Jgi*jfj
BD
m
v^
m
3 -
■N "1
BD
Figures 2-5. Spire of juvenile shells ot Bellnmya. 2-4. Bellamtja chinensis. 2. Black Pond, Connecticut. 3. Wachusett Reservoir,
Massachusetts. 4. Campus pond, Amherst, Massachusetts. Figures 3, 4, apical whorls only. 5. Bcllami/a jnponica. Lake Mohegan,
Connecticut. BD = hodv whorl. Scale line = 0.5 mm.
hke B. chinensis, however, the portion of the vas defer-
ens pro>diiial to the prostate gland is invested with col-
umellar muscle tissue. Odier aspects of gross anatomy
of the male reproductive system, including testes size
and shape and prostate size and shape, are similar in the
two species.
The characteristics of the vas deferens in each species
were most pronounced in the larger animals. The hvo
patterns were concordant with shell characters in all but
one case, the Black Pond locality. Both species occur in
this pond and examined males show features of shell and
reproductive anatomy consistent with above observations
or variations of each. Most males from this collection,
however, are young adults (<.'35 mm shell length) and,
as stated above, the anatomical characters inchcative of
each species are best developed in larger specimens.
Nevertheless, it is possible that hybridization is occur-
ring. Previously, in North America, both species have
been reported in sympatiy (Lake Erie; Wolfert and Hil-
tunen, 196S), but not in svmtopy so it is not known if
hydridization is a usuiJ outcome of contact.
DISCUSSION
Although adult shell structure as presented by Clench
and Fuller (1965) does not in and of itself provide con-
\incing evidence for the recognition of two distinct spe-
cies, the characters of the embrvonic shell and male re-
proilucti\e system in combination with shell features in-
dicate that at least Uvo similar but distinct species of
Bcllami/a are present in North America. The question
remains, however, regarding which names to assign
these species; is enough information available to warrant
use of the two specific epithets, mallcata and japonica
as hsted by Hannibal (1911) soon after the species were
first reported in North America? If so, then what is the
the status of the name B. chinensis?
Clench and Fuller (1965) gave a partial history of the
D. G. Smith, 2000
Page 35
Figures 6-8. Penostracal surface of body whorl ol ju\eiiile Bellami/a^ 6. B. chinensis from Black Pond, Connecticwt. 7. Same,
Forest Park ponds, Springfield, Massachusetts. 8. B. japonica from Lake Mohegan, Connecticut. Scale line = 0..5 mm. Figures 9-
10. Radula (central and lateral teeth). 9. Bilhiim/a japonica. 10. Bcllainija chinensis. Scale line = 0.05 mm.
taxonomy and nomenclature of these species. As can be
deduced from their account, the original descriptions of
these species were essentially brief accounts of the adult
shell with very little geographical data provided. Pace's
(1973) review of the titxonomv of B. chinensis probably
best summarizes the nomenclatural and taxonomic con-
fusion that accompanies this species. Seemingly every
race or form encountered by earlv workers was estab-
lished on the most subtle of characters. Differences of
opinion on the validity of named forms and generic as-
signment was quite likely compounded by difficulties in
communication between Asian and European investiga-
tors. Unfortunately, the practice of naming new species
of Asiatic viviparids on the basis of a few qualitative shell
characters continues (Li, 1990; Liu ct ai, 1994). Until
future study requires otherwise, I follow Pace (1973) and
other earlier workers who assert that many of the sub-
sequentlv named forms related to B. chinensis. including
B. mallcata, are at most subspecies. Given that subspe-
cific status is normal!)- maintained through geographic.
Page 36
THE NAUTILUS, Vol. 114, No. 2
CM
VD
CM
Figures 11-12. Anatomy of male reproductive structures.
11. Bellaimja chinensis. 12. Bellamya japonica. Scale applies
to figures 11 and 12. CM = coliimellar muscle, CT = con-
nective tissue (mesentery), F = fibers of columellar muscle, P
= prostate, T = testes, VD = vas deferens.
(1912) in his description, the foundation of Cipangppa-
liidina hes chiefly in certain anatomical features dis-
cussed above. Folding of the gill filament, a character of
Cipangopahidina estabhshed by Rao (1925), was not ob-
served in either species. Folding of the filament mav be
caused by contraction or mav represent distortion as a
result of preservation. A thick mantle edge and a devel-
oped sphincter muscle are present in both species, but
based on comparison with smaller Vivipants georgianus
(I. Lea, 1834) thickness and muscle size can be related
to animal size (Smith, pers. observ.). A comparison of
mantle types illustrated by Annandale (1920: 112) and
used to characterize Lecijthoconcha (= Cipangopahidi-
na) apart from other genera more clearlv demonstrates
a gradation of mantle development among the groups he
discussed. In relation to brain comple.xity (sensu Rao,
1925), more detailed studies are necessary for the prop-
er evaluation of this character. Following Rohrbach's
(1937) anatomical svstem, which was somewhat extend-
ed by Pace (1973), B. japonica represents a group within
Bellamya that is characterized by a branched vas defer-
ens proximal to the testes; Bellamya chinensis represents
a sister group that has an unbranched tree portion of
the vas deferens. Vail (1977) has addressed the problems
of subgroups within Bellamya in a more general fashion
and suggested that further studies are necessary to es-
tablish natural groups within the Bellamyinae. It is thus
proposed that Cipangopahidina should be treated as a
subgenus of Bellamya, a decision with some precedent.
Cipangopahidina would provisionally embrace the large
bellamvids with unhanded shells during any part of their
life historv and with native distributions fimited to Asia.
ACKNOWLEDGMENTS
I thank Eileen Jokinen for providing useful input and
comment on various drafts of the paper. Kenneth Boss
provided extensive information on the taxonomy and lit-
erature of Asian bellamvids.
not genetic, separation, and that several populations of
interbreeding B. chinensis have been introduced into
North America, the features that defined any particular
subspecies have most likelv been obliterated. Further-
more, in that most opinion leans towards a Japanese or-
igin for at least some of the North American populations
and that populations of each species have been reported
in Japan (Kuroda, 1929), I believe that B. japonica s. I.
and B chinensis s. I. are the species involved.
The decision to place both species with Bellannia re-
sults in part from Taylor's (1981) statement, substanti-
ated by anatomical data pro\ided in this studv, that B.
japonica belongs to the Bellamvinae. With respect to the
continued use of the name Cipangopahidina lor 6, chi-
nensis, those characters used to substantiate the genus
are either variable or characteristic of animals reaching
a relatively large size. Notwithstanding the absence of a
carina on the adult shell, originally used by Hannibal
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Page 37
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THE NAUTILUS 114(2):38-58, 2000
Page 38
A revision of the Patagonian genus Xijryienopsis Powell, 1951
(Gastropoda: Muricidae)
Cuido Pastorino
Museo Argentino de Ciencias Natiirales
Av. Angel G;illardo 470, 3° piso, lab. 57
CUOsbjR Bvienos Aires
ARGENTINA
rvpastor@criba.edu . ar
M. G. Harasewych
Department of Inxertebrate Zoology
National Museum of Natural History
Smithsonian Institution
Washmgton. D.C. 20560-0118 USA
Harasewych@nmnh.si.edu
ABSTRACT
The genus Xt/menopsi.s Powell, 1951 is re\ised and restricted
to 4 Recent species: Xtjmenopsis miiriciformis (King and Brod-
erip, 1832), X. comigatus (Reeve, 1848), X. huccineus (La-
marck, 1816) and X. suhnodosus (Gray, 1839). Of the 34 nom-
inal species that have been described as or assigned to Xtjmen-
opsis by various authors, 3 belong to the buccinid genus Pa-
reuthria and I is a trophonine nuiricid not closely related to
Xymenopsis. The ta.xononiic affinities of each of the remaining
.30 names (one is a replacement name) are discussed. Ele\en
holot)pes and ten lectotypes (nine newly designated) are illus-
trated, many for the first time. Tvpes of .3 taxa were destroyed
during World War II and another 5 t)pes are lost. Neotvpes
are designated for Fusus huccineus Lamarck, 1816, the oldest
name to be applied to any species of Xymenopsis, as well as
for Buccinum subnodosa Gray, 1839, Trophon brucei Strebel,
1904, Trophon fcnestratus Strebel, 1904, Trophon paessleri tur-
rita Strebel, 1904, Trophon ringci Strebel, 1904 and Trophon
standcni Strebel, 1904. This is done to remo\e anv ambiguity
regarding the identity of these ta.\a, and thus stabilize the no-
menclature of Recent species of Xymenopsis. The gross anat-
omy and moqjhology of the radula, egg capsule, protoconch,
and shell ultrastructure of the type species of Xymenopsis are
described and illustrated. Xymenopsis is compared to, and dif-
ferentiated from, the genera Xynwne. which is restricted to
New Zealand, and Trophon. with which it co-occurs in the
Magellanic province.
Key words: Neogastropoda, Trophoninae, Patagonia, Magel-
lanic Province.
INTRODUCTION
The genus Xymenopsis encompasses a group of small,
conchologicaUy variable muricid gastropods endemic to
the Magellanic Prox-ince. These shell-drilling predators
commonly co-occur wdth species of Trophon on mussel
beds, and range from the intertidal zone to depths ex-
ceeding 100 meters. The majority of the published Bt-
erature on this group dates from the early era of Ant-
arctic and subAntarctic exploration, and has concentrat-
ed on describing numerous, minor phenotypic variants
as species. The biologv' ot these animals has not previ-
ously been stuched.
Powell (1951) erected the genus Xymenopsis to dis-
tinguish Patagonian muricids with a conical, multi-
whorled protoconch and rounded ;mal ribs from those
with a rounded, paucispiral protoconch and numerous,
lamellose varices that belong to the genus Trophon. He
attributed 30 nominal taxa to Xymenopsis, but recog-
nized that many would prove to be synonyms, stating
that "An evaluation of these names is not possible with-
out recourse to the tyj^e material which is in European
museums." Imphcit in the generic name Xymenopsis is
Powell's recognition of the close affinity of this Magel-
lanic group to Xymenc Iredale, 1915, which is endemic
to New Zealand. Powell (1951) noted that the shell
sculpture of Xymenopsis was similar to that of Xyniene,
but that its protoconch resembled that of Zcatroplwn
Finlay, 1927, another New Zealand genus.
In his revision of New Zealand muricids assigned to
the genus Trophon, Finlay (1926) proposed several su-
praspecific taxa, each representing what he regarded to
be a hneage or "natural grouping." He divided these taxa
into 2 groups, based primarily on protoconch morphol-
ogy. One group, defined on the basis of having a sym-
metrically conical protoconch of > 2 whorls and a small
nucleus, contained the genera Xymenc Iredale, 1915,
XymcncUa Finlav, 1926, and Zcatrophon Finlaw 1927.
The second group, recognized by having an asymmetri-
cal, rounded protoconch of 1-2 whorls, with a large, lat-
eral nucleus, included Axymene .scvi.si/ stricto Finlay,
1926, Axymcnc (Lcnitrophon) Finlay, 1926, Comptella
Finlay, 1926, Tcrcfundus scnsit stiicfo Finlay, 1926, and
Terefiindus iMinoiirophon) Finlay, 1926.
Ponder (1972) rexdewed the Recent and fossil New
Zealand species related to Xymenc. Based on an analysis
of gross anatomy, shell, and radular moqihology, he con-
cluded that the taxa Axymene, Lenitrophon, XymeneUo,
Zcafroplion, and probably Vc.5flri(//fl Finlay, 1926, did not
merit taxonomic recognition even at the subgeneric lev-
el, and reduced all but Vesatuda to .svmonyms oi Xymenc.
However, he regarded Xymenopsis sufficiently distinct to
G. Pastorino and M. G. Harasewvch, 2()()0
Page 39
Table 1. Tiixa attributed to the genus Xijiiu'iiopsis by Powell (1951) and Dell (1971, 1972). Taxa listed ni bold are valid species.
Troplion iiciiininntus Strebel, 1904
Trcphon (dints Strebel, 1904
Fiisiis cilhithis Philippi, 1845
Tniplioti bnitti Strebel, 1904
Xymenopsis buccineus (Lamarck, 1816)
Troplion canccllarioidi's Ree\e, 1847
Xymenopsis canccllinns (Philippi, 1S45)
Fiisiis candidatiis Rochebnnie and Mabille, 1889
Xymenopsis corrttgattts (Reeve, 1S4S)
Troplion coiithoiii/i Strebel, 1904
Fiisiis decolor Philippi, 1845
Fiisiis dispar Rochebnine and Mabille, 1889
Troplion elcfians Strebel, 1904
Troplion elongatiis Strebel, 1904
Trojihon fnlklandiciis Strebel, 1908
Troplion fenestratiis Strebel, 1904
Troplion hoijlei Strebel, 1904
Fiisns jarqiiinoti Philippi, 18.55
Fiisiis lebnini Mabille and RochebiTnie, 1889
Fiisiis liratiis Gould, 1849
Fiisiis loebbeekei Kobelt, 1878
Xymenopsis muriciformis (King and Broderip, 1832)
Troplion obesiis Strebel, 1904
Troplion ornatiis Strebel, 1904
Trophon paessleri Strebel, 1904
Troplion paessleri turrita Strebel, 1904
Fiisiis pliimbeiis Gould, 19.52
Trophon pseiidoelonoatiis Strebel, 1904
Trophon ringei Strebel, 1904
Fiisiis roseiis Honibron and Jacquinot, 1854
Trophon standeni Strebel, 1904
Xymenopsis subnodosus (Gray, 1839)
Fiisiis textdiosiis Honibron and Jacquinot, 1854
Fiisiis violaceiis Mabille and Rochebnnie, 1889
(syiiony-m of Xipnenopsis nuiricifoniiis <
(synonym of Xiimenopsis iniirieifonnis)
(synonyiii ol Xipm-nopsis hiiriineiis)
(.synonym ol Xiinuiu>psis rornio/itiis)
(synonym ot Xt/menopsis iniiririfonnis)
(synonym of Xymenopsis subnodosus)
(belongs in the buccinid genus Fareuthria Strebel, 1905)
(synonym of Xynwnopsis muririfonnis)
(synonym of Xymenopsis muririfonnis)
(belongs to different niuricid genus, not Xymenopsis)
(synonym ot Xymenopsis miiricifonnis)
(synonym of Xymenojisis muriciformis)
(synonym o( Xymenopsis corrugatiis)
(synonym of Xymenopsis muriciformis)
(synonym of Xymenopsis cornigatus)
(new name for F. textiliosus Honibron and Jacquinot. 1854, not
F. textiliosus Deshayes. 18.35)
(synonym of Xymenopsis miiricifonnis)
(syiionyiii of Xymenopsis miiricifonnis)
(sviionym of Xymenopsis muriciformis)
(synonym of Xymenopsis miiricifonnis)
(synonym of Xymenopsis cornigatus)
(synonym of Xymenopsis muriciformis)
(synonym of Xymenopsis muriciformis)
(belongs in the buccinid genus Fareuthria Strebel, 1905)
(synonym of Xymenopsis nuiriciformis)
(synonym of Xymenopsis buccineus)
(belongs in the buccinid genus Pareiithria Strebel, 1905)
(synonym of Xymenopsis cornigatus)
(synonym of Xymenopsis buccineus)
(synonym of Xymenopsis miiricifonnis)
be treated as a subgenus of Xijmene. Despite reducing
their taxonomic rank. Ponder (1972) recognized 5 dis-
tinctive groups within the Xijmenc complex, correspond-
ing to: 1) Xymene + Xijinenclla; 2) Zcatrophon; 3) a
group consisting of 2 fossil species (1 Eocene, 1 Mio-
cene) with features expected in the "ancestor of all the
species of Xymene"; 4) Axymciw; and 5) Xi/menopsis.
Beu and Maxwell (1990:39) reported Xymene to range
from the Kaiatan (= Bartonian, Late Eocene) to the
Recent in New Zealand. The fossil record of Xymenopsis
is thus far limited to 4 species recently described from
the Late Miocene Entrerriense Formation along the Val-
des Peninsula in northern Patagonia, Argentina (Bninet,
1997). While there is little doubt that Xymene and Xy-
menopsis are closely related, these lineages are treated
here as separate genera.
In the present study, we review and discuss all Recent
nominal species that have been included in Xymenopsis
(Table 1) based on an examination of available type ma-
terial. Type specimens of all taxa referable to Xt/men-
opsis that could be located are illustratetl, some for the
first time. Data on shell ultrastructure, radular mor-
phology, and gross anatomy are provided for Xymenopsis
miiricifonnis, the type species oi Xymenopsis. Compar-
ative data are provided for Xymene plcbeiiis, the type
species of Xymene, and for the other Recent species of
Xymenopsis.
MATERIALS AND METHODS
The majority of specimens examined in this study are in
the collections of: the National Museum of Natural His-
tory, Smithsonian Institution, Washington, DC (USNM);
Museo de La Plata, La Plata, Argentina (MLP); Museo
Argentino de Ciencias Naturales "Bernardino Rivada-
via", Buenos Aires (MACN); and the Los Angeles Coun-
ty Museum of Natural History (LACM). Type material
is housed in the following museimis: The Natural His-
tory Museum, London, (BMNH); Zoologisches Institut
und Zoologisches Museum der Universitat Hamburg,
(ZMH); Swedish Museum of Natural History, Stock-
holm, (NHRM); Museum national d'Histoire naturelle,
Paris (MNHN); Museo Nacional de Historia Natural,
Santiago, Chile (MNHNS); and, Loebbecke- Museum
und Aquazoo, Dusseldorf, (LM).
Dissections were performed on ethanol preserved
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THE NAUTILUS, Vol. 114. No. 2
G. Pastorino aiul M. G. Harasewych, 2000
Page 41
specimens to studv their gross anatomy, with emphasis
on the nioiphologN' of the anterior alimentary system,
and the palli;il portions ol the male ami female repro-
ductiye systems. Radulae were prepared according to
the method described by Solem (1972) and observed
using a LEO 440 scanning electron microscope (SEM).
Radular terniinolog) follows Kool (199.3a: fig. 6B). ,Shell
ultrastnicture data were procured from freshly fractured
collabral sections taken from the central portion of the
lip on the last whorl of 2 individuals per taxon, whenever
sufficient material was available.
Most photographs were taken using a Leaf Lumina
digital scanning camera. Several images were scanned
from black and white .35 mm negatives using a Nikon
Coolscan III slide scanner. All images were processed
with the software Photoshop 4.01 and 5.02.
SYSTEM ATICS
Class Gastropoda Cuvier, 1797
Order Neogastropoda Wenz, 1938
Family Muricidae Rafinesque, 1815
Subfamily Trophoninae Cossniann, 1903
Genus Xymenopsis Powell, 1951
Xijinciiopsis Powell, 1951:1.58; Radwiii and D'Attilio, 1976:190.
Xijnwne iXtjmenopsis) Ponder, 1972:474; Yokes, 1991:10.
Type species: Ftistts Uratiis Gould, 1.S49 (by original designa-
tion), a junior synonym of Bticciiiuin iniiricifonne King
and Broderip, 18.32. '
Diagnosis: The genus Xi/incuopsis contains species
characterized by a small to medium-sized (to 48 mm),
fusiform, high-spired shell with a tall, conical, multi-
whorled (==3 whorls) protoconch that lacks a keel, and
a teleoconch with a rounded shoulder, sculpture of
rounded axial ribs that never develop lamellae, and nar-
row to broad spiral cords that may or may not produce
beads at intersections with a.xial ribs. The siphonal canal
is short, open, and broad. Shell ultrastructure consists of
an outer amorphous calcific layer and an inner, crossed-
lamellar aragonitic layer. The rachichan tooth of the rad-
ula has a basal plate that is simple and concave anteri-
orly, and inner lateral denticles that are completely free
from the central and lateral cusps. The mantle edge is
always lobulated.
Remarks: In his treatment of the Xi/mcne complex.
Ponder (1972) identified the oldest known member of
the group in the Late Eocene fauna of South Island,
New Zealand. He recognized that Xi/inciw apipagpdus
Ponder, 1972, characterized by a small, strongly shoul-
dered shell with ;L\ial lamellae, smooth aperture, and a
tall, conical, 4y2-whorled protoconch with a sinuated var-
L\ indicative of a pelagic larval stage, had features from
which all subsefjuent Xi/mene lineages could be derived,
and suggested that several lineages evolved from this
phenotype.
One hneage compri.ses the Zcatrophoti group, which
appeared during the Late Oligocene {Xtfiiwrw chatto-
ncnsis Ponder, 1972, Duntroonian) and persists in the
Recent fauna (e.g., Zcafrophou amhitnius Finlay, 1927,
the type species oi Zcatwphon). This hneage is charac-
terized l)y a tall, strongly shouldered shell with axial
nodes or weak lamellae, an aperture with or without lir-
ae, and a protoconch that is tall and conical, yet smaller
and with fewer (2%-3V4) whorls than X apipagodns.
Within this hneage, there is a trend for a spiral keel to
develop on the last protoconch whorl, and for the nu-
cleus of the protoconch to increase in size. A second
lineage iXijmcnc + Xymcnclla group) also appeared in
the Late OUgocene (Trophon lepidiis Suter, 1917, Dun-
troonian) and survives in the Recent fauna (e.g., Ftistis
pk'bciiis Hntton, 1873, the tvpe species of Xijmcnc, and
Trophon pii.sillns Suter, 1917, the type species of X(/-
iiicncUa). Shells are small, strongly to weakly shouldered,
with strong spiral cords and axial ribs, but without la-
mellae, and with apertures that are usually lirate. Pro-
toconchs are depressed, with a trend to fewer (2 whorls
in X. plchcuis, 2 Vi whorls in X. gouldi = T. piisiUus, see
Ponder, 1972), more inflated whorls, and an increase in
the size of the nucleus. Another hneage (Axipnene
group) is limited to Pliocene and Recent species. Shells
tend to be large, strongly shouldered, with axial rilis and
spiral cords, but without lamellae, and generally have
lirate apertiues. Protoconchs consist of 1-2 roimded, in-
flated whorls, with a large nucleus.
Ben et al. (1997) regarded Xifmcnc and Xymcnclla to
be distinct genera, and reassigned Triton dauizcnhcrgi
von Ihering, 1897, and Urosalpinx elegans Ortmann,
1900, both from the Monte Leon Formation (Late Oli-
gocene-Early Miocene) of Patagonia, to Xymcnc. and
Xymcnella respectively. Based on the first occurrences
of these taxa in the fossil record, they concluded that
Xymcnclla originated in New Zealand and dispersed to
South America with the origin of the Antarctic Circum-
polar Current at the time the Drake Passage opened
(Late Oligocene), while Xymene evolved in South Amer-
ica and dispersed to New Zealand, also along the Ant-
Figures 1-19. Xi/incnopsis luiiricifonnis (King and Broderip, 18.32). 1-3. Holotvpe of Fiisus liratiis Gould, 1S49, USNM 5680,
Orange Harbor, Tierra del Fuego. 4-6. HoJotype of Trophon loebheckei Kobelt, 1878, Loebbecke Museum unnumbered, lacks
locality data. 7-8. Lectot\pe of Trophon violacetis Mabille and Rochebmne, 1889, MNHN unnumbered, Baie Orange, Tierra del
Fuego. 9-10. Holotype of Fusiis decolor Philippi, 1845, MNHNS unnumbered. Strait of Magellan. 11-12. Lectotype of Trophon
elegans Strebel, 1904, ZMH unnumbered. Port Stanley, Malvinas (Falkland) Is. 13. Leetotype of Trophon lebnini Mabille and
Rochebrune, 1889. MNHN unnumbered, Santa Cruz, Argentina. 14-16. Leetotype of Biiccimim niuricifonne King and Broderip.
1832, BMNH 1837.12.15.2695, Strait of Magellan. 17-19. Leetotype as Bnrciniim cnncrUnrioidcs Reeve, 1847. BMNH 19920.55,
lacks locality data. Scale bar = 1 cm for all specimens.
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THE NAUTILUS, Vol. 114, No. 2
G. Pastorino and M. G. Harasewvch, 2000
Page 43
arctic Circunipolar (^iinciil, diiriiit;; (lie Middle Mio-
cene.
The origin of the Xt/incitc complex in New Zealand is
amplv supported In tlic fossil record. The hvpothesized
dispersal ot this liiu'age to Southern South America dur-
ing the Late Oligocene is concordant with its appearance
in the fossil record of the region, and is supported bv
the prexalence of narrow, polvgyrate protoconchs, inchc-
ative of pelagic lanal stage (see Thorson, 19.50; Shuto,
1974; Jablonsk)- and Lutz, 1980), in Paleogene members
of this complex. Recent and fossil species of Xijmenopsis
are most similar to members of the Xt/iiicuc + Xi/inc-
nclla group, especially to early members of this lineage
such as the Oligocene Xi/mcnc Icpichis. with which they
share a sculptural pattern of axial ribs and spiral cords,
but not axial lamellae, and a conical, .3 whorled proto-
conch with a small, apical nucleus. We suggest that Xi/-
meiwpsis represents a radiation endemic to the Magel-
lanic region from ancestors of the Xijmcne + Xi/iucnclla
group that dispersed as larvae to Patagonia tluring the
Late Oligocene.
While it is possible that multiple lineages were intro-
duced to South America, or that 1 lineage subsequently
dispersed back to New Zealand while becoming extinct
in South America, evidence for such hypothe.ses is more
tentative or lacking. Xi/mcnc are characterized bv a trend
to protoconchs with fewer, more roimded whorls that
are indicative of lecithotrophic rather than planktotroph-
ic development. This would argue against their abihty to
disperse as plank-tonic laivae from South America east-
ward on the Antarctic Circunipolar Current to New Zea-
land. Clearly, a rigorous re-assessment of the Xymene
complex in a phylogenetic context would resolve many
of the systematic and biogeographic questions that have
plagued this group.
Xijincnopsis lack the strongly shouldered shell of the
Xymene + Xymenella group. While strong apertural lirae
are prevalent in Xi/mcnc, they are rare in Xymcuopsis.
occurring only in the X. .siihnodosus (Gray, 1839). X(/-
mcnop.sis may also be distinguished from Xtpticitc on the
basis of shell ultrastiiicture, radular moiphology and by
features of their mantle edge and egg capsules. Xymen-
opsis (figures 45, 79, 80) has a thick (> Vi shell thick-
ness) outer layer of calcite, and a single layer of crossed-
lamellar aragonite in which the crystal faces are comar-
ginal. In Xymene (figure 50), the calcitic layer is thin,
the co-marginal layer of aragonite thickest, and an in-
nermost layer of crossed-lamellar aragonite, with civstal
faces perpendicular to those of the co-marginal layer, is
also pre.sent. The radula i)^ Xymene pleheiiis has rachi-
dian teeth (figure 51) that ari> characteristically chevron-
shaped, eac'h with its apex at the mid-point of the an-
terior (>dge of the basal plate, which has a concave pos-
terior edge. Rachidian teeth oi' Xymcuopsis (figures 48-
49, 75-76, 81-82, 102-103) have a straight to sfightly
concave anterior edge, and a convex posterior edge of
the basal plate. The mantle edge of Xymene is smooth,
while the mantle edge oi' Xymenopsis is lobulated. While
egg capsules ui' Xymene (figure 43) and Xymenopsis (fig-
ure 42) are similar, the exit aperture is apical in Xymene,
Init is situated at the base of a shallow depression in
Xymenopsis.
There are no direct observations on development in
Xymenopsis. Shuto (1974) reported that the ratio of the
protoconch chameter (D) to the number of whorls (V)
is a reasonable estimator of the t\pe of development,
and that a ratio below 0.3 is characteristic of plankto-
trophic larvae, especially when the number of whorls is
s 3. Both Xymenopsis muriciformis (figure 41) and X.
huecineus (figures 77-78) have narrow, conical proto-
conchs of 3 whorls. The DA' ratios for these species are
0.23 and 0.21 respectively, predicting that, unlike Xy-
mene, Xymenopsis retains planktotrophic larval devel-
opment.
Powell (1951) provisionally included the species Fusus
rosens Hombron and Jac(juinot, 1854 and Trophon ean-
didatiis RochebiTine and Mabille, 1889 in his genus Xy-
menopsis. Ceniohorsky (1977) subsequently transferred
Fusus ro.seus to the buccinid genus Pareuthria Strebel,
1905. He proposed the new name Pareuthria powelli for
this species because Fusus roseus Hombron and Jac-
quinot, 1854 was preoccupied by Fusus roseus Anton,
1838. The type material of these taxa was examined by
the senior author at the Museum national d'Histoire na-
turelle, and both are clearly referable to the buccinid
genus Pareuthria. The type material of Fusus dispar
Hombron and Jacquinot, 1854 was also examined
(MNHN). This taxon has affinities with the Antarctic
Trophoninae, but does not belong to the genus Xymen-
opsis.
Xymenopsis muriciformis (King and Broderip, 1832)
(Figures 1-42, 45-49, 83-95, 105-106)
Biicciniiin miiricifonne King and Broderip, 18.32:.348.
Fusus muricifonuis King and Broderip — Gray, 18.39:118.
Fusus huecineus Sowerby in Gray. 18.39:15.5, pi. .36, fig. 12.
Fusus decolor Pfiilippi, 1845:68; 1846:118, pi. 3, fig. 3; Hupe
Figures 20-40. Xymenopsis muriciformis (King and Broderip, 1832). 20-22. Holot\pe of Trophon ncuniinntus Strebel. 1904,
ZMH unnumbered. Punta Arenas. Strait of Magellan. 23-25. Lectotype of Trophon couthoui/i Strebel, 1904, ZMH unnumbered.
Port Grappler, Smyth Gliannel. 26-28. Lectotype of Trophon paessleri Strebel, 1904. (specimen coated with ammonium cliloride),
ZMH unnumbered. Port Grappler, Sm\th Channel, 29-.31. Holotvpe oi'TropIion pscudoehinaatus Strebel. 1904, ZMH unnumbered,
Ushuaia. 32-34. Lectotype olTroplion ohciiis Strebel, 1904, ZMH unnumbered, Punta Arenas, Chile. 35-37. Leetot^-pe of Troplwn
elongatus Strebel, 1904, ZMH unnumbered, Puerto Angosto. Strait of Magellan. 38-40. Holotyjie of Trophon albus Strebel, 1904.
ZMH unnumbered, Ushuaia. Scale bar = 1 cm for all specimens.
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THE NAUTILUS, Vol. 114, No. 2
G. Pastorino and M. G. Harasewych, 2000
Page 45
in Gav, 1854;162; Homhroii and |a<.(|uin()t in Rousseau,
1854:i08, pi. 2.5, figs. 6-8; Kolx-lt', 1878:291, pi. 74, figs.
5-6; Rochebrune aiid Mabille, 1889; H.54.
Buccinum cancellarioicles T{ee\e, lS47:pl. 14, fig. 11.3.
Fusiis liratus Gould, 1849:141.
Trophon liratus Couthous- — Kobelt, 1878:.31(); Tryon, 1880:
14.3, pi. 31, fig. 3.33; Watson 1886:165; Lamv. 1906:3.
Trophon Locbbcckci Kobelt, 1878:294, pi. 74, 'figs. 13, 14;
TnoH, 1880:145, pi. 31. fig. .3.35.
Trophon nuiricifonnis King — Tnon. 1880:145.
Trophon Icbnini Mabille and Rochebnnie in Rochebnine and
Mabille, 1889: H..55.
Trophon violaceus Mabille and Rochebnine in Rochebnine
and Mabille, 1889: H.56, pi. 2, fig. 1.
Trophon paessleri Strebel, 1904:213. pi. 7, figs. 56a-f.
Trophon paessleri \'ar. turrita Strebel, 1904:215, pi. 7, fig. 57.
Trophon elon^atus Strebel, 1904:217, pi. 7, figs. .58a-f.
Trophon pseudoelong,atiis Strebel, 1904:220, pi. 7, figs. 60a,b.
Trophon albus Strebel, 1904:221, pi. 7, fig. 61.
Trophon acuminatus Strebel, 1904:222, pi. 7, fig. 63.
Trophon obesus Strebel, 1904:223, pi. 7, fig. 62.
Trophon fenestrattis Strebel, 1904:225, pi. 7, fig. 59a-d.
Trophon couthoinji Strebel, 1904:236, pi. 7, fig. 65a-e; Pi. 8,
fig. 76.
Trophon elegans Strebel, 1904:241, pi. 8, fig. 71.
Xt/menopsis hratiis (Gould) — Powell, 1951:158; Radwin and
D'Attilio, 1976:190, fig. 1.36.
Xijmenopsis decolor (Philippi) — Dell. 1971:211.
Xtjmenopsis muricifonnis (King and Brodenp) — Dell, 1972:8,
figs. 31, .32; Yokes, 1991: 7, unnumbered fig.; Yokes, 1992:
3, figs. 8a-c; Castellanos and Landoni, 1993:16, pi. 3, figs.
.39, 40C, D.
Diagnosis: Axial sculpture of irregular, rounded ribs,
16-20 on body whorl. Spiral sculpture of flat cords (4—
6 on early whorls, 14-20 on body whorl), much broader
than intervening spaces, which appear as incised fur-
rows.
Description: Shell large tor genus (reaching 48 mm),
fusiform, slender, chalky. Protoconch of 3 tall, conical,
whorls. Teleoconch of up to 6 weakly shouldered or
rounded whorls. Spire high, = V2 shell length, spire an-
gle ~ 45°. Suture deeply impressed; subsutural ramp
narrow in early whorls, then absent. Aperture subovoi-
dal; outer lip rounded, anterior half-reflected; inner Up
curved, adpressed; interior glossy pinkish to brownish.
Siphonal canal short (< V2 aperture length), obhcjue,
open. Umbilicus absent. Axial sculpture of irregular,
rounded ribs, 16-20 on body whorl. Spiral sculpture of
flat cords (4-6 on early whorls, 14-20 on body whorl),
much broader than intei-v'ening spaces, which appear as
incised furrows. (Growth lines irregular, faint to obsolete
throughout shell. Shell composed of 2 layers: outer layer
thick (0.6.5 slicll thickness), of amoqihoiis calcitc; inner
layer (0..35 shell thickness), of crossed-lamellar aragouite
with crystal planes oriented perpendicular to growing
edge. Operculum (figure 47) oval, subpolvgonal, v\ath
terminal nucleus. External surface covered bv irregular
growth hues. Inner surface with .3—4 horseshoe-sliapt'd
lines; posterior rim with slight callus, glazed in adult and
young specimens.
Aniiual large. Gephalic tentacles medium in size,
blunt, thick, with small black eyes. Mantle edge with flat,
rounded lobules (figure S3, 1). Siphon (figure 83, s) of
medium length. Accessory boring organ (figure 95, abo)
situated along ventral midline of foot, shares opening
with ventral pedal gland in females. Osphradium (figure
84, os) < V2 ctenidium length, thin, veiy asymmetrical,
with 45-50 leaflets per side. Ctenidium (figure 84, ct)
3-4 times as wide as osphradium, with 120-135 trian-
gular leaflets. Pleuroembolic proboscis very long, broad.
Radular ribbon (figures 48^9) small, short (0.31 X ap-
erture length vs. 0.78 X aperture length in Trophon gev-
ersianus), extends just beyond rear of buccal mass (fig-
ure 94, ra). Rachidian tooth wide (to 230|xm), central
cusp large, needle-shaped, lateral cusps outwardly point-
ed, shorter than central cusp, inner lateral denticle
smaU, thin, separate from lateral cusps. Basal plate of
rachidian tooth rectilinear or gently curved, with low,
broad, marginal areas. Lateral teeth large, each with sin-
gle, long, scythe-shaped cusp and broad basal plate. Sal-
ivary glands (figure 94, sg), ascinous, white (yeUow in
fixed animals) veiy large, flanking retracted proboscis.
Salivary ducts join esophagus just anterior to valve of
Leiblein (figure 94, vl). Accessory sahvars' glands (figure
94, asg) small, pyriform, white to brownish, situated be-
low salivary glands. Glande framboisee absent. Gland of
Leiblein (figure 94, gl) large, broad anteriorlv, tapering
posteriorly to form long, sinuous, blind duct with small,
terminal ampulla (figure 94, dgl). Anterior aorta (figure
94, aa) passes through fold in gland of Leiblein en route
to buccal mass. Stomach (figure 94, sto, 89) U-shaped,
small, almost completely enveloped bv digestive gland.
Both digestive gland ducts (figure 89, dd) near esopha-
geal opening, situated in deep pouch (figure 89, dp),
separated from posterior mbdng area (figure 89, pma) by
small horizontal fold (figure 89, hf). Two tyj^hlosoles (fig-
Figures 41—42, 45-49. Xijmenopsis muricifonnis (King and Broderlp, 1832). 41. Protoconch, USNM 901629, Strait of Magellan,
53°.39.4'S-70°55.5'W, in 24 m. Scale bar = 100 (xm. 42. Apical and lateral views of the egg capsule. Scale bar = 800 [im. 45.
Shell ultrastructure, fracture surface comarginal. Scale bar = 30 \x.m. 46. Penis, critical-point dried. Scale bar = 40 |xni. 47.
Operculum, external (left) and internal (right) \iews. Scale bar = 1 cm. 48-49. Radula. USNM 9016.35, Strait of Magellan,
5.3°39.8'S-70°54.9'W, in 27-73 m. 48. Dorsal \new of radular ribbon. Scale bar = 40 fxm. 49. Lateral \iew of rachidian teeth. Scale
bar = 20 (jim. Figures 43-44, 50-51. Xi/ineiw picbeius (Hutton, 1873). 43. Lateral and apical \iews of egg capsule, USNM
6815.38, Spit Beach, Dunedin Harbor, New Zealand. Scale bar = 1 mm. 44. Operculum, external (left) and internal (right) \iews,
same specimen as 43. Scale bar = 1 cm. 50. Shell iiltrastnicture, fracture surface comarginal. AK 80295, Northland, Bay of Islands,
Parekuta Bay, New Zealand. Scale bar = 100 |xm. 51. Dorsal view of radular ribbon, same specimen as 43. Scale bar = 20 (jim.
Page 46
THE NAUTILUS. Vol. 114, No. 2
Figures 52—36. Xi/menopsis bticcinetis (Lamarck, 1816). 52-54. Neotvpe of Fiistis biiccincus Lamarck, L816. USNM 870410,
5.3°.32'S, 64°.57'\\', in 119-124 m, 55-56. Holohpe of Ftistis texiiliostis Hombroii and |ac(juinot, 1854, MNHN unnumbered. Strait
of Magelkui, Figures 57-71. Xi/rnenopsis comioatus (Reeve, 1848). 57-59. Holot\pe of Fusus cornigatiis Reeve, BMNH
1874. 12. 11. 15.3, lacks localits data. 60-62. Lectohpe of Trophon hoijlei Strebel, 1904, ZMH mmumbered. Port Stanlev, .VlaKinas
(Falkland) Is. 63-65. Holotvpe of Trophon falklandicus Strebel, 1908, NHRM 1049, 5r35'S-57°56'\\', Islas MaMnas '(Falkland).
66-68. USNM 368350, Port' Stanley, MaKinas (Falkland) Is. 69-71. Holotvpe of Trophon ornatns Strebel, 1904, ZMH unnumbered,
Port Stanley, Malvinas (Falkland) Is. Figures 72-74. Xymrne plebeius (Hiitton, 1873). USNM 681538. Spit Beach, Dunedin Harbor,
New Zealand. Scale bar = 1 cm for all specimens.
G. Pastorino and M. G. Harasew\'ch, 2000
Page 47
Figures 75-79. Xi/iiii-nopsis biiccinciis (Lamarck, 1S16). 75. Dorsal view ol radnlar nbhoii from specimen in figures 52-54. Scale
bar = 40 p-ni. 76. Oblique (45°) lateral Wew, of radular ribbon, MACN 12553, Tierra del Fuego. Scale bar = 40 |jim. 77-78.
Protoconch, MACN 25012, 54°26'S-64°53'W, in 112 m. 77. Apical, and 78. lateral views. Scale bars = ISO jxm. 79. Shell ultra-
structure, fracture surface comarginal. Scale bar = 40 |j.m. Figures 80-82. Xi/menopsis comigatus (Reeve, 1848). 80. Shell
ultrastnicture, fracture surface comarginal. USNM 368350, Port Stanlev, MaKinas (Falkland) Is. Scale bar = 40 |j,m. 81-82. Radula.
USNM 421884, Port W'iUiams, York Bay, MaKinas (Falkland) Is. 81. Dorsal, and 82. obliijue lateral view. Scale bars = 20 (xm.
Page 48
THE NAUTILUS, Vol. 114, No. 2
G. Pastorino and M. G. Harasewvcli, 2{)0()
Page 49
nre S9, tl, t2) flank' intestinal i^rooN-e (figure 89, ig) sep-
arating it ironi expantled eonipacting area (figure 89, ea).
Intestine (figures 89, 94, i) runs anteriorly alongside pal-
lial gonoduct, forming rectum with cylindrical papilla
(figin-es 86, 90 ap) o\'er anus (figiu'es 86, 90 a). Rectal
gland (figure 93, rg) small, inconspicuous, confined to
anterior region ot rectum. Prostate gland (figures 86-88,
pg) rvms alongside rectum in mantle cavity, lacking open-
ings to mantle cavitv" (unlike Trophoii <yi:crsianus, see
Kool, 199.3h: fig. 57). Vas deferens (figure 86, vd) leads
from anterior end of prostate to base of penis (figures
46, 83, p). Penis large (> 3 X tentacle length), wide,
elongate, flattened to semitriangular in cross-section,
with centrallv situated sperm duct (figure 85, pvd), dor-
sal iilood sinus (figure 85, ds). Penis tapers ahruptly to
form small, cylindrical papilla (figures 46, 83). Pallial oyi-
duct broad posteriorly, tapered anteriorly. Albumen
gland (figure 90, ag) situated at rear of mantle cavity,
joins posterior of capsule gland (figure 90, eg). Left and
right lobes of capsule gland similar to T. ^eversianus
(Harasewych, 1984: fig. 22; Kool, 1993b), Nucella lapil-
lits (Fretter and Graham, 1994: fig. 171), but ventral and
dorsal glandular areas proportionally much smaller (fig-
ure 92). Bursa copulatri.x (figures 91, 93, be) joins an-
terior of capsule gland, leads to vaginal opening (figures
90, 91, vg), situated below, posterior to anal opening,
papilla (figure 90).
Egg capsules of Xi/mcnopsis Duihciftinnis were dis-
cussed but not illustrated by D'Asaro (1991:54). Cap-
sules are attached to the dorsal surface of empty shells
of X. miiricifonnis, densely grouped, overlapping each
other. Egg capsule (figure 42) bulliform, approximately
6-7 mm in diameter, 2 mm high, outline subcircular,
may vary according to substrate. Preformed exit aperture
oval, situated at center of dorsal surface in shallow, sub-
ovate depression, sealed by a mucus plug until hatching.
Suture between capsule, plug weakly defined, nmning
parallel to large axis of depression. Pattern of non-con-
centrically oriented fibers visible on upper surface of
capsules. External morphology of egg capsules veiT sim-
ilar to that observed in dry specimens of Xi/mcnc plc-
bciits (figure 43), which differ in having aperture situated
apically rather than in depression.
Type material: iHiirriniiin iiiuricifoniw] Lectotvpe
(figures 14-16), BMNII 1837.12.15.2695, 6 paralecto-
t>pes, BMNII 1992056, all from Strait of Magellan: [Fii-
sii.s decolor] Ilokitype (figures 9-10), MNHNS unnum-
bered. Strait of Magellan; [Buccinum caiiccllarioklcs]
Lectot\pe (figures 17-19), BMNII 1992055-1, here des-
ignated, I paralectotype BMNH 1992055-2, lack locality
data; [Fusus liratus] Holotype (figures 1-3), USNM
5680, Orange Harbor, Tierra del Fuego: [Trophon loeh-
bcckci] II()Iot\pe (figures 4—6), Lobbecke-Museum, no
catalog ninnber, lacks locafity data; [Tropliou Ichnini]
Lectotype (figure 13), MNHN unnumbered, here des-
ignated, 2 paralectotypes, all from Santa Cruz, Argenti-
na; [Trophon violaceiis] Lectotype (figures 7-8), MNHN
unnumbereil, figured .syntyjae here designated as lecto-
type, from Bale Orange, Tierra del Fuego; [Trophon
paessleri[ Lectotype (figures 26-28), ZMH unnumbered,
here designated, 4 paralectotypes, all from Port Grap-
pler, Smvih Channel, Strait of Magellan; [Troi)hon paes-
sleri var. turiita] Original tspe material, from Cape
Horn, Tierra del Fuego, was destroyed (Hausdorf hi
Utt.). The lectotvpe of Bucchmm nuiiiciformc (BMNH
1837.12.15.2695) is here designated as neotype of Tro-
plion pac.'islcri var. titrrita.; [Trophon elon^iatus] Lecto-
tvpe (figures 35-37), ZMH unnumbered, here designat-
ed, from Puerto Angosto, Strait of Magellan, 4 paralec-
totypes, 1 from Navarino Is., Chile, 1 from Puerto
Bueno, 1 from Eden Harbor, 1 from Puerto Angosto,
Strait of Magellan: [Trophon pseudoclongatns] Holotype
(figures 29-31), ZMH unnumbered, Ushuaia; [Trophon
alhus] Holotvpe (figures 38—40), ZMH unnumbered, Us-
hutiia; [Troplion acuinimitiis] Holot\pe (figures 20-22),
ZMH unnumbered, Punta Arenas, Strait of Magellan;
[Trophon obcsus] Lectotype (figures 32-34), ZMH un-
ninubered, here designated, from, Punta Arenas, Chile,
1 p;u;ilectot\pe from Punta Arenas, Chile; [Trophon fe-
nc.stratu.s] Original t\pe material, from GregoiT Bank,
Strait of Magellan, was destroyed (Hausdorf //i htt.). The
lectotype of Buccinum muriciforme (BMNH
1837.12.15.2695) is here designated as neot\pe of Tro-
phon fcncstratus; [Trophon confhouyi] Lectotvpe (fig-
ures 23-25), ZMH unnumbered, here designated, 4
paralectotypes, all from Port Grappler, Smvth Channel;
Figures 83-95. Xymcnopsi.s iiiioicifoniiis (King and Broderip, 18.32). 83. Anterior piirtion of mule specimen, mantle reHected.
84. Ctenidium and osphradium. 85. Transverse section of the penis, (figure 83 at 1-1'). 86. Male pallial gonoduct. 87. Transverse
section (figure 86 at 2-2'). 88. Transverse section (figure 86 at .3-3'). 89. Stomach, opened dorsally. 90. Female pallial gonoduct.
91. Transverse section through capsule gland (figure 90 at 4—4'). 92. Transverse section (figure 90 at 6-6'). 93. Transverse section
through bursa eopulatrix (figure 84 at 5-.5'). 94. Diagrammatic representation of the alimentary system. 95. Sagittal section throua;h
the anterior portion of the foot.
a = anus; aa = anterior aorta; abo = accessory boring organ; ag = albumen gland; ap = anal papilla; asg = accessory salivarv^
gland; be = bursa eopulatrix; ca = compacting area; eg = capsule gland; ct = ctenidium; dd = ducts to digestive diverticula; dgl
= ampulla of gland of Leiblein; dp = duct pouch; ds = dorsal blood sinus; e = esophagus; gl = gland of Leiblein; hf = horizontal
fold; hg = hypobranchial gland; i = intestine; ig = intestinal groove; 1 = lobes along meuitle edge; leg = left lobe of capsule gland;
mo = mouth; nr = nerve ring; os = osphradium; p = penis; pg = prostate glanil; pma = posterior niLxing area; pro = propodial
groove; pvd = penial vas deferens; r = rectum; ra = radula; rcg = right lobe of capsule gland; rg = rectal gland; s = siphon; sg
= salivary gland; sto = stomach; tl and t2 = tyjihlosoles; vd = vas deferens; vg = vagina; vl = valve of Leiblein.
Page 50
THE NAUTILUS, Vol. 114, No. 2
Figures 96-103. Xijincnopsis subnodosus (Gray, 1839) 96-97. Holotype of Fusns cancelVmus PhiLippi, 1845, and 11601)^6 of
Buccinum suhnodosn Gray, 18.39. MNHNS unnumbered. Strait of' Magellan. 98-100. BMNH 19990.3.30, 4.3°.3S.9'17"S.
7.3°37.2'.38"\\'. 101. Operculum, external (left) and internal (right) Ndews, same specimen of 98-100. Scale bar = 1 cm. 102. Dorsal
view of radular ribbon from specimen in figures 98-100. Scale bar = .50 fj.m. 103. Oblique (45°) lateral view, of radular ribbon.
Scale bar = 25 |j,m.
[Trophon elegans] Lectotype (figures 11-12), ZMH un-
numbered, here designated, from Port Stanley, Mahinas
(Falkland) Is., 2 paralectotypes from Port Stanley, Mal-
vinas (Falkland) Is.
Additional material examined: AMNH 50211, Strait
of Magellan; AMNH 8.5428, Canadon de las Vacas;
AMNH 99610, West Malvinas (Falkland) Is.; AMNH
137057, Beagle Channel; AMNH 17929.3, Puerto De-
seado; AMNH 271757, 53°37.7'S, 69°54.6'W, in 42 ni;
AMNH 271758, 54°10.2'S, 65°57.5'W, in 101 m; MACN
10043-1, Ushuaia; MACN 12374, Punta Arenas; MACN
12376, 53°10'S, 70°55'W; MACN 12448, Puerto Harris.
Dawson Is.; MACN 12552, Ri'o Grande; MACN 12555,
Rio del Fuego, Tierra del Fuego; MACN 13120, Punta
Arenas; MACN 13568, Ushuaia^i MACN 1.3569, Ushuaia;
MACN 17754, Puerto Deseado; MACN 22567, Punta
Colnet, Isla de los Estados; MACN 22717, 54°48'S,
64°55'W, in 103 ni; MACN 23943, 20°07'S, 66°33'W, in
82 m; MACN 30876, Lapataia, Tierra del Fuego; USNM
96228, Strait of Magellan; USNM 96842, Puerto Mayiie,
G. Pastorino and M. G. Harasewvch, 2000
Page 51
104
105
Figure 104. Original illustration of Fusiis biiccineiis La-
marck, 1816 (pi. 427, figs. 3a, b).
Figure 105. Sowerby in Gray's (1839, pi. 36. fig. 12) illus-
tration of Fusus buccineus. The specimen depicted is Xipnen-
opsis mtiricifonnis.
Chile; USNM 126899, Tierra del Fuego, Intertidal;
USNM 348720, Puerto Harberton, Tierra del Fuego;
USNM .368273, Port William.s, Malviiias (Falkland) Is.,
in 18 m; USNM 368401, Port Stanley, MaKdnas (Falk-
land) Is.; USNM 368639, Punta Arenas, Chile; USNM
368641, Punta Arenas, Chile, intertidal; USNM 368654,
Punta Arenas, Chile; USNM 368761, Punta Arenas, In-
tertidal, Chile; USNM 381693. Bahia San Sebastian, Tie-
rra del Fuego; USNM 710029, Puerto Deseado, Santa
Cruz, Intertidal; USNM 870002, 53°50'54"S,
70°30'42"W, in 15-17 m; USNM 870165. 54°05'S.
58°52"W, in 119 m; USNM 886188, 53°51'32"S.
70°25'52"W, in 2-3 ni; USNM 886190, 53°51'32"S.
70°25'52"W, in 2-3 ni; USNM 886737, 53°39'S,
70°55'30"W, in 20 ni; USNM 886745, 53°39'S,
70°55'30"\V, in 15-18 ni; USNM 901628, 53°39'S,
Figure 106. Localities at which Xi/menopsis species (0
A', muricifonnis; O = X. cornigatiis: # = A', buccineus; -k
X. subnodosus ) were collected off Chile and Argentina.
70°55'30"W, in 20 m; USNM 901629, Strait of Magellan,
53°39.4'S, 70°55.5'W, in 24 m; USNM 901630,
53°39.4'S, 70°55.0'W, in 82 m; USNM 901631,
54°47.25'S, 64°18.3'W. in 35 m; USNM 901632.
53°33.9'S, 69°58.8'W, in 82-91 m; USNM 901633,
53°39.3'S, 70°55.4'W, 38-42 m; USNM 901634,
53°17'S, 6S°13'W, in 0-1 m; USNM 901635, 53°39.8'S,
70°54.9'W, in 27-73 m; LACM 69170, Islas Guarello,
Chile, 52°40'S, 73°41'W; LACM 10503. MoKiiieux
Sound. Strait of Magellan. Chile; LACM 118051, Lively
Island, East Malvinas (Falkland) Is., 52°00'S, 58°2S'W;
LACM 71-262, KN Hkko Cruise 712. Sta. 672. W of
Puerto Aiio Nuevo. Isla de los Estados. Tierra del Fue-
go, Argentina, 54°45.1'S, 64°07.3'W, in 50 m; LACM 71-
305, IW Hkro Cruise 715, Sta. 690, 8 miles E Ensena-
da Patagones, SE Tierra del Fuego, Argentina. 54°52'S,
65°05'W, in 144 m; LACM 71-337, R>V Hkho Cruise
715, Sta. 888, W of Bahia York, Isla de los Estados, Tie-
rra del Fuego, Argentina, 54°49.5'S, 64°19.6'W, in 56-
63 m; LACM 73-66, IW Hkro, Cabo Colnett, Isla de
los Estados, Tierra del Fuego, Argentina, 54°43'27"S,
64°14'18"W, in 15 ni; LACM 73-68, IW Hkho. Beagle
Canal. C;ileta Aw;iiakirrh, Chile, 55°0'S, 69°02.2'W, in
17 m; LACM 73-69, IW Hero, Punta Valparaiso. Canal
Cockburn, Chile, 54°22.2'S, 7r21.7'W. in 15 ni; LACM
73-70, Isla Carlos III, Strait of Magellan. Chile,
53°39.4'S. 72°14.8"W. in 11-12 ni; LACM 73-71. Punta
Dashwood. Canal Smyth, southern Chile, 52°24'S,
73°39.7'W, in 12 ni; LACM 73-72, Bahia Tom, Chile,
Page 52
THE NAUTILUS, Vol. 114, No. 2
5()°11.3'S, 74°47.9'W, in 14 m; LACM 73-107, RA^
Hero, Colling%vood, Chile, 5r52'S, 73°43.6'W, intertid-
al to shallow subtidal; LACM 75-49, Puerto el Hambre,
Brunswick Peninsula, Strait of Magellan, ChLle,53°37'S,
70°56'W, intertidal; LACM 78-84, IW Hero Sta, B 4-
6, N of Cabo Buen Tiempo, Rio Gallegos, Santa Cruz
Prov., Argentina, 51°16-20'S, 68°50-54"W, in 30 m, mud
bottom: LACM 86-268.5, Canal Oeste, S side Isla madre
de Dios, Ultima Esperanza, Magallanes Prov. Chile,
50°27.7'S, 75°11.5'W, in 30 m.
Literature records: RA' Discoxerv: Sta. 52. 7.4 ca-
bles N, 17°E of Naw Point, Port William, East Mahinas
(Falkland) Islands, in 17 ni; Sta. 1230, 6.7 miles N, 62°W
of Dungenes Light, Strait of Magellan, in 27 m; Sta.
WS784, N of Malvdnas (Falklandy Islands, 49°47.75'S,
61°05'W, in 170 m (Powell, 1951); Sta. 24,25, Puerto
Eden in 10-12, 6-7 m respectively; 30,33 Puerto Eden,
in 8-10 and 11-12 m; Sta. Caleta Lackawana in 4-6 m;
Sta. 43 Paso Indio; Sta. 50, 63, 65 Puerto Williams, Nav-
arino Is. (Dell, 1971).
Distribution (figure 106): Knov\ni from 45° S (Chonos
Archipelago), Southern Chile {fide Dell, 1971 as X. de-
color); Tierra del Fuego, Strait of Magellan, Beagle
Channel (Argentina) and the Malvinas (Falkland) Is-
lands. The bathvmetric range for X. imihciformis is 0-
170 m.
Remarks: Xiimcuop.sis miuiciformis has a long and
comphcated taxonomic histoiy. The oldest name to have
been applied to the Xymenopsis characterized by spiral
sculpture that appears as incised grooves is Buccinum
luuriciformc King and Broderip, 1832. There were 2 lots
of svntvpes, BMNH 1837.12.15.2695 (2 specimens) and
BMNH 1992056 (5 specimens), both from Str;iit of Ma-
gellan. One specimen BMNH 1837.12.15.2695 (figures
14-16), was illustrated by Dell (1972:8, figs. 31,32) as
the holotvpe (an inads'ertent lectotype designation). The
holotvpe of Fh.si/.s decolor Philippi, 1845 (figures 9-10),
iilso from the Strait of Magellan, clearly represents a
worn specimen of X mttiicifonnis. The next name to be
apphed to this species is Buccinum cancellarioidcs
Reeve, 1847, based on 2 syntyjjes lacking locafity data.
One specimen is here designated as lectotype (figures
17-19). Powell (1951) recognized B. cancellarioidcs to
be an earher name for Ftisus lirafus Gould, 1849 (Ho-
lot\-pe, figures 1-3). Because he was unsure if Reeve's
(February, 1847) name was a junior homonvan of Buc-
cinum cancellaroides Basterot in Grateloup, given as
1847 by Sherborn (1924:1030). he ret;iined the use of
X. liratus. The holotvpe of Trophon loebbeckei Kobelt,
1878 (figures 4-6), from an unkniown locality, also
matches closely the holotype of B. muricifimnc, as do
the lectotypes of Trophon lebnini and Trophon viola-
ceus, both Mabille and Rochelinme in Rochebrune and
MabiUe, 1889. Trophon Ichruni was based on 3 .svntypes,
MNHN unnumbered, all from Santa Cruz, Argentina.
One specimen is here designated as the lectoty|3e (figure
13). The figured s)'ntype of Trophon violaceus MNHN
unnumbered, from Baie Orange, Tierra del Fuego is
here designated lectotvpe (figures 7-8).
In his publication on the molluscan fauna of the Ma-
gellanic Province, Strebel (1904) proposed numerous
taxa based on minor phenotypic variants. Among these
were 16 species and varieties of Trophon that were sub-
sequentlv referred to Xipncnopsis bv Powell (1951). Ac-
cording to Dance (1986:227), Strebel's collections were
housed in the Hamburg Museum and "totally destroyed "
during World War II. However, this appears to be true
only for the "dry" (shell only) specimens. The alcohol
preserved material on which much of Strebel's (1904)
Magellanic publication was based, survived the war and
is in the collections of the Zoologisches Institut und
Zoologisches Museum der Universitat Hamburg. Mate-
rial collected b\- the Swedish Sudpolar-Expedition, in-
cluding types of taxa described by Strebel (1908), is in
the Swedish Museum of Natural History in Stockholm.
The senior author visited both these museums in the
course of this study, and was able to locate much of
Strebel's tspe material. Examination of the t\pes ot; Tro-
phon paessleri, T clongatus, T. pscudoelongatus, T al-
bus, T acuminahis, T couthouiji, T elegans and T. obesus
leaves no doubt that these are, at most, minor moq:)ho-
logical variants oi Xipnenopsis nuiriciformis. The taxon
Trophon paessleri is based on 6 syiitypes. ZMH unnum-
bered, 5 from Port Grappler, Smyth Channel, Strait of
Magellan and 1 from Punta Arenas. One specimen (fig-
ures 26-28) from Port Grappler is here designated as
lectotype. The type material of Trophon clongatus con-
sists of 7 syntypes, ZMH unnumbered, 2 from Puerto
Angosto, Strait of Magellan, 3 from Puerto Bueno, 1
from Navarino Is. and I from Eden Harbor One spec-
imen (figures 35-37) from Puerto Angosto is here des-
ignated as lectotype. Trophon couthouiji is based on 3
syntypes, ZMH unnumbered, from Port Grappler,
Smvth Channel. One specimen (figures 23-25) is here
designated as lectotvpe. Holotvpes are illustrated for
Trophon pscudoelongatus (figures 29-31), ZMH unnum-
bered, and T. albus (figures 38—40), ZMH unnumbered,
both from Ushuaia; and T. acuminatus (figures 20-22),
ZMH unnumbered, from Punta Arenas, Strait of Ma-
gellan. Trophon elegans is based on 3 specimens from
Port Stanley, MiJvinas (Falkland) Is. One specimen (fig-
ures 11-12) ZMH unnumbered, is here designated as
lectotype. Trophon obesus is represented by 2 syntypes
from Punta Arenas, Chile; one (figures 32-34), ZMH
unnumbered, is here designated as lectotype.
The type material of Trophon paessleri var. turrita and
of T fenestratus could not be found, and was among the
material destroyed during World War II (Hausdorf in
litt.). Based on Strebel's (1904) descriptions and figures,
there is no doubt that both these taxa are conspecific
with Xymenopsis muricifonnis. We therefore designate
the lectotype of Buccinum muriciforme (BMNH
1837.12.15.2695) as the neotype for both Trophon paes-
sleri var turrita and T fenestratus, making both these
taxa objective junior synomins of Buccinum muricifiir-
G. Pastorino and M. G. Harasewych, 2000
Page 53
Xijinenopsis comi^atiis (Reeve, 1848)
(Figures 57-71, 80-82, 106)
Fusus cornif^atiis Kee\e, 1848: pi. 20 figs. 84 a. h. Kolielt,
1878: 293, pi. 74. fi<is. 1.5-16.
Trophon corni'^^dliis Ki'tne — Tnon, 1880: 145. pi. 3.3. fig. .352;
Rocliehniiii' ami Maliille, 1889: II ,54.
Trophon miiricifonnis Sowerby, 1880: 66, pi. 3, fig. 41. [not
Bucriiiiim muricifonne King and Broderip, 1832]
Trophon hot/lei Strebel, 1904: 227. pi. 8, figs. 68 a-f, 69 a-c;
MelviU'and Standen, 1907: 1.37.
Trophon hnicci Streliel, 1904: 2.30. pi. 8. fig. 72; MeKill and
.Stiuiden. 1907: 1.35.
Trophon ornntus Strehel. 1904: 231. pi. 8. fig. 73.
Trophon standeni Strehel. 1904: 2.32, pi. 7, fig. 67.
Trophon A— Strehel, 1904: 2.34, PI. 8, fig. 78.
Trophon B— Strebel, 1904: 2.35, Pi. 8, fig. 79.
Trophon falklanclicus Strebel, 1908: .39, PI. 1, figs. 8a-c.
Xymenopsis falklandicus Strebel — Powell, 1951:159, PI. 9, figs.
46, 47; Castellanos and Landoni, 1993:18, pi. 3. figs. 37. A.
Xijmenopsis cornigattis (Reeve) — Ceniohorskv. 1977:118, fig.
19.
Diagnosi.s: Axial .sculpture of regular, thin, .slender,
rounded rih.s, 19-24 on body whorl. Spiral sculpture of
rounded cords (4-6 on penultimate whorl, 19-26 on
body whorl), slightly broader to slightly narrower than
intervening spaces, producing weakly cancellate surface
at intersection with axial ribs. Spiral threads present be-
tween adjacent cords. Outer lip without apertural teeth.
Description: Shell of medium size (2.5-.32 mm), thin,
fusiform. Protoconch worn on all specimens, but clearly
multispiral, conical. Teleoconch of up to 6 rounded
whorls. Spire high, <V2 shell length. Spire angle = 45°.
Suture deeply impressed; subsutural ramp small, but
present. Aperture semicircular; outer hp rounded, dis-
tinctly crenulated, reflecting spiral cords at lip edge; in-
ner hp cur^'ed. adpressed; interior glossv brownish. Si-
phonal canal short, oblique, open. Umbilicus absent. A.x-
ial sculpture of regular, thin, slender, rounded ribs, 19-
24 on body whorl. Growth lines present throughout
shell, clearly defined over the nodes. Spiral sculpture of
rounded cords (4-6 on penultimate whorl, 19-26 on
body whorl), slightly broader to shghtly narrower than
intervening spaces, producing weakly cancellate surface
at intersection with axial ribs. Finer spiral threads pre-
sent between adjacent cords. Shell ultrastructure as in
X. miiricifonnis, composed of 2 layers: outer layer (0..55
shell thickness) ot amorphous calcite, with ribs, cords
confined to this layer; inner layer (0.45 shell thickness),
crossed-lamellar aragonite with ciTstal planes oriented
perpendicular to growing edge, of relatively constant
thick-ness. Operculum, gross anatomy, as in X. murici-
fonnis. Radula (figures 75-76) very similar to that of X.
miiricifonnis. Rachidian teeth narrower (< 100|xm), in
proportion to smaller size of this species. Central, lateral
cusps more conical, less cyhndrical that in X. nutricifor-
mis, inner lateral denticles of X. cornigattis proportion-
ally larger.
Type material: [Fiisiis comifiafiis] Hoiotvpe (figures
57-59), BMNH 74.12.11.1,5.3, lacks locality data; \Tro-
plnni hoijh'i] Lectotvpe (figure 60-62). ZMH unnum-
bered, here- designated, with 4 paralectotvpes, all from
Port Stanley, Isias Malvinas (Falkland); {Trophon brucei]
Tyi^e material could not be located at ZMH. No locaUty
exphcitly associated with this species l)v Strebel. The ho-
iotvpe of Fusus cormgatus (BMNH 74.12.11.1.53) is
here designated as neotype of Trophon brucei; [Trophon
onmtus] Holotyj^e (figures 69-71) ZMH tmnumbered,
from Port Stanley, Malvinas (Falkland) Is; [Trophim
standcni] Original tyj^e material, from Malvinas (Falk-
land) Is., could not be located at ZMH. The holotype of
Fusus corrufiatiis (BMNH 74.12.11.1.53) is here desig-
nated as neotype oi Trophon standcni; [Trophon falklan-
dicus] Holot\pe (figures 6.3-65), NHRM 1049, Berkeley
Sound, Malvinas (Falkland) Is., (51°.35'S, .57°.56'W), in
2.5-30 m. Station 49.
Additional material examined: MACN 10136, Mal-
Ndnas (Falkland) Is., m 0 ni; USNM 173062, Malvinas
(Falkland) Is.; USNM 368288, Port Stanley; USNM
368292, Port Stanley, shore; USNM 368311, between
Pembrooke Is and Tussock Is. Malvinas (Falkland) Is.,
in 27 m; USNM .368342, Port Stanley, shore; USNM
368347, Port Stanley, shore; USNM 368.3.50, Port Stan-
ley, Malvinas (Falkland) Is.; USNM 368360, Port Stan-
ley, shore; USNM 3683,89, Port Stanley, shore; USNM
368422, Port Stanley, shore; USNM .368432, Port Stan-
ley; USNM 421877,' Port Stanley; USNM 421884, Port
Williams, York Bay, Malvinas '(Falkland) Is.; USNM
421890, Port Stanley; USNM 6.5.5342, Port Stanley area;
USNM 702124, Port William, in 16 ni; LACM 15394,
LACM 15395, LACM 55989, LACM 61583, all from
Fox Bay, East Malvinas (Falkland) Is.
Literature records: [as X. falklandicus] WW Disco\-
ERV: Sta. .55, 2 cables S, 24°E of Naw Point, Entrance
to Port Stanley, East Falkland Island, in 10-16 m; Sta.
56, 1.5 cables N, 50°E of Sparrow Point. Sparrow Cove,
Port William, East Falkland Island, in 10.5-16 m (Pow-
ell, 1951).
Distribution: All specimens belonging to this species
that we were able to examine were from the Malvinas
(Falkland) Islands. The bathymetric range of X. corru-
gatiis is 0-27 m.
Remarks: The holoUpe of Fusus cornigatus BMNH
1874.12.11.153, was illustrated by Cernohorsky (1977,
fig. 19). Trophon ornatus is based on 1 specimen (figures
69-71) ZMH unnumbered, from Port Stanley, Malvinas
(Falkland) Is. The tvpe material oi Trophon bnicei, and
T. standcni could not be found at ZMH. In the original
description, Streliel wrote that this material was sent to
him from Manchester Museum by Bruce. According to
D. Penney {in litt.), these specimens never reached
Manchester again. We therefore consider the tvpe ma-
terial ol both species to be lost. These taxa are consid-
ered sviionyms ol Xijmenopsis cornigatus based on Stre-
bel's (1904) descriptions and figures. The holotype of
Fusus corrugatus (BMNH 1874.12.11.1.53) is here des-
Page 54
THE NAUTILUS, Vol. 114, No. 2
ignated as the neotype for both Trophon bntcei, and T.
standeni making both these taxa objective junior syno-
nyms of Fiisus cornigatus.
Xijmenopsis huccineus (Lamarck, 1816)
(Figures 52-56, 75-79, 104, 106)
Fusus bucciiH'us Lamarck, 1816: pL 427, figs. .3a, b, Liste: 6.
Ftisus albidus Philippi, 1846: 119 pi .3. fig. 5.
Fusus textiliosus Honibron and Jactjuinot in Rousseau, 1854:
108, Pi 25, fig. 9-10, non Deshayes, 1835.
Fusus textilosus Honibron and Jacquinot [error for F. textilio-
sus]. Hupe in Gay, 1854: 162; Philippi, 1855: 206.
Fusus Jacqtiinoti Philippi, 18.55: 206, new name for F. textilio-
sus Honibron and Jacquinot. 1854, not F. textiliosus De-
shayes. 1835.
Trophon albidus Phifippi — Kobelt, 1878: 293, pi 74, figs. 11-
12; Strebel 1904: 222. pi 7. figs. 64 a-cl
Trophon nuiricifonnis Sowerby, 1880: 66, pf 3, fig. 40. [not
Buccinuin muriciforme King and Broderip, 1832]
Trophon buccineus Gray— Tryon, 1880:146, p!. 39, fig. 490.
Trophon textiliosus (Honibron and Jacquinot) — Rochebrune
and Mabille, 1889: H..55.
Trophon rinff'i Strebel, 1904: 242, pi. 8, fig. 77.
Xijmenopsis albidus (Philippi)— Powell, 1951:159. fig. M. 90;
Yokes, 1991: 7. fig. ininunibered; Castellanos and Lan-
doni, 1993: 17, pl."3, figs. .388, 41-42.
Diagnosis: Axial sculpture of irregular, \'erv weak ribs
(25-28 on body whorl). Irregular, obsolete growth lines
present throughout shell. Spiral sculpture of flattish
cords (9 on penultimate whorl, 17-20 on body whorl) as
broad as intei"vening spaces, forming weakly cancellate
sculpture at intersections with axial ribs. No spiral
threads between adjacent cords.
Description: Shell of medium size (s 30 mm), thin,
fusiform, cUrty white to brownish tan. Protoconch taU,
conic, of .3 whorls. Teleoconch of up to 6 convex whorls,
spire high, = Va shell length. Suture deeply impressed.
Aperture subovate; outer lip evenly rounded, weakly
crenulated; inner Up gently concave; interior glossy,
whitish. Siphonal canal long, narrow for genus, oblique,
open. Umbilicus absent, pseudoumbilical chink in some
specimens. A,xial sculpture of irregular, veiy weak ribs
(25-28 on body whorl). Irregular, obsolete growth lines
present throughout shell. Spiral sculpture of flattish
cords (9 on penultimate whorl, 17-20 on bodv whorl) as
broad as inten'ening spaces, forming weakly cancellate
sculpture at intersections with a.xial ribs. Shell ultrastnrc-
ture of two layers, as in other Xymenopsis, but outer,
calcific laver thinner (0.35 shell thickness), than inner
aragonitic laver (0.65 shell thickness). Operculum, gross
anatomy, as in X. mtiriciformis. Radula (figures 75-76)
more similar to that of X. cornigatus than to X. miiri-
ciformis in that lateral cusps broader, more triangular in
outline, inner lateral denticles more pronounced. Weak
outer lateral denticles present in some individuals of X.
buccineus (figure 75, arrow).
Type material: \Fusus buccineus] Lost, not in Paris
or Geneva (Bouchet in litt. and Finet in lift.), type lo-
cality unspecified. Neotype, (figures 52-54), USNM
870410, here designated, 5.3°32'S, 64°57'W, in 119-124
m; [Fusus albidus] Probablv lost, not in MNHNS, type
localits' unspecified; [Fusus textiliosus Hombron and Jac-
quinot, 1854, not F. tcxtdiosus Deshayes, 1835] Holotype
(figures 55-56), MNHN no catalog number, Strait of
Magellan; [Trophon lingei] Original tvpe material, fnnn
Strait of IVIagellan, destroyed, (B. Hausdorf, in litt.). The
Neotype of Fusus buccineus, USNM 870410, is here
designated as the neotype of Trophon ringei.
Additional material examined: MACN 12553, Ti-
erra del Fuego; MACN 2.3862, 5r46'S, 68°45'W, in 22
m; MACN 25012 + MACN 25013, 54°26'S, 64°53'W,
in 112 m; USNM 110731, Strait of Magellan, East En-
trance, in 10 m; USNM 110782, Strait of Magellan, East
Entrance, in 18 m; USNM 152S92, Santa Cruz, Pata-
gonia; USNM 870481, 53°40'S, 66°20'W, in 81 m;
USNM 870491, 53°42'S, 66°19'W, in 81 m; USNM
881098, 54°34'S. 63°50'VV. in 118 m; USNM 881924,
54°27'S, 66°12'W, in 0 m; USNM 881961, 5.3°32'S,
64°57'W, in 119-124 m; USNM 881966, 52°30'S,
67°14'W, in 82 m; USNM 901625, 53°39.8'S, 70°54.9'W,
in 27-73 m; USNM 901626, 5.3°()6'S, 67°04'W, in 86 m;
USNM 901627, 54°59.9'S, 64°50'W, in 438 m (dead
specimens); LACM 71-302, IW Hero Cruise 715, sta.
687, 5 miles E of San Mauricio, SE end Tierra del Fue-
go, Argentina, 54°45'S, 64°04.6'W, in 75 m; LACM 71-
313, IW Hero Cruise 715, sta. 853, 9 miles N of Cabo
Colnett, Isla de los Estados, Tierra del Fuego, Argentina,
54°34'S, 64°20'W, in 91 m. LACM 71-320, RA^ Hero
Cruise 715, sta. 865, 4 miles E of Isla Observatorio, Isla
de los Estados, Tierra del Fuego, Argentina, 54°39'S,
64°00'W, in 75 m; LACM 71-324", IW Hero Cruise 715,
sta. 870, 6 miles NE of Isla Observatorio, Isla de los
Estados, Tierra del Fuego, Argentina, 54°34'S,
64°00.3'W, in 84 m; LACM 71-327,' IW Hero Cruise
715, sta. 873, 9 miles N of Cabo San Juan E end of Isla
de los Estados, Tierra del Fuego, Argentina, 54°.34'S,
63°50"W, in 118 m; LACM 71-329, IW Hero Cruise
715, sta. 875, 5 miles S of Punta Ventana, S side of Isla
de los Estados, Tierra del Fuego, Argentina, 54°54.5'S,
63°56'W, in 771-903 m (dead' specimens); LACM 71-
330, IW Hero Cmise 715, sta. 876, 14 miles N of Cabo
San Juan, Isla de los Estados, Tierra del Fuego, Argen-
tina,'54°29'S, 63°50'W, in 112 m; LACM 71-333, IW
Hero Cmise 715, sta. 881, Puerto Vancouver, Isla de los
Estados, Tierra del Fuego, Argentina, 54°39'S, 64°00'W,
grab; LACM 71-341, RA' Hero Cmise 715, sta. 894, 5
miles SE of Cabo Kempe, Isla de los Estados, Tierra del
Fuego, Argentina, 54°54.9'S, 64°19.5"W, in 263-285 m
(dead specimens); LACM 71-348, RA^ Hero Cmise 715,
sta. 903, 13 miles N of Baliia Crosslev, Isla de los Es-
tados, Tierra del Fuego, Argentina, 54°34.3'S, 64°40'W,
in 84-85 m; LACM 71-349, RA^ Hero Cmise 715, sta.
904, 8 miles N of Baliia Crosslev, Isla de los Estados,
Tierra del Fuego, Argentina, 54°39.0'S, 64°40'W, in 84-
85 m; LACM 71-351, RA' Hero Cmise 715, sta. 906,
14 miles N of Cabo San Antonio, Isla de los Estados,
G. Pastorino and M. G. Harasewvch, 2()()()
Page 55
Tierra del Fuego, Argentina, 54°29'S, 64°29.2'W, in
122-124 m; LACM 71-352, RA' Hemo Cniise 715, sta.
907, 9 miles N of Cabo San Antonio, Isla de lo.s Estado.s,
Tierra del Fuego. Argentina, 54°34'S, 64°3()'W, in 73-
76 m; LACM 71-353, RA' Hi;ho Cruise 715, Sta. 908,
5 miles NNE of Cabo San Antonio, Isla de los Estados,
Tierra del Fuego, ArgenHna, 54°38.9'S, 64°30'VV, in 60
ni.
Literature records: RA' Disccn krv: Sta. WS71, 6
miles N 60° E of Cape Pembroke Liglit, East Falkland
Island, in 82 m; Sta. WS88, Off Staten Island (Isla de
los Estados), Tierra del Fuego, 54°S, 65°W to 54°S.
64°55'W, in 118 m; Sta. VVS97,' Between Malvinas (Falk-
land) Islands and Patagonia, 49°S,62°W to 49°01'S,
erse'W, in 145-145 m; sta. WS222, SE of Puerto De-
seado, Patagonia, 48°23'S, 65°W, in 100 m; Sta. WS243,
Off Santa Cruz, Patagonia, 51°06'S, 64°30'W, in 144-
141 m; Sta. WS750, NE of MaKdnas (Falkland) Islands
51°50'S, 57°15.2'W, in 135-144 ni; Sta. WS805, Be-
tween Malvinas (Falkland) Islands and Patagonia,
50°11'S, 63°27'W to 50°09.5'S, 63°31'W, in 150-148 m:
Sta. SW808, Off Santa Cruz, Patagonia, 49°40.25'S,
65°42'W. in 109-107 m; Sta. WS829, Between MaKinas
(Falkland) Islands and Patagonia, 50°51'S, 63n3.5'W, in
155 m; Sta. WS834, Off Baliia Grande, Patagonia,
52°57.75'S, 68°08.25'W, in 27-38 m; Sta. WS838, Be-
tween Malvinas (Falkland) Islands and Patagonia,
53°11,75'S, 65°W, in 148 m; Sta. WS861, SE of Puerto
Deseado, Patagonia, 47°40'S, 64°12'W, in 117-124 m;
Sta. WS863, Between Malvinas (Falkland) Islands and
Patagonia, 49°05'S, 64°09'W, in 127-117 ni; Sta. WSS65,
Between Malxdnas (Falkland) Islands and Patagonia,
50°03'S, 64°14'W, in 126-128 m; Sta. WS867, Between
Malvinas (Falkland) Islands and Patagonia, 51°10'S,
64°15'W, in 137-144 ni; Sta. WS869, Between MaKinas
(Falkland) Islands and Patagonia, 52°15.5'S, 64°13.75'W,
in 187-0 [.sic] m.
Distribution: KnowTi from Southern Chile and Ar-
gentina; Tierra del Fuego, Strait of Magellan, Beagle
Channel, MaKinas (Falkland) Is. The vertical distribu-
tion oi X. biiccinettf; ranges between 0 and 155 m. Rec-
ords from greater depths are dead shells. The batliy-
metric and geographic ranges of this species are nearly
identical with those of of X muriciformis, and the two
species have been collected together in some trawls.
(e.g. USNM 901625 (X. biux-iiicu.s) and USNM 901635
(X muricifonnis) both from 53°39.8'S, 70°54.9'W, in
27-73 m.)
Remarks: Ftistis buccincus (Lamarck, 1816) was pub-
lished without localitv or detailed description. The t\pe
specimen is lost (Finet, in ht., Bo\ichet ni Ut.). Although
Sowerby [in Gray, 1839) labelled a figure F. buccincus,
the specimen illustrated (figure 105) is clearly X muri-
cifonnis, and bears little resemblance to Lamarck's fig-
ure of K buccincus (fig. 104). Strebel (1904:237) hkewise
noted that F. buccincus of Gray [actually Sowerby in
Gray] was a different species than F buccincus Lamarck.
The specimen illustrateil bv Sowerby is also lost (K. Way,
(■/( lift.).
As Fusus bucciiwus is the oldest name to be applied
to anv species of Xi/mcnopsis, we designate as neotyi^e
(figures 52-54) a specimen (USNM 870410) that rea-
sonably conforms to Lamarck's (fig. 104) illustration of
this species. This serves to remove anv ambiguit\' re-
garding the identity of Fusus buccincus and thus stabi-
lize the nomenclature of the Recent Xyinenopsis. The
t\pe locLllit\- for Fusus buccincus becomes the continen-
tal shelf east of Tierra del Fuego (53°32'S, 64°57'W), in
119-124 m.
The next available name for this species is F(/.s7/.s al-
bidus Philippi, 1846, for which no type locality was des-
ignated. As the type specimen could not be located at
MNIINS, it is included in the synonymy based on Phi-
hppis description and figure. We have not designated a
neotyj^e for Fusus albidus because there remiiins a pos-
sibility- that the type will yet be located at MNHNS. The
ty|3e of Fusus tcxtiliosus Hombron and Jacquinot, 1854
from the Strait of Magellan, housed in MNHN, is illus-
trated in figures 55-56, and undoubted!\- belongs to this
species. The type materiid of Trophon lingci could not
be found, and was among the material destroyed during
World War II (Hausdorf (>i lift. ). This taxon is considered
to be a svnonvm of X. buccincus based on Strebel's
(1904) descriptions and figures. We therefore designate
the neotype of Fusus buccincus (USNM 870410) to
serve as the neotype of Trophon ringei. Trophon ringei
thus becomes an objective synonym of Fusus buccincus.
Xyincnopsis subnodosus (Gray, 1839)
(Figures 96-103, 106)
B[uccimnn] suhtiodosa Gray, 1S39: 118.
Fu.ms cancellinus Philippi, 1845: 67; 1846: 117, pi. 3, fit;. 2;
Hupe in Gay, 1854: 163.
Trophon cnncellinii.i Philippi — Kobelt, 1878: 291, pi. 74, figs.
7, 8; Rochehnme and Mabille, 1889: H.59
Diagnosis: Axial sculpture of strong, irregular ribs
(12-16 on body whorl), nearly as broad and intenening
spaces. Spiral sculpture of dense, evenly rounded cords,
(6 on penultimate whorl, 22-24 on body whorl), broader
than intervening spaces. Spiral threads present between
adjacent cords. Outer lip with apertural teeth.
Description: Shell large (to 37 mm), solid, slender,
fusiform, dirty white, chalkT. Protoconch miknown. Te-
leoconch of up to 6 gently convex whorls. Spire high,
= Vi shell length. Spire angle == 45°. Suture strongly
impressed. Aperture small, ovate; outer lip thickened,
with 8-10 weak teeth; inner fip concave, thickly glazed;
interior whitish. Siphonal canal long, obfique, open.
PseudoumbiUcal chink, small but present. Axial sculp-
ture of strong, irregular ribs (12-16 on body whorl),
nearly as broad and intenening spaces. Spiral sculpture
of dense, evenK' roundeil cords, (6 on penultimate
whorl, 22-24 on body whorl), broader than intei-vening
spaces. General morphology- of animal and operculum
Page 56
THE NAUTILUS, Vol. 114, No. 2
(fi2;ure 101) as in X. miiriciformi.s. Osphradium < V2 cte-
nidium length, asymmetrical, with 48 and 32 leaflets on
the external and internal side respectively. Ctenidium 2-
.3 times as wide as osph/adium, witli 85-90 triangular
leaflets. Radular ribbon small, short (0.23X aperture
length). Radula (figures 102-103) similar to those of X.
corntgattis and X. huccincus, but with single weak den-
ticle along outer edge of each lateral cusp.
Type material: [Buccinum stibnodosa] Original type
material from the Pacific Ocean lost (K. Way, in lift.).
The holotype of Fusits cancellintis, MNHNS, is here
designated as neot\pe of Bticciniim subiuxlo.m. [Fiisiis
cancellintis] Holot)'pe, MNHNS unnumbered. Strait of
Magellan.
Additional material examined: BMNH 19990330,
43°38.9'17"S, 73°37.2'38"W, East side Traiguen Is., Es-
tero Elefantes, Region 11, Chile. Dredged in 5-15 m on
bottom of colibles and dead \enerids; sheltered bay.
Distribution: Known from the Str;ut of Magellan, and
Traiguen Island, Chile.
Remarks: Gray (1839) introduced Buccinum suhno-
closa as a variety of Buccinum muriciformc (=Xi/mcn-
opsis muiiciformis King and Broderip) in a two Une de-
scription without illustration. As Gray's type material is
lost (K. Wav, in Jitt.) this leaves some doubt as to the
identitv' of this species. Grav's description refers to "al-
ternate narrow low and wider convex spiral ridges" that
produce tubercles as they rise over the axial ribs, fea-
tures characteristic of both X. corrugatus and a species
subsequently named Fu.su.s canccUinus. Grav does not
mention the prominent apertural teeth that are diagnos-
tic of X. canccUinus, but it is possible that he had a sub-
adult specimen lacking apertural teeth. Gray states that
B. subnodoso inhabits the Pacific Ocean. Fusus cancel-
linus occurs along the Pacific Coast of Chile, while X.
corrugatus is known only from the Malvinas (Falkland)
Islands and Isla de los Estados. In order to stabihze the
nomenclature of Recent Xi/mcnopsis. we designate the
holot^pe oi Fusus canccUinus Phihppi, 1845 (MNHNS)
to serve as neotvpe of Buccinum subuodosa Grav, 1839.
Fusus canccUinus thus becomes a junior objective syn-
onym of Buccinum subnodosa.
We know of only two specimens of Xi/mcnopsis sub-
nodosus. incluchng the neotspe (shell onK ) housed at the
Museum of Santiago, Chile. Xtjmenopsis subnodosus re-
sembles both X. muiiciformis and X. corntgatus in size,
general shape, and in the coarseness of its axial ribs. It
differs from X. muricifonnis in ha\ing a thicker shell,
narrower more numerous, and more rounded spiral
cords, and shares with X. corrugatus the presence of fine
spiral threads interspersed between adjacent cords. Xy-
menopsis subnodosus is larger has a higher spire, and
coarser sculpture than X. buccincus^ The most distinctive
features of X. subnodosus are the thickening oi the outer
hp, and the presence of weU defined apertural teeth,
which occur in New Zealand members of the Xi/mcnc
complex, but not in any other Xymcnopsis. Xymcnopsis
subnodosus is most similar to X. corntgatus. which is
restricted to the Mahinas (Falkland) Islands. We provi-
sionally retain this taxon, recognizing that it may prove
to be a subspecies or rare variant of X. corrugatus char-
acterized by an atavistic expression of a rare allele or
alleles for apertural dentition.
SYSTEMATIC KEY TO THE GENUS XYMENOPSIS
1. Shell large, with strong, well defined axial ribs . . 2
Shell small, with weak, poorly defined axial ribs 3
2. Shell thin, with spiral sculpture of flat cords
much broader than intervening spaces, which
appear as incised furrows X. muiicifoiinis
Shell thick, spiral sculptine ot dense, evenly
rounded cords, (6 on penultimate whorl, 22-
24 on body whorl), broader than intervening
spaces. Outer lip thickened, with 8-10 weak
teeth X. subnodosus
3. Spiral sculpture of rounded cords slightly
broader to sUghtlv narrower than intervening
spaces, producing weakly canceUate tubercles
at intersection with axial ribs. Weak spiral
threads present between adjacent spiral cords
X. corrugatus
Spiral sculpture of flattish cords as broad as
interx'ening spaces, forming weakly cancellate
sculpture at intersections with axial ribs
X. buccinciis
ACKNOWLEDGMENTS
We thank the following people for access to material in
their collections: K. Wav (BMNH); A. Waren (NHRM);
P Bouchet and V. Heros (MNHN): J. H. McLean
(LAGM): P Mikkelsen (AMNH); B. Hausdorf (ZMH);
O. Galvez Herrera (MNHNS); J. Boscheinem (Loeb-
becke-Museum); H. Irigoyen and A. Tablado (MAGN);
C. Ituarte (MLP). R. Prasad (Auckland Museum) pro-
vided specimens oi Xt/mcnc plcbcius. P. Louzet took the
photographs of specimens at MNHN. D. Reid (BMNH)
provided the presened specimen of X. subnodosus. Yu.
Kantor provided useful discussions during the course of
this work. V. Ivanov prepared the anatomical drawings
of X. muricifonnis. R. Petit provided information on
nineteenth century hterature. E. H. Yokes provided
helpful discussions of muricid systematics. We are grate-
ful to A. Beu and J. H. McLean for thorough reviews
and helpful suggestions that improved this paper
This study was conducted during a Postdoctoral Fel-
lowship granted to the senior author by the Consejo Na-
cional de Investigaciones Cientificas v Tecnicas (CON-
ICET), Argentina, to work at the National Museum of
Natural History, Smithsonian Institution, Washington.
DC. It was supported in part by a Research Award from
the NSF-USAP United States Antarctic Program [Con-
tract No. OPP-9509761] and a grant in aid from the
Conchologists of America and the Walter E. Sage Me-
moriid Award.
G. Pastorino and M. G. Harasewvch, 2000
Page 5"
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THE NAUTILUS 114(2):59-68. 2000
Pa^e 59
Copulahijssia riosi, a new deep-sea limpet (Gastropoda:
Pseudococculinidae) from the continental slope off Brazil with
comments on the systematics of the genus
Jose H. Leal
The BaileN-Mattliews Shell Muscinii
P.O. Bo.x 1580
Sanibel, FL 33957 USA
jleal@gate.net
Luiz Ricardo L. Sinione
Museu lie Zoologia da Uiii\ersidade
de Sao Paulo
Cai.xa Postal 42694
04299-970 Siio Paulo
BRAZIL
lrsimoiie@usp.br
ABSTRACT
A new bathval species of the family Pseudococculinidae is de-
scribed from samples dredged in 1987 along the continental
slope of southeastern-eastern Brazil b> the French research
vessel Marion-Diifresne. The new species, allocated in the ge-
nus Copulahijssia. differs from the 4 other known congeners
by characters of shell, external morphology, mantle cavity, and
radula. Descriptions of internal moqihology based on micro-
dissections are provided, including the digestive system and the
complex muscular apparatus ot the odontopliore. The distri-
bution of characters ot taxonomic significance at the species
level in Copulabyssia is given in tabular format and discussed.
Key words: MoUusca, Cocculiniformia, Vetigastropoda, Lepe-
telioidea, bathval, anatomy, taxonomy, odontopliore.
INTRODUCTION
Bathyal samples dredged off E-SE Brazil yielded spec-
imens of an unnamed species of the genus Copulabi/ssia,
family Pseudococculinidae. Two live specimens and one
empty shell were collected at three stations performed
between 960-L320 m. The Pseudococcuhnidae and oth-
er families comprising the superlamily Lepetelloidea
Dall, 1882, are included amongst the mollusks living at
greatest depths in the ocean (Leal and Harasewych,
1999; Lesicki, 1998; Marshall, 1986; Wolff, 1979). The
new taxon exhibits the diagnostic characters of the genus
Copulabyssia Haszpmnar, 1988. Copulabyssia riosi new
species is herein compared with the 4 other species of
the genus named to date (Lesicki, 1998): C. corni^ata
(Jeffreys. 1883) (NE Atlantic); C. ii,mda1a (Marshall,
1986) (SW Pacific); C. Icptah-a (Verrill, 1884) (N Atlan-
tic); C. similaris Hasegawa, 1997 (Japan).
MATERIALS AND METHODS
Two live-collected specimens and one empty shell were
available for studv. A single specimen was dissected. Mi-
crodissection was performed with the specimen im-
mersed in 70% ethanol. The apical (distal) region of vis-
ceral mass was damaged; adjacent structures were de-
scribed and are shown herein based on reconstruction.
After dehydration in a standard alcoholic series, the sec-
ond specimen was chemically dried tor 10 min in hex-
amethykUsilizane (HMDS). Shells, radula, and chemi-
cally dried soft parts were coated with carbon and gold
and e.xamined and photographed under Hitachi S-57()
(at National Museum of Natural History, Smithsonian
Institution), Leo 440 (at MZSP), or Philips XL30
ESEM-FEG (Center for Advanced Microscopy, Univer-
sity of Miami) electron microscopes. Institutional abbre-
viations used are; MNHN, Museum national dTIistoire
naturelle, Paris, France; MZSP, Museu de Zoologia da
Universidade de Siio Paulo, Brazil; NMNH, Museum of
New Zealand Te Papa Tongarewa, Wellington; NSMT,
National Science Museum, Tokyo, Japan; SMNH, Natur
Historika Riksmuseet, Stockliolm, Sweden; USNM, Na-
tional Museum of Natural History, Smithsonian Institu-
tion, Washington. Other alilirexiations and text conven-
tions are: 1, 5, lateral teeth (lateral 5 = pluricuspid
tooth); 1, 2, marginal teeth; ac, anterior cartilages of
odontophore; an, anus; bm, buccal mass; br, subradular
membrane; bs, Iniccal sphincter; df, dorsiil folds oi buc-
cal mass; dg, digestive gland; ep, epipodium; es, esoph-
agus; et, epipodial tentacles; gi, gill; go, gonad; gp, gen-
ital pore; if, inner mantle fold; in, intestine; ir, insertion
of m4 in radular sac; is, insertion ot m5 in radular sac;
ki, kidney; It, left cephalic tentacle; mb, mantle edge;
mj, jaw and peribuccal muscles; mo, mouth; mp, me-
sopochum; m2, pair of buccal mass retractors; m3, inner
buccal mass protractors; m4, pair of antero-dorsal ten-
sors; mS, pair of postero-dorsal tensors; ni6, horizontal
muscle; ni7, pair of odontophore approximators; mS,
pair ot cartilage approximators; no, nuchal ca\its: of,
outer mantle fold; pa, mantle papillae; pc, posterior car-
tilages of odontophore; pr, protuberance on right ten-
Page 60
THE NAUTILUS, Vol. 114, No. 2
tacle; re, rectum; ra, radula; m, radiilar caecum; rs,
radular sac; rt, right cephalic tentacle; sc, subradular
cartilage; sf, fold along gill; sg, seminal groove; sm, shell
muscle; sn, snout; st, stomach; vg, vestigial left gill leaf-
let. The odontophore muscles examined in this studv
were also described bv Haszpnuiar (1988: 165-167, fig.
.3) for Kluilahijssia vcnczuclcnsis McLean, 1988. Ter-
minology used herein (boldface) corresponds to the one
used bv HaszpiTuiar as follows: mj = br -I- otr; bs = bs;
in2 = dr2; in4 = rd2; m5 = rr; m6 = ho; m7 = sr3
(?); mS = ci. The remaining small muscles described by
Haszpnmar (1988) could not be observed in the single
specimen a\';ulable for microdissection.
SYSTEMATICS
Class Gastropoda Cuvier, 1797
Subclass Orthogastropoda Ponder and Lindberg, 1996
Order Vetigastropoda Salvini-Plawen, 1980
Remarks: The superfamilies Cocculinoidea Dall,
1S82, and Lepetelloidea Dall, 1882 have been united
under the order Coccuhformia Haszprunar, 1987. Re-
cent studies of gastropod phylogeny based on moi"pho-
logical characters (Ponder and Lindberg, 1996; 1997)
suggest that CoccuMnoidea is sister taxon to Neritopsina,
and that Lepetelloidea is part of the order Vetigastro-
poda (see also Haszpioinar, 1998: 664). This arrangement
is followed herein. Harasewvch ct al. (1997) indicated,
based on partial 18S rDNA sequences, that CoccuHni-
formia may not constitute a clade. These latter authors,
however, suggested that Cocculinoidea and Lepetello-
idea are more closely related to each other and to Pa-
teUogastropoda than to Neritopsina or Vetigastropoda.
Superfamily Lepetelloidea Dall, 1882
Family Pseudococcuhnidae Hickman, 1983
Subfamily Caymanabyssinae Marshall, 1986
Genus Copiilabijssia Haszprunar, 1988
T\pe species: CoccuUna oirn/gflffl Jeffreys, 1883, p.
394, pi. 44, figs. 2-2a. Type locaUty-; 59°40'N, 7°21'W,
930 m, Triton Ex]:)ecUtion station 10.
Diagnosis: Protoconch sculpture of microscopic pris-
matic crvstals; right cephalic tentacle exceptionallv large,
"swollen"; right cephalic tentacle with deep, open glan-
dular seminal groove situated postero-dorsallv; large
pedal gland; gills palhal, several well-developed gill leaf-
lets on right side, a single one on left side.
Copidabi/ssia riosi new species
(Figures 1-24, Table 1)
Diagnosis: Teleoconch at first with radial sculpture
then with closely set concentric ribs (interspaces about
25 (Jim in width); internally with narrow but well-defined
anterior apical septum; radial sculpture only on early te-
leoconch; cutting area of rachidian tooth with blunt
cusp; left side of subpalhal cavity with small structure
that could represent a vestigial gill leaflet; right cephalic
tentacle with prominent subterminal protuberance; left
cephahc tentacle small for genus; inner branches of epi-
podial tentacles filamentous.
Description: Shell (Figures 1-6): Small (length to
3.50 nun), thin, arched, elevated (height/length about
0.5), with apex at posterior quarter pointing in posterior
direction. Anterior slope convex, about 88% of shell
length. Posterior slope concave, about 30% of shell
length. Shell surface usually lightlv eroded, milky white.
Protoconch (figure 4) length about 200 |jLm, surface bad-
ly eroded in type material. Teleoconch sculpture of con-
centric (commarginal) ribs separated by intervals of
about 25 |jLm. Concentric ribs narrow (about 10 jim) and
crossed bv fine radial lines on earlv part of teleoconch
(figure 5). Concentric ribs on latter part of teleoconch
proportionally thicker, radial lines absent (figure 6). In-
ternally with narrow, but well-defined, anterior apical
septum. Aperture elhptical (figure 3), not conforming to
a planar surface, convex. Shell muscle scar continuous,
horseshoe-shaped.
Head-foot (Figures 7, 8, 13, 14, 17): Head prominent
and large (about % foot length) (figures 7, 13, 14, 17).
Cephahc tentacles (figures 7, 13, 14, 17, rt. It) on dorso-
lateral surface of head. Right tentacle about 4 times larg-
er than left tentacle, modified as copulatory organ (de-
scribed below). Eyes apparently lacking (unpigmented?).
Snout (figures 7, 13, 14, 16, 17, sn) very large, cyhndrical
on base, gradualK' becoming slightK' flattened dorso-ven-
trally. Anterior extremity of snout almost flat, broader
than region immediately behind it, with pair of small
lateral projections. Foot large and flat (figures 7, 13, 14),
smaller than shell aperture in presened animal. Meso-
pochum (figures 7, 13, 14, mp) flattened. Epipodium
(figures 7, 13, 14, ep) flange-Uke, surrounthng entire me-
sopodium, larger on anterior edge, which covers baso-
ventral region of snout. Pair of epipodial tentacles (figure
7, 9, 13, 14, et) well-developed, projecting from poste-
rior region at both sides of longitudinal axis of animal,
slightly dorsal to epipodium, on intersection between
mantle and shell muscle. Each epipothal tentacle bifid;
outer branch shorter and with broad tip; inner branch
longer and pointed. Shell muscle (figures 15-17, sm)
horseshoe-shaped (concaNdty towards anterior region);
anterior extremities broader, pointing away from shell
apex. Almost all head-foot muscles converge toward in-
sertion of shell muscle.
Mantle cavity (Figures 12-15, 17): Mande edge (fig-
ures 12-14, 17, mb) thick, with 2 folds; outer fold (fig-
ures 12, 14, 17, ofO covered by slender and very small,
translucent papillae (figure 12); inner fold (figures 14,
17, if) about twice as broad as outer fold, richlv glan-
dular, white. A small, transparent, yellowish protuber-
ance (figure 13, vg) on inner margin of inner told, in
region adjacent to left cephafic tentacle, may represent
vestigial left gill leaflet. Mantle cavity surrounding entire
head-foot, somewhat deep, i.e., with ample space be-
J. H. Leal and L. R. L. Simone, 2000
Page 61
Figures 1-6. Coptilabt/ssia riosi new species: shell of holotrvpe, MZSP 32150. 1. Dorsal view. 2. Lateral \iew. 3. X'entral view.
Scale line = 1.0 mm. 4. Protoconch. Scale line = 100 p-m. 5-6. Shell sculpture. 5. On early teleoconch. Scale hne = 50 jxm. 6.
Close to shell margin. Scale line = 100 [xm.
tween mantle edge and shell muscle. Nuchal cavitv (fig-
ures 14, 15, 17, nc) deeper than remainder of mantle
cavity. Gill (figures 13, 14, 17, gi) small, situated on right
side of mantle cavity, somewhat parallel to mantle edge
and extending for about half of foot lenijth, consisting of
aliout 14 successively smaller leaflets. Anterior extremity
oi gill (figure 5, gi) just posterior to head-foot Umit. Each
leaflet low and triangular, relatively thick. Most posterior
leaflets situated peqjendicularlv to mantle edge, gradu-
ally becoming obfique to it on anteri(jr region. A small,
narrow, and low fold (figure 14, sf) nms between gill
and shell muscle along posterior half of gill. Anus (fig-
ures 15-17, an) and genital pore (figure l7, gp) on right
side, at head and foot hniit, just anterior to right extrem-
ity of shell muscle.
Circulatonj and excretory sijstem.'i (Figures 15-17):
Heart not observed. Large blood vessels ;ilong thick-
mantle border Kidney (figures 15, 17, la) verv small,
white, sohd, slightly triangular; situated in right-posterior
region ot head, just posterior to rectum.
Visceral mass (Fifiures 15, 16): Round, surrounded by
following stmctures: laterally and in posterior direction
by shell muscle, in anterior direction by buccal mass,
ventraliv by inner surface of mesopodium, and dorsallv
by central region of mantle and shell. Gonad (figure 15,
go) and digestive gland (figure 15, dg) cream in color,
intersected by several intestinal loops (figure 16). Gonad
situated mainly on left region and digestive gland mainlv
on central region.
Digestive si/sfem (Figures 7. 13-24): Mouth (figures 7,
13, 14, 18, mo) on middle-ventral region oi anterior sur-
Page 62
THE NAUTILUS, Vol. 114, No. 2
Figures 7-12. Copulabi/ssit] riosi new species; paraUpe, MNHN unnumbered, gross external moipholoi^ and radula. 7. N'entral
\ie\v ot animal. Scale line = .500 p,m. 8. Detail of right cephalic tentacle (copulatorN- organ). 9. Inner branches ot epipodial tentacles
(damaged during preparation). Scale Unes = 100 |j.m. 10-11. Radula. 10. View of 5 rows. Scale hue = 50 (jim. 11. Detail of lateral
and first marginal teeth. Scale line = 10 [j.m. 12. Papillae on outer mantle fold. Scale line = .50 |xm.
face oi snout, oriented transversally. Buccal mass (figure
16, bm) somewhat large, occupying about entire head
cavit\'. Buccal sphincter (figure 18, 19, bs) well devel-
oped. Superficial protractor muscle of buccal mass rel-
atively narrow, connected to lateral and dorsal regions of
buccal sphincter and adjacent region of snout, iiinning
along lateral and dorsal sinface of buccal mass, con-
nected to lateral and ventral region of buccal mass. Dor-
sal wall of buccal mass ver\' thin, with pair of thick lon-
gitudinal folds (figure 19, df) that join together in an-
terior direction at median fine, becoming gradiuillv
weaker toward esophagus (figures 16, 19, es). Odonto-
phore (figures 18-24) large, comprising most of buccal
mass, oval in outline. Odontophore muscles (figures 18-
24): (ml) (not illustrated) several small and short fibers
connecting buccal mass to adjacent inner lining of snout,
more concentrated on dorsal surface; (m2) (figures 18,
19) pair of narrow retractor muscles of buccal mass con-
nected to inner ventral lining of snout just posterior to
buccal mass, running parallel to radular sac (figures 19-
23, rs), connected to postero-dorsal surface of buccal
mass on lateral surface of beginning of esophagus; (m3)
(figure 21, 22) pair of thin inner protractor muscles of
buccid mass connected to inner lateral lining ot mouth,
running on (and covering) lateral surface of odonto-
phore, connected to antero-ventral margin of posterior
cartilages; (m4) (figures 20-24) pair of antero-dorsal ten-
sor muscles connected in part to outer ventral surface
of anterior cartilages and in part to lateral surface of
posterior cartilages, running along (and covering) pos-
J. H. Leal and L. R. L. Simone, 2000
Page 63
Figures 13-17. Copiilabi/ssin nasi new species; paratope, MZSP 32149, gross inorphologv. 13. \'entral \ne\v. 14. Lateral \iew,
right side, margin of mantle deflected to show its inner surface. 15. Dorsal \iew. 16. Digestixe system, dorso-lateral \iew, left side,
shown by transparency, only dorsal contour and part of shell muscle shown. 17. Detail of head, lateral view, right side, adjacent
mantle removed by means of an incision around shell muscle. Scale lines = 500 jjim.
Page 64
THE NAUTILUS, Vol. 114, No. 2
mo
J. H. Leal and L. R. L. Siiiioiu', 2()()()
Page 65
Table 1. Diagnoses of species oi Copulnl}yssia. "Shell length" is miLximinn size for species, "Rih interspaces" is the distance between
concentric ribs on posterior shell slope. "Lett gill leaflet" is size of single-leaflet gill in relation to right gill leaflets; medinni wonld
be about the same size as right gill leaflets. "Right cephalic tentacle" = copulator>- organ ("RT"). Unknown character states indicali'd
b\' "NA", Degree of de\elopment of cephalic tentacles is relatixe to other congeneric species.
C. riosi
C. Icptalea
C. t^iriddta
C. cornii^ata
C. similah.s
Di.stribution
Off SE, E Brazil
NW Atlantic
Off New Zealaml
NE Atlantic. Med
japan
Character
Shell leiiijth (nun)
3.50
2.45
1.95
1.35
3.36
Rib interspaces (jxni)
±25
±40
±40
±130
±50
Radial sculpture
early Icleo only
strong
lacking
present
very weak
Postition of apex
anterior 2/10
anterior .3/10
anterior .'VIO
anterior 1/10
variable
Apical septum
present
absent
absent
absent
absent
Rachidian
broad
broad, rounti sides
broad
elongate
broad
Racliidian cutting area
blunt cusp
long, pointed cusp
cuspless, rounded
cuspless, s(juarish
cuspless, round
Cusjis lateral tooth 5
2-3
4
NA
2
2
Epipodial tentacles
filamentous
NA
NA
stubby
present
Right ce ihalic tentacle
well-developed
NA
swollen base
swollen base
"bilobed"
Left cep lalic tentacle
vei-y reduced
NA
normal
normal
normal
RT protuberance
well-deyeloped
NA
absent
absent
absent
Left gill leaflet
?vestigial
NA
medium
small
Pabsent
References
this work
Waren, 1991
Marshall. 19.S6
Haszpnuiar 1988
Hasegawa, 1997
McLean and Hara-
Ilaszprunar, 1988
Dantart and
sewych, 1995
Luque, 1994
tenor surface of odontophore (figure 24), connected to
ventral surface of radular sac on region posterior to
emergence of radula; (m5) (figures 20-24) pair of pos-
tero-dorsal tensor muscles connected to postero-ventral
surface of posterior cartilages, ninning dorsallv and me-
dially along (and covering) posterior surface ot odonto-
phore, connected to radular sac just posterior to m4 in-
sertion; m6) (figures 20, 24) horizontal muscle relatively
narrow, connected to antero-ventral margin (jf anterior
cartilages along about % oi their length; m7) (figiu'es 20,
22, 24) pair of narrow ventral tensor muscles connected
to meso-ventral margin of posterior region of anterior
cartilages, running along meso-ventral surface of odon-
tophore, connected to antero-ventral e.xtremih of sub-
radular cartilage (figures 21-23, sc); m8) (figures 10, 12)
pair of broad approximator muscles of cartilages con-
nected to antero-lateral surface of posterior cartilages
(figures 22, 24, pc), nmning toward anterior cartilages,
connected along lateral surface of anterior cartilages (fig-
ure 24, ac). Anterior cartilages ot odontophore flattened,
long, narrower in anterior direction, broader in posterior
direction. Posterior cartilages short (about 1/5 of anterior
cartilage length), semi-spherical. Anterior and posterior
cartilages joined together on small area close to median
fine (figure 24). Esophagus (figures, 16, 19, es) narrow
and simple, running toward postero-ventral region of vis-
ceral mass, where it suddenly bends in anterior direction
to its insertion in stomach (figure 16, st). Stomach large,
cylindrical, directed toward shell apex; inner surface uni-
form, iridescent, greenish. Single duct to digestiye gland
situated close to shell apex. Stomach suddenly narrows
giving origin to intestine (figures 16, in), which runs to-
ward the right and then in posterior direction, surround-
ing dorsal margin of shell muscle, gradually turning ven-
trallv and in anterior tlirection to buccal mass, where it
suddenly curves in posterior cbrection, running along
dorsal surface of mesopodium dorsalK to its posterior
edge, looping dorsally to the right, nmning ventrally
back to preceding loop, near posterior region of head,
where it crosses transversally from right to left dorsallv
to left extremit)- f)f shell muscle, suddenly turning suc-
cessively in posterior, dorsal, and anterior directions; last
loop represented by rectum (figures 15-17, re) crossing
transversally from left to right through kidney along pos-
terior hmit of mantle ca\iU'. Anus (figure 15-17, an)
small and simple, located on posterior right side of man-
tle cax-ity.
Radula (Fifiiirvs 10-11): A.s)anmetrical, narrow, rela-
tively short (about tsvice odontophore length). Rachidian
tooth rhomboid, broad for genus, broader at mid-sec-
tion, and blunt (worn?) cusp. First lateral tooth trian-
Figures 18-24. Coptilabi/ssin riosi new species: paratvpe, MZSP 32149, buccal mass and odontophore. 18-19. Buccal mass
extracted from snout. 18. Neutral \iew, 19. Dorsal \ie\v. 20-24. Odontophore. 20. Neutral \iew, supei^ficial layer ot muscles and
membranes partially excised. 21. Dorsal \iew 22. Neutral \iew, superficial la\er of nniscles anil membranes fully excised, 23. Dorsal
view. 24. Dorsal view, radular ribbon and radula sac extracted, most of muscles and cartilages deflected to expose inner surfaces,
right-side structures more deflected than those on left side. Scale hnes = 500 (jlui.
Page 66
THE NAUTILUS, Vol. 114, No. 2
Figures 25-28. Dorsal and lateral views of shells of other species o{ Copulabijssia. 25. C. leptalea (Verrill, 1884). USNM 757345.
NE of Norfolk, \'irginia, 3080-,3090 m, RA' Gillis cniise 7508, station 36. 26. C. cornioata (Jeffrevs, 1883). SMNH unnumbered,
SE of Reykjanes Ridge, off southern Iceland, 2.50-350 m, on sunken wood. 27. C. gracfnto'( Marshall, 1986). NMNZ M. 75007,
holohpe, off \\'hite Island, New Zealand, 107.5-1100 m, on sunken wood. 28. C. similaris Hazegawa, 1997. NSMT-Mo 70822. off
Toi, Suniga Bay, Japan, 4.30-710 m, on sunken wood. Scale lines = 1.0 mm.
gular with outer basal projection that fits into a depres-
sion on second lateral tooth, and pointed single cusp.
First lateral tooth (figure 11, 1), broad, triangular. Sec-
ond, third, and fourth lateral teeth strongly ciu^ed. with
two short cusps. Fifth lateral (pluricuspid) tooth (figure
11, 5) massive, club-like, with 3 subterniinal denticle-
hke cusps. Latero-marginal plate present. Inner marginal
teeth pointed, with two denticle-like lateral cusps and
thick shafts (e.g., figure 11, 1. 2), decreasing in size out-
ward. Second marginal tooth largest. Outer marginal
o o o
teeth with serrations.
Reproductive system (Figures 7, 8, 13, 14, 15, 17): Go-
nad (figure 15, go) relatively small, on posterior left re-
gion of visceral mass, surrounded bv left branch of shell
muscle, right surface of digestive gland, and some intes-
tinal loops. A ver)' narrow gonoduct on right side (not
fully examined), running in anterior direction and api-
calK' toward right side of mantle cavity, where it opens.
Genital pore (figure 17, gp) turned ventrally, just pos-
terior to anus. Seminal groove (figure 17. sg) beginning
on genital pore, running on integument surface for short
distance, up to posterior region of base of right tentacle.
Right tentacle broad, sfightlv flattened dorso-ventnilly,
graduallv tapering to flat tip (figures 7, S, 13, 14, 17, rt).
Edges of seminal groove on posterior surface of tentacle,
ending on posterior region of tip. A well-developed sub-
terminal protuberance present on anterior surface of
tentacle (figure 14).
Type material: Holotype MZSP 32150, 3.25 mm
length X 2.50 mm width X 1.60 mm height, from t\pe
localitv, P. Bouchet, J. Leal, and B. Metivier, 27 May
1987, dead shell. Paratypes: MNHN unnumbered, 3.3.5
J. H. Leal and L. R. L. Simone, 2000
Page 67
mm length X 2.35 mm width X 1.75 mm height, MZSP
32149 (same specimen, soft parts onlv), E of Caho Siio
Tome, off Rio de Janeno .State, Brazil,'2r24'S, 39°56'W,
1320°1360 m depth, RA' Mahoit-Dufrcsnc cruise
MD55, station CP-04, R Bouchet, J. Leal, B. Metivier,
9 Mav 1987, bottom of basaltic gravel and o.>ddized iron
pelibles; MZSP 32151, 3.50 mm length X 2.35 mm
width X 1.90 mm height, Doce Ri\er Canvon, off Es-
pinto Santo State, Brazil, 19°38'S, 38°43'W, 960 m
depth, RA' Marion-Diifrcsnc cruise MD55, station CB-
95, R Bouchet, J. Leal, B. Metivier 30 May 1987, bottom
of basaltic gra\el and o>dcbzed iron pebbles (shell broken
during SEM session in Miami).
Tjpe locality: Continental slope SE off Abrolhos coral
reef system, off Bahia State, Brazil, 19°00.4'S,
37°48.8'W, 950-1050 m depth, compact dark mud and
shell hash bottom, (RA' Marion-Dufrcsne cruise MD55,
station DC-72).
Geographic distribution: Continental slope off
E-SE Brazil.
Bathymetry: 960-1320 m.
Et\Tnology: Named after Prof. EUezer de C. Rios, en-
thusiastic Brazilian author and mentor to an entire gen-
eration oi malacologists.
DISCUSSION
Specimens of Copniabi/.ssia rio.si were found apparently
removed from the actual organic substrate ol the species
(see Lesicld, 1998, for a Usting of species-specific sub-
strates and food preferences in the family). The new
species differs morphologically from the other four spe-
cies allocated in the genus Copiilabyssia (see figures 25-
28, table 1) by the presence of an apical septum on the
inner shell surface, narrow sculptural interspaces, fila-
mentous, longer epipodial tentacles, presence of a stnic-
ture on the left side of subpallial cavity that could proxe
to be a vestigial left gill leaflet, and by the presence of
an anterior, subterminal protuberance on the right ce-
phalic tentacle. The double insertion of the m4 and the
expanded insertion of the m5 are character states unique
to Copiilabyssia nasi when compared to other specie.s
of Coccuhnoidea and Lepetelloidea for which these
characters are known (see Haszpnmar, 1987; Simone,
1996); however, the states of these characters are so far
unknown for the other four species ol the genus Co-
piilabyssia.
The mantle organs of Copiilabyssia riosi are typical of
the genus, with nuchal cavity and gill leaflets situated in
the right side of the mantle cavity. Copulabyssia riosi
shows a satellite fold in the inner margin ol the gill, and
a small protuberance that could represent a vestigial gill
leaflet in the left region of the mantle border. In the
superfamiK' Lepetelloidea, similar structures are also
present in the Addisonia cnodis Simone, 1996 (Lepetel-
loidea, Addisoniidae). The arrangement of loops of the
digestive system looks similar to that descrilied by Has-
zpmnar (1988: 167-168, fig. 4) kr Amphiplica ktiiidseni
McLean, 1988 (Lepetelloidea: Pseudococculinidae), but
differs by the reduction of salivarv glands, jaw plates, and
e.sophageai pouthes.
The complex odontopliore oi Copiilabyssia riosi pre-
sents a combination oi apparently plesiomorphic and au-
tapomori^hic characti'rs The presence of 4 odontophore
cartilages and their approximator muscle (m8) repre-
sents apparently plesiomoq^hic states present in several
species oi Patellogastropoda, Vetigastropoda (including
Lepetelloidea), Cocculinoidea, and Neritopsina (L. R. L.
Simone, personal observation). The wefl-developed sub-
radular cartilage, the partial connection between the an-
terior and posterior odontophore cartilages and the hor-
izontal muscle (m6) connected only in a side of the an-
terior cartilages seem to represent apomorphic charac-
ters (at least in relation to Patellogastropoda).
ACKNOWLEDGMENTS
Gerhard Haszprunar (Zoologische Staatssammlung
Miinchen, Germany), Anders Waren (SMNH), and
Bruce Marshall (NMNZ) critically reviewed the manu-
script. We are grateful to Philippe Bouchet and Virginie
Heros at the original repositoiy institution (National mu-
seum d'Histoire naturelle, Paris) for making availalile the
type material. We are also indebted to Suzanne R. Bra-
den (National Museum of Natural History, Smithsonian
Institution), for help with some of the SEM illustrations.
M. G. Harasewych (National Museum of Natural His-
tory, Smithsonian Institution), Anders Waren (SMNH),
Bruce Marshall (NMNZ), and Kazunori Hasegawa
(NSMT) kindlv sent photographs or negatives of relevant
species of Copiilabi/ssia for illustration. This study was
supported in part Iiy FAPESP (Funda^ao de Amparo a
Pesquisa dcj Estado de Sao Paulo, Brazil) Grant # 96-
6756-2 to L. R. L. Simone.
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Simone, L. R. L. 1996. Addisonia enodis, a new species of
Addisoniidae (Mollusca, Archaeogastropoda) from the
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775-785.
Waren, A. 1991. New and little kiioyvn Mollusca from Iceland
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Wolff, T. 1979. Macrofaunal utiUzation of plant remains in the
deep sea. Sarsia 64:117-1.36.
THE NAUTILUS 114(2):69-73, 2()()()
Page 69
Invasion of the exotic freshwater mussel Limnoperna fortiinei
(Dunker, 1857) (Bivalvia: MytiHdae) in South America
G. Darrigran
Departamento Cientifico de Zoologi'a
de linertebrados
P'atultad Ciencias Naturales v Museo
1900 La Plata
ARGENTINA
in\asion@wav.coni.ar
L Ezcurra de Drago
Instituto National de Liiimologfa
(INALI/CONICET)
Maciii 1933, 3016 Santo Tome
Santa Fe
ARGENTINA
ABSTRACT
We traced the im'asion and iinestigated the (.hstiibntion of the
Asian bivaKe Limnopenui foriiinci (Dnnker. 1857) in South
America. In addition, we comment on the problems caused bv
this in\'asive species. In 1991, L. fortiinei was introduced into
la Plata Basin (currently the onlv American continent drainage
system invaded bv this species) through Ri'o de la Plata River
B\' the end of 1994 and during 1995 this species dispersed
throughout the Argentine coast of the Rfo de la Plata River
and was reported from the Uruguayan coast. In 199.5 and 1996,
it was first discovered in the Parana Ri\'er, in Santo Tome ( Sal-
ado del Norte River), and later up in Goya. In November,
1996, L. fortiinei was reported in Cerrito Island, where the
Paraguay River joins the Parana River In April 1997, it was
collected in Paraguay River on Asuncion Harbor, Paraguay. In
1999, if was detected in Brazil (Itapuii Beach, MunicipaUty of
Viamao, Rio Grande do Sul State). These recent records doc-
ument tlie fast and ongoing e.xjiansion ot the species geograph-
ic range, as well as its prompt adaptation to the ditterent en-
\ironments of the la Plata Basin
Ki'ij words: Soutli America; Neotropical Region; la Plata Basin;
invasive species; distribution; biofouling.
INTRODUCTION
The la Plata Basin is one of the most important hydro-
graphic systems in South America. It has a drainage area
of approximately 3X10'' km-, and comprises 4 main sub-
hasins (Bonetto, 1994): (1) Uniguav River, (2) Parana-
Paraguay system, (3) Rio de la Plata River, and (4) the
Andean tributaries (figure 1).
A diverse, native molluscan fauna occurs along the Ar-
gentine shore of the Rio de la Plata estuan' (Darrigran,
1994), including 27 gastropod and 21 bivalve species.
Only 4 of the bivalves are strictly freshwater and intaunal
species: Anodontites tenebricosus (Lea, 1834), Diplodon
parancnsis (Lea, 1834), MtisciiUum orfictitimnn
(d'Orhigny, 1835) and Pisiclimn stcrkiaiiinn Pilsbi"v,
1897. The only epifaunal species on the Argentine coast
of Rio de la Plata River is the estuarine Mi/tclla clior-
niana (d'Orbigny, 1842). Until 1993, A/, charniana was
the only Mytilidae found in Rio de la Plata River, in
Punta Piedras, Argentina and Montevideo, Uruguay
(Darrigran and Pastorino, 1995a).
In the 1970s, 2 asiatic freshwater bi\aKes, Corhicida
largiUiciii (Philippi, 1844) and C. fliiininca (Miiller,
1774) (Corbicuhdae), entered South America along the
Argentine shores of Ri'o de la Plata River (Ituarte, 1981).
In 1991 we detected, for the first time in South Amer-
ica, the presence of a mytilid, Limnoperna foiinnci
(Dunker, 1857), in the Rio de la Plata River shore at
Baghardi Beach (Pastorino et al., 1993). This is an eu-
ryhaline freshwater species, native to China and to
southeastern Asia (Morton, 1977), which resembles ma-
rine mussels (Mytifidae) in its moiphology and biology.
Commerce beUveen Argentina and the countries
where L. fortiinei is supposedlv native takes place m;unly
by sea. Following Carlton (1992) and Carlton and Geller
(1993), Darrigran and Pastorino (1995a) hypothesized
that L. fortiinei and other invading organisms may have
arrived in ballast water of ships coming from southeast-
em Asia.
Other authors have inthcated that L. foi-fiinei was in-
troduced in and recorded from Hong Kong in 1966
(Morton, 1975, 1996) and Japan in 1991 (Kimura, 1994).
In the Americas, L. foiiiinei is known to have invaded
only Rio de la Plata Basin. VIorton (1973) suggested that
the morpho-functional features of this species allow for
rapid expansion of its distribution range, in similar fash-
ion to the invasive abilities of the zebra mussel, Drei.s-
sena polijmorpha (Pallas, 1771), in the Northern Hemi-
sphere. The species exhibits 2 features that mav contrib-
ute to its abilities as an invader: (1) it is the onlv relevant
mollusk in the freshwater littoral ha\ang a bvssus, and
(2) has no known native competitors for physiciil space.
As a result of the high rates of invasion, as we further
chscuss below, L foiiiinei causes serious biofouling of
municipal drinking water and industrial water svstems.
As we demonstrate below, populations of Limnopenui
fortiinei are not onlv rapidly increasing in densit\- in sev-
Page 70
THE NAUTILUS, Vol. 114, No. 2
tial localities but are also quickly expanding geographi-
cidly, mostly in northward direction.
Since 1991, when it was first found at Bagliardi Beach,
until the end of 1993, the species was found only in
mLxohaline (e.g., Punta Piedras and Punta Indio) and
eur\'haline environments (e.g., Magadalena Beach, Ata-
laya Beach, Punta Blanca, La Balandra Beach). At that
time, the species had not been collected farther north
than the freshwater environment of Punta Lara Beach,
and was apparently absent from all other countries and
rivers comprising the la Plata Basin (Darrigran and Pas-
torino, 1993).
The objectives of this paper are to investigate the in-
vasion of L. foiiunci in South America, to provide an
update of its cbstribution in the Neotropical Region, and
to emphasize the importance of this invasive bivalve in
biofouling processes in the la Plata Basin.
MATERIALS AND METHODS
Collections were made along the Rio de la Plata River
shore at low tides. In the Parana Ri\'er, samples were
collected with a 319 cm- "Tamura" dredge (Marchese
and Ezcurra de Drago, 1992). Periph\tic populations
were sampled by hand. In the mouth of Paraguay River,
"macrofouling" samplers (Stupak et al, 1996) were used.
Environmental parameters taken into account were:
temperature, pH, and conductivity. The study localities
are showni in figure 1. Specimens from the Malacological
Collection of La Plata Museum, Argentina, (MLP) were
examined. Samphng for larvae was made using a mesh
of 25 (xm in Umguav River (towns of Colon and Con-
cepcion del Uiiiguay), at 3 stations in the Carcaraiia Riv-
er, and Correntoso River
RESULTS AND DISCUSSION
Liinnopenw foifunei was first found in South America
in 1991 at Bagliardi Beach (Argentina) with densities of
5 individualsm- (Pastorino et al, 1993). In 1992, the
maximum densitv' recorded was about 3X10^ indixidu-
als-m -. In 1993, in the same locality, the maximum den-
sity recorded was SXIO' individualsm -. In 1998, den-
sities of about 15X10' individuals-m"- were commonly
recorded, values equivalent to those for mytilid densities
at the seashore in Mar del Plata, Argentina (Penchasz-
adeh, 1973).
In 1994 and 1995, L. fotiiinei was found in the water
intakes of the town of Bemal (MLP 5204) and Retiro,
and on Buenos Aires Harbor (MLP 5205). Scarabino
and Verde (1994) reported the species from the town of
Colonia del Sacramento, Uruguay (MLP 5202). All these
localities are on the Rio de la Plata estuaiy. During 1996,
the species expanded to the town of Goya (29°10'S,
59°16'W), in Corrientes Province (Di Persia and Bonet-
to, 1997) and nearby lotic bodies, and was collected in
the middle Parana River, near the city of Santa Fe,
where the river has a \'erv
width; Drago, 1990).
wide alluvial plain (25 km in
Figure 1. Studied localities on the la Plata Basin. A, Punta
Piedras; B, Punta Indio; C, Magdalena beach; D, Atalaya
Beach; E. Pmita Blanca; F, La Balandra Beach; G, Bagliardi
Beach; H, Pnnta Lara Beach; L Benial Beach; ]. Buenos Aires
Harbor; K, Atncha I Nuclear Power Plant; L, City of Rosario;
M, Town of Santo Tome; N, City of Santa Fe; O, Esquina; P,
Goya; Q, Cerrito Island; R, Town of Formosa; S, Asuncion
Harbor; T, Posadas Harbor; U, Praia de Itapna (Rio Grande
do Sul State, Brazil); V, Town of Colonia del Sacramento; 1,
Town of Colon; 2, Town of Concepcion del Umguav; 3, Car-
caraiia River.
Litnnopcrna foiiunci was first collected in Parana Riv-
er at Vuelta del Este, Zarate, on the Parana de Las Pal-
mas River (MLP 5206), and at Paso Burghi, city of Ro-
sario, on the lower Parana River (MLP 5207) toward the
end of 1995 (figure 1). The species settles on all kinds
of substrates across the entire floodplain. It was found
in the main channel, on the left bank at town of Parana
and associated alluvial plain, in San Javier and Corren-
toso (MLP 5287) rivers, near the city of Santa Fe. It was
also found on the right bank of the lower Salado del
Norte River (MLP 5285), in the town of Santo Tome
(31°40'S, 60°45"W).
Limnopcnia foiiinwi was part of the epifauna present
on Solanaceas and Paspahun .sp. (MLP 5286) in all hab-
itats observed, but was not found on the sandy, moving
bars (Drago, 1997) in the main channel. Perhaps due to
the unfavorable sandy substrate, the central part of the
G. Darrigran and I. Ezcurra de Drago, 2000
Page 71
main channel pro\ides haliitat to onK- a few henthic spe-
cies (Marchese and Ezcurra de Drago, 1992). In the
Correntoso River (a secondary channel of the middle
Parana Ri\er\ L. foiiiiiici i-olonized the silt\ cla\ lieds
at all locations sanipleil
The eun,haline attributes of L. foiinnci probably fa-
cilitates its rapid spread. The mean salinitv at the main
channel of the Parana River is 0.05 %r, and in Corren-
toso River it ranges bet\veen ().()fi4-().345 %c. In Salado
del Norte Rixer, which mi.\es with the waters of the Pa-
rana River, sahnitv varies from 0.5 to 4 %c (Ezcurra de
Drago, personal obser\'ation). Mean pH is 7.4 in the Pa-
rana m;un channel and 7.2 in secondaiy courses (Mar-
chese and Ezcurra de Drago, 1992), \s'hile in Salado tlel
Norte River pH reaches 8.7.
In 1996, this species was collected on "fouling" sam-
plers in Cerrito Island (27°20'S, 5S°43'W), near the con-
fluence of the Paraguay and Parana rivers (MLP 5340).
In April 1997, it was collected on Asuncion Harbor
(25°17'21"S, 57°38'0S"W), in the Paraguay River, in Par-
aguay (figure 1). It was also collected during the last
months of 1998, at Posadas Harbor, on the upper Parana
River. In November 1999, L foiiimci was detected in
Brazil on Itapua Beach, Municipality of Viamao, Rio
Grande do Sul State (MLP 5550). No larvae, juveniles
or adults have been found at anv of the locahties ex-
amined in UiTiguav- River (Colon, Concepcion del Uru-
guay) or Carcarana River (Carcaraiia and la Ribera).
The biofouling problems caused by L. fortunei in
South America are similar to those described for Drcis-
scna pohjinoiyha, the zebra mussel, in the Northern
Hemisphere (Darrigran, 1995).
The principal problems caused by zebra mussel in-
vasion, settlement, and maturity, into water distribution
systems (Nalepa and Schloesser, 1993) are listed below
(the problems which have already been detected in Ar-
gentina resulting from invasion bv L foiiuiici are
marked with (X)).
• ( X ) Reduction of pipe diameter
• ( X ) Blockage of the pipeUne
• Decreased water velocitv caused bv friction (turbulent
flows).
• (X) Accumulation of enipt\' shells
• Contamination of water pipelines by mass mortality
• ( X ) Filter occlusion
These problems have occurred in the intakes of water
treatment plants in the city of La Plata; water treatment
plants along the Corrientes River (MLP 5365), and also
in industrial and power-generating plants. They cause an
increase in the operational costs of these facilities due
to reduced pump efficiency, increased tube corrosion
(caused by proUferation of bacteria and fungi), and in-
creased frequenc)' of shutdownis for cleaning and filter
changes.
Absence of relevant records in the numerous benthic
studies conducted prior to 1991 (Darrigran, 1991, 1994;
Marchese and Ezcurra de Drago, 1992) indicate that
colonization by L. foiiiinci is a recent event. By late 1996
and early 1997, the first cases of fouling bv L. fniiunei
in nearby industries were reported in the Parana River
(e.g., Atucha I Nuclear Power Plant and San Nicolas de
Los Arroyos Electric Plant (MLP 5300), Buenos Aires
Province).
Based on the facts above described, it appears that
the geographic range of L. foi-tunci is in continuous ex-
pansion in South America, and that the species is ap-
parently adapting to different environments along its in-
vasion routes. Between 1991-1999 this species invaded
4 c(juntries (Argentina, Uruguay, Paraguay, and Brazil);
3 of the Ri'o de la Plata Basin main rivers (la Plata, Pa-
rana, and Paraguay). It traveled upstream at a speed of
about 240 kmvear '. Throughout its distribution range,
L. fdiiiinci inhabits a wide variety of environments: from
euryhaline waters in the La Plata estuary to strictly
freshwater habitats along the Paraguay and Parana riv-
ers.
This expansion is proiiably favored by the moqiho-
functional features of the species, and by the apparent
absence of competitive interactions along the httoral of
la Plata Basin. Lininopcnio foiitinci is the onlv relevant
species using bvssal epifaunal attachment among local
freshwater species.
Although the distribution of L. foiiunci is currently
still limited to la Plata Basin, there are no apparent con-
straints that could prevent the invasion of other drainage
systems. Moreover, this expansion may be favored by the
increase in trade between Argentina, Uruguay, Paraguay
and Brazil, as a consequence of the recently establi,shed
MERCOSUR international economic consortium (Dar-
rigran, 1995; Darrigran and Pastorino, 1995b). Addition-
al dispersal of the species could also be favored by the
international project HIDROVIA, which consists of a
wateiAvay connecting the mtiin hvdrographic systems of
South America. The project comprises a complex fluvial
network system that involves and interconnects Rio de
la Plata, Parana, and Paraguay rivers, and includes plans
for extensive basin dredging, harbor construction, and
improvement of the harbors and highways. Connections
among the main South American basins (e.g., Amazonas,
Orinoco) are likely to be artificially established in the
future. Up to now no effective control mechanisms have
been proposed to prevent further spread oi L. fortunei.
The impact of L. foiiintci will not be restricted onlv
to the economy, but will also affect the diversit>- of the
native molluscan communities. Darrigran et al. (1998)
showed that, since the introduction o{L. fortunei at Bag-
liarili Beach, populations of 2 common gastropods have
been displaced: Ciiilina jiuminea (Maton, 1809) is no
longer found, while Gundhiehia conccnfiica (d'Orbigny,
1835) is becoming rare (figure 2).
In contrast, several benthic species, uncommon or ab-
sent before the occurrence of L. fortunei. are now pre-
sent. These include Annelida Ofigochaeta (8 species),
Aphanoneura (1 species) and Himdinea (8 species); plus
assorted Crustacea and Insecta (Darrigran et ai, 1998).
Additionallv, we observed the epizoic colonization and
snujthering of native bivalves (e.g., Anodontite.s trapesi-
Page
THE NAUTILUS, Vol. 114, No. 2
DENSITY
Helobia piscium
10' ■•
Chilina fluminea
I .
]«|«jB|*|«|«|«|*|B|«|*|B|
I ■ I ■ I ■ I ■ I ■
Gundlachia concentnca
I'i'i'i'i'i — I * I ■ I ■ I ■ I
Limnoperna fortune!
H 1 1 1 1
-•-h ( 1 1 1 (-1 — I 1 h
■3 7 8 9 10 12 1 2 3 5 8 10 12 |l 2 3 4 6 9 10 11 I 3
88 I 92 |93 194 I 95
MONTH/YEAR
Figure 2. Temporal \ariation of density (individuals-m"-,
represented bv mean and standard deviation) of some native
mollusks associated with the byssus of L, fortiinei in Bae;liardi
Beach (34°55'S, 57°49'W), Wentina.
alis (Lamarck, 1819) and A. tcncbricosus (Lea, 1834)) by
L. foiiiinei, in a behavior similar to that shown by Dreis-
seno poli/inoi-f)ha on unionids (Parker ct al, 1998).
Last but not least, further expansion of the natural
range ot Limnoperna foi-tunci and the possibilitv of in-
vasion of parts of Noith America by this species should
not be rejected. As Ricciardi (1998) obserx'ed, "Given
that shipping traffic from both Asia and South America
has alreadv resulted in recent introduction of exotic bi-
valves to the USA, a future North American invasion bv
L. fortunci is highly probable."
ACKNOWLEDGMENTS
The work was supported by the grants of the Consejo
Nacional de Investigaciones Cienti'ficas y Tecnicas (PEI
N° 548/97), Facultad Ciencias Naturales v Museo
(UNLP), and Agencia Nacional Promocion Cientifica y
Tecnologica (PICT98 No. 01-03453). We thank Dr. Ri-
chard Sparks and Ruth Sparks for the revision of the
manuscript. Dr. Edmundo Drago and M. C. Dambore-
nea for helping in assorted tasks, and Lionel Mehaudy
for the technical assistance. Maria CrisHna Dreher Man-
sur collected and provided the specimens from Itapua
Beach, Rio Grande do Sul, Brazil.
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THE NAUTILUS 114(2):74-79, 2000
Page 74
Location of allospermatozoa in the freshwater gastropod
Biomphalaria fenagophila (d'Orbigny, 1835) (Puhiionata:
Planorbidae)
Warton Monteiro
Depaitiimento de Ecologia
Uiu\ersidade de Brasilia
Brasilia, DF
BRAZIL
warton@uol.c-oni.br
Toshie Kawano'
Laboratorio de Parasitologia
Instituto Butantan
A\'. Vital Brasil, 1500
0550.3-900 Sao Paulo
BRAZIL
The freshwater puhnonate Biomphalaria fenagophila is
a simultaneous hermaphrodite. The route ot allosper-
matozoa in the receiving partner was used in the analysis
of resource allocation in the male function in this spe-
cies. Allospermatozoa enter the vagina, mav or may not
bvpass the spermatheca, continuing through nidamental
gland, o\'iduct-muciparous gland, albumen gland, oNds-
permioduct, seminal vesicle, ovotestis collecting canal,
and folhcles of ovotestis. A new technique is proposed
to label spermatozoa xaa injection oi tritiated th\iiiitline
through the pneumostome (under anesthesia). Labeled
allospermatozoa were located in the spermatheca, ni-
damental gland, oviduct-muciparous gland, albumen
gland, seminal vesicle, and follicles of ovotestis. No re-
lation was found between the duration of pairing and
movement of the allospermatozoa through the repro-
ductive system. It is suggested that the final destination
of allospermatozoa are the folhcles of ovotestis. Their
presence in the spermatheca, where thev ma\' be dis-
solved, could be fatal. Presence of allospermatozoa in
the nidamental gland, oviduct-muciparous gland, or ;il-
bumen gland may be a consequence of unilateral cop-
ulation (snail plavs only a recei\ing role), which packs
the seminal vesicle with autospermatozoa. Allosperma-
tozoa may wait in the interior of the female tract until
the snail becomes a donor in a subsequent pairing. From
then on, allospermatozoa may pass through an empty
seminal vesicle toward their final destination, the folh-
cles of ovotestis.
Key words: Reproduction, spermatozoa, hermaphrocUt-
ic, pulmonates.
INTRODUCTION
The location of spermatozoa within the reproductive sys-
tem of inseminated puhnonate gastropods plavs an im-
' Author for correspondence; tkawano@usp.br
portant role in the processes of self-fertilization, cross-
fertilization and, in particular, preferential cross-fertiliza-
tion in these mollusks (Larembergue, 1939; Paraense,
1959).
In the genus Phijsa, 2 or 3 possible chambers for fer-
tilization were described. Although these chambers open
in the oviduct, the actual site of fertifization may be lo-
cated in the hermaphrodite region, close to the carrefour
(Duncan, 1969). In planorbids, the seminal vesicle has
been cited as the main location of spermatozoa (Lar-
ambergue, 1939). The fertilization chamber, in the car-
refour, where the spermatozoa received from the part-
ner are stocked, is also a possible ferhhzation site (Ab-
del-Malek, 1954; Duncan, 1975). The oviduct (Fretter
and Graham, 1964) and the upper part of the o\isper-
mioduct mav be sites where the oocytes are fertilized by
the allospermatozoa (Abdel-Malek, 1954). Some authors
consider the spermatheca as a location where sperma-
tozoa remain immecfiatelv after copulation, proceeding
subsequently through the female ducts (Duncan, 1975).
Notwithstanding, the spermatheca in B. glahrata also
behaves as a site of lysis of spermatozoa (Horstmman,
1955; Jong-Brink, 1969; Kitajima and Paraense, 1983).
In planorbids, the spermatheca is a blind, pvriform or-
gan, opening in the vagina through a short duct (Par-
aense, 1975; Kitajima and Paraense, 1983). This is also
called bursa copulatrix (Duncan, 1975), or seminal re-
ceptacle. In euth\aieuran gastropods, the evolutionary
acquisition of reproductive s\stems such as functional
simultaneous hermaphrocUtism has been associated with,
among other traits, fundamental changes in the structure
of the spermatozoa (Thompson, 1973).
A past experiment iuNolving incorporation ot '"Fe by
BioinpJialaria tAahrata took place in water containing
this rachoisotope (Gazzinelli ct al. 1970). Incoiporated
isotope was transferred, during pairing, from labeled B.
glabrata to non-labeled partners. The presence of the
rachoisotope in snails receiving spermatozoa was record-
ed chiefly in the spermatheca and collecting canal of the
ovotestis (Paraense, 1976).
W. Monteiro and T. Kawano, 2()()()
Page 75
Bioinphdldhd <iliil>i'iitti is known tu pivfcTfntiallv con-
centrate iron in the (notestis, as well as in non-repro-
tluetive organs such as chgestive gland and mantle (He-
neine et al, 1969). Therefore, it is plausible that ^'^Fe
transferred from labeled to non-labeled snails could be
incoiporated in the ovotestis of receptor snails, indepen-
dentK of spermatozoa being the carrier of ''Fe within
the receptor suiiil.
On the other hand, the use of DNA-specific labels can
be an efficient wav of tracking the location of allosper-
matozoa in the inseminated snail partner. Tlie route of
spermatozoa heads in the inseminated snail can be de-
termined by the use of tritiated thymidine ('H Td). This
method also allows for the detection of possible areas of
storage and sites of cross-fertilization.
MATERIALS AND METHODS
One hundred and six specimens of Biomphalaria tcna-
gophila were used both of the wild txpe and albino mu-
tants. Specimens were collected in Bom Retiro, Joinville,
Santa Catarina State, Brazil. They were kept for over 4
vears under laboratorv' conditions. Each aquarium con-
tained a tablespoon of red earth sterilized in <\t\ incu-
bator at 90°C for 12 h. One hundred and eightv ml fil-
tered water, saturated with calcium carbonate, was add-
ed to each aquarium. Snails were fed daily with fresh
lettuce and twice a week with a meal consisting of equal
amounts of red earth, powdered whole milk, wheat germ
flakes, powdered calcium carbonate, and dry powdered
alfalfa. To a 5 1 amount of diis mixture 350 mg of vitamin
E was added. Except in some cases, snails were kept in
isolation from sexual immaturity onward.
Two suppfies of aqueous solutions of 'H Td were used
in the ex-periments. Ten pi of one (USP, kindlv offered
by Dr. Mariano Amabis, University of Sao Paulo) yielded
218687 counts per min. (cpm); the other commercial
solution (\VM) was purchased as 1 millicurie, or .37 me-
gabequerel/ml; 5|xl from this solution \ielded 314850
cpm in a Beckmann Liquid Scintillator 7200, using "pro-
gram 2 for tritium". Each of the 106 specimens was
anesthetized by immersion in a 0.05% nembutal solution
for 3^ h, depending on snail size. Aftei-ward, they were
inoculated with 5-10|jl1 of 'H Td injected using micro-
syringe into the lung cavity, through the pneumostome.
Recovery from anesthesia took place in a humid cham-
ber, for 3—4 h, with each snail placed on its right side in
a plate with water covering half shell. After this period,
each inoculated snail was returned to its aquarium for
completion of recovery from anesthesia and radioisotope
incoiporation.
Between 4—29 days after treatment, each inoculated
snail (IC) was paired with a non-inoculated snail (NIC)
for a period of 6 — 984 h. NIC snails were dissected un-
der stereoscopic microscope within a period of 0—24 h
after separation. The following organs were extracted:
spermatheca, oothecal gland + muciparous gland, o\i-
duct or oothecal gland by itself, but muciparous gland
with oviduct, part of digestive gland, carrefour, albinnen
Figure L Diagram of tlie reproductive system of Biomphal-
aria tcnaf^ophiln. 1. Hind-part of ovotestis; 2. Follicles of the
ovotestis; 3. Ovotestis collecting canal; 4. Seminal vesicle; 5.
Albumen gland; 6. 0\'idiict; 7. Muciparous gland; 8. Oothecal
gland; 9. Nidamental gland; 10. Spermatheca; 11. Vagina; 12.
Spermioviduct; 13. Prostate; 14. Deferens canal; 15. Penis
sheath; 16. Prepntiiim
gland, seminal vesicle and ovotestis (Figure 1). Counting
in a section of the digestive gland determined the
amount of incorporation of radioisotope outside the re-
productixe system, the background radioisotope incor-
poration. The ovotestis was macerated releasing material
from the collecting canal and follicles. These contents
were collected separately from the rest of the macerate.
Each sample was transferred to a vial containing 0.3 or
0.5 ml of a solution of 3 % sodiiun hvpochloride (com-
mercial bleach). The material was repeatedly refluxed
with a Pasteur pipette until completely dissolved. Prep-
aration of filter paper strips imbibed with samples for
measuring in the liijuid scintillator was based on the
methodology of Byfiekl and Scherbaum (1966).
Though spermatozoa may be found and counted in
chfferent organs of the reproductive system during and
after the pairing process (Monteiro and Kawano, 1998),
in this work the occurrence of allosperTnatozoa in the
examined organs was accounted tor only by counting in
the hquid scintillator
Some controls were used to test the efficiencv of the
method. Processing of each series of paper strips with
samples included a paper strip without sample, a "blank"
that allowed us to investigate the amount of free racho-
active material that could be absorbed from solutions
where the papers with samples were being treated (Ta-
ble 1).
The radiation in the water where the snail recovered
from anesthesia was measured by scintillation to evaluate
the efficiency of the inoculation in the lung cavitv and
the draining of H Td into the mechum during the re-
coveiy period. The amount of radiation injected into
each snail was also measured (Table 1).
RESULTS AND DISCUSSION
The technique of inoculation in the lung ca\it\ through
the pneumostome of the anesthetized snail was here
used for the first time. The evaluation of this technique
Page 76
THE NAUTILUS, Vol. 114, No. 2
Table 1. Experiments with different supplies of tritiated th^inidine (USP and WM supplies)
minute. Blanks = data not available
Cpni = scintillation counts per
Exp. 1
Exp. 2
Exp. 3
Exp. 4
No. snails
5
5
5
5
Microliters inoculated/snail
lOUSP
lOUSP
lOUSP
5WM
Inoculation-pairing (days)
7
7
11
6
Duration of pairing (h)
24
24
24
24
Pairing-dissection (h)
52
48
216
40
Separation-dissection (h)
28
24
192
16
Inoculation to-dissection (approx. days)
9
9
20
8
Diameter of snails (mm)
12-14
12-13
12-13
13-14
Reference (cpm)
27507
26911
23534
Background (cpm)
71
65
84
75
Blank (cpm)
105
119
0\nduct (cpm)
109
89
78
0\'otestis collecting canal (cpm)
91
84
76
105
Follicles of ovotestis (cpm)
174
84
107
121
Spermatheca (cpm)
81
114
114
110
Nidamental gland (cpm)
96
890
884
Oothecal gland (cpm)
135
Seminal vesicle (cpm)
1184
63
139
121
Digesti\'e gland (cpm)
87
104
Carrefour (cpm)
76
107
Albumen gland (cpm)
427
0\iduct -muciparous gland (cpm)
102
° USP, supplv kindh' offered by Mariano Amabis, Universitv of Sao Paulo: WM, supplv purchased by one of the authors.
was carried out in 18 snails inoculated with a total oi 90
jjlI of ^H Td. Retention of inoculate in the lung cavity
was tested through measurements of the relative amount
of radioisotope that drained during the 4 h recovery
from anesthesia. The snails recovered in 27.5 ml of water
that yielded 81152.5 cpm. As each 5 |xl of the applied
radioisotope solution counted 314850 cpm, there was,
on average, a 1.4 % loss of radioactive material from
snails to the water. This result encourages the use of this
inoculation method in tests of prospective toxicology, se-
lection of mutagens, and of the mechanism of action of
water pollutants.
The results of 1 1 out of a total of 30 e.xperiments are
shown in Table 1. The remaining experiments did not
record high counts for any of the examined organs. The
low counts in all examined organs may have occurred in
sniiils that did not act as females in relation to the in-
oculated partner. An arbitraiy criterion was established;
to consider onlv the experiments in which the counting
in the most labeled organ was at least twice as those in
the least labeled one.
As a natural consequence of metabolism, the long du-
ration of an e.xperiment might cause the incoqjoration
of the radioisotope in an organ absolutely lacking sper-
matozoa. This does not seem to be the case here, even
in experiments lasting for 216 and 948 h (e.xperiments
3, 10, and 11), from pairing to dissection time. In these
conditions, the most labeled organs were the nidamental
gland (884 cpm), the albumen gland (210 cpm) and fol-
licles of ovotestis (365 cpm), respectively (Table 1). We
looked for possible transfer of the radioisotope label
from the reproductive system to a highly metabolically
active organ such as the chgestive gland. A tragment of
digestive gland, similar in volume to the ovotestis, was
simultaneously tested in experiments 2 and 3 (respec-
tively 48 and 216 h after pmring). The relatively low
counts, 87 and 104 cpm respectively, discarded that pos-
sibilit)' (Table 1).
After a specimen of B. glabrata behaves as female
during pairing, its spermatheca is packed with sperma-
tozoa. That organ is site ot lysis of spermatozoa (Kitajima
and Paraense, 1983). Suiprisingly, among all the e.xper-
iments, only one presented relatix'ely elevated countings
for spermatheca (206 cpm): experiment 8 (Table 1). Be-
sides, in experiment 9, where the time lapse from pair-
ing to dissection was only 7 h, the spermatheca counting,
87 cpm, was equivalent to the blank (Table I). Given the
countings in the digestive gland (458 cpm), it is possible
that the spermatozoa have either bypassed or spent a
verv brief time in the spermatheca on their way to the
digestive gland. Also, clue to the relatively short time
elapsed from pairing to dissection, 7 h, the hypothesis
of radioisotope transfer from spermatheca to digestive
gland was not taken into account in the analysis of the
data.
No relation was found between the duration of pairing
and progression of the allospermatozoa along the repro-
ductive ducts. After only 54 h from the beginning of
pairing, in experiment 6, the allospermatozoa were in
the folhcles of the most distant organ from the vagina,
the ovotestis (585 cpm). But 216 h after the beginning
of p;iiring, the iillospermatozoa were in the nidamental
gland (216 cpm, experiment 3), the organ closest to the
vagina (Table 1).
W. Monteiro and T.
Kawano, 2000
Page 77
Tabic 1. Exteiuled
Exp. 5
Exp. 6
E.\p. T
Exp. S
Exp. 9
Exp. 10
Exp. 11
4
5
3
.5
3
2
lOUSP
5\\M
lOVVM
lOW'M
lOWM
lOWM
lOWM
19
7
/
11
19
29
29
96
24
8
9
6
984
984
120
54
8
31
6
984
24
30
0
22
0
?
0
24
9
-'
12
19
70
12-14
12-14
9-13
9-11
11-12
12-13
11-12
24765
24383
24357
24357
24027
24585
75
103
72
99
99
55
65
119
103
110
87
87
92
77
103
117
89
76
68
68
787
585
106
89
73
59
365
168
93
172
206
87
76
147
133
120
74
77
78
71
84
111
105
275
74
57
75
68
115
166
119
92
458
210
63
314
131
9.3
84
81
S7
65
The simultaneous occurrence of high counting in the
toUicles of o\otestis and in the oviduct-muciparous gland
in a single experiment (experiment 5), after 96 h of pair-
ing, suggests the occurrence of double copulation (Dias,
1995). Spermatozoa transferred in the initial copulation
could be located in the organ most distant from the va-
gina, the folHcles of ovotestis. The spermatozoa trans-
ferred in a subsequent copulation may be located in an
organ closer to the vagina, such as the oviduct-mucipa-
rous gland (Table 1). This explanation, however, could
be inconsistent. Even if the last copulation happened at
the end of pairing, the 24 hours that passed after the
separation of the partners would be enough tor these
spermatozoa to advance along the genital tract, bxpass-
ing the oviduct-muciparous gland. In a shorter period of
time, from pairing to dissection, allospermatozoa pro-
ceeded to the seminal vesicle and albumen gland, re-
spectively, in experiments 7 and 9. The results of exper-
iment 3, however, show that it is possible that the sper-
matozoa remain in the nidamental gland for up to 192
h after the separation of the partners. Therefore, under
the experimental conditions, the scintillation counting
may indicate that, in a single or in diiferent snails, from
a group of 4 (experiment 5, Table 1), the spermatozoa
may be located in sites as separated as the ovotestis and
organs closer to the vagina such as the oviduct-mucipa-
rous gland. It is possible that, rather than suggesting ran-
dom differences in locomotion abilit), these results could
indicate strategic, differential placement of allosperma-
tozoa.
All the occurrences of allospermatozoa along the re-
productive system, registered in the nidamental gland,
seminal vesicle, albumen gland, and iolhcles of the ovo-
testis are difficult to explain At first sight, the nidamen-
tal gland seems to be a transient site ot allospermatozoa
on their way to their final destination, where the\- will
fertilize the oocytes (Paraense, 1959). However, their
stay in the nidamental gland for 216 h from pairing to
dissection time (experiment 3, Table 1), a period of time
much longer than that necessary for the spermatozoa to
reach the follicles of ovotestis (experiments 5 and 6: 120
h and 54 h, respectivelv; Table 1), contradicts this pre-
mise. Considering that the seminal vesicle of the donor
may be empty after pairing (Monteiro and Kawano,
1998), the presence of labeled allospennatozoa in this
organ (experiments 1 and 7) suggests that autosperma-
tozoa were replaced b\' allospermatozoa. This inteq^re-
tation apparently conflicts with the occurrence ot labeled
allospermatozoa both in the folficles of ovotestis and in
the albumen gland, both within short and long intervals
from pairing to dissection (e.xperiments 4, 5, 6, 9, 10,
and 11).
No relation was found between the duration of pairing
and progression of the allosperm through the reproduc-
tive system. The labeled allospermatozoa were located
in the spermatheca, nidamental gland, oviduct-mucipa-
rous gland, albumen gland, seminal vesicle and follicles
of ovotestis. It seems that the destination of allosper-
matozoa are the follicles of the ovotestis. Their occur-
rence in the spermatheca, where Ksis takes place, may
be highly detrimental or fatal. Copulation in B. tcna^o-
phila may be unilateral or reciprocal (Dias, 1995). Con-
sequently, the length of stav of labeled allospermatozoa
in the nidamental gland, oxiduct-muciparous gland, or
albumen gland may be the result of imilateral copula-
tion, when the snail played only' a receiving role, which
Page 78
THE NAUTILUS. Vol. 114. No. 2
resulted in a seminal \esitle full of autospermatozoa. Al-
lospermatozoa may wait within the female tract until the
snail plays a donor role in a subsequent pairing, which
can be unilateral or reciprocal. Then, allospermatozoa
ma\' pass through an empt)^ seminal \esicle toward the
follicles of the ovotestis. Within an o\otestis follicle, in
the oocyte formation site and co-existing with immature
autospermatozoa (Homan, 1972), allospermatozoa may
fertihze the oocytes (Laramberg, 1939; Paraense, 1955).
The many possible locations for strategic storage of al-
lospermatozoa suggests displacement of autospermato-
zoa, which makes possible the appropriate deplo\nnent
of allospermatozoa.
Allospennatozoa were present in ovotestis follicles in
experiments 5, 6, and 11, but were not found in the
collecting canal of ovotestis in any of the 11 experiments.
NoUvithstanding. Paraense (1976), labeUng snails with
'"Fe, found e\idence of allospermatozoa in the collecting
canal. A possible explanation for this result is the re-
incorporation of iron. In fact, the ovotestis has a noted
avidity for iron (Heneine ei a/., 1969; 1970a; 1970b). Of
all these locations, the one more consistent with data
from the hterature is the alliumen gland, although all
searches for spermatozoa in the canals of the gland and
nearby areas during the preparation of the present work
have yielded negative results (not even spermatozoa
heads were found). Nevertheless, a chamber of fertiliza-
tion, in the carrefour, next to the albinnen gland, is often
referred as the final site for storage of spermatozoa in
studies carried out on several other species of moUusks
(Duncan, 1958; 1960; Lind, 1973; Geraerts and Joosse,
1984).
CONCLUSIONS
Inoculation of a solution of tritiated thymidine through
the lung cavity of individuals of Biomphalaria tcnago-
phila is an adequate method to label spermatozoa for
determining their location in the partner after pairing.
Labeled spermatozoa were detected in the recei\ing
snail, through significant levels of scintillation counting,
in the spennatheca, seminal vesicle, folhcles of ovotestis,
nidamental gland, albumen gland, and oviduct-mucipa-
rous gland. Material extracted from the collecting canal
of the ovotestis did not show countings for labeled sper-
matozoa. The presence of labeled spermatozoa simul-
taneouslv in the follicles of the o\'otestis and in the o\i-
duct-muciparous gland suggests options for tlifferential
storage locations, in a process that includes displacement
of autospermatozoa to allow for adequate positioning of
allospermatozoa.
ACKNOWLEDGMENTS
We thank Dr. Mara Liicia Ferreira Dias for valuable sug-
gestions and criticism to this work, and to fellowships
from CAPES (Coordena9ao e Aperfei^oamento de Pes-
soal de Nivel Superior, Brazil).
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THE NAUTILUS 114{2):S0-83, 2000
Paee 80
Status of the tidewater mucket, Leptodea ochracea (Say, 1817)
(Bivalvia: Unionidae), in Halfway Pond, Massachusetts, USA
Jay Cordeiro
Department of Invertebrates
American Museum of Natural History
Central Park West at 79th Street
New York, NY 10024 USA
corcleiro@amnh.orCT
ABSTRACT
The tidewater mucket, Leptodea ochracea (Say, 1817), is dis-
tributed along the Atlantic coast of North America and is often
found on sandy substrates with little or no flow. Halfwav Pond,
in PKinouth, Massachusetts, is one of the few remaining hab-
itats in Massachusetts for tliis species, but li\e specimens have
not been collected there since 1981. In summer 1995, the
pond was sur\'eyed in an attempt to determine if the tidewater
mucket had been extiipated. Of 213 li\'e unionids collected,
comprising 6 different species, only 1 specimen was identified
as L. ochracea. The single specimen was found in the Agawam
River outflow area in the southwest comer of the pond along
with 4 of the 5 other species of unionids occurring in the pond.
This high flow area had a high proportion of benthic macro-
phvtes in a sanch' substrate — hpical habitat for L. ochracea.
Other species found in the pond include EUiptio coiuplanata
(Lightfoot, 1786), LampsiUs radiata radiata (Gmelin, 1791),
Alasmidonta undulata (Say, 1817). Strophitiis undidatus (Say,
1817), and Pijganodon cataracta (Say, 1817). This study con-
firms the decline of L. ochracea in Halfway Pond, Massachu-
setts, over the last 15 years. If not already gone, this species
may disappear from the pond once the remaining indi\iduals
die.
Keij words: Unionoidea, freshwater clams, freshwater mussels,
extirpation
INTRODUCTION
The tidewater mucket, Leptodea ochracea (Say, 1817),
is a freshwater mussel (family Unionidae) distributed
along the Atlantic coast of North America from Nova
Scotia to Georgia (Johnson, 1947; 1970; Strayer and Jir-
ka, 1997). Populations are often found on sandy sub-
strates with httle or no flow (Smith, 1981), usually in
water bodies near the ocean but not necessarily con-
nected to it.
In Massachusetts, Leptodea ochracea is found in
coastal plain ponds larger dian four hectares, along the
southeastern portion of the state, from the South Shore
to Buzzard's Bay to Cape Cod (Smith, 1991). Because
of its highly restricted geographic distribution and de-
creasing abundance in ponds throughout its range, the
tidewater mucket is listed as a species of special concern
(Smith, 1981; Williams et al, 1993; MDFW, 1997).
Over the past 65 years, Leptodea ochracea was found
in Halfvvay Pond in PlvTnouth County on several occa-
sions (Table 1). Since 1981, however, it has not been
recorded there (Nature Conservancv, unpublished data).
In the summer of 1995, the author surveved Half\yay
Pond in an attempt to determine the distribution status
of L. ochracea and other unionids.
Halfwav Pond is a 94 ha freshwater pond with a 4.9
ha island preserve in its center located just south of
Plymouth, Massachusetts, next to Miles Standish State
Forest. The island preserve is a candidate for designa-
tion as a National Natural Landmark bv the Department
of the Interior mainly because it contains one of the
oldest forests rem;uning in Massachusetts (Nature Con-
servancy, unpublished data) and is located in the area
with the fastest development rates in the state (Living-
ston, 1987).
MATERIALS AND METHODS
Live mussels were collected by hand with a meter-long
dip net with 2.5 cm mesh. Surveys were supplemented
by snorkeUng to a depth of 1.5 meters. The net handle
was used to delineate a circular quadrat for each sample
area (1 m- area). Surveys were conducted at 2 to 4 m
intervals; 30 samples were taken at the first 2 sites and
15 samples at the remaining 4 sites around the lake. For
each specimen, species name, total length in miUimeters,
degree of dissolution of the shell (shell wear), collection
localit\-, and sechment t\pe (estimated visually as sand,
mud, or cobble) were recorded. Specimens were ex-
amined for identification with a 6 X hand lens and dis-
secting microscope to 30 X , when necessary. Specimens
were only dissected when internal characters were re-
quired for identification. Species were identified using
Smith (1991) as a primarv' .source and McM;Jion (1991)
and Peckarsky et al. (1990) as supplemental sources.
J. Cordeiro, 2000
Page 81
Tabic 1. Li'ptodcn ochmcca in H;ilf\\':i\' Pond. Massacliusetts: specimens in major American mnsenni collections
No. specimens
Localih
Collector! s)
Date
Collection No.
1
Haltwas- Pond
ex-MCZ
USNM 656539
3
Halt\va\ Pond
R. I. Johnson
USNM 592091
1
alonCT Mast Roail. Hal
K\a\ Pond
ex-MCZ
[pre-1975]
OSUM 38073
4.5
HalR\a\- Pond
R. E. M.. W. F.
C.
(William F.
Clapp?) ex-MCZ
Aug. 19, 1933
OSUM 26550
9
HalKvaN- Pond
R I Johnson
Jul. 1, 1941
AMNH 72936,
DMNH 48551,
USNM 600325
3
Halfway Pom! outlet
R. I. Johnson
June 1943
MCZ 134.841.
MCZ 159150
4
Halfway Pond
M. K. Jacohson
Aug. 22, 1952
AMNH 121013
4
South shore, Half\va\' Pond
M. K. Jacohson
Aug. 23, 1952
AMNH 127888
12
Agawani River outlet.
Halfway Pond
D. G. Smith. A.
E.
Pratt
July 1981
UMAMZ 5.39
Voucher .specimens ior Lcptodca ochracca were not .sub-
mitted due to the scarcity of specimens.
Over the past 300 years there has been some contu-
sion as to the proper nomenclature o( Lcptoclca ochracca
(Johnson, 1947; 1970; Morrison, 1975; Bereza and Ful-
ler, 1975), since its original description as Pectunculus
fluviatilis Lister, 1685. A forthcoming manuscript (Cor-
deiro, in preparation) should clarifv manv of the complex
nomenclatural issues inxoKing this species. In hght of
this uncertainty in nomenclature, the author herein will
refer to the species as Leptodea ochracca (Say, 1817) as
per its listing in Turgeon ct al. (1998).
Institutional abbreviations used are: AMNH, Ameri-
can Museum of Natural History, New York; DMNH,
Delaware Museum of Natural History, Greenville, Del-
aware; MCZ, Museum of Comparative Zoology, Harvard
University, Cambridge, Massachusetts; OSUM, Museum
of Biological Diversity, Ohio State Universitv, Colimibus,
Ohio; UMAMZ, Universit\- of Massachusetts Museum of
Comparative Zoology, Amherst, Massachu.setts; USNM,
National Museum of Natural History, Smithsonian In-
stitution, Washington, DC.
RESULTS
The freshwater mussels EUiptio complanata (Lightfoot,
1786), Laiupsilis radiata radiata (Gmelin, 1791), A]as-
mkhmta iiudulata (Sav, 1817), Strophitiis iindulatus (Say,
1817), Pijganodon cataracta (Say, 1817), and Leptodea
ochracca were collected along the shores of Halfway
Pond and the Halfwav Pond Island Preserve. Table 2
depicts results of sur\eys at the 6 sites around the lake.
Survey site 1 is sandy with no benthic, macrophvtic
plants and frequently used for sport fishing. All mussels
collected there were identified as E. complanata. Site 2
was also sandy and clear Only 2 live specimens of E.
complanata were found. Site 3 had a sandy substrate that
was hghtly (15%) plant-covered. Foi+y-seven live speci-
mens of E. complanata and 6 L. radiata radiata were
found. Site 4 was sandy and moderatelv (50%) plant-
covered with 80 live .specimens of E. complanata, 5 L.
radiata radiata, and 1 A. undulata. Site 5 at the Agawani
River outflow was choked with macrophytes amidst oc-
casional spots of bare sand. Although not measured, cur-
rent flow was estimated to be higher than in the other
Table 2. Sampling results: samples taken, species, and specimen number obtai
ned m sur\e\s o
f Half\vav Pond, Massachusetts.
Site
Locality
Samples
Species
No.
specimens
1 0.3 km S of Mast Rd., west bank
2 N end Mast Rd., northernmost shore
3 NW comer Island
Preserve
4 SW shore Island
Preser\'e
5 Agawam River outflow, SW corner
6 SW comer, at pumping station, NW of site 5
30
£, complanata
14
30
E. complanata
2
15
E. complanata
47
L. radiata radiata
6
15
E. complanata
80
L radiata radiata
5
A iindnlata
1
15
E ci>mplanata
22
L. radiata radiata
2
S. undulatus
1
P. cataracta
1
L. ochracca
1
15
E. complanata
31
Page 82
THE NAUTILUS, Vol. 114, No. 2
sun^eyed areas in the pond. Maximum depth was less
than 1 m. Twenty-two specimens of E. coinplaiuita. 2 L.
radiata radiata, 1 S. iiiuhdatus, 1 P. cataracta. 1 un-
known juvenile mussel, and the only specimen of the
target species, L. ochracca. from the entire survey, were
found. The water on survey site 6 was cloudv; the bot-
tom at this site was lightly covered with plants and sandy.
Thirty-one specimens plus 1 unknov^ai juvenile were
identified as E. complanata.
A total of 213 live specimens comprising 6 different
species were collected in 6 sites around the lake. AH
specimens showed evidence of shell dissolution, mostly
light wear (nacre exposed on 25% or less of the shell
surface). Mean specimen length for Elliptio coinphmata,
the only species collected in significant numbers for
analysis, was 76.2 mm (n = 191), although this figure is
most hkelv inflated due to bias in sampling methodology.
At sample site 5, the only area where the target species
was found, specimens of E. complanata were 11.6% larg-
er than in the other sites. In addition, the greatest di-
versity (5 species) was found at this site.
DISCUSSION
The density oi Lcptodea ochracca, is decreasing in Half-
way Pond. This study confirms general observations of
dechne over the past 15 years. The single specimen
found in this survey is the only documentation of the
existence of L. ochracca in Halfway Pond since 1981
when Doug G. Smith and A. E. Pratt, University of Mas-
sachusetts Museum of Comparative Zoology, collected
12 specimens (UMAMZ 5.39). Agricultural nmoff from
nearby cranberr}' bogs recently contributed to decreased
water clarity accompanied by fish kills and potential de-
crease in mussel densitv (Douglas G. Smith, personal
communication). Lcptodea ochracca is typically found at
low densities across its range in northeastern North
America (Smidi, 1991; Strayer et al, 1994; Strayer and
Smith, 1996; Strayer and Jirka, 1997). The single speci-
men represents 0.47% of all specimens found (n = 213).
Strayer ct al. (1994) found onlv 33 in their study of the
Hudson River estuary in eastern New York and report
the species constituting appro.ximately 5% of the unionid
community of over one biUion animals. Repeated sam-
phng of the same area in 1993-1995, subsequent to ze-
bra mussel (Drcisscna polipiu>if)ha (Pallas, 1771)) inva-
sion, resulted in only 16 specimens found. At the time
of this studv (1995), zebra mussels had not reached Half-
way Pond.
The Lcptodea ochracca found in this stucK' was in the
pond outflow in an area of high benthic macrophyte cov-
er and sandy substrate that is typical habitat for this spe-
cies (Johnson, 1947; 1970). Increased species diversih-
in this area (5 of 6 total) and increased mean length of
the most common species, Elliptio complanata, supports
the prevision that the outflow area is a vital microhabitat
for freshwater mussels in Halfway Pond. Increased den-
sities of other freshwater mussel species (Nalepa and
Gauvin, 1988) and filter-feeding insects (/Vllan, 1995;
142) have also been observed at other lake outflows. Fa-
vorable conditions may include increased nutrient flow
across mussel ctenidia induced by the increased stream
flow, or protection from fish and mammal predators
amidst the macrophvtic plants.
Whatever the cause, the Agawam Ri\er outflow area
is an important refugial microhabitat for the continued
survival oi Lcptodea ochracca in Halfway Pond. The out-
look for this species in the pond, however, is not good.
With such a low density, reproductive potential may not
be high enough to maintain a population. Surveys of sim-
ilar areas in other coastal ponds should be conducted
and appropriate protective measures taken if L. ochracca
is to remain as a species of special concern or upgraded
to endangered status in Massachusetts.
LITERATURE CITED
Allan, ]. D. 1995. Stream Ecolog\'. Stnicture and Function of
Running Waters. Cliapman and Half London, 388 pp.
Bereza, D. J. and S. L. H. Fuller. 1975. Notes on "LampsiUs"
ochracca (Say) (Mollusca; BivaMa). Association of South-
eastern Biologists Bulletin 22:42.
Johnson, R. I. 1947. Lampsilis cariosn Say and Lampsilis
ochracca Say. Occasional Papers on Mollusks 1:14.5-1.56.
Johnson, R. I. 1970. The systematics and zoogeography of the
Unionidae of the southern Atlantic slope region. Bulletin
of the Museum of Comparative Zoologv 140:26.3—449.
Livingston, T. (ed.) 1987. Massachusetts and Rhode Island Pre-
serve Guide. Nature Conservancy Press, Boston, 56 pp.
MDFW (Massachusetts Division of Fisheries and Wildlife).
1997. Massachusetts list of endangered, threatened, and
special concern species. 321 CMR 10.60. Natural Heri-
tage and Endangered Species Program, Massachusetts Di-
vision of Fisheries and Wildlife, Westborough,
Morrison, J. P. E, 1975. Maryland and Virginia Mussels of List-
er. Bulletin of the American Malacological Union for
1974:.36-.39.
Nalepa, T. F and J. M. Gauvin. 1988. Distriljution, abundance,
and biomass of freshwater mussels (Bivalvia: Unionidae)
in Lake St. Clair. Journal of Great Lakes Research 14(4):
411-419.
Peckarsky, B. L., P. R. Fraissinet, M. A. Penton and D. J. Conk-
lin. Jr 1990. Freshwater Macroinvertebrates of North-
eastern North America. Cornell University Press, Ithaca,
442 pp.
Smith, D. G. 1991. Keys to the Freshwater Macroinvertebrates
of Massachusetts, v. 1.2. Universih' of Massachusetts
Press, Amherst, Massachusetts, 236 pp.
Smith, D. G. 1981. Selected freshwater invertebrates proposed
for special concern status in Massachusetts. Massachusetts
Department of Environmental Quality Engineering, Di-
vision of Water Pollution Control, Westborough, 26 pp.
Strayer, D. L., D. C. Hunter, L. C. Smith and C. K. Borg,
1994. Distribution, abundance, and roles of freshwater
clams (Bivalvia: Unionidae) in tlie freshwater tidal Hudson
River Freshwater Biology 31:239-248.
Strayer, D. L. and K. J. Jirka. 1997. The Pearl Mussels of New
York State. The New York State Education Department,
New York, 113 pp.
Straver, D. L. and L. C. Smith 1996. Relationship between
zebra mussels (Dreissena polipnorpha ) and unionid clams
J. Cordeiro, 2000
Page 83
(liiriiii; the earlv stages of tlie zebra mussel imasiiiii dlllic
Hudson Rh'er. Fresliwater Biolog)' 36:771-779.
Turgeon, D. D., J. F. Quinii |r., A. E. Bogan, E. \'. Coan, F.
G. Hochberg, VV. G. Lyons, P. M. Mikkelsen, R. J. Neves,
C. F E. Roper, G. Rosenberg, B. Roth, A. Sche'ltenia, F.
G. Tlionipson, M. Vecchione and W'ilhanis, ]. D. 199S.
Common and Scientific Names of Aquatic In\ertel)rates
troni the United States and Canada: Molhi.sks. 2nd. Edi-
tion. American Fisheries Society Special P\iblication, Be-
thesda, 509 pp.
Williams, J. D., M. L. Warren Jr, K. S. Cummings, J. L. Harris
and R. J. Neves. 1993. Consen'ation status of freshwater
nnissels of the United States and Canada. Fisheries 18(9):
6-22.
In Memoriam
Ruth D. Turner Rudolf Stohler
1914-2()()() 1901-2()()()
THE NAUTILUS 114(2):84, 2000
Page 84
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THEt7NAUTILUS
CONTENTS
.^ '^^^ Vb/u/JK? 114, Number 3
°°'''''°"'-September5,2000
ISSN 0028-1344
Phylogeny of some gastropod mollusks derived from 18S
rDNA swquences with emphasis on the Euthyneura 85
Size-depth patterns in two bathyal turrid gastropods:
Benthoinangelia antonia (Dall) and Oenopota ovalis
(Friele) 93
Four new genera for northeastern Pacific gastropods 99
ObscuraneUa papyrodcs, a new genus and species ot
abyssal tonnoidean gastropod from Antarctica 103
Host-tree selection by Florida tree snails, Liguus fasciatus
(Miiller, 1774), in Big Cypress National Preserve, Florida,
USA 112
The development of three heterobranch mollusks from
California, USA 117
Diminishing species richness of mollusks in Oneida Lake,
New York State, USA 120
Sook Hee Yoon
Won Kim
Alisabet J. Clain
Michael A. Rex
James H. McLean
Yuri L Kantor
M.G. Harasewych
Robert E. Bennetts
Steven A. Sparks
Deborah Jansen
Rachel Collin
Willard N. Harmann
THE NAUTILUS 114(3):84-92, 2000
Page 85
Phylogeny of some gastropod mollusks derived from 18S rDNA
sequences wdth emphasis on the Euthyneura
Sook Hee Yoon
Department ot Biological Sciences
College of Natural Sciences
Sung Kmui Kwan University
Suwon 440-746, KOREA
Won Kim'
Department of Molecular Biology
College ot Natural Sciences
Seoul National Universitv'
Seoul 151-742. KOREA'
W()nkim@plaza.snu.ac.kr
ABSTRACT
The phvlogenetic relationships among gastropod subgroups,
with emphasis on the Euthviieura, were investigated through
the analyses of nearly complete ISS rDNA sequences of 29
representati\e gastropods. Neighbor-joining, maximum-likeli-
hood, and maximum-parsimonN' methods were used ni the con-
stniction of phvlogenetic trees. The 18S rDNA data support
the monophyK' of Vetigastropoda, the \etigastropod clade Tro-
choidea, and Caenogastropoda. However, the monophylies of
two caenogastropod subgroups, Neotaenioglossa and Neogas-
tropoda, are not supported. The basal position of Neritopsina
is confirmed. Within the Euthyneura, the Stvlommatophora
and the Systellommatophora are monophyletic, but the Opis-
thobranchia, the Pulnionata, and the Basonnnatophora are not.
The present study supports the inclusion of Succineidae within
Stylommatophora. However the phylogenetic position of Sys-
tellommatophora within Gastropoda remains unresolved.
Additional key words: Mollusca, molecular phylogeny, Apo-
gastropoda, Caenogastropoda, Opisthobranchia, Pulnionata,
Vetigastropoda, Stylommatophora, Basonnnatophora, Systel-
lommatophora, Archaeopulmonata.
INTRODUCTION
Of the molluscan classes. Gastropoda is the most diverse
and the most ubiquitous group. It has successfully adapt-
ed to most habitats, including marine, freshwater, and
terrestrial emdronments.
Many comparative studies were published based on
morjDho-anatomical characters, including those of shell,
pallial complex, and nervous, reproductive, and digestive
systems (for recent reviews, see Haszpnmar, 198Sa; Bie-
ler, 1992; Ponder and Lindberg, 1997). However, the
status of knowledge of the phylogenetic relationships
among and within the gastropod subgroups is still con-
troversial (e.g., Golikov and Starobogatov, 1975; Gra-
ham, 1985; Haszprunar, 1988a; Bieler, 1992; Ponder and
Lindberg, 1996; 1997). This uncertainty is largely due to
the lack of informative morphological characters com-
' Author for correspondence.
men to the different taxa and the presence of the high
level of phenotvpic diversity observed in the Gastropoda.
In atkUtion to moiphological characters, molecular se-
quences have proven to be very useful for in phyloge-
netic reconstructions. 18S rDNA sequences are amongst
the most informative molecular characters along a broad
range of taxa within the Mollusca (e.g., Steiner and
Miiller, 1996; Winnepenninckx ct al., 1996; Winnepen-
ninckx ct a]., 1998a; Winnepenninckx et al., 1998b; Ada-
mkewicz ct al., 1997; Bargues and Coma, 1997; Canapa
ct al., 1999) and other animal phyla. Several studies were
pubhshed on the molecular phylogeny of Gastropoda
based on the sequence data of 28S rDNA (Rosenberg
ct al, 1994; 1997; Tillier ct al.. 1994; Tillier et al, 1996)
and 18S rDNA (Winnepenninckx ct al, 1996; Winne-
penninckx ct al. 1998a; Harasewych et al, 1997a; b;
1998). Winnepenninckx ct al recently (1998a) investi-
gated the phylogeny of gastropod groups below the class
rank using the complete 18S rDNA sequences from 18
gastropod species.
To further address gastropod phylogeny with empha-
sis on Euthyneura (Opisthobranchia + Pulnionata), a
group that has not been examined or discussed in detail
from 18S rDNA data, we determined the complete 18S
rDNA sequences for five representative gastropods.
They include the first complete sequence data from Ce-
phalaspidea (within Opisthobranchia) and Archaeopul-
monata (within Pulnionata), and additional sequence
data from Vetigastropoda and Stylommatophora (this lat-
ter within Pulmonata). These sequences were analyzed
in conjunction with previously published sequences of
24 other gastropotls. We focus on testing the monophyly
of each of the euthvneuran subgroups, the Opisthobran-
chia (e.g., Boettger,' 1955; Ghisehn, 1965; Gosfiner, 1981;
1985; 1991; Goshner and Ghisehn, 1984; Pouhcek et al,
1991; Ponder and Lindberg, 1997), the Basommatopho-
ra (e.g., Tilher, 1984; Haszpnmar and Huber, 1990;
Nordsieck, 1992), the Stylommatophora (e.g., Nord-
sieck, 1992), and the Systellommatophora (Salvini-Plaw-
en, 1980; Chnio, 1980; Tilher, 1984; Haszpnmar and
Huber, 1990; Nordsieck, 1992). We also discuss the phy-
Page 86
THE NAUTILUS, Vol. 114, No. 3
logenetic position of the Succineidae in the Stylomma-
tophora (Rigby, 196.5; Solem, 1978; Tillier, 1989; Nord-
sieck, 1992). In addition, we examine the monophylies
of the Vetigastropoda (Salvini-Plawen, 1980; Salvini-
Plawen and Haszprunar, 1987; Haszprunar, 1988a; b;
Ponder and Lindberg, 1996) and the vetigastropod clade
Trochoidea (Haszprunar, 1988a).
MATERIALS AND METHODS
Specimens An,\lyzed
The 188 rDNA sequences of two vetigastropods (Nor-
dotis disciis, 1858 base pairs, from Cheju Island and Ba-
tilhis comutus, 1859 base pairs, from Mara Island), one
opisthobranch {Bidlacta cxarata, 1849 base pairs, from
Inchon), and two pulmonates {EUobium chinensis, 1845
base pairs, from Tamjin River, and Acusta dcspccta sie-
boldiana, 1847 base pairs, from the Campus of Seoul
National University). The material above was collected
in Korea, and their sequences are described for the first
time in the present study. The sequences of two neo-
gastropods (Rapana venosa and Rcishia bronni), one
pulmonate (Antliosiphonaria .siriti.s), and one chiton
(Lcpidozona (Lcpidozona) corcanica) were reported in
our previous study (Yoon et al, 1996) and the sequences
of the remaining 21 other gastropods and 2 bivalves
were obtained from GenBank.
The nearly complete 18S rDNA sequences were an-
alyzed for the 29 representative gastropods (one neri-
toid, three vetigastropods, nine caenogastropods, two
opisthobranchs, and 14 pulmonates). two bivalves, and
one chiton species. Of these, the poK-placophoran Lcp-
idozona {Lcpidozona) corcanica was used as an out-
group, as the class Polyplacophora (included in the Acu-
Ufera) is currently accepted as the stem group of the
classes Gastropoda and Bivalvia (included in Conchi-
fera), from studies based on morphological characters
(see Salvini-Plawen, 1980; 1990; Haas, 1981; Runnegar
and Pojeta, 1985; Brusca and Brusca, 1990; Ponder and
Lindberg, 1996) as well as molecular results (Adamke-
wicz et al, 1997; Bargues and Mas-Coma, 1997; Hara-
sewych et al, 1997b). Table 1 Usts the studied taxa and
GenBank accession numbers for the respective sequenc-
es. The baseUne classification used in this work follows
Haszprunar (1988a) for Streptoneura, Vaught (1989) for
Opisthobranchia, and Boss (1982) for Pulmonata.
DNA Extraction, PCR Amplification, and
Sequencing
Total nucleic acids were extracted from foot muscle of
hve-collected and ethanol-preserved snails bv modifica-
tions of standard procedure of Sambrook et al (1989).
The 18S rDNAs were amphfied using the polymerase
chain reaction (PCR) with two oUgonucleotide primers
corresponding to conserved sequences proximal to 5'
and 3' termini of metazoans (Nelles ct al, 1984: 1-19,
5'-CCTGGTTGATCCTGCCAG-3'; 1848-1868, 5'-
TAATGATCCTTCCGCAGGTTA-3': the numbers cor-
Table 1. Gastropod species used in the present study, with
GenBank accession nvuiihers for sequences.
NERITOPSINA
NERITOIDEA
Neritidae
Nerita albicilla X91971
VETIGASTROPODA
HALIOTOIDEA
Haliotidae
'Nordotis disais
AF082177
TROCHOIDEA
Trochidae
Monodoiita labia X94271
Turhinidae
'Btitillus comutus
AF 16.5.3 11
CAENOGASTROPODA
NEOTAENIOGLOSSA
LITTORINOIDEA
Littorinidae
Littorina littorea
X91970
Nodilittorina punctata
Y11755
CALYPTRAEOIDEA
Calvptraeidae
Crepidula adunca
X94277
TONNOIDEA
Bursidae
Bursa rana X94269
NEOGASTROPODA
MURICOIDEA
Muricidae
Reishia bronni X98827
Rapana venosa X98826
Buccinidae
Pisania striata X94272
Nassariidae
Nassarius singuijorensis
X94273
Fasciolariidae
Fasciolaria lignaria
X94275
EUTHYNEURA
OPISTHOBRANCHIA
CEPHALASPIDEA
PHILINOIDEA
Haniineidae
'BuUacta exarta
AF 18867.5
APLYSIOMORPHA
APLYSIOIDEA
Aplysiidae
Aphisia sp. X94268
PULMONATA
ARCHAEOPULMONATA
ELLOBIOIDEA
Ellobiidae
'EUobium chinensis
AF190452
BASOMMATOPHORA
SIPHONARIOIDEA
Siphonariidae
Anthosiphonaria sirius
X98S28
Siplionaria algesirae
X91973
LYMNAEOIDEA
Lviunaeidae
Ltjmnaea glabra Z739S2
Bakerihpnnaea ctibensis
Z83831
STYLOMMATOPHORA
MEASURETHRA
CLAUSILIOIDEA
Clausihidae
Balea biplicata X94278
HETERURETHRA
Succineidae
Oxijloma sp. X94276
Omalomjx matheroni
AF047199
Athoracophoridae
Athoracophonis bitenta-
culatus AF047198
SIGMURETHRA
ACHATINOIDEA
Achatinidae
Limicolaria kambcxd
X66374
HELICOIDEA
Bradvbaenidae
'Acusta despecta sieboldi-
ana AF190453
Hehcidae
Helix aspcrsa X91976
SYSTELLOMMATOPHO-
RA
ONCHIDIIOIDEA
Onchidiidae
Oncliidella celtica
X70211
VERONICELLOIDEA
X'eroniceUidae
Laevicaulis alte X94270
Note: Classification follows Haszimniar (1988a) for Strepto-
neura, Vaught (1989) for Opisthobranchia, and Boss (1982) for
Pulmonata. " New sequences marked with asterisk.
S. H. Yoon and W. Kim, 2()()()
Page 87
respond to positions of liunian ISS rDNA). PCR ampli-
fications were performed with Taij DNA pol\merase for
30 cycles (94° C for 1 min, 52° C for 2 min, and 72° C
for 3 min). The ends of the amplified DNA fragments
were modified for blunt-ended ligation using T4 kinase
and T4 polymerase. The hlunt-endeil 18S rDNAs were
hgated into pGEM-3zf(-) plasmid vector and trans-
formed into DH5-a cell fines. Sequencing primers used
in this study were reported in a previous paper (Moon
ct «/., 1996). ISS rRNA-coding regions were completely
sequenced in both directions with complete overlap. The
DNA sequencing was performed by the dideoxynucleo-
tide ch;iin-termination method (Sanger ct al., 1977) us-
ing a Taq-Track kit (Promega Co.), accorcfing to the
manufacturer's instructions. Eli'ctrophoresis of sequenc-
ing reaction mixtures was periormed on butler-gradient
6% polyacrylamide gels and examined by autoradiogra-
phy.
Piivi,ck;enetic Analysis of 18S rDNA Sequences
The sequences were initially aligned with the CLUSTAL
W multiple-aUgnment program (Thompson ct al., 1994)
and the alignment refined manualK'. A data-set of align-
ment-stable positions was produced by excluding those
positions that differed between alignments (Gatesy cf aZ.,
1993). Analyses were limited to refiablv aligned regions,
which included a total of 1754 nucleotide positions. Phv-
logenetic reconstructions were performed using the
neighbor-joining (NJ), maximum-likelihood (ML), and
maximum-parsimony (MP) methods. PHYLIP version
3.572c (Felsenstein, 1995) was used for the neighbor-
joining (Saitou and Nei, 1987) analyses. The distance
analyses were done using Kimura (1980) and Jukes and
Cantor (1969) matrices as input for the neighbor-joining
analyses. Maximum-likelihood analvses were performed
using the HKY (Hasegawa ct al. 1985) model in PAUP
4.0b2 (Swofford, 1999). For the quartet puzzling meth-
od (the number of puzzling steps is 1000), empirical nu-
cleotide frequencies, and transition/transversion ratio of
1.5 were estimated. Parsimony analvses were also per-
formed using the computer program PAUP version
4.0b2 with closest stepwise addition options. The anal-
yses employed a heuristic search using TBR branch
swapping with random taxon addition. Branch length
was optimized according to the ACCTRAN option.
Bootstrap analyses (Felsenstein, 1985) of one hundred
rephcates were performed to examine the confidence of
nodes in NJ, ML, and MP analyses.
RESULTS
Figure lA shows the phylogenetic tree resulting from
the neighbor-joining (NJ) analysis using the Kimura
(1980) distances of an alignment of complete 18S rDNA
sequences of 29 gastropod species. The polyplacophoran
Lepidozona (Lcpidozoua) corcanica was used as out-
group. The same tree topology was also obtained using
Jukes and Cantor (1969) distances. The Neritoidea
branches off first and the Vetigastropoda (Trochoidea -I-
Haliotoidea) diverges next as an independent clade be-
fore the clade Apogastropoda (Caenogastropoda + Eu-
thvTieura). The monophyly of the Vetigastropoda and its
subclade the Trochoidea (represented by Monodonta
and BatiUus) is clearly shovvni in the tree, with ven' high
boostrap support (100%: 100%). The Caenogastropoda
shows a sister group relationship with the Euthyneura
with very high bootstrap support (94%). Monophyly of
the Caenogastropoda is supported (boostrap value =
100%), though neither the Neotaenioglossa (= Meso-
gastropoda) nor the Neogastropoda emerged as mono-
phyletic clades.
There is strong bootstrap support (100%) for the
monophvlv of Euthviieura (Opisthobranchia + Pulmon-
ata), though the monophyhes of Opisthobranchia (Ce-
phalaspidea + Anaspioidea) and Pulmonata are not sup-
ported. The Basommatophora, consisting of the Siphon-
arioidea and Lymnaeoidea, did not emerge as a mono-
phyletic group. On the other hand, there is good support
for the monoph)'fies of hvo additional groups in the Eu-
thyneura, the Stylommatophora (boostrap value = 84%)
and the Systellommatophora (boostrap value = 87%).
Bootstrap values strongly support the position of the
Succineidae (Oxi/loma and Omalonijx) within the sty-
lommatophoran clade. However, the position of the Sys-
tellommatophora within the Gastropoda was not posi-
tively determined in the present study.
The resulting tree from maximum-fikefihood (ML)
analyses of the same data set is shown in figure IB. The
ML tree confirms all the major results of the NJ tree
(figure lA), with the exception that clades within Eu-
thyneura lack significant bootstrap-support. The new
branching order of Systellommatophora {Onchidclla and
Laevicaulis) , Aplysiomoipha (Aplijsia), Archaeopulmon-
ata (E//oi>((/)7()-Siphonarioidea {Siphonaria and Antho-
siphonaiia), Cephalaspidea (BuUacta). and Stvlomma-
tophora in the clade chffers from the order shouni in the
NJ tree (figure lA), Aplysiomoipha-Svstellommatopho-
ra-Siphonarioidea and Archaeopulmonata-Cephalaspi-
dea-Stylommatophora.
The maximum parsimony (MP) analyses produced a
single tree with minimum length of 950 steps (figure
IC). Generally speaking, MP analyses also yielded sim-
ilar results except for minor differences in topologies
among groups within the caenogastropod and the euthv-
neuran clades. Maximum parsimony shows topological
shifts within the caenogastropod clade, e.g., the new
branching order of Bursa, Na.ssariiis, and Pisania-Fas-
ciolaiia-Crcpidiila instead of the order shown in the NJ
tree (figure lA), Crcpidida, Bursa, Pisania, Nassarius,
and Fasciolaria. Within the Euthviieura, the MP tree
differs from the NJ tree only in those branching points
\vith low bootstrap values. There is no sister-group re-
lationship among the Cephala.spidea [BuUacta). Aply-
siomorpha {Aphjsia), Archaeopulmonata (Ellohium), Si-
phonarioidea, Stvlommatophora, and Systellommatopho-
ra.
Ne.xt, we focused on the Euthvneura in separate.
Page 88
THE NAUTILUS, Vol. 114, No. 3
KHlTl
Omalonyx
Athoracophorus
Oxyloma
r^Limicolaria
^ Helix
Acusta
Bullacta
— Ellobium
ZT Anthosiphonaria
Siphonaria
'gj~ Onchidelta
•evicaulis
Aplysia
100 t—tymnea
Bakerilymnea
Fasciolaria
Nassarius
Pisania
Bursa
Crepidula
Rapana
■j^Reishia
{r^Litlorina
— Nodilittorina
I
100
Siylommatophora
Pulmonata
Cephalaspidea Opisthobranchia
Archaeopulmonata
J Basommatophora
J Systellommalophora
Aplysiomorpha
J Basommatophora
Neogastropoda
J Neotaenioglossa
J Neogastropoda
J Neotaenioglossa
Nerita
[r~ Placopeclen
Chlamys
Lepidozona
^Balii
' fl
Monodonta
Batillus
Nordotis
Pulmonata
Opisthobranchia
Pulmonata
Caenogastropoda
Euth /neura
Vetigasiropoda
Nentopsina
J Bivalvia
Polyplacophora
Apogastropoda
B
11 I An
^' I — LimUolaria
Helix
Acusta
Balea
Omalonyx
Athoracophorus
Oxyloma
Bullacta
Antbosiphonaria
Siphonaria
Ellobium
Aplysia
Hj — Onchidella
— iMevicaulis
J Lymnaea
— Bakerilymnea
Fasciolaria
Nassarius
Pisania
Bursa
Crepidula
U Rapana
— Reishia
Lj Littorina
— Nodilittorina
Monodonta
Batillus
Nordotis
Nerita
91
Omalonyx
Athoracophorus
Oxyloma
Limicolaria
Helix
Balea
Acusta
A nrhosiphonaria
Siphonaria
Onchidella
iMevicaulis
Bullae Ui
Aplysia
Ellobium
Lymnaea
Bakerilymnea
Crepidula
Fasciolaria
Pisania
Nassarius
Bursa
Rapana
Reishia
Littorina
Nodilittorina
Monodonta
Batillus
Nordotis
Nerita
Placopecten
Chlamys
Lepidozona
Figure 1. A. Neighbor-joining tree detemiined by an alignment ol 29 nearly complete 18S rDNA sequence data for gastropods
witli Lepidozona coreanica (Polvplacophora) as outgroup. Bootstrap percentages are shown abo\'e branches supported in at least
50% of 100 replicates. B. Strict consensus tree resulting from maximum-likelihood analyses of :29 nearly complete gastropod 18S
rDNA sequences. Quartet puzzling method and HKY (Hasegawa et al, 1985) setting model were used. Lepidozona coreanica
(Polyplacophora) was the outgroup. Bootstrap analysis was performed with 100 rephcates; values above 50% are indicated above
the nodes. C. Strict consensus tree of maximum parsimony analyses based on the 333 informative sites of an alignment of 29 nearly
complete gastropod 18S rDNA sequences (length = 950; CI = 0.6611; RI = 0.8418). Lepidozona coreanica (PoKplacophora) was
die outgroup. Bootstrap values higher than 50% are indicated above the nodes.
IIJU|
LI Placopecten
^~ Chlamys
Lepidozona
— 1
c
(.}
551
1
_ 85 1
6i
1
"1
1
100 1
85
1
54
74
57
97
<»
"l
1
81,
100
100
1
100 1
1
mainly because the use of outgroups that are too far
removed from the elade in studv mav give origin to ad-
ditional homoplasies between ingroup and outgroup spe-
cies. Figure 2A shows the results of NJ analyses of 16
nearly complete euthyneuran 18S rDNA sequences,
with the caenogastropod Littorina littorca as outgroup.
The resulting tree exhibits the same topology as the
complete NJ tree (figure lA), with the exception that
Ellohiitm (Archaeopulmonata) becomes the sister group
to the clade Aplysiomoq^ha (Aphfsia) + Systellomma-
tophora-Siphonarioidea, instead of clade Cephalaspidea
(Bullacta) + Stvlommatophora, as present in the com-
S. H. Yoon and W. Kim, 2000
Page 89
0.01
~NodUittorina
~Littorina
3ol
84
88 pOma/on^ijr
'"*' ' Alhoraco^horus
Oxytoma
' Balea
_ Limicolaria
so"
Helix
■Icuito
Bullacta
% [~Antbosiphonaria
Siphonaria
Oncbideila
icaulis
—Aplysia
'Ellobium
^PQ[ Lymnaea
Bakerilymnea
hrA
I Ont/i
taeii
Styloninialophora
Cephalaspidea Opisthobranchia
Basomniatophora
Systellommalophora
Aplysiomorpha Opisthobranchia
Archaeopulmonala -
Basomniatophora
Pulmonata
Ncotacnioglossa
Limicolaria
Helix
Acusta
Balea
Omalonyx
Arhoracophorus
Oxyloma
Bullacta
A nthosiphonaria
Siphonaria
Aplysia
Onchidella
Laevicaulis
Ellobium
Lymnea
Bakerilymnea
Nodilittorina
Littorina
" Omalonyx
' Athoracophorus
' Oxyloma
" Limicolaria
' Helix
' Balea
~ Acusta
' Anthosiphonaria
~ Siphonaria
~ Lymnaea
~ Bakerilymnea
~ Onchidella
~ Laevicaulis
~ Aplysia
~ Ellobium
- Bullacta
~ Nodilittorina
- Littorina
Figure 2. A. Euthviieuran neighbor-joining tree detennined by an alignment of 16 nearly complete euth>Tieuran 18S rDNA
sequences, using Littorina littorea (Caenogastropoda: Littorinidae) as outgroup. Numbers at a node indicate bootstrap \alues higher
than 50%. B. Euthyneuran maximum-likelihood tree detennined by an ahgnment of 16 nearly complete euthyneuran 18S rDNA
sequences, using Littorina littorea (Caenogastropoda: Littorinidae) as outgroup. Quartet puzzling method and HKY (Hasegawapf
ai. 1985) setting model were used. Bootstrap values above 50% are indicated above the nodes. C. Euthyneuran maximum parsimony
tree calculated from the 149 infomiative sites of an alignment of 16 nearly complete euthyneuran 18S rDNA sequences, using
Littorina littorea (Caenogastropoda: Littorinidae) as outgroup (length = 415; CI = 0.7494; Rl = 0.6750). Only bootstrap values
higher than 50% are indicated.
plete NJ tree. These two clades are not supported by
bootstrap analysis of the euthyneuran clade. When the
euthyneuran ML tree (figure 2B) is compared to the
entire ML tree (figure IB), small topological shifts are
discernible. The Siphonarioidea shows a sister group re-
lationship with Aplysiomorpha (Aplysia) instead of with
Archaeopulmonata {Ellobium), and this Siphonarioidea-
Aplysiomorpha cluster appears as sister group of the Sys-
tellommatophora instead of Cephalaspidea-Stylomma-
tophora. However, bootstrap values that support these
nodes are very low. Nevertheless, the euthyneuran ML
tree strongly supported most of the major nodes found
in the entire ML tree, with generally higher bootstrap
values. Maximum parsimony analyses based on the 149
phylogenetically informative characters of the alignment
of 16 euthyneuran species produced a single tree with
minimum length of 415 steps (figure 2C). In the euthy-
neuran MP tree, the first branching member is Cepha-
laspidea (Bullacta) rather than Lymnaeoidea (Basom-
matophora) found in the entire MP tree. The topologies
Page 90
THE NAUTILUS, Vol. 114, No. 3
for the remaining taxa are generally identical to the ones
in the tree containing all taxa. The euthyneuran trees
resulting from NJ, ML, and MP analyses confirmed the
topology of trees generated from the same types of anal-
yses but based on all ta.xa.
DISCUSSION
For the phylogenetic relationships among and within the
gastropod major subgroups, our study supports several
aspects of the studv bv Winnepennickx ct al. (1998a).
The Neritoidea diverged first, followed by the Vetigas-
tropoda. Next, the clade Apogastropoda, comprising the
Caenogastropoda and Euthyneura (each well supported
as monophyletic groups), appears as a monophyletic
group. However, the Neotaenioglossa (= Mesogastro-
poda) and the Neogastropoda (included in Caenogastro-
poda) and the Pulmonata (included in Euthyneura) do
not appear as monophyletic groups. In addition, the po-
sition of Systellommatophora within the Gastropoda
could not be defined in the present study.
In contrast to previous reports, our study provides
more details on gastropod phylogeny, especially with re-
gard to the phylogenetic status of the subgroups within
the Euthyneura. All trees resulting from NJ, ML, and
MP analyses refute the monophyly of the Opisthobran-
chia. This result supports the claims of many opistho-
branch workers, whom observed that parallelism and
convergence ha\'e occured in most major organ systems
within the opisthobranchs (Ghiselin, 1965; Gosliner,
19S1; 1985; 1991; Gosliner and Ghiselin, 1984; Pouhcek
et al, 1991) and that the high degree of homoplasy in
many characters in opisthobranchs contribute to diffi-
culties in obtaining robust results from cladistic analyses
(Goshner and Ghiselin, 1984; GosHner, 1985; 1991).
Boettger (1955) maintained that the Opisthobranchia is
paraphyletic. Ponder and Lindberg (1997) also suggest-
ed that the Opisthobranchia is not monophyletic, a \dew-
point in agreement with the results of TiUier ct al. (1994)
from 28S rDNA data. It is not surprising, therefore, that
many contradictory phylogenies and classification
schemes have been suggested for the Opisthobranchia
(e.g., Boettger, 19.55; Taylor and Sohl, 1962; Ghisefin,
1965).
In relation to the phylogeny of the Pulmonata, we
have mentioned that the Basommatophora {scmtt Ha-
szprunar and Huber, 1990, Siphonarioidea -I- Lymnaeo-
idea), is not monophyletic. Tillier (1984) considered that
only Lyinnaeoidea belongs to Basommatophora and Si-
phonarioidea to Archaeopulmonata. He suggested that
pulmonates radiated into freshwater habitats as Basom-
matophora and into marine habitats as Archaeopulmon-
ata. Tillier et al. (1996), based on 28S rDNA data,
showed that the Basommatophora is not monophyletic.
However, Haszprunar and Huber (1990) suggested that
both Siphonarioidea and Lymnaeoidea could be allocat-
ed in Basommatophora due to the presence of common
morphological characters such as a procerebrum com-
prising only large cells, the lack of a contractile pneu-
mostome, and the presence of an osphradium and pallial
ciliary tracts. Nordsieck (1992) based on the presence of
an anal opening shifted to the posterior mantle lobe, also
considered the marine Thalassophila (Siphonarioidea) to
be the sister group of the limnic Hygrophila (Lymnaeo-
idea). Therefore, the common morphological characters
found in the Basommatophoran, rather than represent-
ing synapomoiphies, could all have been derived by con-
vergence. Nordsieck (1992), based on morphological
characters found in tentacles, kidney, central nervous
system, and aspects of ontogeny, considered the SKlom-
matophora to be a monophyletic group, which is con-
cordance with the results derived from 28S rDNA se-
quence data (Rosenberg et al, 1994; 1997; TilUer ct al,
1994; Tillier ct al, 1996). Although there is instability of
branching pattern, the results for the euthvnieuran clade
in the present study indicate that the Succineidae (rep-
resented by Oxijloma and Omalomfx) belongs to the Sty-
lommatophora (e.g., Solem, 1978; Tillier, 1989; Nord-
sieck, 1992). These results, however, contradict the view
of Rigby (1965) whom, on the basis ol moq^hological
similarities of the digestive and reproductive systems, al-
located the Succineidae in the Opisthobranchia. Syna-
pomorphic characters such as the more or less reduced
shell and mantle, and a visceral ganglion situated cen-
trally or on the left side with respect to the axis of the
central nervous system (e.g., Salvini-Plawen, 1980;
Nordsieck, 1992) support the monophvlv of the Systel-
lommatophora (represented by Onchidudae and Veron-
icellidae). However, this monophyly has been questioned
by several authors (e.g., Chmo, 1980; Tilfier, 1984; Ha-
szprunar and Huber, 1990). Climo (1980) in particular
considered the systellommatophorans as a polyphyletic
assemblage diverging at the base of the euthvmeurans.
Tillier (1984) studied the morpho-anatomical characters
of the pallial complex, digestive tract, reproductive, and
central nervous systems, and divided the Pulmonata into
only three orders; Archaeopulmonata, Basommatophora,
and Stylommatophora. He included the Systellommato-
phora in the Archaeopulmonata and suggested that the
Onchidudae (within Systellommatophora) is more close-
ly related to the Ellobiidae (within Archaeopulmonata)
than to the VeroniceUidae (within Systellonunatophora).
However, our present result supports the monophyly of
Systellommatophora.
Since the erection of the Vetigastropoda by Salvini-
Plawen (1980), the presence of .synapomorphic charac-
ters such as ctenidial sense organs, the epipodial sense
organs, and the special structure of the esophagus have
generally supported the monophyly of this clade (Sal\'ini-
Plawen and Haszprunar, 1987; Haszpnmar, 1988a; b;
Ponder and Lindberg, 1996; 1997). Other vetigastropod
features include the dominant presence of the right dor-
soventral retractor muscle, the right excretory organ, and
bilamellate ctenidia with skeletal rods. Previous molec-
ular data using partial 18S rDNA (Harasewvch ct al,
1997a; b) and' the 28S rDNA (Tillier ct a/.,' 1994) se-
quences also supported the monophyly of the Vetigas-
tropoda, which is also supported in the present study.
S. H. Yoon and W. Kim. 2000
Page 91
Moiioplnlv of the Trochoidea (represented by Mono-
chmta and Batillus) is also confirmed herein. The Tro-
choidea is defined hv SNiiapomoqihies such as loss of the
right ctenuhum in relation to the loss of the shell slit
(Haszpnniar, IBSSa; h) and the nionophvK' ol the gronp
is also in concordance \\'ith the stud)- based on 28S
rDNA sequences by TilUer et al. (1994).
In conchision, the ISS rDNA data stronglv support
the monoph\l\ of the following higher gastropod clades:
Vetigastropoda, Trochoidea (within Vetigastropoda),
Apogastropoda, and the two included clades Caenogas-
tropotla and Euth\meura. Within the euthyneuran clade,
both the Stslommatophora and the Systellommatophora
are monophyletic. However, our 18S rDNA data failed
to support monophyly of the Neotaenioglossa and the
Neogastropoda (within Caenogastropoda), Opisthobran-
chia, Pulmonata, and the puhnoTiate Basommatophora.
These non-monophvletic subgroups, therefore, at pre-
sent can be considered as grades rather than clades. The
basal position of Neritopsina is confirmed in this study.
In addition, the Succineidae is included in Stylomma-
tophora. Still, the Svstellommatophoran position within
the Gastropoda, that is, its immediate relationship to ei-
ther Opisthobranchia or Pulmonata, or to any other
group for that matter, could not be defined. The insta-
bility of topology and short branch lengths within the
Caenogastropoda and the Euthyneura may be due to the
fact that the mollusks, including gastropods, apparently
rachated in an "explosive" fashion during a relatively
short period of time. Most extant major groups of mol-
lusks appeared around a relatively short time at the Pre-
cambrianyCambrian boundary (e.g., Runnegar and Po-
jeta, 19S5; Winnepenninckx et al, 1996; Adamkewicz ct
al. 1997; Harasewych ct al, 1997a). Futtire studies at-
tempting to define phylogenetic relationships at these
levels may take into consideration other molecules such
as cytochrome c oxidase I and/or 16S rDNA. Such mol-
ecules evolve more rapidly than 18S rDNA, and seem
more likelv to contain information needed to solve phy-
logenetic relationships within these clades.
ACKNOWLEDGMENTS
This work was supported bv a grant from KOSEF (95-
0401-04-01-3) for years 1995-1998. We thank Dr. B. L.
Choe, Mr. J. L. Lee (Sung Kyun Kwan University, Ko-
rea), Dr. J. S. Lee (Kang Won University, Korea), and
Mr D. G. Min (Shell House, Seoul, Korea) for providing
specimens. We are also indebted to Dr. C. B. Kim (Yale
University, USA) and Dr. J. K. Park (University of Mich-
igan, USA) for providing many references. We thank Ms.
D. W. Jung (Seoul National University) for proofreading
the manuscript. Special thanks are due to Dr. S. Y. Moon
(University of Koln, Germany) for her assistance in soft-
ware analyses. We are especially grateful to Dr. S. Y
Moon and to Dr. M. G. Harasewych (Smithsonian In-
stitution, Washington, USA) for their comments and
suggestions.
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THE NAUTILUS 114(3):93-98, 2000
Page 93
Size-depth patterns in two bathyal turrid gastropods:
Benthomangelia antonid (Dall) and Oenopota ovalis (Friele)
Alisabet J. Clain
Department of Biologv'
UiiiversiU' of Massachusetts, Boston
100 Morrissev Boulexard
Boston, MA 02125 USA
Michael A. Rex'
Department of Biology
Uni\ersit\' of Massachusetts, Boston
100 Morrissev Boulexard
Boston, MA 02125 USA
nnchael.rexCffumb.edu
ABSTRACT
During the past decade, there has been a resurgence of interest
in the evolutionars' and ecological significance of animal body
size. Geographic patterns of body size in deep-sea organisms
remain poorly described. In this paper, we analyze depth-re-
lated trends of larxiil and adult shell size in two turrids (Gas-
tropoda) from the western North Atlantic. The upper bathyal
Oenopota ovalis (478-2022 m), which has non-planktotrophic
de\elopment, shows significant positixe size-depth clines for
laryal. but not adult shells. The lower bathyal Benthomangelia
antonia (2359-3834 ni), with planktotrophic development,
shows no trend for lan'al shells, but a positive relationship of
size to depth for adult shells. The increase in size with depth
confirms earher obser\'ations of size-depth clines in deep-sea
snails, which may reflect selection for greater competitive abil-
it\' and foraging efficiency with increased depth. Contrasts in
clina! \ariation between lar\al and adult shells suggest that dif-
ferent stages of life history in deep-sea snails may respond in-
dependently to environmental gradients.
Additional key words: Gastropoda, Turridae, deep sea, size-
depth patterns, western North Atlantic.
INTRODUCTION
Animal body size has been related to a wide range of
physiological (Peters, 1983; Chown and Gaston, 1999),
evolutionary (Stanley, 1979), and ecological phenomena
(LaBarbera, 1989). There is also considerable new in-
terest in the imphcations of body size for geographic
range (Brown, 1995), species diversity (Finlay et al.,
1996; Nee and Lawton, 1996), abundance (Siemann et
al, 1996) and conservation of biodiversity (May, 1988;
Marquet ct al, 1990; Gaston and Blackbum, 1996). One
of the most striking characteristics ot the deep-sea fauna,
including moUusks, is the small size of most organisms.
Explanations for this have centered primarily on mea-
suring size-depth trends in various deep-sea t;L\a or func-
tional groups, and relating these to food availability,
which decreases with depth (Thiel, 1975, 1979; Gage
' Author for correspondence.
and Tyler, 1991). Size-depth relationships appear to vary
considerably among faunal components (Rex and Etter,
1998). It is unclear the degree to which this inconsisten-
cy represents biologically meaningful differences in how
organisms respond to environmental gradients, or meth-
odological differences associated with how size is mea-
sured and the way that morphologically and taxonomi-
cally heterogeneous groups of species have been com-
bined to obtain composite estimates of size. To study
size as an adaptation, it is important to standardize mea-
surements to common growth stages and to examine pat-
terns within species (Gould, 1969; Rex and Etter, 1998).
Rex (1979) and Rex and Etter (1990, 1998) showed
that size, standardized to specific larval and adult growth
stages within individual deep-sea snail species, shows a
strong tendency to increase with depth. These studies
were based on average interpopulation size differences
using relatively few sampling sites, often located near the
extremes of the species' depth ranges. Here, we present
detailed analy,ses of size-depth trends in populations of
two species of deep-sea snails, using larger sample sizes
and much more thorough depth co\'erage. Results gen-
erally support the positive size-depth trends reported
earlier, but also suggest that larxae and adults may re-
spond differently to selective differences associated with
change in depth.
MATERIALS AND METHODS
This study focuses on two common and taxonomically
well-known bathyal turrids, Benthomangelia antonia
(Dall, 1881) and Oenopota ovalis (Friele, 1877), showni
in figures 1^. They were collected from the western
North Atlantic, south of New England (table 1, figure
5), using epibenthic sleds (Hessler and Sanders, 1967),
box cores (Hessler and Jumars, 1974), Blake deep-sea
trawls or beam trawls (Tanner, 1897). The two species
were chosen primarily because they were abundant
enough in existing collections to allow reasonable statis-
tical analyses across broad depth ranges.
B antonia and O. ovalis differ in their mode of de-
Paee 94
THE NAUTILUS, Vol. 114, No. 3
Figure 1. SEM of the adult shell of Oenopota ovalis (Station
87, 1102 m, 4.01 mm total length). Figure 2. SEM of the
adult shell of Bcnthoinanoelia antonia (Station 76, 2862 m,
6.51 mm total length). Figure 3. SEM of the larval shell of
Oenopota ovalis (Station 87, 1102m, 0.45mm protoconch
height). The indentation before the first readily detectable
adult rib (at a magnification of .30x) was used as the lanal-
adult transition (see text for further discussion). Figure
4. SEM of the larval shell oi BenthomangeUa antonia (Station
76, 2862 m, 1.18 nun protoconch height). Horizontal arrow
indicates the lar\al-adult transition (see text for further discus-
sion).
velopnient (Bouchet and Waren, 1980). O. ovalis ap-
pears to haw direct or leeithotrophic development in
which larvae mature in a protected egg capsule and ei-
ther emerge crawhng or undergo a brief pelagic or de-
mersal dispersal phase (e.g., Thorson 1935, 1944;
Bouchet and Waren, 1980; Shimek, 1983). In B. antonia.
larvae hatch at a small size and develop planktotrophi-
cally. Veligers evidently undergo ontogenic vertical mi-
gration in the water column, and consequentlv have
more dispersal potential than do the laivae of O. ovalis
(Killinglev and Bex, 1985). An increa.se in the proportion
of species that have planktotrophic development with
increased depth seems to be a general pattern in deep-
sea turrids of the western and eastern North Atlantic
(Potter and Bex, 1992).
Mollusks are useful for this tvpe of study because their
calcareous shells record the hfe history of each inchvid-
ual, and are not subject to the changes in form that are
caused by preservation in soft-bodied organisms. We
40° -
38°
36
207 73
N13.
^ W3
.••62
N4_
N10 _r--> •^084
2041* 2569 <^
»2037 ^/ "^
/
340
'*\ -.^"
L-1-^
2714
,95 - -
'-'2038
74°
72°
70°
68°
66°
64°
Figure 5. Map of Northwest Atlantic showing the localities
of collection stations. See table 1 for station data. Depth con-
tours are in meters. Diamonds represent stations where Oen-
opota ovalis was collected; circles represent sites for Benthom-
anoelia antonia.
chose only specimens that were collected hve. Measure-
ments of size were standarchzed to the transition be-
tween laival and adult shells (figures 3 and 4). If this
was undetectable due to erosion or breaking, the spec-
imen was not used. In B. antonia, the transition is clearly
marked by changes in bodi color and sculpture (Bouchet
and Wart^n, 1980; Bex and Etter, 1990). In O. ovalis,
both larvae and adults are heaviK- calcified ami are the
same white color making the transition less chstinct. The
protoconch is smooth and the adult shell has fine vertical
ribs. We used the indentation before the first readily
detectable adult rib as the lar\'al-adult transition for this
species.
Shells were measured microscopically, orienting them
by the method described in Bex and Etter (1990). Each
shell was mounted on a disk of clav and then placed on
a 4-diniensional stage of an Olvmpus dissecting micro-
scope equipped with a Sony 3 CCD Color Video Camera
mount. The camera was attached to a NuVista Imaging
Board in a Macintosh Centris 650 computer. Using
NuVista Capture+ Software, the images of the mounted
shells were digitized. The saved images were then load-
ed into the NIH Image program. Previously digitized
images of a 1.0 mm stage micrometer with 0.01 mm
gradations were used to calibrate and measure the shell
images.
Size-depth trends in the two species were analv^zed
using three variables: standardized lar\al, and adult size,
and estimates of final size attained. EarK' protoconch
whorls for one species, B. antonia. were often corroded,
making it impossible to accurately measure protoconch
height in all specimens. Consequentlv, larval size was
taken as protoconch width. Standardized adult size,
hereafter referred to as Whorl- 1 Size, was measured as
A. J. Clain and M. A. Rex, 2000
Pa^e 95
Table 1. Station data for samples of O. ovalis and B antonia measured in this stud\. Tlie species collected, sampling nietliodolog)-,
and number of specimens used in this study are also given. For sampling method: ES = epibenthic sled (Hessler and Sanders,
1967), BC = box core (Hessler and Jumars, 1974), BT = beam trawl, DSf = Blake deep-sea trawl (Tanner, 1897). ACSR indicates
Atlantic Continental Slope and Rise Study (Maciolek et ai, 1986).
i:).-|)tli
Saiiiplins:
.Number of
Species
Station
Cruise
1 m '
Latitude °.\'
Longitude ° W
method
indi\iduals
Oenopota ovalis
88
Ch.mn
478
39°54.10'
70°37.00'
ES
3
96
Cn.\iN
498
39°55.20'
70°39.50'
ES
3
N4
ACSR
550
40°21.17'
67°.32.18'
BC
1
207
Chain
808
.39°51.15'
70°55.35'
ES
6
87
Chain
1102
.39°48.70'
70°40.80'
ES
29
NIO
ACSR
1220
39°48.10'
70°05.30'
BC
2
N13
ACSR
1250
39°48..35'
70°54.94'
BC
1
N13
ACSR
1250
39°48.35'
70°54.94'
BC
1
7.3
Atlantis
1400
39°46.50'
70°43.30'
ES
15
103
Chain
2022
39°43.60'
70°37.40'
ES
8
BenthomangeUa
2084
Albatross
•7.3,59
40°16.S3'
67°05.25'
BT
4
antonia
62
Atlantis
2496
39°26.00'
70°33.00'
ES
1
2096
Alb.atross
2654
39°22.33'
70°52.33'
BT
3
2221
Alb.^tross
2789
39°05.50'
70°44.50'
BT
9
76
Chain
2862
39°38..30'
67°57.80'
ES
23
72
Atlantis
2864
38°16.00'
71°47.00'
ES
12
64
Atlantis
2886
38°46.00'
70°06.00'
ES
10
2174
.\lb.atross
2915
38°15.00'
72°03.00'
BT
3
2041
Albatross
2941
39°22.83'
6S°25.00'
DST
5
2716
Alb.atross
2983
38°29.50'
70°57.00'
BT
14
2037
Alb.^tross
3166
38°53.00'
69°23.50'
BT
3
2569
Albatross
3259
39°26.00'
68°03.50'
BT
2
.340
Knorr
3310
38°16.00'
70°21.55'
ES
13
2570
Alb.\tross
3316
39°54.00'
67°05.50'
BT
4
2714
Alb.\tross
3338
38°22.00'
70°17.50'
BT
4
2038
Albatross
3718
38°30.50'
69°08.42'
DST
3
95
Atlantis
3753
38°33.00'
68°.32.00'
ES
2
126
Atlantis
3806
39°.37.25'
66°45.50'
ES
18
"*"*
Chain
3806
38°00.70'
69°16.00'
ES
7
78
Chain
3828
. 38°00.80'
69°18.70'
ES
8
85
Chain
38.34
37°59.20'
69°26,20'
ES
8
the height plus width of the first post-lar\al whorl
(Gould,l969; Re.\ and Etter. 1990). Final size attained
by adults, hereafter referred to as Adult Size, was mea-
sured as the maximum height plus width of the post-
larval shell. Adult Size can not be standardized to a com-
mon de\elopment stage, because the species appear to
have indeterminate growth. The distribution of Adult
Size in a population reflects the recent history of re-
cruitment and growth more than size as an adaptive
property. To estimate the final size attained, we selected
the largest two indi\iduals (from anv station) found in
250 m depth increments. These three measures of size
(Protoconch Width, Whorl-l Size, and Adult Size at-
tained) were regressed against depth to anal\-ze bath\-
metric cUnal patterns.
RESULTS AND DISCUSSION
Relationships of size \'ariables to depth are showTi in fig-
ure 6. Regression fines are fitted onl\' for significant re-
lationships (see table 2 for regression equations and their
statistics). All significant regressions are positi\e, indi-
cating an increase in size with depth. There is no indi-
cation that size decreases significantly with depth for an\'
variable in either species. In O. ovalis, lanal size in-
creases with depth, but post-lar\'al stages show no pat-
tern. In contrast, B. antonia shows no relationship of
lar\-al size to depth, but both Whorl- 1 Size and .\dult
Size do increase with depth.
These results largeK" confinu those reported bv Rex
and Etter (1998) for B. antonia and O. ovalis. The pre-
sent study is more statisticallv accurate in that it includes
larger sample sizes, broader depth co\erage. and a much
more continuous distribution of samples across the
depth gradient. For Whorl-l Size, both studies detected
a strong positi\e increase with depth in B antonia and
no apparent trend in O. ovalis. For protoconch size. Rex
and Etter (I99S) reported a weaklv significant (p<0.051
increase with depth in B. antonia. and no relationship
in O. ovalis. \\ith more extensi\e sampling, the proto-
conch size-depth relationship becomes just insignificant
(p = 0.05S9) in B antonia. and strongly significant in
Page 96
THE NAUTILUS, Vol. 114. No. 3
1.50
1500
2000
2500
3000
3500
4000
Depth (m)
A. J. Clain and M. A. Rex. 2(K)()
Page 97
Tabic 2. Regression siuiiiiuin tor rclatioiisliips ol sr/.i- to dt-ptli in fiilure 6. For eacli regression, tlie niiiMt)er of iiuli\i(luals,
regression einiations, F-\'alues. r- \alues, ant! tlie sigiiitieanee are gi\en.
Number of
Significance
Measurement
Species
specimens
Regression equation
r*
F-\alue
(p)
Protoconcli widtli
B. antonia
156
Y = 0.982 + 2.69E - 5x
0.230
3.622
00589
Protoconch width
O. ovalis
69
Y = 0.6.39 + 4..54E - 5x
0.147
11.507
0.0012
Whorl 1 size
B. antonia
135
Y = 2.219 + 1.78E - 4x
0.106
15.850
0.0001
Whorl 1 size
0. ovalis
62
Y = 2.016 + 7.44E - 5x
0.046
2.863
0.0958
Adult size
B. antonia
156
Y = 7.644 + l.OOE - .3x
0.007
1.116
0.2925
Adult size
0. ovalis
69
Y = 5.171 - 2.S8E - .5x
0.000
0.010
0.9221
Largest adult
B. antonia
14
Y = 1.694 + 4.00E - 3x
0.332
5.963
0.0310
Largest ailult
O. ovalis
11
Y = 5.915 + 1.2.3E - 5x
0.000
0.001
0.9772
O. ovalis. Rex and Etter (1998) did not e.stiniate final
adult size. As with studies of biodiversity (Rex et al,
1997) and life-history characteristics (Stuart and Rex,
1994), the patterns in protoconch size that are revealed
with better sampling demonstrate the importance of us-
ing large databases, and broad continuous depth gradi-
ents to establish biogeographic patterns in the deep sea.
This is especiallv relevant for species like B. antonia that
show high variabihtv in shell architecture (figure 6).
It is interesting that O. ovalis, with non-planktotrophic
development shows a size-depth cline only for larvae;
whereas B. antonia with plankiotrophic development ex-
hibits no trend for larvae, but a significant positive cline
for Whorl- 1 Size that also persists at final size attained.
For B. antonia, an e.xplanation might be that larvae show
no pattern because they migrate from numerous distant
sites that may exert quite different selective regimes, and
that selection for size at settlement along the depth gra-
dients is not strong enough to overcome the mitigating
effects of dispersal. In this context, it is interesting that
larvae (and adults) of B. antonia show considerably more
variation in size than those of O. ovalis, possibly reflect-
ing multiple geographic origins for the former (figure 6).
Selection for increased size with depth may be imposed
largely during subsequent growth resulting in the posi-
tive size-depth cfine seen in adult shells of B. antonia.
The nature of the relevant depth-related selective gra-
dient remains unk-nown. Rex and Etter (1998) suggested
that the decrease in nutrient input with depth may select
for larger size because of its metabolic and competitive
advantages.
The opposite pattern observed in O. ovalis is difficult
to interpret in a consistent way. Larger size at hatching
may confer advantages of lower vulnerabifity to preda-
tors, greater locomotion to forage, a greater range of
food, and more abilitv to withstand star\'ation (Spight,
1976). However, the absence of a size cfine at adult stag-
es is puzzUng. In general, the results do indicate that
different life stages can respond differently and inde-
pendently to environmental changes associated with
depth. Since the species live at different depths, a geo-
graphically controlled comparison is not possible. Also,
because we are analyzing just two species, the results
may represent idiosyncratic effects that are phenotypic
plastic responses or phvlogenetic constraints, rather than
general patterns that are related to selective gradients
and developmental modes.
In summary, the upper bathyal O. ovalis shows a sig-
nificant positive size-depth cfine for larvae, but not
adults. The lower bathval B. antonia reveals no depth-
related pattern for lai-val shells, but a significant increase
in size with depth for adults. The exact causes of these
opposing trends are necessarily speculative; but, the re-
sults do suggest that larvae and adults may respond dif-
ferently to selective gradients in species with contrasting
modes of development in the deep sea as they appear
to do in coastal moUusks (Pechenik, 1999; Pechenik ct
al, 1996). The increase in size with depth generallv sup-
ports earlier studies on geographic variation in deep-sea
gastropods (Rex and Etter, 1990, 1998; Rexet al., 1999).
However, detailed analyses of individual species high-
light the need for large databases and good sampUng
coverage throughout species' bathvmetric ranges to ac-
curately assess biogeographic patterns in deep-sea or-
ganisms.
ACKNOWLEDGMENTS
We thank Ron Etter Carol Stuart, John Ebersole, and
Rob Stevenson for reacfing drafts of the manuscript. Bill
Fowle for the SEMs and Jack Cook for the map of the
Northwestern Atlantic Ocean. Howard Sanders, Fred
Grassle, Nancy Maciolek, James Blake and Jerrv' Hara-
sewych helped provide the original material that was
Figure 6. Relationships of Protoconch Width (top), Whorl-1 Size (middle), and Adult Size (bottom) to depth in populations of
Oenopota ovalis (diamonds) and Benthoinan^i'lia antonia (circles) collected in the deep sea of the western North Atlantic. The
solid symbols in the Adult Size graph indicate the largest two individuals found in each 250 m interval. Lines indicate significant
regressions. See table 2 for regression statistics.
Page 98
THE NAUTILUS, Vol. 114, No, 3
measured and analv^zed here. This research was sup-
ported by the National Science Foundation Grant OCE-
9301687 to MAR, and by the University of Massachu-
setts.
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THE NAUTILUS 114(3):99-1()2, 2()()()
Page 99
Four new genera for northeastern Pacific gastropods
James H. McLean
Natural Histors' Museum of Los
Angeles Counh'
900 Exposition BKd.
Los Angeles. CA 90007 USA
jniclean@nhni.org
ABSTRACT
Four new genera for nortlieasteni Pacific Gastropoda are pro-
posed; V'elutinidae: Torcllivclutina. type species "Torellia" am-
monia Dall, 1919; Euliniidae; Subniso. type species "Chemnit-
zia" ranai de Folin. 1867; Turridae. Clathurellinae; Retidrillia.
tspe species "Suavodrillia" willctti Dall. 1919; Mangeliinae;
PcrimangeUa. t\pe species "Mangelia" intcrfossa Carpenter,
1864.
Additional kci/ words:
lutinidae.
Gastropoda, Euliniidae, Turridae, V'e-
INTRODUCTION
This is the third in a series of papers in which new gen-
era for northeastern Pacific gastropods are introduced
(see McLean, 1995a, b). I had prexaously indicated (Mc-
Lean, 1995a) that a checklist of the northeastern Pacific
gastropods was in preparation; however, as indicated in
McLean (1996: 2), I am preparing a more complete
work rather than a checklist. Taxa described here are to
be used in an illustrated rexasion of all shelled gastropods
of the northeastern Pacific, ranging from Arctic Alaska
and the Aleutian Islands to central I3aja Cahfomia, Mex-
ico. Description of these genera in advance of the book
allows for a more detailed treatment than will be pos-
sible in the larger effort. Further papers in this series
will describe genera in which the tyjie species or other
included species are new.
To distinguish original combinations for type species
of the new genera I am here using the convention of
placing all citations of original genera within quotation
marks. Illustrations are proxaded here for type species of
each new genus.
Although monotvpic genera are not encouraged in
phylogenetic classifications, I do not refrain from intro-
ducing a few such genera where necessarv-, allowing that
additional living or fossil species may yet be discovered
that would render those genera no longer monotypic.
Museum acronvms are: LACM, Natural History Mu-
seum of Los Angeles Counb,'; USNM, National Museum
of Natural History, Washington.
SYSTEM ATICS
Family Velutinidae Gray, 1840
Genus Torcllivclutina new genus
Type species: "Torellia" ammonia Dall, 1919 (Figure
1). The shriveled liolotvpe from offshore depths at the
Aleutian Islands, Alaska, was illustrated by Waren (1989:
16, fig. llf). A more recently collected, preserved spec-
imen from the Aleutian Islands is illustrated here.
Included species: The genus is monotypic.
Diagnosis: Shell large (to 30 mm diameter), apical
whorl depressed, profile nearly planispiral, of two rapidly
inflated whorls, calcareous layer lacking in large speci-
mens except for that which borders the apertural hp;
shell consisting of chitinous periostracum after attaining
3 mm diameter; protoconch with spiral sculpture (ac-
cording to original description of Dall); suture deep, um-
bilicus broad; mature surface composed of thick, chitin-
ous, colabral a.xial lamellae.
Remarks: Waren (1989: 16) examined the type spe-
cies for purposes of comparison with his then described
new genus and species Pscudotorcllia fragilis from Ice-
land. He illustrated the radula of "Torellia" ammonia
(op. cit., fig. IIC), which he found to agree with that of
other velutinid radulae, and reported that the operculum
and other trichotropine features are lacking. Although
Waren removed "T." ammonia from the trichotropid ge-
nus Torellia, and transferred it to the Velutinidae, he did
not assign it to a genus. Torellivehitina is therefore here
proposed for "T" ammonia. It differs from Pseudotorcl-
lia in not having a sohd calcified shell with spiral sculp-
ture and not having the large, projecting protoconch of
Pseudotorellia.
Because the calcareous layer is lacking, fresh speci-
mens of Torellivehitina ammonia should be retiiined in
fluid preservative and should not be dried, which results
in the shrinkage and buckling of the thick periostracal
layer.
Etymology: The name is a compound of the tricho-
tropid genus Torrellia and the velutinid genus Vclutirm,
Page 100
THE NAUTILUS, Vol. 114, No. 3
A
Figures 1^. T)pe species of new genera. 1. Torellivehttina ammonia (Dall, 1919), apertural and spire views. LACM 152281,
Kanaga Pass, between Kanaga Island and Tanaga Island, Andreanof Islands, Aleutian Islands, Alaska, 61 ni. Maximum diameter .30
mm. 2. Subniso rangi (de Folin, 1867). LACM 1972-38.7, Punta Penca, N of Bahia Potrero, Guanacaste Pro\., Costa Rica, 10 ni.
Length 3.2 mm. 3. Retidrillia willetti (Dall, 1919). USNM 216409, lectotype. Forrester Island, southeasteam Alaska, dredged.
Length 11.5 mm. 4. Perimangelia inferfossa (Carpenter, 1864). LACM 1959-13.42, Granite Creek, Monterey County, California,
10 m. Length 8.5 mm.
to emphasize that it represents a velutiiiid with the su-
perficial aspect of the trichotropid genus Torrellia.
Family Euhmidae Philippi, 1853
Genus Subniso new genus
Type species: "Chemnitzia" rangi de Fohn, 1867
(Figure 2). Type locality: Perlas Islands, Panama. Waren
(1992: 183) could not locate type material, but the spe-
cies was well figured bv de Folin and subsequently by
Waren (1992, figs. 17, 20-22, 25-27, 30, 31), so there is
little doubt as to its identity. The species occurs from
southern Baja Cahfomia, Mexico, to Ecuador.
Included species: Two species, the type species and
"Niso" hipolitcnsis Bartsch, 1917, for which the holotype
from Punta San Hipohto, Baja California, Mexico, was
illustrated by Emerson (1965, fig. 9) and Waren (1992:
figs. 19, 23, 24). Both species have previously been
placed in Niso Risso, 1826, bv Emerson (1965) and War-
en (1992).
Diagnosis: Shell small (length to 4 mm), slender
(length to breadth ratio 2.5-2.9), non-umbilicate, basal
angulation pronounced, coloration brown, without color
pattern.
Remarks: The two species of Subniso are unUke other
species of Niso in size, profile, and color. The two spe-
cies are small, non-umbilicate, and have a basal angula-
tion (strongly projecting in Subniso rangi) and a uniform
brown coloration. Waren (1992: 185) remarked: "Both
Niso hipolitcnsis and N. rangi are unusual among the
species of Niso in their small size, 3^ mm shell height,
whereas most species of the genus have a shell that is
10-30 mm high, occasionally even higher." Additionally,
I point out that Niso species are usually broadly umbil-
icate, except for the large N. atiilloi (Hertz and Hertz,
1982), usually not angulate at the base, and have color
patterns that may be banded or variegated. Taken to-
gether, these differences are sufficient to justify' generic
recognition of Subniso.
Waren (1992: 1S3) noted that a starfish host is known
for one Indo-Pacific species of Niso, but nothing is
known of the host echinoderm for the two species of
Subniso.
Etymology: The generic name combines the generic
name Niso, with the prefix sub-, to emphasize the small
size, compared to Niso.
Family Turridae Swainson, 1840
Subfamily Clathurelhnae H. and A. Adams, 1858
Genus Rctidrillia new genus
Type species: ' Suavodrillia" willetti Dall, 1919 (Fig-
ure 3). Type locality: Forrester Island, Southeast Alaska.
Until now the species has been unfigured (it was not
illustrated by Kosuge, 1972). The here selected lectotype
(Figure 7) is the largest (11.3 mm) of seven original syn-
type specimens in the type lot. The radular tooth of the
type species was figured by McLean (1971, fig. 114)
(from LACM 66-66, Graham Island, Queen Charlotte
Islands, British Columbia). A specimen from the Rae
Baxter collection in the LACM extends the distribution
to Akutan, Aleutian Islands (LACM 83-345. 263 m
depth).
J. H. McLean, 2000
Page 101
Included species: At least three species, the t\pe spe-
cies and two species from the northeastern Atlantic dis-
cussed and illustrated bv Bouchet and Waren (1980: 32)
in the genus Drilliola Locard, 1897: "D. " pntina (Wat-
son, 1881), and "D." megalacmc (Sykes, 1906).
Diagnosis: Shell profile with concave shoulder and
projecting peripheral carination below which base is
rounded and has strong spiral sculpture. Anal sinus on
concave shoulder, deep and broad. Axial sculpture ex-
pressed as nodes, strongest at peripheral carination,
more f;iintlv expressed on strong spiral cords of base.
Peripheral carination of early whorls at midvvhorl. Pro-
toconch paucispiral, with early development of periph-
eral carination. Radular tooth long, haqioon-like, with
broad base.
Remarks: The type species was described in the ge-
nus SiiavodriUia Dall, 1918 (tvpe species: "Drillia" kcn-
nicotti Dall, 1871), with which it shares the long har-
poon-like radular tooth. Dall (1921: 69) indicated doubt
that "S." willetti was congeneric by placing a question
mark preceding the genus. Differences are that Reti-
drillia iLillctti and the tvvo additional species here as-
signed to the genus are half the size of S. kcnnicotti, and
have sculpture that is axial and spiral, rather than strictly
spiral as in SiiavodriUia. The newly restricted Siiavod-
riUia is monot\pic for S. kcnnicotti, a species broadly
distributed in the north Pacific from Hokkaido, Japan,
the Kurile and Aleutian Islands, and the Gulf of Alaska
to Southeastern Alaska.
Bouchet and Waren (1980: 32) retained "a wide va-
riety of species" in Drilliola, including those that 'look
rather different but have a similar radula and opercu-
lum." They elected "to keep them in Drilliola rather
than placing them in any of the perhaps more similar,
but anatomically unkiiown genera hsted by Powell
(1966) in different subfamihes. ' Species tvpical of Dril-
liola are more slender than those of Rctidrillia and do
not ha\e the broad, excavated shoulder. The proposal of
Rctidrillia thus provides a genus with a type species hav-
ing knowii radular characters for the two species cited
by Bouchet and Waren (1980).
On shell characters, Retidrillia resembles species as-
signed to Plicisifrinx Sysoev and Kantor, 1986, in which
the radular tooth is of the modified wishbone t)pe, in-
dicative of the less derived turrid subfamily Cochlespi-
30-4). Synonym: "Man^elia" interlirata Stearns, 1872.
The species occurs from Clallnm County, Washington,
to Isla San Ceroninio, Baja Cahfomia, Mexico, based on
specimens in the LACM collection.
Included species: Two species, the type species and
the less familiar "Manficlia" nitcns Carpenter, 1864 (syn-
type figured by Palmer, 1958, pi. 28, fig. 1). It ranges
from Sonoma County, California, to Ensenada, Baja Cal-
ifornia.
Diagnosis: Shell relatively small and slender with
dominant axial sculpture, crossed by narrow spiral cords
of lesser strength. Protoconch of 1.5 whorls, strongly
projecting, smooth at first, developing fine spiral sculp-
ture after first half whorl, followed by weaker axials (ax-
ials more numerous than that of mature sculpture),
changing imperceptibly to adult sculpture.
Remarks: Earlier (McLean, 1978: 74), I placed the
type species of the new genus ("Mangelia" intcrfossa)
along with "Daphnclla" ftiscoligata Dall, 1871 in Clatli-
romangclia Monterosato, 1884. I now consider Clath-
romangclia (type species "Plcurotoma" grantiin Philippi,
1844; see Powell, 1966: 106) to be appropriate for two
species in southern Cahfomia: "Daphnclla" fuscoligata
and "Mangilia iClafhmmangclia)" rhi/ssa Dall, 1919.
These two species have coarse clathrate sculpture and
relatively low, paucispiral protoconchs.
Pcrimangclia differs from the two species of Clath-
romangclia in having numerous, narrow spiral cords
overriding the dominant axial ribs, rather than having
coarsely clathrate sculpture with nodes at intersections.
Protoconchs differ: the paucispiral protoconch of the
two species of Pcrimangclia is strongly projecting,
whereas the paucispiral protoconch of the two species
of Clathromangclia is much lower.
Etymology: The name combines the prefix pcri-
(near) with Mangelia Risso, 1826, one of die oldest gen-
era in the subfamily Mangeliinae.
ACKNOWLEDGMENTS
Photographic prints were made by Michael Eraser. I am
grateful to Lindsey Groves, Daniel Geiger, Anders War-
en, and a further anonymous reviewer for offering help-
ful suggestions.
Etymology: The name is a compound of rcti-, mean-
ing net, with reference to the axial and spiral sculpture,
and Drillia Gray, 1838, one of the earliest named of tur-
rid genera.
Subfamily Mangehinae Fischer, 1883
Genus Pcrimangclia new genus
Type species: "Mangelia" intcrfossa Caqienter, 1864
(Figure 4). Syiitypes were figured by Palmer (1958, pi.
27,' figs. 5, 6)' Also figured by McLean (1969; 1978, fig.
LITERATURE CITED
Bouchet, P. and A. Waren. 1980. Revision of the northeast
Atlantic bath\al and abyssal Turridae (Mollvisca, Gastro-
poda). Joiinial of Moiluscan Studies, Supplement 8:1-119.
Dall, W. H. 1919. Descriptions of new species of mollusks of
tlie family Turritidae from the west coast of America and
adjacent regions. Proceedings of the United States Na-
tional Museum, 56(2288): 1-86, pis. 1-24.
Dall, VV. H. 1921. Summary of the marine shellbearing mol-
lusks of the northwest coast of America, from San Diego,
Califoniia, to the Polar Sea, mostly contained in the col-
lection of the United States National Museum, with illus-
Page 102
THE NAUTILUS, Vol. 114, No. 3
tratdons of hitherto unfigiired species. United States Na-
tional Museum, Bulletin 112, 217 pp., 22 pis.
Emerson, W. K. 1965. The eastern Pacific species oiNiso (Mol-
lusca: Gastropoda). American Museum Novitates 2218:1-
12.
Kosuge, S. 1972. Illustrations of type specimens of molluscs
described bv William Healev Dall (Northwestern Pacific
gastropods). Special publication of the National Science
Museum, Tokyo, 29 plates and unpaged captions.
McLean, J. H. 1969. Marine shells of Southern California. Los
Angeles County Museum of Natural History, Science Se-
ries, no. 11, 104 pp.
McLean, J. H. 1971. A revised classification of the family Tur-
ridae, with the proposal of new subfamilies, genera, and
subgenera from the Eastern Pacific. The V'efiger 14:114-
130.
McLean, J. H. 1978. Marine shells of .southern California, Re-
vised edition. Natural Histors' Museum of Los Angeles
County, Science Series, no. 24, 104 pp.
McLean, J. H. 1995a. Four new genera for northeastern Pacific
prosobranch gastropods. The Nautilus 108:39-41.
McLean, J. H. 1995b. Three additional new genera and two
replacement names for northeastern Pacific prosobranch
gastropods. The Nautilus 108:80-83.
McLean, J. H. 1996. The Prosobranchia. In: P H. Scott, J. A.
Blake, and A. L. Lissner (eds.) Taxonomic atlas of the
benthic fauna of the Santa Maria Basin and western Santa
Barbara Channel. Volume 9. The MoUusca Part 2 — The
Gastropoda. Santa Barbara Museum of Natural History,
Santa Barbara, v -t- 160 pp.
Palmer, K. V. W. 1958. Type specimens of marine Mollusca
described by P. P. Carpenter from the west coast (San
Diego to British Columbia). The Geological Society of
America, Memoir 76, vi -I- .376 pp., 35 pis.
Powell, A. W. B. 1966. The molluscan families Speightiidae and
Turridae. Bulletin of the Auckland Institute and .Museum,
no. 5, 184 pp., 23 pis.
Sysoev, A. V. and Y. 1. Kantor. 1986. [New and rare abyssal
species of the tamilv Turridae (Gastropoda, Toxoglossa) in
the northern part of the Pacific Ocean.] Zoologicheskii
Zhumal, 65(10): 1457-1469. [In Russian]
Waren, A. 1989. New and little known Mollusca from Iceland.
Sarsia 74:1-28.
Waren, A. 1992. Comments on and descriptions of eulimid
gastropods from Tropical West America. The Veliger 35:
177-194.
THE NAUTILUS 114(3):103-111, 2000
Page 103
Ohscuranella papijrodes, a new genus and species of abyssal
tonnoidean gastropod from Antarctica
Yuri I. Kantor
A. N. Se\ertzov Institute of Problems
of E\oliition
Russian Academy of Sciences
Leninski Prospect 33
Moscow 117071, RUSSIA
kantor@malaco-se\in.msk.ni
M.G. Harasevvych
Department of In\ertel)rate Zoology
National Museum of Natural History
Smitlisonian Institution
Washington, DC. 20560-0118, USA
HanisevvTchS'nmnh. si.edu
ABSTRACT
The new genus Ohscuranella and O. papijrodes. its type spe-
cies, are described from the abyssal plain off the Ross Sea,
Antarctica. Obsntranella is included in the primarily tropical,
shallow water superfamiK Tonnoidea because it has a taenio-
glossan radula, extensible proboscis, large sali\'arv glands com-
posed of anterior and posterior lobes, salixary ducts that pass
through die nerve ring, and an undifferentiated oesophageal
gland. This taxon is precluded from the families Laubierinidae,
Pisanianuridae, and Tounidae because it lacks a monopectinate
osphradium, paired proboscis retractor muscles passing
through the nerve ring, buccal glands, and rachidian teeth with
lateral basal denticles. Ohscuranella is assigned to tlie family
Ranellidae primarily on the basis of shell, radular, and oper-
cular morphology. This is the first report of the Tonnoidea in
Antarctic waters, and the first record of Ranellidae from abyssal
depths.
Additional key words: Caenogastropoda, Ranellidae, anatomy,
systemafics.
INTRODUCTION
In the course of examining Antarctic Buccinoidea sam-
pled under the auspices of the United States Antarctic
Program (USAP) and housed in the National Museum
of Natural Histoiy, Smithsonian In,stitution, we encoun-
tered five lots of gastropods with large bucciniform shells
that had tentatively been attributed to the buccinoidean
genus Bathijdomus Thiele, 1912, by Dell (1990:198-
199). Dell identified four of these lots as Bathiidomus
obicctus Thiele, 1912, but considered the filth lot, con-
sisting of a single specimen, to represent an undescribed
species of Bathijdomus. Dissections of preserved mate-
rial clearly demonstrate that these gastropods are not
referable to Buccinoidea, nor even to Neogastropoda,
but rather represent an unnamed genus and species of
the superfamily Tonnoidea. This is the first report of this
superfamily in the Antarctic nialacofaimu, UTid one of
very few records of the Tonnoidea from the abyssal zone.
The family Ranelfidae, to which this genus is assigned.
has not prcNitjusly been reported from die Antarctic or
from abyssal depths.
In this paper, we provide descriptions of this new ge-
nus and new species, and infer its taxonomic position
within the Tonnoidea by comparing its anatomy, radula
and operculum with published anatomical reports (e.g.
Weber, 1927; Houbrick and Fretter, 1969; Day, 1969;
Beu, 1981; Hughes and Hughes, 1981). Waren and
Bouchet (1990), Riedel (1995). and Beu (1998) each
provide useful, if not entirely congruent, syntheses of
tonnoidean families, and include anatomical descriptions
as well as numerous illustrations of radulae, opercula and
protoconchs. Abbreviations used in the descriptions of
morphometric characters are explained in Table 1.
SYSTEMATICS
Class Gastropoda CuNaer, 1797
Superfamily Tonnoidea Suter, 1913
Family Ranelhdae Gray, 1854
Genus OhsciirancUa new genus
Type species: Ohscuranella papijrodes new species
Diagnosis: Protoconch unknown. Teleoconch large,
pyriform, thin, with large aperture, single, rounded, un-
thickened terminal varix adjacent to thin, flared outer lip
in adult specimens. Shell sculpture limited to fine, wide-
ly spaced, spiral cords. Operculum very small, shaqily
tapering anteriorly, with anterior terminal nucleus. Pro-
boscis wall extremely thick, paired proboscis retractor
muscles absent. Rachidian teeth lacking lateral basal
denticles. Salivary glands large, differentiated. Osphra-
dium bipectinate.
Etymology: Ohscunis (L.) — obscure, unclear + Ra-
nclla — genus of Ranellidae.
Ohscuranella papijrodes new species
(Figures 1-36, Table 1)
Bathijdomus obtectus Thiele, 1912— Dell, 1990:198-199, figs.
299-300.
Page 104
THE NAUTILUS, Vol. 114, No. 3
Table 1. Obscuranella papifrodes. new species. Measurements of shell characters. Linear measurements in mm.
USNM
USNM
USNM
Character
Holotvpe
Paratype 1
Paratype 3
901317
870610
870610
Shell LensTth (SL)
63 +
58 +
33+
57.0
43.6+
33.2+
Last Whorl Len.^th (LWL)
55.2
51.8
28.5
47.3
38.5
30.4
Aperture Length (AL)
45.1
43.3
23.0
38.4
31.5
25.5
Shell Width (SW)
40.8
41.5
19+
34.1
24+
20.2+
Number of spiral cords on
last whorl
14
12
14
5
14
13
Number of spiral cords on
penultimate
whorl
6
7
7
2
5
3
Bathjdomns sp.— Dell, 1990:199.
Description: Shell large (exceeding 63 mm), very thin,
fragile, ovate-pvrifonin. Protoconch and upper whorls
missing in ;ill t\pe material. Preserved portions of teleo-
conch of 2V2 rapidly expanding, evenly rounded whorls.
Shoulder rounded, indistinct. Suture adpressed, shallow.
Axial sculpture limited to fine, straight, weakly prosocline
growth hues. Adult specimens with a single, weak, hollow
vailx adjacent to thin, flared outer Up (figures 2, 7, arrow).
Spiral sculpture of sharp, narrow, evenly spaced cords (14
on last whorl, 6 on penultimate whorl), with much weaker
sinuous threads (22-.30) of varying width between adja-
cent cords. Aperture large [—0.7 shell length (SL)],
broadly ovate, deflected from shell axis by 9-11°. Outer
lip tliin, evenly rounded in upper part and concave at
transition to siphonal canal, weakly reflected. Inner hp
consisting of long, convex, tnedially indented parietal re-
gion and short, smootli, a.xial columeOa with strong, long
siphonal fold that crosses cofling axis of shell. Siphonal
canal short, broad, weakly recurved dorsally. Callus of
thin, wliite, porcellaneous glaze overlying parietal region,
adapical portion of broad, nearly axial siphonal fasciole.
Shell color pale ohve-tan, confined to outermost shell lay-
er. Aperture white. Periostracum very thin, yeflowish
brown, with densely spaced a.xial lamellae, occasional
short hairs at intersection of lamellae with spiral cords.
Operculum (figures 4, 5) very small (0.16 AL), x'estigial,
dark yellow, subtriangular, with straight sides, terminal
nucleus. Dorsal surface with numerous, closely spaced
growth lines. Ventral surface with thin, glazed lateral mar-
gins. Operculum attached over most oi its surface.
Shell ultrastructure (Figure 23): Shell thin (101
|xm), composed of three layers. Outermost laver (figure
23, ca) thinnest (4 |xni), composed of columnar crystals.
Middle layer (figure 23, ccl) thickest (79 jjim), composed
of collabrally oriented cross-lameUar crystals. Inner layer
(figure 23, rcl) thin (IS p-m), composed of cross-lamellar
crystals oriented perpendicular to growing edge of the
shell.
Anatomy (Paratype 1, 9): Soft tissues comprising
appro.ximately 3V2 whorls. Mantle cavity spans just under
V2 whorl, nephridium (figures 24, 25, 27, n) about %
whorl, digestive gland (figures 24, 25, dg) 2V^ whorls.
Mantle edge (figures 24, 25, 27, me) thickened, smooth,
completely covers head. Columellar muscle (figure 25,
cm) thick, broad, spanning sUghtly more than one whorl,
attached to shell at rear of nephridium. Foot short in
contracted state (LengthAVidth == 1.0), with conspicu-
ous propodium. Body color uniform reddish-tan, without
pattern in alcohol preserved specimens. Head (figure 26)
very large, as wide as foot, with broad, blunt, tapering
tentacles (figure 26, tn) with black eyes at their bases.
Operculum about 4 mm long (0.09 AL), otherwise sim-
flar to that of holotvpe. Paratype 1 (and all other pre-
served specimens) with proboscis protruded through
very wide rhynchostome (figure 26).
Mantle cavity (Figure 27): Mantle cavity as deep as
broad (—Vi whorl). Siphon (figures 24, 25, 27, s) broad,
muscular, very short, extending shghtly beyond mantle
edge (figures 24-27, me). Osphrachum (figures 24—27,
os) situated along central half of ctenidiuni, bipectinate,
nearly symmetrical, sUghtly narrower on left side than
right. Ctenidium (figures 24-27, ct) long, spanning near-
ly entire mantle length, formed of tall triangular lamel-
lae, nearly twice as high as broad. Hvpobranchial gland
(figure 27, hg) poorly developed, lacking distinct folds.
Rectum (figure 27, re) runs along inner surface of palfial
oviduct, narrow, terminating in simple anus (figure 27,
a) behind thickened mantle edge.
Alimentary system (Figures 15, 19-22, 24, 32-35):
Everted proboscis (figures 24-26, pr) —30 mm long (0.7
AL), unpigmented, with folded walls indicating potential
for further extension. Proboscis wall very thick, —60%
Figures 1-14. Obscuranella papyrodes new species. 1. Apertural, 2. right lateral, and 3. dorsal views of the holotype, USNM
898683. 4. External and 5. internal views of the operculum of the holotype (internal view coated with Ammonium chloride to
emphasize sculpture). 6. Apertural and 7. dorsal views of paratype 1, USNM 896131. 8. Apertural and 9. dorsal views of the larger
shell, 10. dorsal view of smaller shell, USNM 870610. 11. Apertural and 12. dorsal views of paratype 3, USNM 886105. 13.
Apertural view and 14. apical view of early whorls of USNM 901317. Scale bar = 1 cm for all shells; Scale bar = 2 mm for
operculum; Scale bar = 5 mm for protoconch.
Y. I. Kantor and M. G. Hamsewvch, 2000
Page 105
Page 106
THE NAUTILUS, Vol. 114, No. 3
Y. I. Kantor and M. G. Harasew\'ch, 2000
Page 107
of proboscis radius, composed of 3 layers of muscles.
Innermost la\er of circular nuiscles (figure 32, cm), mid-
dle layer tliickest (2/3 of proboscis wall), of longitudinal
muscles (figure 32, Im), outer layer of circular muscle.
Buccal mass (figure 33, bm) small, attached to proboscis
walls b\ numerous, thin tensor muscles (figures 15, 32,
33, tm), as is the anterior oesophagus (figures 15, 32,
aoe). Retractor muscles passing through ner\'e ring and
joining buccal mass and columellar muscle absent.
Mouth (figure 32, mo) a narrow, vertical slit. Buccal tube
(figure 33, bt) short, leading to cuticle-lined buccal cavity
with ventral p;ur of semicircular jaws (figure 33, j). Jaws
(figures 16-18) dark brown, pappilate along outer edge
(figure 17). Inner surface of jaw composed of small,
closeK- spaced platelets that produce "coiibled" surface
distally (figure 18), smooth pro.ximally (figure 16). Odon-
tophore (figure 15, od) small, oval, lining bottom of the
buccal cavity. Walls of buccal cavity very thick. Proboscis
nerves (figure 32, pn) paired, very thick, nuining from
cerebro-pIeur;il gangfia along proboscis length, inner\'at-
ing buccal mass and anterior part of proboscis. Anterior
esophagus divided into dorsal and ventral channels by
prominent longituchnal folds (figures 15, 34, 35, If) that
extend from the buccal cavitv to the posterior edge of
esophageal gland. The right fold overlaps the left (figure
34). Radular ribbon (figure 19) short (5.8 mm, 0.13 AL),
nearly twice as long as cartilages, narrow (~ 580 |xm,
0.013 AL), consisting of 45 rows of teeth, posteriormost
4 rows nascent. Rachidian tooth (figure 21, rt) with large,
broad median cusp, flanked by 5-9 denticles per side.
Base broad, strongly concave posteriorly, lacking cusps
along tooth base. Lateral teeth (figures 21, 22, It) narrow,
with long, thin, cusp flanked by 3—4 denticles on inner
edge, 4—6 denticles on outer edge. Two long, recurved,
distally flattened marginal teeth (figures 20; 22, mt) per
side, outer tooth longer than inner Inner distal edges
serrated with 2-7 cusps. Salivarv' glands large, irregularly
shaped, completely covering the esophageal gland (fig-
ure 32, oeg). Right salivary gland more elongated, slight-
ly larger than left. Each gland consists of two lobes. Pos-
terior lobe (figure 32, plsg) massive, composed of curved
radially oriented bfind tubules. Anterior lobe (figure 32,
alsg) smaller, acinous, ventral. Salivary ducts (figures 32-
34, sd) thick, extending from posterior lobes, becoming
attached to oesophagus wafls before passing through
nerve ring. We were not able to identify connections
between the salivary ducts and the anterior lobes of the
salivary glands, as reported for Cymafium intermedium
(Pease, 1869) by Andrews ct al. (1999). Salivary glands
attached to oesophagus by thin muscular and connective
tissue fibers and innervated by several nei^ve branches.
Esophageal gland formed of deeply glandular dorso-ven-
tral folds, small relative to salivary glands, of the same
color as surrounding tissues and esophagus. Stomach
large, U-shaped, similar to that of Ci/mathiin nicolxiri-
cum (Houbrick and Fretter, 1969) in external moqihol-
ogy, too poorly preserved to reveal details of internal
morphology, except that the ducts of the digestive gland
are paired, closely spaced, and situated in the middle
region of the stomach. Posterior duct twice the diameter
of anterior duct. After leaving stomach intestine curves
dorsally, passing under then along posterior edge of ne-
phridium towards rear of mantle cavity (figures 24, 25,
m).
Female reproductive system (Figures 25, 27-30):
The only specimen dissected (Paratype 1) was a mature
female. Pallial oviduct consists of small albumen gland
(figure 25, ag) along outer wall of nephridium, large cap-
sule gland (figures 25, 27, eg) fining right wall of pallial
cavity. Lumen of capsule gland small anteriorly (figure
29), broad posteriorly (figure 28), at juncture to albumen
gland. No seminal receptacles were identified, possibly
due to poor fixation. Bursa copulatrix (figures 27, 29, 30,
be) large, long, spanning more than half length of cap-
sule gland. Pallial oxiduct opens (figures 27, 29, go) by
long, narrow slit at midlength.
Male reproductive system (Figure 31): The repro-
ductive system of a male specimen lacking shell (para-
type 2) was examined. Testes occupy upper half of
whorls of visceral mass above posterior border of stom-
ach, giving rise to seminal duct. Seminal duct forms
large, convoluted seminal vesicle before entering mantle
cavity. Duct descends to floor of mantle cavity at mid-
length, opening to form groove with thickened, obvious-
ly glandular walls leading to penis base. Penis (figure 31.
p) broad, dorsoventrally flattened, with seminal groove
(figure 31, sgr) nmning along inner edge, around the
bluntly rounded distal edge, halfvvay down the outer
edge, terminating in a verv small, inconspicuous papilla
(figure 31, pap).
Type locality: Victoria Land, Balleny Islands, Sturge
Island, RA' Eltanin. .st. 1949, 66252'S, 164a32'E, \n
2507-2525 m, 5 February 1967.
Type material: Holotype, USNM 898683 (figures 1-
5, shell and operculum only, soft parts not present), from
the type locahty; paratype 1, USNM 896131 (figures 6-
Figures 15-23. Obsairanella papijrodes new species. Parat\pe 1, USNM 8961.31. 15. Distal end of the proboscis opened dorsally.
16-18. Left jaw. 16. Entire inner surface of jaw. 17. Enlarged section of the upper edge. 18. Enlarged section of the surface in
the middle part of the jaw. 19-22. Radiila. 19. View spanning width of radular ribbon. 20. Left marginal teeth. 21. Rachidian anil
lateral teeth. 22. Right lateral and marginal teeth, tilted to .30°. 23. Ultrastnicture of the shell (Paratvpe 3. USNM 886105).
aoe, anterior oesophagus; If, lateral folds; od, odontophore; ca. columnar shell layer; ccl, comarginal crossed lamellar shell layer; j,
jaw; It, lateral teeth; mt, marginal teeth; r, radula; rcl, radial crossed lamellar shell layer; rt, racliidian tooth; tm, tensor muscles.
Page 108
THE NAUTILUS, Vol. 114, No. 3
ov
1 cm
Figures 24-31. Ohscuranella papijrodes new species. Paratope 1, USNM 896131. 24. Neutral and 25. dorsal news of animal
removed from the shell. 26. Antero-dorsal \iew of the head. 27. Mantle complex, opened from left side and reflected. 28-30.
Schematic sections through the pallial gonoduct. 31. Penis (Parat)'pe 2).
a, anus; ag, albumen gland; be, bursa copulatrix; eg. capsule gland; cm, columellar muscle; cnie, cut mantle edge; ct. ctenidium;
dg, digestive gland; go, genital opening; hg, hypobranchial gland; in, intestine; me, mantle edge; n, nephridiuni; no, nephrichal
opening; op, operculum; os, osphradium; ov, ovary; p, penis; pap, papilla; pr, proboscis; re, rectum; s, siphon; se, siphonal edge;
sgr, seminal groove; st, stomach; tn, cephalic tentacle.
Y. I. Kantor and M. G. Harasewvch, 2()()()
Page 109
5 mm
Figures 32-35. Obscitranella papijrodes new species. Anterior alimentary system, Paratype 1, USNM 896131 32. Proboscis
(opened ventrallv) and organs of cephalic haeniocoel. 33. Anterior part of the proboscis, opened ventrally. 34. Transverse section
through anterior oesophagus, viewed from anterior 35. Esophageal gland, opened dorsally. Dashed line indicates \entral midline.
alsg, anterior lobe of the salivary gland; ao, anterior aorta; aoe, anterior oesophagus; bm, buccal mass; bt, buccal tube; cm, circular
muscle layer of the proboscis wall; j, jaw; If, longitudinal fold of anterior oesophagus; !m, longitudinal nuiscle layer of the proboscis
wall; mo, mouth opening; nr, nerve ring; ode, odontophore caitilages; oeg, oesophageal gland; plsg, posterior lobe of the salivary
gland; pn, proboscis nerve; poe, posterior oesophagus; pw, proboscis wall; rs, radiilar sack; sd, salivary duct; tm, tensor muscles.
7, 9 pecimen, anatomical de.scription.s based on diis
specimen), paratype 2, USNM 896139 {6 specimen,
shell not present, male reproductive system based on
this specimen), both irom south of Hjort Seamount,
RA' Eltanin, stn. 1964, 59°5H'S. ISS^arW. in 29S5-2992
m, 10 February 1967; paratype 3, USNM 886105 (fig-
ures 11-12, sex undetermined) Victoria Land, south of
Scott Island Bank, IW Eltanin. stn. 1939, 69203'S,
I7904IE, in 3519-3.596 m, 1 February 1967.
Other material examined: USNM 901317 (Figs 13-
14, 1 specimen, sex undetermined) Victoria Land,
Moubray Bay, RA^ Eltanin. stn. 2002, 72218'S, 177e:35'E,
in 2005-2010 m, 11 January 1968; USNM 870610 (fig-
ures 8-10, 2 dead shells) Antarctic Peninsula, IW £/-
tanin, stn. 1003, 62^41S, 54243W, in 210-220 m, 15
March 1964.
Etymology: papijrodes — made from papyrus, refer-
ring to the thinness of the shell.
Remarks: The type series oi ObsciirancUa papijrodes,
n. sp., consists of lour specimens, incluchng one paratvpe
that lacks a shell. All were collected hving on the abyssal
Page 110
THE NAUTILUS, Vol. 114, No. 3
Figure 36. Geographic and bath\nietric distribution of Obsairnnelln papijrodes new species.
plain off the Ross Sea. We are provisionally attributing
three additional specimens to this species. One live-col-
lected specimen (figure 13; USNM 901317), also from
the abyssal plain off the Ross Sea, was considered by
Dell (1990:199) to be congeneric but not conspecific
with Obsctiranella papijrodes n. sp. (which he identified
as Bathi/domiis ohtcctus Thiele, 1912) because of its
more elongated shell, longer siphon;il canal, and angular
shoulder. Even the earliest teleoconch whorls of this
specimen appear angular because of a prev;ilent spiral
cord along the periphery. This is exaggerated by a break
in the shell and subsequent repair, evidenced bv a thick-
ened scar on the posterior part of the last whorl. The
elongated shell and prominent siphonal canal are fea-
tures shared with an immature paratvpe (paratype 3, fig-
ures 11-12) of O. papi/rodes. This is the only specimen
of Obscuranella with some portion of the earlv whorls
intact (figure 14). The protoconch (2.0 mm estimated
diameter) is eroded and replaced by a plug, but the ear-
hest teleoconch whorls are well preserved and clearly
show spiral cords.
Two dead collected shells (figures 8-10; USNM
870610), labeled as coming from upper slope depths
(210-220 m) off the Antarctic Peninsula, closely match
the moiphology of this new species. We regard these
specimens to represent O papijrodes, but are skeptical
of the accuracy of the locality data. Not only is this lo-
cation on the opposite side of the Antarctic continent
from all records of live collected O. papijrodes, it is also
from much shallower depths (220 m vs. 2000-1- m).
DISCUSSION
Ohscuraiudla can readily be attributed to the superfam-
ily Tonnoidea on the basis of its pyriform shell with large
aperture and conspicuous, if short siphonal canal; its ex-
tensible proboscis; its taenioglossan radula; its large sal-
ivarv glands composed of moqihologicallv differentiated
anterior and posterior lobes and sahvarv ducts that pass
through the nen'e ring, as well as its undifferentiated
oesophageal gland. It can be excluded from Ficidae,
which was removed from Tonnoidea and elevated to su-
perfamily status by Riedel (1994), by its high spire, lack
of long siphonal canal, and also because Ficidae is char-
acterized by small, tubular sali\arv glands. Similarly, it
can be excluded from Laubierinidae, a family diagnosed
by its monopectinate osphradium and excluded from
Tonnoidea by Bandel and Riedel (1994), by its nearly
symmetrical, bipectinate osphradium.
The shell of Obscuranella suggests an affinitv' with the
deep-sea family Pisanianuridae (originall)' proposed as a
subfamily of RanelHdae by Waren and Bouchet, 1990,
transferred to Laubierinidae by Bandel and Riedel,
1994, and elevated to family status by Beu, 1998) by
\irtue of its smooth shell lacking regular varices and
weakly defined anterior canal. The operculum of Pis-
anianiira is shghtly coiled but has a terminal nucleus, as
does Obscuranella. Howe\er, the rachidian teeth of Ob-
scuranella lack the lateral basal denticles present in Pis-
anianuridae (e.g. Waren and Bouchet, 1990:figs. 25-27),
Bursidae (e.g. Waren and Bouchet, 1990:figs. 6, 8), Ton-
nidae (e.g. Waren and Bouchet, 1990:figs. 9-14), and
Laubierinidae (e.g. Waren and Bouchet, 1990:figs. 41-
44), but absent in Cassidae (e.g. Waren and Bouchet,
1990:figs. 15, 16, 18), Personidae (e.g. Beu, 1998:fig.
15.140 E), and Ranellidae (e.g. Waren and Bouchet,
1990;figs. 28, 30, 32, 40).
The shell of Obscuranella somewhat resembles that of
Oocorijs sulcata Fischer, 1883 (Oocorythinae, Cassidae)
Y. I. Kantor and M. G. Harasewvch, 2000
Page 111
(see, eg. Bouchet aiu! W'aivii, 19y3:fig,s. 1936-1943), and
some ranellids, such as Ar^obticcinmn pnstulosuin
(Ughtfoot, 1786) (.see e.^. Beii, 1998:fig. 15.12 D). The
operculum of Obscuranella has a shaqjly pointed, ter-
minal nucleus, and differs from the spiralK' coiled oper-
culum of Oocon/s (W'aren and Bouciu't. 1990: fig. 66).
In adult Ai-fiobuccinuin the nucleus ot the operculum is
subcentnJ, hut in ver\' young specimens of A. pustulo-
siim (Waren and Bouchet, I990:fig. 69) the nucleus is
terminal. Howexer, the operculmn of Ohscuraiwlla is
distincti\e in its veiy small size, relatixe to the aperture,
and in having straight, anteriorly converging margins.
The anatomv of Obscuranella is tvqiicallv tonnoidean,
most closelv resembling that of the ranelliil Ci/inatiinn
(Houhrick and Fretter, 1969). Obscuranella can be dis-
tinguished anatomically from the Tonnidae by its lack of
a buccal gland, and from Pisaniamiridae and Laubierin-
idae hv its lack of long proboscis retractor muscles that
pass through the nen'e ring.
We assign this genus to the family Ranellidae because
of it general similaritx' to Arfiobucchuun in shell form,
radular moi-pholog\, and gross anatomy. Moreover, Ra-
nellidae is the onlv tonnoidean familv to occur in Ant-
arctic waters — Fusitriton ma^icllanicus (Roding, 1798), a
species with a wide geographic range, has been taken
from several stations in the Weddell and Ross Quadrants
(e.g. USNM S96058, USNM 896103, USNM 896277,
USNM 898520— see Polar Invertebrate Catalog http://
www.nmnh.si.edu/cgi-bin/wdlViz/pci/form). Obscuranel-
la papi/rodcs represents the first record of Ranelfidae
from abyssal depths.
ACKNOWLEDGMENTS
This study was supported by a USAP Research Program
Award from the Biological Collections from Polar Re-
gions at the National Museum of National History [Na-
tional Science Foundation (Office of Polar Programs)
Cooperative Agreement OPP-9509761]. We are grateful
to Drs. Alan Beu and Klaus Bandel for their constructive
reviews of this manuscript.
LITERATURE CITED
Aii(lrew.s, K. B., A. M. Page and ], 13. Taylor 1999. Tfie fine
.stnictiire and function of the anterior foregnt glands of
Ci/uuitiiim iiitenneclius (Cassoidea: Ranellidae). Journal of
\iolluscan Studies 6.5:1-19.
Bandel, K. and F. Riedel, 1994. Classification of fossil and Re-
cent CaKptraeoidea (Caenogastropoda) with a discussion
on neoniesogastropod phylogeny. Berliner geowissen-
schafdiche Abhandlungen (E) 13:329-367.
Beu, A. G. 1981. Australian gastropods of the family Bursidae.
Part 1. The families of Tonnacea, the genera of Bursidae,
and revision of species prexiously assigned to Tutufa Jous-
seaume, 1881. Records of the Australian Museinn 33:248-
324.
Beu, A.G. 1998. Superfamily Tonnoidea. In: Beesley, P L., G.
J. B. Ross and A. Wells (eds). MoUusca: The Southern
Synthesis. Fauna of Australia, volume .5, part B. CSIRO
Publishing, Melboum, pp. 792-803.
Bouchet, P. and A. Waren. 1993. Revision of the northeast
Atlantic hathyal and abyssal Mesogastropoda, Bolletino
Malacologico, Supplemento 3:.580-840.
Day, J. A. 1969. Feeding of the cvniatiid gastropod Argofci/c-
cintim argus, in relation to the stRicture and secretion of
the proboscis glands. American Zoologist 9:909-916.
Dell, R. K. 1990. Antarctic MoUusca. Bulletin of the Royal
Society of New Zealand 27:1-311.
Houhrick, J. R. and V. Fretter 1969. Some aspects of the func-
tional anatomy and hiologv' of Cipnatium and Bursa. Pro-
ceedings of the Malacological Society of London .38:41.5-
429.
Hughes, R. N. and H. R I. Hughes. 1981. Moiphological and
behavioural aspects of feeding in the Cassidae (Tonnacea,
Mesogastropoda). Malacologia 20:385—102.
Riedel, F. 1994. Recognition of the superfamily Ficoidea Meek
1864 and definiton of the Thalassocvniidae fam. nov. (Gas-
tropoda). Zoologische Jahrbiicher 121:457-474,
Riedel, F. 1995. An outline of cassoidean phylogeny (MoUusca,
Gastropoda). Contributions to Tertiary and Quateniary
Geolog)' .32:97-1.32.
Waren, A. and P. Bouchet. 1990. Laubierinidae and Pisanianu-
rinae (Ranellidae), two new deep-sea taxa of the Tonno-
idea (Gastropoda: Prosobranchia). The Veliger 33:56-102.
Weber, H. 1927. Der Darm von Dolium galea L., eine ver-
gleichend anatomische Untersuchung unter besonderer
Beriicksichtigung der rn^()»(i/»i-Arten. Zeitschrift fiir
Morphologic tmd Okologie der Tiere 8:66.3-804.
THE NAUTILUS 114(3):112-116, 2000
Page 112
Host-tree selection by Florida tree snails, Ligiiiis fasciatus
(Miiller, 1774), in Big Cypress National Preserve, Florida, USA
Robert E. Bennetts'
Department of Wildlife Ecology and
Conservation
Florida Cooperative Fish and Wildlife
Research Unit
P.O. Box 110450, University of Florida
GainesN-ille, FL 32611-0450 USA
bennetts@tour-du-valat.com
Steven A. Sparks
Deborah Jansen
Big Cvpress National Preserve
HCR'61, Box 110
Ochopee. FL 34141 USA
ABSTRACT
It has frequently been suggested that the Florida tree snail,
Liguiis fasciatus, exhibit preferences for specific host trees, al-
though most accounts of host-tree selection are based on an-
ecdotal observations. We assessed the relative use of host trees
in eight hammocks in the Big C)'press National Preserve for
which the relative availability of each potential host-tree spe-
cies was known. Based on a total of 1,464 tree snail obsei-va-
tions on 21 species of host tree within our study plots, host
trees were not used in proportion to their availability when the
expected values are derived either from the number of trees
or from basal area. Of the most common tree species on our
study area, wild tamarind (Ltjsiloma latisiliqurn) was consis-
tentlv used in excess of its availabilitv. Wild lime (Zanthoxi/him
fagarn), was not a common tree species, but was also used far
in excess of its availabilitv. Pigeon plum {Coccoloba diversifolia)
and gimibo-limbo {Bursern simanibti) were consistently used
less than expected from their respective availabilities. Based on
Akaike's Information Criterion (AIC), the most parsimonious
loglinear model, after accounting for availabilitv, was one that
included only tree species effects. In contrast to the model
selected using AIC, likelihood ratio tests indicated that there
may also be differences among hammocks, but not in relation
to a linear gradient of hurricane damage. We obsers'ed differ-
ences in length among 3-year-old snails on different host trees,
and these differences were consistent with the hypothesis that
host-tree selection reflects food availabilitv'. Snails found on
host-tree species that were used in greater than expected fre-
quency had the greatest length, those found on trees used less
than expected frequency were the smallest, and those found in
proportion to their availability were intermediate in length.
Additional key iiords: Big Cypress National Preserve, host
tree, humcane, Liguus fasciatus. tree snail, Florida, hammock.
INTRODUCTION
Snails of the genus Liguus are native to Cuba, Hispan-
iola, and Florida (Pilsbry, 1912). The Florida tree snail
' Author for correspondence. Present address: Station Biolo-
glque de la Tour du Valat, Le Sambuc. F-I320() Aries, France
Liguus fasciatus (Mtiller, 1774) is found within a restrict-
ed part of this range, primarily some islands within the
Florida Keys, the Atlantic coastal ridge. Everglades Na-
tional Park, and Big Cypress National Preserve. Primar-
ily because of agricultural and urban expansion, only a
few isolated populations remain outside of protected
public lands and a few isolated islands in the Keys. Con-
sequently, they are hsted as a species of special concern
by the state of Florida. Thus, understanding the rela-
tionship between snails and their habitat is essential for
the conservation and management of remaining popu-
lations.
In the Everglades, L. fasciatus is found on islands of
subtropical hardwood trees and scrub known as ham-
mocks. Hammocks are widely scattered throughout
South Florida and may be separated by water, sawgrass,
or other habitat types such as pines. It is widely beUeved
that Florida tree snails exliibit strong preferences for
host trees, particularly smooth-barked trees upon which
their algal food source can easily be grazed (Pilsbry,
1912). In particular, snails are suggested to exhibit pref-
erence for Jamaica dogwood (Piscidia piscipula) in the
Florida Keys and wild tamarind (Li/siloma latisiliqurn)
on the mainland (Pilsbry, 1912), although most accounts
of host-tree selection are based on anecdotal observa-
tions, and few quantitative data are available. Voss (1976)
reported numbers of snails found on each tree species
in 2 hammocks on the coastal ridge. However, he did
not account for the aviulabihty of these host trees; thus,
cUfferential selection can not be reliably assessed. Brown
(1978) is the only study of which we are aware that com-
pared the use and availabihty of host trees, although this
was restricted to 1 hammock in Everglades National
Park. Here we assess the relative use of host trees in
eight hammocks in the Big Cvpress National Preserve
for which the relative availability of each tree species was
knowni.
Brown (1978) also hypothesized that differences in
(juantitv' and qualitv' of food resources of different host-
R. E. Bennetts ct al, 2000
Page 113
tree species mav result in size ditferences among snails
using olifferent host trees, although she was unable to
statisticallv confirm such clifferences. We tested this hy-
pothesis h\ comparing size cbfferences among snails
found on host-tree species that were used (1) in greater
than expected fretjuencies (selected), (2) did not differ
from expected frequencies (neutral), and (3) in less than
expected frequencies (avoided).
MATERIALS AND METHODS
Our studv population was in Big Cypress National Pre-
sene (BCNP). The Pinecrest area of the BCNP contains
one of the largest remaining populations of Florida tree
snails. Within BCNP, 136 hanunocks have been indi\'id-
ually identified and mapped (Pilsbiy, 1946); a few others
may e.xist that have not been identified. We selected 8
of the 136 hammocks from this pof)l for our study sites.
Eight hanunocks proxaded a reasonable representation
of the potential variability and represented a logistically
feasible number of sites. This study was initiated to in-
vestigate the survival and movements of Florida tree
sn;iils following Hurricane Andrew. Hurricane Andrew
crossed southern Florida from east to west on 24 August
1992. The eye of the storm passed along the southern
boundarv of our study area creating a decreasing lati-
tudinal gradient of damage toward the north with in-
creasing distance from the eye. Because we were inter-
ested in the potential effects of Hurricane Andrew, we
also wanted our study sites to reflect the latitudinal gra-
dient of hurricane impacts. Consequently, we divided
the initial pool of hamiuocks into 4 zones reflecting clus-
ters of hammocks positioned along a gradient from little
or no hurricane impact to severe impact (Bennetts ct al.,
in press). There also exists considerable variabifity in the
size of these hammocks, which we beheved could ha\'e
greatly influenced their susceptibihty to damage by Hur-
ricane Andrew and consequently affected tree snails.
Therefore, we digitized each hammock from USGS 7.5-
minute ortho photos and used a Geographic Information
System (CIS) to estimate the appro.ximate size of each
hammock. We then used stratified random sampling to
select 1 hammock of greater size than the median size
and 1 hammock of lesser size from each of the 4 impact
zones. Thus, our sample reflected the latitudinal gradi-
ent of hurricane damage and was balanced among larger
and smaller hammocks.
We estabhshed two 80 m- study plots (sub-samples)
in each hammock. These plots were randomly located in
parts of the hammock where tree snails occurred. The
center of each plot was marked with a steel rod and we
subsequently marked all trees with a diameter at breast
height (DBH) > 5 cm within a 5 m radius of the plot
center. We recorded the species and DBH of each live
tree within these plots.
During each of seven sampling occasions, we searched
for all tree snails within each plot, and as part of a con-
current study on movements (Bennetts et al.. in press),
for marked snails within an extended radius of approxi-
mately 20 HI around the plot. Sampling was conducted
each autumn and spring from autumn 1993 through
spring 1996. Our sampfing occasions were intended to
reflect the biology of the animal and to minimize the
potential for handling to influence a snail's survival. Our
spring sampling occasion was conducted as soon as pos-
sible after emergence of the snails from aestivation. This
coincided with the onset of the annual rainy season. At
this time snails begin to put on new growth, which be-
comes yerv' fragile as it extends as a thin layer from the
previous growth. Thus, our sampling was intended to
precede the period during which time shells are fragile,
although some growth had occurred on some snails. Our
autumn sampfing occasion coincided with the onset of
the dry season just prior to aestivation. At this time the
summer's growth had been terminated, the shells had
thickened, but the animals had not yet entered aestiva-
tion. Animals that were visually determined to be in aes-
tivation (<1%) by presence of an epiphragm (dried mu-
cus membrane across the aperture) were not disturbed.
For each snail we determined its age from annual
growth scars (Tuskes, 1981), measured its length from
tip to tip parallel to the axis and width perpentficular to
the axis at its widest point. We also recorded the host
tree from which it was collected. We then returned each
snail to the same host tree by placing them in a conical
paper cup attached to the trunk of the tree.
Statistical Analyses: As a prefiminary analysis we test-
ed for an association between use and availabiliK' of all
host-tree species within our study plots using a chi-
square goodness of fit test. This was done for a descrip-
tive account of the relative selection of all host species;
however, cells having expected values <5 could produce
unreliable test statistics (Cochran, 1954). Thus, for fur-
ther analyses including adcbtional effects of hammock of
hurricane influence, we pooled cells with expected val-
ues <5 into an "other " category.
We tested whether host trees were used in proportion
to their availabihty using a loghnear model. To account
for host tree availability we used either the log number
of trees, or the log basal area as an offset (Agresti, 1990;
McCullagh and Nelder, 1989). Thus, the frequency of
snails observed was modeled per available number and
basal area of each species. We used basal area in addition
to the number of trees because the surface area of trees
are generally related to its bas;il area (Whittaker and
WoodweU, 1967; Brown, 1978). We then tested whether
the number of snails was influenced by tree species, and
then whether this association cfiffered among hammock
or hurricane zone.
Model selection was based on Akaike's Information
Criterion (AlC) (Akaike, 1973; Shibata, 1989), which is
defined as: —llni'/) + 2np, where —2 ln(l''), repre-
sents the Ukehhood ratio between the given model and
a corresponding saturated model; thus, represents a
measure of model fit. The second term, 2np. is the num-
ber of parameters estimated in the model antl can be
viewed as a cost for adding excessive parameters that do
Page 114
THE NAUTILUS, Vol. 114, No. 3
Table 1. Common and scientific name of the host-tree species within our study plots. Also shown are the total number of trees,
total basal area, and total number of snails observed for each species.
Common name
Scientific name
Acronvin
No. trees
Basal area
No. snails
Cocoplum
Chnjsobalanus icaco
Ci
1
174
1
Dahoon holly
Ilex cassine
Ic
2
365
21
Gumbo Umbo
Bursera simaniha
Gl
26
5423
85
Hackberry'
Celtis laevigflta
CI
2
212
15
Inkwood
Exothea paniculata
Ep
2
93
3
Lancewood
Nectandra coriaceae
No
25
2362
52
Wild lime
Zanthoxi/him faopra
Zf
1
79
20
Li\e oak
Quercus virainiana
Qv
2
480
2
Wild tamarind
Li/siloina latisiqua
LI
128
41820
983
Mastic
Mastichodendron foetidissimii m
Mf
2
711
8
Paradise tree
Simarouba gjmica
Sg
2
240
11
Pigeon plum
Coccoloba diversifolia
Cd
80
9489
145
Poisonwood
Metopium taxifera
Mt
2
252
5
Pond apple
Annona glabra
Ag
1
47
1
Red bay
Persea borbonia
Pb
1
620
9
Red stopper
Eugenia rhombea
Er
1
22
1
Satinleaf
Ch n/.wphijUu m olivifomie
Co
1
85
1
Simpson stopper
Mtjrcianthcs fraarans
Mf
6
723
18
Strangler fio;
Fiats aurea
Fa
1
90
2
White stopper
Eugenia axillaris
Ea
7
273
9
\\'illow bustic
Biimelia salicifolia
Wb
19
2646
72
not contribute substantially to the overall model fit.
Thus, AIC indicates an appropriate balance between
precision and bias (i.e., over and under-fitting the model)
from a set of candidate models (Bumham and Anderson,
1998). In contrast to AIC, which is used as an optimi-
zation tool for comparison among models, we also used
Ukelihood-ratio tests (LRTs) to test for specific effects of
interest (Lebreton et al, 1992; Bumham and Anderson,
1998).
The selection of host trees may be influenced by the
quantity and quality of food resources (Brown. 1978),
which mav in turn result in size differences of snails
using different host trees. We tested this hypothesis by
comparing size differences among snails found on host-
tree species that were used (1) in greater than expected
frequencies (selected), (2) did not differ from expected
frequencies (neutral), and (.3) in less than expected fre-
quencies (avoided). We compared the size of snails (i.e.,
length and width) within each age class among host-tree
species using a fixed-effects analysis of variance (ANO-
VA) model. For this analysis we were not concerned with
the avaHabihty of host trees, only species. Consequendy,
we included all snails encountered on our studv ham-
mocks for this analysis, regardless of whether they were
found within the designated plots (used to compare se-
lection with availabihty) or the extended radius (used for
analyses of movement) (Bennetts ct al, in press). How-
ever, we restricted our sample to snails collected during
the autumn sampling occasion to minimize any con-
founding attributable to variation in the extent of new
growth during spring.
RESULTS
We observed 1464 tree snails on 21 host-tree species
within our study plots (Table 1). Host trees were not
used in proportion to their availabiUtv when the expect-
ed values are derived either from the number of trees
(X' = 554.18, 20 df P < 0.001) or from basal area (x'
= 296.14, 20 df P < 0.001). Of the common tree spe-
cies on our study area, wild tamarind was consistently
used in excess of its availability (figure 1). Wild Ume
(Zant]uixijlum fagara). was not common, but our obser-
vations indicated that it was used far in excess of its
availabilitv', regardless of which measure of availabihty
was used. Although the sample for this species used in
our analysis included only 1 tree, we observed others on
our study area that had similar high use. In contrast,
pigeon plum [Coccoloba diversifolia) and gumbo-hmbo
(Bursera simaniha) were relatively common, but were
consistentlv used less than expected. Willow bustic (Bu-
melia salicifolia) and lancewood (Nectandra coriaceae)
also were relatively common in our study plots, but our
results were conflicting for these species. In relation to
the number of trees, willow bustic was used slightly less
than expected whereas, based on basal area, it was used
shghtlv more than expected. Lancewood was used less
than expected in reference to the number of trees, but
in proportion with its availabihty- in relation to basal area.
After pooling cells with low expected values, the most
parsimonious model based on AIC included only tree
species effects (x" = 101.05, 5 df, P < 0.001). Depar-
tures from ex-pected values were consistent vdth our pre-
hminary analysis in that wild tamarind was used in great-
er proportion than expected from its avaflabifit)-; pigeon
R. E. Bennetts et al, 2000
Page 115
LI Zf Ic Pb CI Sg Mf Fa Ml Ag Ci Er Co Wb Mf Ep Qv Gl Ea Nc Cd
Host-Tree Species
llll
■ ■
Zf LI CI Ic Sg Wb Ea Er Ep Mf Fa Ag Nc Mt Co Pb CI Mf Qv Gl Cd
Host-tree Species
Figure 1. Adjusted residuals (Haberinan 1973) from good-
ness-of-fit test between the number of snails found on different
host-tree species in relation to their availability. Host-tree spe-
cies are displayed in rank order from selected in greatest pro-
portion relative to its availabilit)' to least. Expected values were
derived based on the number of trees of a given species (top)
and the total basal area for a given species (bottom). Positive
residuals >1.96 indicate use greater than expected from avail-
ability and residuals < — 1.96 indicate use less than expected
from a\ailability.
plum and gumbo limbo were used less than expected.
Lancewood and willow bustic were intermediate as was
our "other" class. In contrast to the model selected using
AIC, LRTs indicated that there may have been a species
X hammock interaction (x' = 110.36, 31 df, P < 0.001),
but not a species X hurricane zone interaction (x" =
9.32, 5 df, P = 0.097). Thus, our data indicated that
selection of host-tree species may have differed among
hammocks, but this difference was not in relation to a
gradient of hurricane damage.
We found size (length) differences among snails found
on host tree species onlv for 3-year-old snails (F^ j,^ =
3.42, P = 0.034) (figure 2). Of the.se, the length of sniiils
was highest for snails found on host trees that were used
in greater frequency than their availabibty (selected) and
lowest for snails found on host trees that were used less
than their availabihtv' (avoided). Sn;uis found on host
trees that were not out of proportion to their availabihty
E
E
o>
c
40 -
263
53
-
39
-
35
38 -
37 -
Selected
Neutral
Avoided
Host-tree Selection Class
Figure 2. Mean length (±SE) of .3-vear-old tree snails found
on host-tree species that were used in excess ot their avail-
ability (Selected), less than their availabilitv' (Avoided) and did
not differ from availabilitv (Neutral). Sample sizes are shown
for each group.
(neutral) were intermediate in length, but did not differ
from either of the other groups (Fisher's Least Signifi-
cant Difference, P>0.05). We did not find differences
in width among any host-tree species for any age class
at the a = 0.05 level.
DISCUSSION
Our data are consistent with previous reports of wild
tamarind being used in excess of availabihty; although
the degree of this association is highly sensitive to what
measure is used to derive the e.xpected values for avail-
ability. When the expected value is derived from basal
area, the association is much weaker than when the ex-
pected value is derixed from the number of trees. Ex-
pected values derived from basal area probablv better
reflect the surface area available tor foraging. The num-
ber of stems would be important if the probabifity of a
dispersing snail moving to a given tree is dependent on
it encountering a trunk on the ground, although most
inter-tree movement on our study area probably was via
intertwined foliage. Brown (1978) reported a remarkably
similar result in Everglades National Park. She reported
an overall significant test statistic based on both number
of tree stems and estimates of bark surface area, al-
though the relationship was substantially weaker based
on bark surface area. Regardless of the statistical signif-
icance, 983 of 1464 (67%) of all snails we observed were
found on wild tamarind. Voss (1976) reported a similar
estimate of 34 of 50 (65%) for 1 hammock in the eastern
Everglades near Miami, and Brown (1978) reported 209
of 39.5 (52%) in another location in Everglades National
Park. Although other trees niav be preferentially select-
ed if available, wild tamarind was the most abundant and
Pase 116
THE NAUTILUS, Vol. 114, No. 3
most used host tree within the Big Cypress National Pre-
serve, which is probably also the case in most of the
mainland habitats. Thus, wild tamarind is clearly an im-
portant component of tree-snail habitat in this region.
Although our model selection did not support that
host-tree selection differed among hammocks, an LRT
chd indicate a species by hammock interaction effect.
Hammocks differed with respect to which host tree spe-
cies were present, which Ukely reflects inter-hammock
differences in attributes such as size, soils, and hydro-
logic regimes. Thus, the interaction effect we observed
could have been attributed to these differences in spe-
cies composition, but our data are insufficient to evaluate
such effects with much reliability.
Bias due to \isibilit\- of snails was not accounted for
by our approach. This effect would have been most in-
fluenced by dense foliage obscuring snails from view.
For most host-tree species, we believe that this bias was
negligible, especially because of reduced foliage as a re-
sult of Hurricane Andrew. However, one notable excep-
tion was pigeon plum, which often had ver)' dense fo-
liage making it difficult to detect snails. Thus, we suspect
that our data indicating that this host tree species was
underutilized may have been, at least in part, an artifact
of detection bias.
Although our data are far from conclusive, they are
consistent with Browni's h\-pothesis that there mav be an
association between selection of chfferent host trees and
size of the snails. We found size differences only among
3-year-old snails. However, even our relatively large sam-
ple sizes tend to become quite small once partitioned by
age and host tree species. Florida tree snails exliibit most
growth during their first 2-3 vears, after which growth
slows dramatically (Tuskes, 1981). Thus, 3-year-old snails
probably represent a peak of cumulative growth, and are
a hkely age class to observe size differences. For this age
class, snails found on host-tree species used less than
expected were smallest in length, those found on trees
used in excess of availabihty were the largest in length,
and those found in proportion to their availability were
intermediate in length.
ACKNOWLEDGMENTS
We thank Jimmy Conner, Phil Darby, Sue Davis, Vicky
Dreitz, Guy Fischer, Paul Hinchcliff, Amy Kazmier,
Steve McGehee, Katie Golden, Teresa Johnson, Jeff
Ripple, Tim Towles, Patty Valentine-Darby for field as-
sistance, and George Francioni for safe helicopter
flights. We also appreciate the helpful comments from 2
anonymous reviewers. Funding was provided by the Na-
tional Park Service through the South Florida Research
Center, and Big Cypress National Preserve provided ad-
ditional logistic support.
LITERATURE CITED
Agresti, A. 1990, Categorical data analysis. John Wiley and
Sons, New York. 5.5Spp.
Akaike, H. 197.3. Information theory' and an e.xtension of the
madmuni likelihood principle. In: B. Petrov and F. Czaldl
(eds.) Proceedings of the 2'"' International Symposium In-
formation Theory, Akademiai Kiado Budapest, pp. 267-
281.
Bennetts. R. E., S. A. Sparks, and D. Jansen. In press. Factors
influencing movement probabilities of Florida tree snails
Liguiis fasciatiis (Miiller) in Big Cvpress National Pre-
serve following Hurricane Andrew. Malacologia.
Brown, C. A. 1978. Demography, dispersal, and microdistri-
bution of a population of the Florida tree snail Liguus
fasciatiis. M.S. Thesis, Uni\ersitv of Florida, Gainesville.
Buniham K. P. and D. R. Anderson. 1998. Model selection
and inference: a practical infoniiation-dieoretic approach.
Springer-Verlag, New York.
Cochran, W. G. 19.54. Some methods for strengthening the
common chi-square tests. Biometrics 10:417-451.
Haberman, S. J. 1973. The analysis of residuals in cross-clas-
sified tables. Biometrics 29:205-220.
Lebreton, J. D., K. P Bumham. J. Clobert, and D R Ander-
son. 1992. Modeling survival and testing biological hy-
potheses using marked animals; a unified approach with
case studies. Ecological Monographs 62:67-118.
McCuUagh. P. and J. A. Nelder 1989. Generalized hnear mod-
els, 2nd edition. Chapman and HaU, New York, 511 pp.
Pilsbry, H. A. 1912. A study of the variation and zoogeography
of Liguus in Florida. Journal of the Academy of Sciences
of Philadelphia 15:429-470.
Pilsbry, H. A. 1946. Land Mollusca of North America. Acad-
emy of Natural Sciences Philadelphia, Monograph 32:1-
520.
Shibata, R. 1989. Statistical aspects of model selection. In: J.
C. Williams (ed.) From data to model. Springer-Verlag,
New York, pp. 21.5-240.
Tuskes, P. M. 1981. Population structure and biology of Liguus
tree snails on Lignumxitae Key, Florida, The Nautilus 95:
162-169.
Voss, R. S. 1976, Obserxations of the biology of the Florida
tree snail, Liguus fasciatiis (Miiller). The Nautilus 90:6.5-
69.
Whittaker, R. H. and G. M. Woodwell. 1967. Surface area re-
lations of woody plants and forest communities. American
Journal of Botany 54:931-9.39.
THE NAUTILUS 114(3): 117-1 19, 2000
Page 117
The development of three heterobranch mollusks
from California, USA
Rachel Collin
Committee on E\olutionar)' Biologv'
Uni\ersits' of Chicago
1025 E. 57th St.
Chicago, IL 60637 USA
and
Department of Zoology
Field Museum of Natural Histor\'
1400 S, Lake Shore Drive
Chicago, IL 60605 USA
rcoHinCSmidwav. uchicago.edu
ABSTRACT
The de\elopnient of Odostomin nitinn. Turbonilla sp., and Wil-
hamia peUoides from Cahtoniia, is t)pical ot heterobranch mol-
lusks. Thev all produce small eggs (about 60 |jLni) that are in-
di\idually encapsulated and embedded in gelatinous egg mas-
ses. The capsules are connected by chalazae. Cleavage is un-
equal and gastrulation occurs by inxagination. Plankiotrophic
larvae hatch at shell lengths of 120-150 |xni.
Additional key words: Pyramidellidae, Tiirbonilln. Odostomia,
gastropod development, Williamin
INTRODUCTION
Although lower heterobranchs and marine pulmonates
are common in shallow marine waters, their develop-
ment remains largely undescribed. Knowledge of their
development may be useful and important because de-
velopmental features such as the structure of egg mas-
ses, cleavage type, presence of the larval pigmented
mantle organ (PMO), and hydrophobic larval shells may-
be important characters for phylogenetic stucbes (Rob-
ertson, 1985; van den Biggelaar, 1996; van den Biggelaar
and Haszprunar, 1996; Collin, 1997). Additionally, there
are a variety of interesting trends in the evolution of
cleavage patterns (Freeman and Lundelius, 1992; van
den Biggelaar and Haszprunar 1996) and heterochro-
nies in larval morphologies (Page, 1994) whose docu-
mentation could benefit from more extensive phyloge-
netic sampling.
Herein I describe the development of two pyranii-
dellid and one siphonariid pulmonate species from the
Califomian coast. All animals were collected by hand in
the summer of 1997 and kept in small dishes in the
laboratory where thev laid egg masses. Egg masses were
observed daily until hatching, but no attempt was made
to raise the larvae to metamorphosis.
RESULTS
Odostomia altina Dall and Bartsch, 1909
(Table 1)
Large numbers of Odostomia altina were found on the
shells oi HaliotLs cornigflta collected at a depth of 10 m
from Point Loma, California (29°40'N, 117°20'W).
Specimens are deposited at the Field Museum of Nat-
ural History (FMNH 282369 and 282370) and were
identified by comparison with the original species de-
scription and illustrations in (Dall and Bartsch, 1909).
There were as many as 50 adult pvTamidellids and nu-
merous egg masses on one abalone. Egg masses were
typical of other pvTamideOids: Single eggs are enclosed
in albumin-filled oval capsules that are embedded in a
clear sticky gelatinous mass. The capsules are connected
by thin extensions of the capsular covering called cha-
lazae (see Robertson, 1985; Collin and Wise, 1997 for
detailed description). A timetable of development is giv-
en in Table 1.
The round, white eggs are 60 |jLm in diameter (mean
= 60.83 |jLm; sd = 1.39 |xm; n = 31; eggs from 3 egg
masses) the inner capsule diameter is 150 (xm (sd = 8.11
|xm; n = 19) and the outer capsule diameter is 176 \x.m
(sd = 6.992 |xm; n = 10). First cleavage is unequal and
at the 4-cell stage the two largest cells are adjacent, as
are the two small ones. Several embryos were observed
in a 3-cell stage, which suggests that second cleavage is
not synchronous. There is no polar lobe and third cleav-
age is unequal. The round blastula gradually flattens and
invaginates to form a horseshoe shaped gastrula. During
subsequent development the embryo grows to fill the
capsule and the larval organs differentiate. Plank-totroph-
ic larvae hatch after about 7 days (Table 1) with 130 |xm
(mean = 130.33 |xm; sd = 8.55 [xni; n = 15; egg masses
from two females) smooth, left-handed, hydrophobic
shells. Each larva has a well-developed metapodial ten-
Page 118
THE NAUTILUS, Vol. 114, No. 3
Table 1. De\elopnient schedule for Odostomiti nltinn at 22-
24°C.
Age
Stage
>3 hours 2-cells
5 hours 4-cells
12 hours 64-cells
1 dav blastula
1.5 days gastnilation by invagination
3 days just moving, foot and velum anlangen visible
5 days red-yellow PMO visible, shell operculum and
statocvsts
~7 days hatchmg at 130 (jim
tacle and statocysts, but no detectable heartbeat, and no
eyes. The larval PMO consists of two parts: A round red
central part and an additional semi-transparent yeUow
lobe on one side. Observation of the yellow lobe under
the dissecting microscope is difficult, but the structure
can be seen easilv' under a compound microscope.
Turbonilla sp.
(Figures 1, 2, table 2)
One adult of an unknown species of Turbonilla was col-
lected on the high mid-intertidal zone at Alegria, Cali-
fornia (34°28'N,^120°17'VV) in July 1997. The species
identification is uncertain because Turbonilla taxonomy
is especially difficult and the single specimen could not
be unambiguously assigned to any Californian species.
The current taxonomy of Californian pyramidellids as-
signs all species with axial-ribbed shells to the genus Tur-
bonilla (Dall and Bartsch, 1909). This snail laid one egg
Figure 2. Earlv developmental stages of Turbonilla .sp. .\. 2-
cell stage at the beginning of second cleavage, the cells are
clearly not equal in size, B. 4-Cell stage, C. blastula, D. gas-
trula, showing the invagination typical of heterobranch devel-
opment. Scale bar = 50 \x.m.
mass of about 100 eggs in the laboratory and develop-
ment was followed until hatching (table 2 and figure 2).
The egg mass consisted of capsules containing one white
egg surrounded by clear albumin, connected together by
chalazae and embedded in a clear sticky gel. The egg
diameter was 65.5 |jLm (n = 10, sd = 1.97 |jLm) and the
capsule length was 187.8 |xm (n = 10, sd = 6.67 (im).
The chalazae are thicker and less tv\dsted than in O. col-
umbiana Dall and Bartsch 1907 (Colhn and Wise, 1997).
First cleavage is slightly unequal but bv the 4-celI stage
the blastomere inequalit)' is yery subtle. The early cleav-
ages do not produce a polar lobe. The polar bodies are
clearK visible throughout development because the al-
bumin is transparent. After 24 hours the embrvos form
flattened blastulas, which begin to invaginate at about 40
hours. Gastnilation continues by invagination for the
next dav. Bv the fourth dav the foot and velum anlagen
are visible. On the fifth dav the embrvos begin to move
Table 2. Developmental schedule for Turbonilla sp. at 16-
18°C.
Figure 1. Adult Turbonithi sp. Shell length is 6 mm.
Age
Stage
7 hours
2-cells
24 hours
blastula
2-3 days
gastnilation by invagination
4 days
just moving, foot and velum anlangen visible
5 days
shell and velum differentiated. Embrvo fills
1/4 of the capsule
6 davs
black PMO visible
9 days
embno fills the capsule
11 days
hatching at 152 |j.m
R. Clolhn, 2(M)()
Page 119
and thev fill alidiit a (juarter of each (.apsiilf. B\' thf next
cla\' the black PMO is \isihle on the right side just pos-
terior to the velum. The enibno grows to completely fill
the capsule, before hatching. Shell length at hatching is
1.52 jjLni (n = 14; sd = 2. .37 p,m; from a single egg mass).
The shell is hydrophobic, left-handed and the lana has
no heart or eyes but has a well-developed metapodial
tentacle on the foot. The planktotrophic lanae swim ac-
tively.
Williamia pchoides (Carpenter, 1864)
Several adult W. peltoidcs (Carpenter, 1864) were col-
lected in the subtidal zone ( — 10 ni), on hard substrates,
in the vicinity of Santa Barbara, California (.34°28'N,
120°17'W). Voucher specimens are deposited at the Bai-
ley-Matthews Shell Museum, Sanibel, Florida (BMSM
4999). Williamia species are unusual among marine pul-
monates because they are predominately subtidal. Adults
produced several egg masses in chshes in the laboratory.
The structure of the egg masses is verv similar to
those of the pvTamidellids. The eggs are each individu-
ally enclosed in a coating of albumin inside an oval cap-
sule. The capsules are connected with chalazae and are
embedded in a gelatinous mass. The capsules are 147
jjim in length (mean = 147.7 ji-m; sd = 3.4 |xm; n =
11). Unfortunately uncleaved eggs and early cleavage
stages were not observed. Gastrulation occurs via invag-
ination forming a horseshoe-shaped gastnila that is 69
(xm in diameter (d = 69.28 |xm; sd = 3.4 |jLm; n = 7;
from one egg mass). Further development progressed as
in the pyramidellids. However, no pigmented PMO de-
velops: I could not determine if there was no PMO or
if the structure was present but not pigmented. There
is some reddish pigmentation along the suture of the
larval shell, but the larval body was pigmentless. After 9
days at 18-22 °C the larvae hatch at a length of 126 |xm
(length = 126.0 jjuni; sd = ■5. .58 |jLm; n = 10). The plank-
totrophic lar\ae have a hydrophobic smooth left-handed
shell. There is still no pigmented PMO, no eyes, and no
metapodial tentacle but the statocysts are clearly visible.
DISCUSSION
These observations are the first descriptions of intracap-
sular development for species in the genera Williamia
and Tttrhonilla.
The features of pyramidellid development described
here generally agree with prexaous descriptions of pyr-
amidellid development. Because Tnrhoiiilla and Odos-
tomia are distantly related genera within the Pyramidel-
lidae (Wise, 1996), characters shared by the species de-
scribed here and O. cohtmhiana (Colhn and Wise, 1997)
may be typical of pyramidellid development in general.
All three species have small eggs, unequal cleavage, gas-
tnilation bv invagination, and hatch with smooth, left-
handed, hydrophobic shells, a metapodial tentacle, dis-
tinct PMO, but without eyes or a larxal heart. The color
oi the larval PMOs varies among species as does the
cok)r of the adult PMO (Robertson, 1985).
The development of Williamia peltoidcs is strikingly
similar to pyramidellid development. The structure of
the egg masses is indistinguishable from that of the pyr-
amidellids. Hatching lar\ae are distinct in their lack of
a metapodial tentacle and pigmented PMO and the
small area of shell pigment. These results are in agree-
ment with Robertson's (1985) conclusion that larval
PMOs are not present in pulmonates while chalazae and
heterostrophy are common. The retldish pigment along
the shell suture is also found in larvae of Siphouaria sp.
from New Zealand (pers. obs.).
ACKNOWLEDGMENTS
This research was conducted during a visit to the labo-
ratories of Dr S. Gaines (University of California at San-
ta Barbara) and Dr K. Roy (University of CaUfornia at
San Diego). I thank Ron McConnaughev and Shane An-
dersen for helping collect animals and two anon\iiious
reviewers for helpful comments on previous versions of
this manuscript. This work was supported financially by
a NSF Predoctoral Fellowship, and grants from the
Western Society of Malacologists, Sigma Xi, the Lemer
Gray Fund (American Museum of Natural Historv) and
the Hinds Fund (University of Chicago).
LITERATURE CITED
Biggelaar, J. A. M. van den. 1996. The significance of the early
cleavage pattern for the reconstruction of gastropod phy-
logeny. In: Taylor, J. D. (ed.) Origin and Evolutionary Ra-
diation of the Molliisca. Oxford University Press, Oxford,
UK.
Biggelaar, J. A. M. van den and G. Hazsprunar 1996, Cleavage
and niesentoblast formation in the Gastropoda: An evo-
lutionarv perspective. Evolution .50:1.520-1.540.
Collin. R. 1997. Hydrophohic larval shells: Another character
for higher level systematics of gastropods. Journal of Mol-
luscan Studies 6.3:425-430.
Collin, R. and J. B. Wise. 1997. Morphology and development
of Odostomin cohnubiann (Gastropoda: PyTamidellidae).
Biological Bulletin 192:24:3-252.
Dall, W. H. and P. Bartsch. 1909. A monograph of west Amer-
ican pvTamidellid mollusks. Bulletin of the United States
National Museum 68:1-258.
Freeman, G. and ]. W. Lundelius. 1992. Evolutionaiy' impli-
cations of the mode of D quadrant specification in coe-
lomates with spiral cleavage. Journal of Evolutionary Bi-
ology 5:20.5-247.
Page, L. R. 1994. The ancestral gastropod larval torm is best
approximated by hatching-stage opisthohranch larvae: ev-
idence from comparative developmental stuthes. In: Wil-
son, W. H., S. A. Strieker, and G. L. Shinn (eds.) Repro-
duction and Development of Manne Invertebrates. Johns
Hopkins University Press, Baltimore.
Robertson, R. 1985. Four characters and the higher category
systematics of gastropods, American Malacologica! Bulle-
tin, Special Edition 1:1-22.
Wise, J, B, 1996. Moqiliologv and phylogenetic relationships
of certain pyramidellid taxa (Heterobranchia). Malacologia
.37:44.3-51 r.
THE NAUTILUS 114(3): 120-126, 2000
Page 120
Diminishing species richness of mollusks in Oneida Lake,
New York State, USA
Willard N. Harman
State Universitv' of New York College at Oneonta
Biological Field Station RD2, Box 1066
Cooperstown, NY 13326 USA
harmamvn@oneonta.edu
ABSTRACT
Between 1915 and 1917, F. C. Baker studied the molluscan
fauna of Oneida Lake, a shallow, eutrophic lake in central New
York State. He hsted 41 living taxa, of which two gastropods,
Bithynia tentacitlata (Linnaeus, 1758) and Pleurocera aaita
(Rafinesque, 1S29), were then recent introductions. In 1967-
68, John Foniey and I (Harman and Foniey, 1970) surveyed
Oneida Lake, \'isiting Baker's original collecting sites. W'e tal-
lied 35 Uving taxa dominated by the introduced European B
tentacitlata. In 1992-95, I again made extensive collections of
mollusks finding a total of 24 h\ing taxa dominated bv Dreis-
sena pohjmorpha (Pallas, 1771), the then recently introduced
Eurasian zebra mussel. Fifty percent of Baker's original euht-
toral collection sites could not be found. An average 1 m- area
in 1992-95 included 6708 individuals of D. pohjmorpha. 60 of
B. tcntactilata and 2 of the unionid bivalve EUiptio complanata
(Lightfoot, 1786). Molluscan species richness was reduced by
15% between 1917 and 1968, a trend concurrent with the in-
crease in abundance of Bithynia. Species richness was hirther
reduced by 31% between 1968 and 1995, as human acti\-ities
impacted euhttoral habitats and D. polymorpha colonized
Oneida. The total decrease in species richness between 1917
and 1995 was of 42%'. Since 1996 no li\ing miionids ha\e been
observed in the lake.
Additional key words: Exotic introductions, habitat destruc-
tion, freshwater, gastropods, bivalves, Bithynia tentacitlata.
Dreissena pohjmorpha.
INTRODUCTION
Oneida Lake is a eutrophic lake in central New York
State, with about 233 kTn- in surface area and a maxi-
mum depth of 16.8 m. It is located in a depression on
the low, open rehef of the Ontario Lake Plain in the
Oswego River drainage basin (figure 1). The lake is ori-
ented with its length parallel to that of the prevailing
westerly winds. It mixes throughout the ice-free period,
with thermal stratification occurring only ephemerally
during wind-free periods (Harman and Forney, 1970).
Tributaries to Oneida drain densely populated areas of
Onondaga Limestone and fertile soils. As a result, the
lake has been considered one of the most naturally pro-
ductive in the world (Mozley, 1954). Historically, popu-
lations of algae and aquatic vascular plants have thrived
in the shallow waters along the shoals, beaches, and is-
lands, on diverse eulittoral substrates providing food and
cover for a varied and abundant molluscan fauna (Har-
man and Forney, 1970).
Central New York has a diverse molluscan fauna de-
rived from species immigrating from Atlantic coastal riv-
ers, the Mississippi River drainage (Interior Basin), and
the Great Lakes, soon after the retreat of the last Pleis-
tocene glaciers (Clarke and Berg, 1959). Oneida Lake is
unique due to its central position on the New York Barge
Canal system and natural waterways (figure 1), which
have continued to provide access to immigrating organ-
isms from the early 1800s. Since then, mollusks from
Lake Erie and the Ohio River basins in the west, and
from the Atlantic coastal drainage in the southeast (via
the Mohawk and Hudson drainage basins) have found
their ways to Oneida Lake. Headwaters of several wa-
tercourses flowing from the Appalachian highlands in
the southern Oswego system join the Susquehanna
drainage via through-viilleys, which facilitates dispersal
of aquatic organisms. The Oswego River drains Oneida
flowing to Lake Ontario and, via the St. Lawrence River,
joins Lake Champlain and other northern waterways,
thus providing access to and Irom North Atlantic drain-
age systems.
During 1915-17, F. C. Baker studied the macroben-
thos in Oneida Lake, concentrating on the molluscan
fauna excepting the fingernail clams (Sphaeriidae) (Bak-
er, 1916a, b, c; 1918a, b, c, d). His research on Oneida's
Lower South Bay is among the earliest quantitative stud-
ies of freshwater macrobenthos in North America (Bak-
er, 1918c). Baker studied Oneida because of its great
diversity of mollusks. In 1967 and 1968 I (Harman and
Forney, 1970) conducted, as part of a survey of the gas-
tropods of the Oswego River drainage basin, a qualitative
study of the molluscan fauna of Oneida Lake. In the
summer of 1967, Forney (Harman and Forney, 1970)
repeated Baker's (1918c) quantitative work in Lower
South Bav as part of a macrobenthic monitoring pro-
gram carried out by Cornell University.
The introduction of zebra mussels {Dreissena poly-
mor-f)ha) into Oneida Lake in 1990 (Mitchell et al. 1996)
W. N. Hai-man, 2000
Page 121
Figure 1. Central New York State showing Oneida Lake and
routes of immigrating mollusks.
has had important impacts on water clarity by reducing
phvtoplankton standing crops. It also appears to be af-
fecting the distribution and abinidance ot aquatic vas-
cular macroph\1:es (E. L. Mills, pers. comm.). The ir-
ruption of the Drcisscna population was expected to
have tremendous impacts on the molluscan fauna (e.g.,
Nalepa ct al. 1991; Ricciardi ct al, 1995; Schloesser ei
al, 1996). That concern prompted my return to Oneida
during 1992-95 to determine the status of the molluscan
communitv. I effectively repeated my (Harman and For-
ney, 1970) 1967-68 qualitative work and in 1993 did a
quantitati\'e studv in Lower South Bay in an attempt to
repeat Baker's 191.5-lS studies (1918c) as well as For-
ney's 1967 work (Harman and Forney, 1970).
This paper describes the changes in the molluscan
fauna since 1915, showing evidence of a constant reduc-
tion of species richness concurrent with destruction of
euhttoral habitats and invasions of immigrating mollusks.
MATERIAL AND METHODS
In 1915-17, during the summer months. Baker obtained
(juantitative samples in Lower South Bay using a sieve,
flattened on one edge, attached to a wooden pole, to
collect bottom samples of about 10- cm-. A variety of
larger dredges were used in deeper water A square met-
al frame, viewed through a glass-bottomed bucket, was
used to estimate densities of large snails and bivalves.
Collections were made while wading, or from a boat
(1918c). Water depths in Lower South Bay are such that
these methods allowed him to sample all areas of the
bay. Baker's samples at each collecting site approximated
10- cm-. He used varying numbers of replicates, typically
2-6. All his computations were presented using 10- cm-
(16 in-) as the basic unit.
My 1967-68 qualitative survey was made throughout
the lake in an attempt to sample every habitat suitable
for mollusks. Samples were retrieved from inorganic
substrates str;iined through a sieve or handpicked vsatli
forceps in shallow water Vegetation was collected and
dried over containers for retrieval of desiccating organ-
isms. Collections from deeper water were done similarly
using SCL'BA. Fornev contributed several Ekman grab
samples to that study. Forney's replication of Baker's
quantitative study in Lower South Bay, again during the
summer months, used Baker's methods as mentioned
aiio\e. However, he relied more on standard Ekman
grabs. Calculations were based on 10- cm- sample areas
to facilitate comparison with Baker's work. Eleven of
Baker's original sample sites (out of a total of 140) were
lost due to artificial modifications of the shoreline.
In 1992-95 the same methodologies were used for the
qualitative work, over the same time period that Forney
(Harman and Forney 1970) had covered in 1967-68.
The 1992-95 (juantitative work in Lower South Bay in-
voked Ekman samples in deep water and square metal
frames in eulittoral waters. Calculations were based on
1 m- sample size. Information is presented using this
size, as well as 10- cm- for comparison with the earlier
studies. It should be noted that when converting to 1 m-
from the earlier 10- cm- sample size, diversity is poten-
tially underestimated since widely separated large indi-
viduals such as unionids often encountered in the former
are rarely foimd in the latter samples, and thus never
appear in the data set. Only 71 of Baker's 140 original
sites were still in existence in the recent survey. All titx-
onomic nomenclature herein has been updated accord-
ing to Turgeon ci al (1998).
RESULTS AND DISCUSSION
Table 1 indicates the taxa that Baker encountered at the
turn of the century. Baker's revised list includes 41 fiving
molluscan taxa inclutling the then recently introduced
European snail Bithijnia tent acid at a, which had ap-
peared around 1880 in Lake Ontario (Beauchamp,
1888). Bithi/nia tcntavtilata was assumed to have been
introduced via ballast water in commercial seagoing ves-
sels plying the Great Lakes (Baker, 1916b). The species
was not abundant in Oneida Lake in 1915-17, but oc-
curred in dense populations near the outlet at the west
end. An average 10- cm- bottom sample made in 1917
contained 7 taxa, all consisting of native species {Pyr-
gulopsis lustrica (Pilsbry, 1890) (Amnicola htstiica, A.
lustrica (var) and A. oncida in Baker's original lists),
Stagnicola catcscopiiiin (Say, 1867) (Galba catascopium
of Baker), Gi/ratilus panii.s (Say, 1817) {Planorhis par-
vus of Baker), FhijscUa gyrina (Say, 1821) (Physa gyiina
of Baker), P. Integra (Haldeman, 1841) (Physa intcgra
of Baker), Prmncnetus cxacuoiis (Say, 1821) [Planorhis
exacuous of Baker), and Valvata tiicarinata (Say, 1817))
(figure 2). A second introduction, Plcnroccra acuta.
Page 122
THE NAUTILUS, Vol. 114, No. .3
Table 1. The moUu.scan fauna of Oneida Lake; reference conditions, 191.5-17 (modified from Baker, 1918).
Taxa
Bivalvia: Palaeohetcrodonta
Margaritifera maraarilifera (Linnaeus, 17.58)
Elliptio complanata (Lightfoot, 1786)
Alasmidonta undidata (Say, 1817)
Pijganodon grandis (Say, 1829)
Pijganodon cataracta (Say, 1817)
Strophifus undulatus (Say, 1812)
Villosa iris (I. Lea, 1829)
Lampsilis radiata radiata (Gmelin, 1791)
Actinonaias ligmcntina (Lamark, 1819)
Total number of species: 41
Gastropoda: Basominatophora
Phi/si'lla gtjrina (Sav, 1821)
Phi/si'lla Integra (Haldeman, 1841)
Phi/sella heterostropha (Say, 1817)
Lijmnaea stagnalis (Linnaeus, 1758)
Fossaria obrussa (Say, 1825)*
Stagnicola elodes (Say, 1821)
Stagnicola enwrginata (Say, 1821)
Stagnicola catescopium (Say, 1867)
Pseudosiiccinea columella (Say, 1817)
Acella haldniani (W. G. Binney, 1867)
Helisomn anceps (Menke, 1830)
Phanorbella trivolvis (Say, 1817)
Planorbella campanulata (Say, 1821)
Gyraulus parvus (Say, 1817)
Gyratdus deflectus (Say, 1824)
Promenetus exacuous (Say, 1821)
Laevapex fuscus (C, B. Adams, 1841)
Ferrissia parallelus (Haldeman, 1841)
Ferrissia rivularis (Sav, 1817)
Gastropoda: Caenogastropoda
Campeloma decisum (Say, 1817)
Vivipams georgianus (I. Lea, 1834)
Pleurocera acuta (Rafinesque, 1820)''
Amnicola limosus (Say, 1817)
Pijrgulopsis lustrica (Pilsbry, 1890)
Pomatiopsis cincinnatiensis (I. Lea, 1840)
Frobijthinella enwrginata (Kuster, 1852)
Soinatogynis depressus (Tryon, 1862)
Bithynia tentaculata (Linnaeus, 1758)'
Valvata tricarinata (Say, 1817)
Valvata sincera (Sav, 1824)
Valvata lewisi (Currier, 1868)
Valvata bicarinata (I. Lea, 1841)
' Fossaria obntssa. as used here includes F. modicelta, (Say, 1825), F. nistica (I. Lea, 1841) and may include F. parva (I. Lea, 1841).
'•pleurocera acuta (Rafinesque, 1820) had invaded Oneida Lake via the Erie Canal system before Baker's 1915 work (Dazo, 1965).
c Bithynia tentaculata was apparently invading at the time of collection. Baker noted high densities in the outlet (Oneida River)
very few in the Lake proper
1
Q
5
8
a
B
3*
5
o
I.
8.
I
5 ^^ I I
Figures 2-5.
Figure 2. Dominant mollusks (individuals 10"- cnr) in Lower South Bay, Oneida Lake, in 191.5-17 (Baker, 1918c). In this, and
figures 3 and 4, species occurring at a density of less than 0.5 individuals 10"- cm- are not considered.
Figure 3. Dominant mollusks (individuals 10- cm-) in Lower South Bay, Oneida Lake in 1967-68 (Harman and Forney, 1970).
Figure 4. Dominant mollusks (incfividuals 10"- cm-) in Lower South Bay, Oneida Lake in 1992-95.
Figure 5. Dominant mollusks (individuals m"-) in Lower South Bay, Oneida Lake in 1992-95. Species occurring at a density of
less than 0.5 indi\iduals m"- are not considered.
W. N. Harman, 2000
Page 123
Table 2. Molluscan species inxadins; Oneitla Lake followed by the approximate dates of iiitnufnctioii and origins.
Tixxa
Approximate dates
of introduction
Origin
Bivalvia: Ileterodonta
Dreissenti polyinoi-plta (Pallas. 1771)
Bivalvia: Palaeoheterodonta
Potamihis alatiis (Sav, 1817)
Li'ptodcii fraailis (Rafinesque, 1820)
Liffiinia recta (Laniark. 1819)
Gastropoda: Caenogastropoda
Bithi/nia tentaculata (Linnaeus, 1758)
Pleiirocera acuta (Rafinesque, 1820)
Elimia livescens (Menke, 1830)
Eliriiin virainica (Say, 1817)
Total number of species: 8
1986 Eurasia, Great Lakes, Oswego River
1920-1950 Interior basin, Erie Canal system
1920-1950 Interior basin, Erie Canal system
1920-1950 Interior basin, Erie Canal system
1910-1918 Eurasia, Great Lakes, Oswego River
1825-1915 Interior basin, Erie Canal system
1920-1950 Interior basin antl/or Hvidson river, Erie Canal system
1920-1950 Susquehanna Basin, through-valleys, Oswego Basin
and/or Interior basin, Erie Canal system
which had arrived via the Erie Canal from the west, was
well established by the time Baker completed his studies
(Dazo, 1965; Baker, 191Sc).
When John Fomey and I (Harman and Fomey, 1970)
collected in the 1960s, 35 taxa were found. Three gas-
tropods, Elimia livescens (Menke, 1830), E. virginica
(Say, 1817), and Plcuroccra acuta, all in the family Pleu-
roceridae, were represented only bv dead specimens.
Three pearly freshwater mussels ((Unionidae), Potamihis
alatus (Say, 1817), Leptodca fragiUs (Rafinesque, 1820),
Ligumia recta (Lamark, 1819)) had immigrated from the
Interior Basin (Clarke and Berg, 1959; Dazo, 1965). Eli-
mia virginica was introduced into the Oswego watershed
before the turn of the century (DeKay, 1843; Beau-
champ, 1888). It is assumed that this species crossed the
divide between the Susquehanna and Oswego River wa-
tersheds via through-valleys after small headwater lakes
and wetlands on the divide were disturbed to provide
water for the Erie Canal after its opening in 1825 (Har-
man, 1970). It also could have moved eastward along
the Erie Can;il from populations in the Interior Basin
(Goodrich, 1942). Bithi/nia tentaculata, present in 1917,
had become abundant by the 1960s. An average 10- cm-
bottom sample in 1967 contained 4 individuals of B. ten-
taculata (table 2, figure 3).
Table 3 lists the taxa collected in 1915-17 (Baker,
1916a, b, c; 1918a, b, c, d) and in 1969 (Harman and
Fomey, 1970) that were not collected in the 1992-95
survey. Only 23 species of mollusks were present in
1992-95, two of them, Ligumia recta, and Valvata sin-
cera Say, 1824 (Valvatidae), represented by dead speci-
mens only. That represents a decrease of species rich-
ness of 42% since 1917. Collections made in 1996 and
1997 by faculty and students at the Cornell Biological
Field Station on Oneida failed to find anv living unionid
bivalves (E. L. MiUs, pers. comm.). Four of the species
of mollusks found in 1993-95 were introductions. Of
those, the population of B. tentaculata had declined
greatly since the 1960s but was exceeded only by the
exotic zebra mussel, Drcissena polijmorpha. This Eur-
asian dreissenid was apparently carried through the Os-
wego River and New York State Barge Canal svstem by
commercial and/or recreational navigation from the
Great Lakes, where it was found in 1988 (Nalepa and
Schloesser, 1993). Like B. tentaculata, D. polymorpha
was supposedly transported in ballast water of ocean-
crossing ships coming from Europe. An average 10- cm-
bottom sample in 1993 contained 12 zebra mussels (fig-
ure 4). An average 1 m- sample collected at the same
time and location included 6,708 specimens of D. polij-
morpha, 60 of B. tentaculata, and 2 of Elliptio complan-
ata (Lightfoot, 1786) (£. complanatus of Baker) (figure
5). The tremendous increase results from large colonies
of D. poh/morpha initially associated with specimens of
E. complanata, which were not encountered in the 10-
cm- samples. These substrates are fine shifting sands
practicallv devoid of zebra mussels, except where the
comparatively widely disbursed unionids support their
colonies.
Harman (1968a, b) proposed that the introduced B.
tentaculata was able to displace the local representatives
of the North American family Pleuroceridae in eutrophic
environments. These observations were based on the
distributions of B. tentaculata, P. acuta, E. livescens
(Goniobasis livescens of Baker) and E. virginica in the
Oswego River drainage basin in central New York (Har-
man and Berg, 1971). Like most caenogastropod snails
of inland waters, the pleurocerids are periphyton grazers
that rely on the benthic algal community as their main
energy source. They typically inhabit waters supporting
comparatively low populations ot phytoplankton (Dazo,
1965). Bithijnia tentaculata also is a grazer but in addi-
tion it can use planktonic algae which it filters from the
water on specialized ctenidia (Jorgensen, 1966) poten-
tially giving it an advantage in eutrophic waters such as
Oneida Lake.
Observations in Oneida in the 1960s regarding the
density of Bithi/nia on rocky shoreLnes, and on the ob-
served behavior of pleurocerid snails associated with B.
tentaculata in aquaria, substantiated these ideas. In
Page 124
THE NAUTILUS,
Vol.
114,
No.
3
Table 3. Ta\a
lost (not
collected ali\'e
since
dates
indicated) followed by
assumed
major contributing factors.
Taxa
Last date
collected
Contributing factors to decimation
Bivalvia: Palaeoheterodonta
Miir^iaritifcra margaritifcra (Linnaeus, 17.58)
Elliptio complanata (Lightfoot, 1786)
Alasmidonta undulata (Say, 1817)
Pijganodon grandis (Say, 1829)
Fijganodon cataracta (Say, 1817)
Strophitus undidatus (Say, 1812)
Leptodea fragilis (Rafinesque, 1820)
Ligumia recta (Lamark, 1819)
ViUosa iris (1. Lea, 1829)
Lampsilis rndiata radiata (GmeUn, 1791)
Actinonaias ligmentina (Lamark, 1819)
Gastropoda: Basommatophora
Plu/sella gyrina {Sax. 1821)
Physelln hcterostrophn (Say, 1817)
Li/mnaea stagnalis Linnaeus, 1758
Stagnicola cmarginata (Say, 1821)
Stagnicola catescopium (Say, 1867)
Acelln haldmani (W. G. Binney 1867)
Qyranulus deflectus (Say, 1824)
Promenetus exacuous (Say, 1821)
Fenissia rivularis (Say 1817)
Gastropoda: Caenogastropoda
Campctoma decisum (Say, 1817)
Pleurocera acuta (Rafinesque, 1820)
Elimia livenscens (Menke, 18.30)
Elimia virginica (Say, 1817)
Pomatiopsis cincinnatiensis (L Lea, 1840)
Pwbi/thineUa emarginata (Kuster, 1852)
Somatogtjnis depnisstis (Tr)-on, 1862)
Valvata sincera (Say, 1824)
Valiata lewisi (Currier, 1868)
Vakata bicnrinata (I. Lea, 1841)
Total number of species: 30
1968
1995
1917
1995
1917
1917
1968
1968
1917
1993
1917
1968
1968
1917
1968
1968
1968
1968
1968
1917
1968
1917
1968
1917
1917
1968
1917
1917
Direct competition with Dreissena
Direct competition with Dreissena
Trophic alteration
Direct competition with Dreissena
Trophic alterations
Trophic alterations
Direct competition with Dreissena
Direct competition with Dreissena
Trophic alterations
Direct competition with Dreissena polymorph
Trophic alterations
polymorpha
polynwrpha
' polymotyha
polymorfiha
polymoiyha
Habitat
Habitat
Habitat
Habitat
Habitat
Habitat
Habitat
Habitat
Habitat
destniction,
destniction,
destniction,
destruction,
destniction,
destruction,
destruction,
destniction,
destniction.
trophic
trophic
trophic
trophic
trophic
trophic
trophic
trophic
trophic
alterations
alterations
alterations
alterations
alterations
alterations
alterations
alterations
alterations
Habitat destniction
Direct competition
Direct competition
Direct competition
Habitat destruction
Habitat destruction
Habitat destniction
Habitat destniction
Habitat destniction
Habitat destniction
, trophic alterations
with Bitht/nia tcntaculata
with Bithynia tentacxdata
with Bithynia tcntaculata
, trophic alterations
, trophic alterations
, trophic alterations
, trophic alterations
, trophic alterations
, trophic alterations
' Empy shells collected in 1968, not collected in 1915; assumed introduction between 1920 and 1950.
aquaria enriched with planktonic algae, pleurocericLs ac-
tively grazed over the substrate. Individuals of B. tcn-
taculata remained in one spot, filtering algae from the
water. Upon encountering specimens of B. tcntaculata,
pleurocerids were rebuffed by a violent twisting of the
shell of that filter-feeder, which invariably caused the
grazing snails to retract into their shells. They remained
in that position for several minutes before resuming
grazing. In situations with high densities of B. tcntacu-
lata, indixidual pleurocerids spent a large fraction of the
time in defensive positions rather than feeding. In Onei-
da Lake in the 1960s, euhttoral cobble substrates were,
in many areas, a solid mass of B. tcntaculata (Harman
and Forney, 1970). Under those conditions, all the spe-
cies representing the family Pleuroceridae chsappeared
from the lake (Wisenden and Bailey, 1995). Nowadays,
decreasing algal populations and increased water clarity
have occurred concurrently with irrupting populations of
D. polymorpha, while populations of B. tcntaculata have
diminished drastically.
A large number of the pulmonate gastropod species
not found in the recent sur^'ev (e.g., one species of the
planorbid genus Gyraulus, three in the family Lymnae-
idae, and two in the Physidae) are typical of eulittoral
substrates and often associated with emergent vegeta-
tion. It is unlikely that these pulmonates are completely
absent from Oneida, but their absence in the recent sur-
vey suggests drastic reductions in their populations cor-
responding with losses of that habitat due to shorehne
development. Most of the shoreline has been modified
as a result of the construction of break'waters or rip-rap.
Many of Baker's euhttoral sites appear to be buried un-
der yards and beaches created bv back-fiUing, which, bv
1993-95, had destroyed considerable areas of emergent
vegetation.
Other species of gastropods that were not found in
the 1990s include several small prosobranchs in the fam-
ily Hydrobiidae, which were typically abundant on sub-
merged plants and nearbv sub-httoral and deeper-water
substrates. These and other gastropods that historically
W. N. Harman, 2000
Page 125
have been present in abundance in Oneida Lake, were
found in very low numbers in the recent survey. An ex-
ception, Amnicola limo.su.s (Say, 1817) {Aiunicohi liinosa
of Baker), occurs in high densities in inanv littoral and
sub-littoral areas. Changes in httoral vegetation and as
vet unrecognized trophic alterations associated at least
indirecth' with colonization by D. pohjmorfiha may be
affecting these organisms (Stewart and Haynes, 1994;
Howells ct al.. 1996; Ricciardi ct al, 1997). '
Seven of the 12 species of freshwater mussels found
in Oneida since 1915 had been lost by 1993, and no
li\ing unionids ha\'e been obser\'ed since 1995 (table 3).
These losses correspond to the introduction and estab-
lishment of Drcissena pohjuunyha. The literature doc-
umenting the loss of unionid species as a result of com-
petition with D. pohjiiwiyha (Nalepa et al, 1991; Grif-
fiths, 1993; Ricciarchrffl/., 1995; Schloesser ef a/., 1996)
and observations of the interaction behA'een unionids
and D. polyinorpha in Oneida (E. L. Mills, pers. comm.)
indicate that a large percent of this loss can be assumed
to be attributed to interactions with D. poJijmotyha.
Since 1915-17, the endemic molluscan community in
Oneida Lake has been greatly modified. Species richness
has declined and the dominant faunal elements are now
Eurasian in origin (figure 5). With the exception of re-
cent changes since the introduction of zebra mussels,
water qualit)- in Oneida Lake has been consistent over
the years (E. L. Mills, pers. comm.). It is assumed the
observed changes are a result of biotic interactions with
introduced taxa and loss of habitat due to human mod-
ifications of the euhttoral emdronment.
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T H Et^N AU T I L U S
CONTENTS
Volume 114, Number 4
December 15, 2000
ISSN 0028-1344
Luiz Ricardo L. Simone
Cuido Pastorino
Pablo E. Penchaszadeh
Richard E. Petit
M. G. Harasewych
Bruce A. Marshall
Douglas G. Smith
Martin Avery Snyder
Crepiclula arg^entina (Gastropoda: Calyptraeidae), a new
species from the littoral of Argentina 127
Three new species of the genus Merica ( Neogastropoda:
Cancellariidae) from South Africa and the Philippines 142
Systematics of the genus Infundibuhiin Montfort, 1810
(Gastropoda: Trochidae) 149
On the taxonomic placement of Unio ochraceus Say, 1817
in the genus Ligiimia (Bivalvia: Unionidae) 155
Latints beckijae, a new species of Fasciolariidae
(Neogastropoda) from Brazil 161
DEC ^ 8 2000
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THE NAUTILUS 114(4):127-141, 2000
Page 127
Crepidiila argentina (Gastropoda: Calyptraeidae), a new species
from the littoral of Argentina
Luiz Ricardo L. Simone
Museu de Zoologia da Universidade
de Sao Paulo
Caixa Postal 42694
04299-970 Sao Paulo
BRAZIL
IrsinioneC&'usp.br
Cuido Pastorino'
Museo Argentino de Ciencias
Naturales
k\. Angel Gallardo 470, 3° piso, lab.
57
C1405 D]R Buenos Aires
ARGENTINA
r\pastor@criba.edu.ar
Pablo E. Penchaszadeh
FCEvN-UBA-CONICET
Museo Argentino de Ciencias
Naturales
Av. Angel Gallardo 470, 3° piso, lab.
57
C1405 DJR Buenos Aires
ARGENTINA
pablop@mail.retina.ar
ABSTRACT
Crepidiila argentina. a new species of gastropod of the famil)'
Calyptraeidae, is described from the littoral of Mar del Plata,
proxince of Buenos Aires, Argentina. The new species is con-
chologicalK similar to C. protea d'Orbignv from southern Bra-
zil. Crepidula argentina has a larger, subcircular shell and low-
er convexitv' than C. protea. Anatomical characters that allow
differentiation from this latter species are; larger lateral shell
muscle and very weak dorsal shell muscle; kidney proportion-
ally smaller, with a characteristic arrangement of inner folds of
dorsal lobe; presence of a renal vessel edging rectum and work-
ing as adrectal sinus; connection between odontophore muscle
pairs m7 and mil; longer salivary gland; four ducts to digestive
gland in stomach (instead of two); distinctive arrangement of
folds in inner surface of stomach between esophageal aperture
and posterior pair of ducts to digestive gland; seminal vesicle
of males broad and few coiled; penis and papilla long and nar-
row; vaginal tube nmning closely attached to capsule gland.
The reproductive biology is also distinctive. Crepidula argen-
tina new species has a very well defined seasonal reproductive
cycle. Females brood between 1 and 46 egg capsules per
spawn. The average total number of embrv'os per spawn is
5600. The uncleaved, laid egg diameter is 170 (xm and the
number of eggs per egg capsule is about 320. All eggs develop,
there are no nurse eggs. Larvae hatch as planktotrophic veli-
gers. The new species is compared with other members of the
genus Crepidula from the southern Atlantic coast of South
America.
Additional key word.?: Crepidula protea, anatomy, reproduc-
tion, littoral.
INTRODUCTION
Most species of moUusks described from the southern
Atlantic coast of South America are based on specimens
collected by nineteenth century expeditions. Crepidula
species are no exception. Alcide d'Orbigny (1841) de-
Author for correspondence.
scribed Crepidula protea for the first time on his large
work "Voyage dans I'Amerique Meridionale". This book
was published in several parts in different dates. Ac-
cording to Sherboni and Woodward (1901), Sherbom
and Griffin (1934), and Keen (1966) the page (465) with
the C. protea description (with no illustration) was pub-
fished on 1841. A year later in the French edition ol the
Atlas of R. de la Sagra's "Histoire ... de la File de
Cuba", d'Orbigny pubfished a plate (pi. 24, figs. 30-32)
with three illustrations of C. protea and no description
(A description was published in 1846 in the Spanish edi-
tion of the same work.) It seems clear that the intention
of d'Orbigny was to publish the chapter of mollusks in
Sagra's work before his 'Voyage ", because he cited that
other book despite its later pubfication. Crepidula protea
was described without mention of a distinct t\pe locality.
A label at The Natural Histor)' Museum, London
(BMNH) states only "Patagonia" without further geo-
graphic details. The examination of the type specimens
did not suggest any precise locafitv nor were there shell
characters that could reveal which population they had
came from.
D'Orbigny's description and illustration of Crepidula
protea clearly groups at least two different species. First
Dall (1889), and later Hoagland (1977), pointed out that
C. plana Say, 1822, and C. iin^uiformis Lamarck, 1822,
might be included within his concept of C. protea. Ac-
cording to d'Orbigny's illustrations and description this
seems to be possible.
Parodiz (1939) studied the species oi Crepidula from
Argentina with particular emphasis on the shell and, for
the first time, on the radula. Based on a large number
of lots from different localities Parodiz described and
illustrated the radula and shell of five previously known
species and two new subspecies. The subspecies are now
considered to be geographical forms. Despite that, Par-
odiz (1939) is still the most authoritative paper on the
genus Crcpidida from southern Atlantic coast of South
Page 128
THE NAUTILUS, Vol. 114, No. 4
America. Unfortunately, no anatomical descriptions or
reproductive features were described in that work. The
specimens examined by Parodiz are stiU housed at the
Museo Argentino de Ciencias Naturales (MACN) and
were re-examined in this paper Since Parodiz's pio-
neering work no further articles on Crepidula from Ar-
gentina have been published.
Hoagland (1977) published a comprehensive study of
living and fossO species of Crepidula. Although her work
was basically restricted to North America and the east-
ern Pacific, she included descriptions and pictures of C.
protea and C. dilatata as well as a few other southern
species. Hoagland (1983) described several specimens
from BrazU of what she concluded was C protea. She
recognized C. protea as a species distinct from C. plana
and C. ungitifonni.s and studied d'Orbigny's type mate-
rial of C. protea. In the same paper, Hoagland described
the larval development of C. protea based on specimens
from the southeastern Brazihan coast. Here we consider
the specimens she studied to represent actual C. protea
mainly because they are conchologically similar to the
lectotype and paralectotypes.
In an annotated Ust of several type specimens from
the coast of Argentina, Aguirre (1993) designated a lec-
totype for C. protea. Unfortunately, she selected the only
complete specimen in d'Orbigny's collection at BMNH.
She seems to have been unaware of the differences
among the southern species of this genus. Aguirre
(1993) mentioned only 4 syn types when the count is ac-
tually 16, arranged in two lots of 5 and 11 specimens
respectivelv (BMNH 1854.12.4.573 and 574) (Hoagland,
1983).
Gallardo (1977, 1979) and Brown and Olivares (1996)
described several new species of Crepidula from Chile
with distinctive reproductive patterns as diagnostic char-
acters. These authors led the way in the search for new
characters in this variable genus, showing that in several
cases the shell lacks real ta.\onomic value at the specific
level.
Hoagland (1983) and Rios (1985) pointed out that
Crepidula protea occurs from Rio de Janeiro, Brazil,
south to Miramar, in the province of Buenos Aires. How-
ever, studies on different population samples along this
range revealed that more than one pattern of reproduc-
tive strategy and anatomical characters are found, indi-
cating the presence of an unnamed species.
In this paper we describe this new species of Crepi-
dula and provide the groundwork for a future revision
of the group in the southwestern Atlantic. The new spe-
cies was originally recognized first by its distinctive re-
productive pattern and second through detailed anatom-
ical studies. Comparison with several kiiown species
from South America is presented. The study of repro-
ductive biology in the new species is the main topic of
another paper (Cledon and Penchaszadeh, submitted.).
MATERIALS AND METHODS
Fresh specimens of Crepidula argentina new species
used in this studv were collected by commercial fish
trawlers at Mar del Plata (38°00' S, 57°33' "W) and
Puerto Quequen (38°35' S, 58°42' 'W) along the coast
of the province of Buenos Aires, Argentina. Tvpes and
material examined are deposited at: Museu Oceanograf-
ico de Rio Grande, Rio Grande do Sul, Brazil (FURG);
Museo Argentino de Ciencias Naturales "Bernardino Ri-
vadavia", Buenos Aires (MACN); Museo Nacional de
Historia Natural, Montevideo, Uruguay (MHNM); Mu-
seu de Zoologia, Universidade de Sao Paulo (MZSP);
National Museum of Natural History, Smithsonian In-
stitution, Washington (USNM). The type material of C.
protea was studied at The Natural History Museum,
London (BMNH).
Specimens were fixed in fomiahn for at least 24 hours
and preserved in 70% ethanol. They were not relaxed.
All observations were made on preserved material. Dis-
sections were perfonned on 3 males and 13 females us-
ing standard techniques under a stereomicroscope with
the specimens immersed on 70% ethanol. Radulae were
prepared (two specimens of C argentina new species of
32.2 and 35 mm length and two of C. protea of 18.5 and
17.4 mm) according to the method described by Solem
(1972) and observed and illustrated using a LEO 440
scanning electron microscope (SEM) at the National
Museum oi Natural History, Washington.
Shell measurements including convexity index, were
done using the parameters established by Hoagland
(1977). Most photographs were taken using a Nikon N70
with a 60 mm Nikkor macro lens. These images were
latter scanned from black and white 35 mm negatives
using a Nikon Coolscan III slide scanner All images and
plates were processed with the software Photoshop 5.02.
In the figures and text, the following abbreviations are
used: aa, anterior aorta; ab, auricle region beyond ven-
tricle connection; ac, anterior extremity of gill on mantle
border; ag, albumen gland; an, anus; au, auricle; bb,
bulged part of br; bg, buccal ganglion; br, subradular
membrane; bv, mantle blood vessel inserting in kidney;
eg, capsule gland; cv, ctenidial vein; da, aperture of duct
to digestive gland; dd, duct to digestive gland; dg, di-
gestive gland; dm, dorsal shell muscle; dp, posterior
duct to digestive gland; ea, esophageal aperture; en, en-
dostv'le; es, esophagus; fd, dorsal surface of foot; fg,
food groove; fl, female papilla; fp, female pore; ft, foot;
gd, gono-pericardial duct; gi, gill; gs, gastric shield; bg,
hypobranchial gland; in, intestine; ir, insertion ol m4 in
tissue on radula preceding its exposed (in use) portion;
iu, U-shaped loop of intestine on palhal roof; kd, dorsal
lobe of kidney; Id, kidney; kv, ventral lobe of kidney
attached to intestine; 11, left lateral ex-pansion (Hap) of
neck; hn, lateral membrane restricting paUial cavity; ml
to ml4, odontophore muscles; mb, mantle border; mj,
muscles of jaws and mouth; ml, mantle region restricting
palhal cavity; mo, mouth; mr, mantle reinforcement;
mt, mantle; ne, nephrostome; nr, nerve ring; ns, neck
"sole"; oc, odontophore cartilage; os, osphradium; ov,
paUial oviduct; oy, ovary; pc, pericardium; pd, penis
sperm groove; pe, penis; pg, pedal gland anterior fur-
row; pp, penis papilla; pr, propodiuni; pt, palfial sperm
L. R. L. Simone et ai, 2000
Page 129
Table 1. Shell morphometries of Crepidula argentina new
species. Linear measurements in mm.
Speci-
Septum
Convex-
men
Total
Diam-
Septum
free
ity
#
length
Height Width
eter
length
area
D/L
1
31.5
6.3
25
37
13.4
17.9
1.17
2
35.7
7.7
24.7
41
15.1
19.8
1.14
3
32.8
8.6
23.1
39
17.6
17.5
4.18
4
35.8
8.9
25
42
17
19.4
1.17
5
33.8
8.8
27
43
13.7
21.8
1.27
6
28.1
7.1
21.7
36
11.8
16.4
1.28
(
32.6
7.3
22.5
39
13.3
17.6
1.23
8
30
7.3
23.4
37
13.3
16.8
1.14
9
29.8
7.1
23.9
34
12.3
16.3
1.14
10
33
9.3
28
41
14.4
19.3
1.24
groove; ra, radiila; rl, right lateral expansion (flap) of
neck; m, radular nucleus; rs, radular sac; sc, subradular
cartilage; sg, salivary gland; sn, snout-proboscis; sp, ap-
erture of vas deferens into pallial cavity; ss, style sac; st,
stomach; sv, seminal vesicle; te, cephalic tentacle; tm,
net of transversal muscles of haemocoel; to, tissue cov-
ering middle region of radula before its exposed part;
ts, testis, vc, visceral connection with haemocoel; ve,
ventricle; vg, vaginal duct; vm, visceral mass; vo, visceral
oviduct; vs, vesicles of pallial oviduct.
SYSTEMATICS
Class Gastropoda Cuvier, 1797
Subclass Orthogastropoda Ponder and Lindberg, 1996
Superorder Caenogastropoda Cox, 1960
Order Sorbeoconcha Ponder and Lindberg, 1997
Family Calyptraeidae Lamarck, 1809
Genus Crepidula Lamarck, 1799
Crepidula argentina new species
Figures 1-21, 28^6
Crepidula protea: Parodiz, 1939: 702, fig. 8, pi. 1, fig. 6 (not
d'Orbigny, 1841).
Diagnosis: Shell: Large and wide, slightly convex. Pro-
toconch smooth, with 1% whorls. Aperture elhptical.
Beak solid, very small. Septum planar, septum margin
with sulcus on left side and clear notch in center. Muscle
scars absent. Shell externally opaque white, internally
white porcelanaceus. Periostracum absent.
Anatomij: Large lateral shell muscle. Dorsal shell mus-
cle weak. Kidney proportionally smaU, with characteristic
arrangement of inner folds of dorsal lobe, renal vessel
edging rectum. Connection between odontophore mus-
cle pairs m7 and mil. Long salivary glands. Four gastric
ducts to digestive gland, distinctive arrangement of folds
(sorting area) in inner surface of stomach between
esophageal aperture and posterior pair of ducts to di-
gestive gland. Seminal vesicle broad and few coiled. Pe-
nis and its apical papilla long and narrow. Vaginal tube
running attached to capsule gland.
Description: Shell (Figures 1-15, 20, 21): Large (up
to 40 nun in length) and wide, thin (0.35—0.45 mm in
thickness), slightly convex, convexity = 1.20 (see table 1
for other measurements), male specimens very thin,
brittle, transparent, planar shells. Protoconch smooth,
with 1% whorls, transition to teleoconch clearly defined.
Aperture elliptical or subcircular. Beak .soUd, very small,
turned to right on females, almost central on males, at
level of or only slightly above margin, in males never
reaching margin, in females never extended beyond it.
Septum planar (never convex), with central ridge almost
imperceptible but present, margin of septum with sulcus
on left side and clear notch in center, covering less than
half of aperture, color bright white with translucent
edge. Muscle scars absent. Growth lines covering entire
shell. Shell externally opaque-white, internally porcehiin-
white; some specimens externally with diffuse radial or-
ange lines and/or internally with radial brownish lines.
Males always translucent-white externally and bright-
white internally. Periostracum absent.
Head-foot (Figures 28, 30, 34, 43): Head protruded, at
the end of long (about same length as foot), dorso-ven-
trally flattened, neck region. Snout short and cylindrical,
able to retract and partially invaginate for about half of
its length within haemocoelic cavity. Tentacles long,
stubby, tip somewhat rounded. Eyes dark, situated on
low ommatophores about midway on lateral margin of
tentacles. Neck region with pair of lateral, flattened ex-
pansions (nuchal lobes); right nuchal lobe bears shallow
food groove along its limit with head (figure 28). Sperm
groove of males (described below) running externally
along food groove (figure 43). Ventral surface of neck
region forming an additional, anterior "sole" (figure 30).
Foot veiy ample (occupies about % of shell aperture),
dorso-ventrally flattened. Shell septum defining dorsal
limit of foot. Mantle fusing with dorsal surface of foot
and protruding beyond its borders. Furrow of pedal
glands transversal, located on central region of anterior
margin of foot (about 1/3 of its width); a small, pointed
expansion present on each side of furrow (figure 30).
Anterior margin of foot covering ventrally posterior re-
gion of neck "sole". Columellar muscle very reduced,
small flap contouring anterior border of shell septum,
only evident on right side. Inner haemocoelic cavity nar-
row, running approximately along center of neck region,
almost entirely filled by mass of salivary glands (de-
scribed below) and numerous, transversal, very slender
muscle fibers (figure 34); these fibers connect ventral
surface of dorsal haemocoelic wall with dorsal surface of
its ventral wall.
Mantle organs (Figures 29, 31-33, 44): Mantle border
very thick, edging entire ventral inargin of sheU, free on
its anterior half and attached to foot edge on its posterior
half. Mantle border without appendages, but entirely
covered by a series of minute glands. Mantle border with
Page 130
THE NAUTILUS, Vol. 114, No. 4
Figures 1-15. Shells of Crepidula argentina new species. 1-3. Holotvpe, MACN .3450S, Mar del Plata, Buenos Aires, Argentina.
4-5. Paratope, MACN .34.509, Mar del Plata, Buenos Aires, Argentina. 6-7. Paratope, MACN .34509. Puerto Quequen. Buenos
Aires, Argentina. 8-9. Paratype. 10-11. Paratype, MACN .34.509, male specimen, scale bar on right side of figure 11 = 0.5 mm
(for figures 10 and 11). 12-13. Paratjpe, MACN .34509 14-15. Parat>pe, MACN .34509. Scale bar under figure 8 = 1 cm for all
specimens, except figures 10 and 11.
L. R. L. Simone ci ai, 2()()()
Page 131
Figures 16-21. Crepidula argentina new species. 16-17. Radula 16. Radula, frontal view. Scale bar = 30 \x.m. 17. Radula,
marginal teeth, scale bar = 30 jxni. 18-19. Penis, critical-point dried. 18. Dorsal view. Scale bar = 200 (xni. 19. Ventral \iew.
Scale bar = 200 \Lm. 20-21. Protoconch. 20. Dorsal view. Scale bar = 300 ^.m. 21. Detail of figure 20. Scale bar = 100 p-ni.
characteristic arrangement of folds along central region
of aperture of pallial cavity (figure 33), a broad furrow
beginning on anterior extremity of gill, running toward
left side, and ending at about right third of osphradium;
this thick fold presents broad central furrow. Dorsal shell
muscle apparently lacking in most specimens, very re-
duced and difficult to observe in others (figure 29). Lat-
eral shell muscle well developed, inserting broadly in left
lateral region of mande border and region posterior to
it, originating shortly in inner shell surface in region
close to left anterior edge of shell septum. Pallial cavity
aperture occupving about 2/3 of anterior half of shell
border, turned to right (drawing an analogy between
shell in dorsal view and a clock, with head occupying
12:00, pallial aperture occupies a sector beginning at
9:00 and ending at 2:00). Pallial cavity deep, broad, tri-
angular, arched and flattened dorso-ventrally (figure 29).
Anterior extremity of pallial cavity slightly larger than its
aperture due to constriction on left and right extremities
produced by fusion of mantle and foot (figures 31, 44).
Pallial ca\ity narrows gradually in posterior direction,
penetrating left side of visceral mass (described below);
cavity length about 3/4 of total length of animal. Os-
phradium (figure 33) long, monopectinate, located be-
tween anterior region of gill and mantle border, occu-
pying about middle region of pallial aperture, somewhat
perpenthcular to longitudinal axis of animal, compressed
between gill and mantle border. Osphradium length
slightlv exceeding 1/5 of palfial aperture length. Osphra-
dium leaflets long, somewhat thick, closely packed, with
rounded tip. Gill very large, with somewhat narrow base,
edging anterior and left margin oi pallial cavity along
almost its entire length; anterior extremity of gill in an-
terior and left region of pallial cavity aperture, near its
Page 132
THE NAUTILUS, Vol. 114, No. 4
Figures 22-27. Crepidula protea dOrbigiiy, 1841. 22-24. Shell, MACN 34511, off Ubatuba, Sao Paulo, Brazil, 2.3°30' S, 44°54'
W, 42 m, dorsal, ventral, and lateral \iews of the same specimen. 25. Shell, MACN 34511, other specimen in lot, ventral view.
Scale bar = 1 cm for all shells. 26. Radula, frontal view. Scale bar = 100 |j.m. 27. Protoconch, dorsal view. Scale bar = 300 (Am.
right limit, on thick mantle border; posterior extremity
of gill in posterior end of palhal cavaty (figure 32). Base
of gill filaments triangular. Gill filament with very long,
almost straight, stiff rod extending to right; rods extend
for about twice as long as their triangular, membranous
base; these rods begin in region of ctenidial, in left mar-
gin of cavity roof, touching food groove of head-foot, in
right margin of cavit)' floor Rod apex rounded and pre-
ceded by a thicker region. Gill filaments connected to
each other by cUia, mainly along their thicker apical re-
gion, which helps maintain somewhat gill structure. Gill
filaments longer in central region of gill, shortening
gradually toward both extremities. Anterior extremity of
gill with short filaments, abruptly turning foiAvards, end-
ing at mantle border (figure 33). Ctenitliiil vein cylin-
drical. Endostyle well developed, yellowish (a somewhat
narrow glandular ridge located on ventral surface of
ctenidial vein and present along its entire length) (figure
33). Hvpobranchial gland whitish, low, slightly devel-
oped, occupying surface between gill and visceral mass
(figures 1, 5). About 1/3 of visceral mass encroaches on
pallial cavity roof, occupying about 1/3 of posterior and
right sectors of this region; pericardium and kidney lo-
cated in posterior part; long intestinal loop, anus, and
palhal oviduct in anterior part (described below).
Visceral mms (Fiffircs 2.9, 31, 32, 44): A dorso-ventrally
flattened cone lying in shell chamber produced by sep-
tum. Thin calcareous septum separating visceral mass
from dorsal surface of foot. Left and anterior region of
L. R. L. Simone ct at., 2()()()
Page 133
30
31
Figures 28-31. Anatomy of Crepklula argentina new species. 28. Female animal with shell, visceral mass, and pallia! cavity-
removed, dorsal view, 29. Same animal, whole, dorsal view. 30. Same, ventral view. 31. Isolated visceral mass and pallial cavity,
ventral view. Scale bar = 5 mm.
visceral ma.ss occupied by palLal cavity (figures 31, 44).
Remaining region of visceral mass with stomach as central
structure, immetliately and iilmost completely surrounded
by digestive gland (except in some ventral and dorsal
parts). Gonad surrounding digestive gland externally.
Visceral mass encroaching on right and posterior re-
gions of palli;il cavitv roof. Anterior extremity of visceral
mass (ventral to posterior pallial cavity region) covering
columellar muscle just posterior to anterior border of
shell septum.
Page 134
THE NAUTILUS, Vol. 114, No. 4
L. R. L. Simone et a/., 2000
Page 135
Circidatani and cxcrctoni si/.stciii.s (Figures 29, 35);
Peric-archiini \en loiiij, soiiiewhat peqieiidicular to loTi-
gitialinal avis ot animal (figure 29); verv' narrow in pos-
terior extreniit)' of gill (posterior and left end of pallial
cavity); running along anterior margin of xasteral mass
where it encroaches on piillial roof, enlarging gradually
and ending at about middle level of this region of vis-
ceral mass, near its mechan line. Pericartlium circum-
scribes (1) palhal cavit)' in anterior and ventral direction,
(2) visceral mass (mostlv gonad) in posterior direction,
(3) mantle in dorsal direction, and (4) kidnev to right.
Auricle thin-walled and vew long, running long entire
pericardium length, attached to its anterior and dorsal
inner surfaces; auricle connects with ventricle approxi-
matelv along its middle and right thirds; auricle portion
beyond connection with ventricle represented by broad
binil sac. Ventricle elliptical, veiT muscular, its connec-
tion with auricle located about middle region of its an-
terior surface; aortas originating in opposite side. Ante-
rior aorta broad, directed awav from posterior aorta. An-
terior aorta directed toward right, edging posterior inner
surface of pericardium. Anterior aorta penetrates head
haemocoel. Kidney small, occupying about 1/4 of area
of visceral mass when projected on inner surface of pal-
lial cavity. Kidnev circumscribes (1) mantle in dorsal ch-
rection, (2) pallial ca\ity in ventral and left lateral direc-
tion, (3) visceral mass (mostly gonad) in posterior and
right direction, (4) pericardium in posterior and left di-
rection, (5) an intestinal loop in anterior direction, (6)
intestine and oviduct (when present) in lateral right di-
rection. Kidney mostly hollow, with pair of veiy irregu-
larly shaped lobes. Ventral lobe with several, slight nar-
row transverse folds attached to posterior surface of ad-
jacent intestine. Dorsal lobe occupies most of dorsal and
lateral surfaces, bearing several irregular folds in left di-
rection; part of lobe covering ventral surface around
nephrostome. Nephridial gland thin, present along
boundary between kidney and pericardium, bearing se-
ries of transverse, narrow folds connected with dorsal
renal lobe. Nephrostome a very small sht in left region
of ventral wall. A broad vessel connected with left ex-
tremity of kidney and ninning along external pallial loop
of intestine for about % of its length.
Digestive system (Figures 29, 31, 32, 34-42): Mouth
longitudinal, in center of anterior surface of snout (figure
34). Buccal mass very large, occupying most of inner
space of snout. Buccal mass capable of some protraction
and invagination. Dorsal wall of buccal mass with pair
of broad and thin jaw plates. Pair of df)rsal folds broad
and low, connected to jaws in posterior direction. Odon-
tophore large, consisting of most of volume of buccal
mass. Odontophore muscles (figures 36-38, 40, 41):
(ml) jugai muscles, several verv narrow muscles con-
necting buccal ma.ss to adjacent wall of snout, more con-
centrated anteriorly around mouth; (mla) pair of dorsal
protractor muscles, narrow, thin and superficial, with or-
igin in antcro-dorsal region of mouth, close to its median
line, insertion in posterio-dorsal and lateral region of
odontophore; (mj) jaws and peribuccal muscles, some-
what thick, surrounding lateral and dorsal wall of buccal
mass, with origin around mouth, insertion in middle re-
gion of lateral and dorsal wall of odontophore; (m2) pair
of retractor muscles of buccal mass (retractor of phar-
ynx), broad, with origin in latero-ventral region of hae-
mocoel just posterior to snout, nmning in anterior di-
rection, with insertion in postero-Iateral and dorsal re-
gion of odontophore cartilages; (m2a) pair of dorsal ten-
sor muscles of radula, continuation of m2 after insertion
in cartilages, nmning in anterit)r direction, with insertion
in subradular cartilage in middle region of its dorsal in-
ner surface; (mt) dorsal transversal muscle or ventral ap-
proximator muscle of cartilages, connecting dorsally pos-
terior-dorsal and lateral surface of both cartilages, lying
between superficial membrane that covers odontophore
and tissue on middle region of radula (to); (m4) pair of
median dorsal tensor muscles of radula, very large and
thick, with origin in ventral-central and posterior region
of odontophore cartilages, running along their middle
region, contouring meso-ventral surface of cartilages,
running along their dorsal surface, with insertion in dor-
sal-posterior and medial extremity of subradular carti-
lage; (mSf) pair of median radular tensor muscles, thick,
with origin in meso-posterior and dorsal regions of odon-
tophore cartilages, just adjacent to m2 insertion and m2a
origin, crossing middle region of m4, running toward
medial region of m4, with insertion along radular sac on
both sides (each branch of m5 nms along a side of rad-
ular sac, medially and dorsally); (m6) horizontal muscle,
very' thin, uniting anterior half of odontophore cartilages,
with insertion on their dorsal margin; (m7) pair of ven-
tral tensor muscles of radula, thin and narrow, with or-
igin in meso-anterior margin of m4, running in posterior
direction adjacent to subradular membrane, bifurcating
in posterior region of odontophore, median branch con-
necting with that of other member of pair and inserted
in meso-posterior region of radular sac, lateral branch
connecting with mil; (m8) pair of strong muscles with
origin in postero-dorsal and lateral region of odonto-
phore cartilages just adjacent to insertion of m2, nmning
along and attached to dorsal margin of odontophore car-
Figures 32-36. Anatomy oi Crepidula ar^entina new species. 32. Pallial cavity, ventral view, part of visceral mass deflected, some
gill filaments of central part of gill removed. 33. Detail of mantle border and pallial cavity at anterior extremity of gill. 34. Head
and haemocoel, ventral view, foot and neck "sole" removed. 35. Detail of visceral mass at border of pallial cavit)-, adjacent to
pericardial structures, ventral view, ventral surface of pericardium and kidney membranes removed. 36. Buccal mass, dorsal view.
All scale bars = 1 nun.
Page 136
THE NAUTILUS, Vol. 114, No. 4
mo
ra
to \
37
mil / .
m rnl4
40
L. R. L. Simone et al., 2000
Page 137
tilages, with insfrtioii in their antero-tlorsal region ad-
jacent to horizontal muscle (m6); (ni9) pair of dorso-
medial tensor muscle of radula, broad and thin, with
origin along ineso-dorsal surface of radular sac (in its
region internal to odontophore), crossiTig to dorsal sur-
face, with insertion in dorso-ventral margin of suhradn-
lar cartilage; (mil) small, narrow pair of muscles, with
origin in meso-ventnd region of mouth, nmning in pos-
terior direction along its median line, penetrating in me-
dian region of odontophore, rumiing between m7 and
m4, with insertion in anterior region of subradular mem-
brane; (ml4) pair of broad and thin muscles, with origin
in postero-dorsal region of otlontophore, close to origins
of m2 and m5, nmning in antero-ventral direction, with
insertion in inner ventral surface of snout at about mid-
dle region of odontophore; to) tissue covering mitldle
region of radida within odontophore, along its dorsal sur-
face; br) subradular membrane, covering ventral surface
of subradular cartilage and some neighboring areas.
Radula taenioglossate, short, measuring little more
than odontophore length (figures 37, 38). Rachidian
tooth tall, narrow with cin^ved, convex base, central cusp
ver) large and shaqi, at least two weak denticles on each
side decreasing in size toward lateral teedi, no basal
cusps but pair of lateral reinforcements present along
borders. Lateral tooth broad (about 3 times rachidian
width), curved inward, with conspicuous apical cusp
turned toward rachidian line and 5-7 short, triangular
denticles along edge on marginal side and 2—3 very
weak denticles on edge on rachidian side, denticles de-
creasing in size in both directions, disappearing at about
middle region of tooth, only a thickened border remain-
ing. Marginal teeth long, curved, tall, tip sharply pointed,
with serrate inner margin (at least 7 denticles); inner
marginal tooth broad, about twice as wide as outer mar-
ginal tooth.
Pair of buccal ganglia large, close together near me-
dian line (figure 37), situated between buccal mass and
adjacent esophagus. Salivary glands very long, tubular,
coiled (about 3 times longer than haemocoel length
when straightened) (figure 34). Several narrow trans-
verse muscles unite internally dorsal and ventral surfaces
of haemocoel, passing both sides of salivary glands,
esophagus, and aorta (figure 34). Salivary glands not
passing through nerve ring. Ducts of salivary glands
thick, running to dorsal surface of buccal mass, pene-
trating adjacent wall of buccal mass; apertures small,
close to site of penetration, located in anterior region of
dorsal folds of buccal mass (figure 36).
Esophagus narrow and long (figure 39). Inner surface
of anterior esophagus with a pair of broad folds. Middle
esophagus with pair of narrow folds (continuation from
those of anterior esophagus) and moderately spacious
glandular chamber. Iimer surface of posterior esophagus
with 4—5 longitudinal, narrow, folds of similar (hmen-
sions. Stomach (figures .39, 42) large, slightly conical, oc-
cupying about half of visceral mass; esophagus inserting
in left side of its po.sterior region of stomach, adjacent
to region of shell apex. Four ducts to digestive gland
present: anterior pair narrow, inserted in ventral surface,
between insertion of esophagus and posterior gastric
end, one turned in anterior direction and other to op-
posite side; posterior pair of ducts thick, located in mid-
dle region of ventral and left surface of stomach, one at
considerable distance from other. Stomach graduallv
narrows in anterior and left direction, close to left and
posterior extremity of paUial cavity. Stomach inner sur-
face (figure 42) with p;ur of narrow and long folds, both
with origin adjacent to insertion of esophagus, lining
posterior surface of stomach, gradually disappearing in
direction posterior to apertures of anterior ducts to di-
gestive gland. Gastric shield thin, presenting transversal
folds marking a somewhat elfiptical, ccjucave area. An-
terior half of stomach with a pair of slight tall, longitu-
dinal folds; posterior region between both folds smaller
than anterior region; smaller region as intestinal branch
of stomach; broader (anterior) region as style sac. Di-
gestive gland pale-brown in color, surrounding stomach
except for some spots in dorsal and ventral surfaces.
Intestine very narrow and sinuous (figure 39); running
from left to right adjacent to anterior border of stomach,
running up near median fine to right and anterior ex-
tremity of visceral mass; in this region and toward left,
it surrounds right and anterior border of kidney, turning
suddenly to right and nmning pandlel to preceding loop;
both loops exposed along pallial roof (figures 29, 32, 35,
39). Anus small, sfightly siphoned, situated in right re-
gion of pallial cavity close to mande border (figures 31,
32, 39). Last loops of intestine contiiin numerous, small,
somewhat elliptical fecal pellets.
Male genital sifstem {Figures 43. 44, 46): Only small
specimens (up to 9 mm) are functional males. Testis sit-
uated in anterior region of visceral mass, color orange.
Seminal vesicle convoluted, very thickened, color cream,
situated in anterior and right region of visceral mass,
where it abruptly narrows, becoming very slender and
opening in postero-ventral and right region of pallial cav-
itv. A shallow groove runs from this aperture to penis
liase, on pallial floor near right margin of head. Sperm
groove better defined and deeper in anterior direction.
Penis long (about 3 times tentacle length), curved, orig-
Figures 37-41. Anatomy oi Crcpidiila nruentina new species. 37. Buc'c;il mass, ventral \iew. 38. Odontophore, dorsal view, some
muscles sectioned and deflected, part of right region of subradular curtilage remo\ed to show muscular insertions in it. 39. Digestive
tubes seen in situ with visceral mass as a transparent structure, ventral view. 40. Odontophore, ventral view, superficial membrane
and muscles removed, nght mj (left in figure) also removed. 4L Odontophore, ventral view, radular sac deflected and only partially
shown, odontophore cartilages deflected from each other, right m4 (left in figure) deflected downward. All scale bars = 1 mm.
Page 138
THE NAUTILUS, Vol. 114, No. 4
L. R. L. Sinione et al, 2000
Page 139
inating dorsallv to right tentacle. Papilla on penis tip,
very long, about half of penis length. Penis duct opened,
running along middle region of ventral surface of penis
to tip of papilla.
Female genital st/stem (Figures 29, 31, 32, 35, 45):
Ovarv pale brown, surrounding digestive gland, denser
in anterior region of visceral mass (figures 29, 31). Vis-
ceral oviduct \er\' narrow, ninning from left to right in
anterior border of \asceral mass. Gonopericardial duct
well developed, slightlv thicker than visceral oviduct,
with origin in ventral and right extremitv of pericardium
(figure 35); nmning along visceral glands encroached in
pallial cavity; inserted in posterior extremity of pallial
oviduct where it joins insertion of visceral oviduct. Al-
bumen gland long, moderately thick, whitish; walls thick,
glandular; situated in anterior and right extremity of vis-
ceral mass; 3 to 4 seminal receptacles inserted along
right surface of albumen gland. Capsule gland a contin-
uation of albumen gland, marked by sudden increase of
secretorv tissue in wall and bv turn toward left; walls
irregular, thick, glandular. Vaginal tube moderately nar-
row, originating in posterior region of capsule gland, run-
ning attached to this latter up to its right limit, where it
abniptlv turns in ventral direction to form tall genital
papilla. Papilla with p;ur of low folds iimning along its
posterior side, from base almost to tip; folds close to
each other with narrow furrow in between. Female gen-
ital pore situated in tip of papilla (figures 31, 32, 45) sfit-
hke, transversal, with posterior and anterior edges slight-
ly projected.
Etymology: The specific epithet, a noun in apposition,
refers to the name of the countiy where the species oc-
curs, Argentina.
Type locality: Mar del Plata, Buenos Aires, Argentina
in 35-50 m, on shells of Mytiliis cdiilis platcnsis
d'Orbigny, 1846.
Type material: Holotyjie, MACN 34508; 20 paratv-
pes, MACN .34509 (10 dn,' specimens) and MACN
34510 (10 specimens preserved in ethanol); 6 paratypes,
MLP 5578; 16 paratypes (3 males, 13 females) MZSP
32152; 6 paratypes USNM 2016009 (1 specimen pre-
served in ethanol); MHNM, 6 specimens without num-
ber; 6 paratypes MHNM 15105; all from type locality.
Additional material examined: MACN 18504, 39
specimens, Puerto Quequen, Buenos Aires; MACN
8887, 9 specimens, off Mar del Plata, in 46 m; MACN
11367, 36 specimens; MACN 9361^9, 5 specimens;
MACN 18374, 2 specimens; MACN 8653, 4 specimens;
MACN 11586, 27 specimens; all from Mar del Plata;
MACN 20529-1 more than 60 specimens, mouth of Rio
Negro.
Literature record.s: Due to similarities with C pro-
tea, most hteratnre records should be re-checked from
now on. Records cited by Parodiz (1939) were revised
and are included in the material examined.
Di.stribution: Province of Buenos Aires, Argentina,
from Mar del Plata to the mouth of Rio Negro, on banks
of Mytiltis edulis phiten.sis, 35-50 m depth. Records
from Uiiiguav and Brazil need to be confirmed.
Reproductive pattern: Crepidula argentina new spe-
cies is a protandrous hermaphrodite that undergoes
complete sex change. Males mature at about 4 mm
length. Sex change begins when individuals reach ap-
proximately 9 mm and is completed when the first pre-
vitelogenic ovocites appear, usually at around 11 mm
length. The smallest broochng female we found was 15.0
mm length and the largest 39.0 mm.
The new species has a well-defined seasonal repro-
ductive cycle. Between September and March more
than 30% of the females are brooding, with maximum
brooding in January (57%). In June and July brooding is
uncommon (0-10%). Females l)rood 1—46 egg capsules
per spawn. The average number of embryos per spawn
is 5600. There is no correlation between size of the fe-
male and number of egg capsules or eggs per spawn.
However, female size, capsule size, and the average
number of embryos per capsule are positively correlated
(Cledon and Penchaszadeh, submitted). Uncleaved egg
diameter is 170 |xm and there are about 320 eggs per
egg capsule. All eggs develop, there are no nurse eggs,
and the onlv extra-embi"vonic nutritit)nal source is the
intracapsular liquid. There is no record of cannibalism
in early or advanced stages of development. The embry-
os hatch as plauktotrophic veliger lanae.
DISCUSSION
Crepidula argentina new species is usually foimd on the
posterior edge of fiviug shells of Mytiliis edulis platensis
d'Orbigny, 1846, typically in association with Calyp-
traeotheres gaiihi (Fenucci, 1975) (Crustacea: Brachi-
ura). Mvtihd banks, distributed all around the coast of
Argentina (Penchaszadeh, 1971a) are a suitable habitat
for Crepidula argentina.
Crepidula argentina was included by different authors
(Parodiz, 1939; Hoagland, 1977; 1983,' in part) in C. pro-
tea and referred to as C. ungiiifonnis bv Penchaszadeh
(1971b: 480). The t\pe specimens of C. protea were ex-
amined by Hoagland (1983). At BMNH, there are two
lots with 5 and 11 syntypes under the numbers
18.54.12.4.573 and 574 respectively. Aguirre (1993) des-
ignated and illustrated the only whole specimen as lec-
totype plus tvvo paralectotypes, with no mention to
Figures 42-46. Anatomy of Crepidula an^cntina new species. 42. Stomach, ventral view, inner surface exposed by means of a
longitudinal incision. 43. Head of male, dorsal view. 44. Visceral mass and adjacent part of pallial cavity, male, ventral view; 45.
Pallial oviduct, ventral view. 46. Penis, ventral view. All scale bars = 1 mm.
Page 140
THE NAUTILUS, Vol. 114. No. 4
Hoagland's paper or d'Orbigny's (in Sagra) illustrations.
Most of the type specimens are smaller than 30 mm and
have the conchological attributes of what Hoagland de-
scribed for C. protea from Brazil. In terms of shell char-
acters, C. protea and C. argcntino new species are sim-
ilar. Measurements of C. argentina in Table 1 are iden-
tical to those given to C. protea by Hoagland (1977).
However, in a later paper, Hoagland (1983) mentioned
that the largest specimen of C. protea was 20 mm long.
Therefore, we suspect that both species were combined
under the name C. protea in her 1977 paper Crepidida
argentina is larger and wider, particularly in young spec-
imens. Crepidula protea has an elliptical aperture with
a thicker and more convex shell, while the new species
has a subcircular aperture and a thinner and flatter shell.
Both species differ primarily in their anatomical features
and reproductive strategy'. Further anatomical study of
C. protea is provided in another paper (Simone, sub-
mitted); some data from that paper are here discussed
for comparative purposes. Crepidula argentina differs
moq^hologically from C. protea in that C. argentina has:
1) a more developed lateral shell muscle, 2) a poorly
developed dorsal shell muscle, 3) the kidney proportion-
ally smaller and with a different arrangement of inner
folds of dorsal lobe, 4) presence of a renal vessel edging
rectum and working as adrectal sinus, 5) a connection
between odontophore muscle p<iirs m7 and mil, 6) a
longer salivary gland, 7) four ducts to digestive gland in
stomach, instead of two, 8) different arrangement of
folds in inner surface of stomach between esophageal
aperture and posterior pair of ducts to digestive gland,
9) seminal vesicles of males broader and less coiled, 10)
penis and papilla longer and narrower, and 11) vaginal
tube running closely attached to capsule gland.
Embyological features of Crepidula argentina are very-
distinct from those of C. protea (fide Hoagland, 1983).
The total number of embryos per spawn and per egg
capsule and the size range of brooding females are die
most remarkable differences. Furthermore, Hoagland
(1986) described later stages of developing embryos (ve-
liger stage) as pinkish in color and embedded in a sticky
gelatinous matrix in which the embryos did not move
freely. We never observed this in pre-hatching stages of
C. argentina.
It is possible to differentiate several species of Cre-
pidula along die southern Atlantic coast of South Amer-
ica. Parodiz (1939) cited five species of Crepidula for
the Argentine coasts: C. ddatata Lamarck; C. aculcata
(Gmelin); C protea d'Orbignv; C onyx Sowerby and C.
tinguiformis Lamarck. Specimens of Crepidula ungui-
fonnis were described by Parodiz as usually associated
with hermit crabs. The distribution of C. unguifonnis is
given by Hoagland (1977) as restricted to the Mediter-
ranean Sea and Northern Africa. It is probable that "C.
unguifonnis" sensu Parodiz is a distinct, perhaps un-
named, species. Crepidula oni/x from the northern Pa-
cific was cited by Parodiz (1939) as Uving in northern
Patagonia. However, Hoagland (1977) based on Parodiz's
drawing of the radula of C. onyx presumed that "C.
onyx" sensu Parodiz is a different species: C aph/sioides
Reeve, 1859. The latter species was cited as a sviionyin
of C. onyx by Parodiz (1939). Hoagland (1977) described
C. aphjsioides as a different species ranging from Gre-
nada south to Brazil and Argentina. Reeve's Upes were
not examined. This type material includes four speci-
mens and is housed at the BMNH (Reg. Number;
1977137). As far as we know, there is no species similar
to C. aphjsioides Reeve on the coast of Argentina.
The study of the family Calyptraeidae and the genus
Crepidula in particular is less than finished for the re-
gion in study. It is expected that additional new species
will be detected and described following detailed studies
on anatomy and reproductive biology of these moUusks.
ACKNOWLEDGMENTS
We thank the following people for access to material in
their collections: K. M. Way (BMNH); A. Tablado
(MACN); and C. Ituarte (MLP). We are grateful to two
anonymous reviewers for thorough revision and helpful
suggestions that considerably improved the clarity of the
manuscript.
Several SEM pictures were taken during a short-term
visit to the National Museum of Natural History, Smith-
sonian Institution, Washington, DC. This study was sup-
ported in part b\' a Cooperative Argentina-Brazil-Chile
Research Grant from Fundacion Antorchas, Argentina,
a grant to L. R. L. Simone from Funda^ao de Amparo
a Pesquisa do Estado de Sao Paulo (FAPESP grant # 96-
06756-2) and the project BID 802/OC-AR-PICT No. 01-
04321 from the National Agency for Scientific and Tech-
nique Promotion, Argentina.
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Veliger 14:327-336.
THE NAUTILUS 114(4): 142-148, 2000
Page 142
Three new species of the genus Merica (Neogastropoda:
Cancellariidae) from South Africa and the PhiUppines
Richard E. Petit'
M. G. Harasewych
Department of Invertebrate Zoology
National Museum of Natural History
Smithsonian Institution
Washington, DC 20560-0118 USA
ABSTRACT
Three new species of the cancellariid genus Merica are de-
scribed: Merica lussii from South Africa, and M. deijnzeri and
M. ektijphos from the southern Philippines. The South African
Merica lussii has previously been misidentified in the literature
as Cancellaria bifasciata Deshayes, 1830, a junior subjective
synon\Tn of C oblonga Sowerby, 1825, from which it differs in
having a broader, stepped spire, a proportionally shorter but
broader aperture, and a deeply impressed sutural canal. Merica
deijnzeri differs from other Philippine species of Merica by its
deeply impressed sutural canal, its much stronger and coarser
axial and spiral sculpture, more rounded apert\ire, and its lack
of banding pattern. Merica ektt/phos can be distinguished from
all other described species of Merica in its distinctively heavy,
inflated shell, as well as by its extremely coarse axial and spiral
sculpture.
Additional key words: Gastropoda, Caenogastropoda, Recent,
western Pacific.
INTRODUCTION
Merica was originally proposed as a subgenus of Can-
cellaria by H. and A. Adams (1S54: 277) to distinguish
those species with reticulate sculpture, oblique colu-
mellar folds and an internally lirate outer Up, but lacking
a prominent emargination or notch on the outer lip at
the base of the siphonal canal. This taxon has been ac-
corded generic status in most twentieth century works
(e.g., Habe, 1961; Petit, 1974; Noda, 1980; Verhecken,
1986a, 1986b), while retained as a subgenus of Cancel-
laria in several faunistic surveys (e.g., Springsteen and
Leobrera, 1986; Wilson, 1994; Higo ct ai, 1999). Merica
has been reported from the later Tertiaiy of Europe
(Cossmann, 1899; Sacco, 1904; Janssen, 1984) and the
Indo-Pacific region (Shuto, 1969; Noda, 1908; Ladd,
1982). In the Recent fauna, Merica appears hmited to
the Indo-West Pacific, ranging from South Africa, along
' Research Associate; mailing address: 806 St. Charles Road,
North M>Ttle Beach, SC 29852-2846 USA.
the northern Indian Ocean, through Indonesia to Aus-
traha and northward to Japan, usually at subUttoriil
depths. As pointed out by Verhecken (1986a: 38—40),
there is considerable confusion in the literature as to the
correct nomenclature for many of the currently recog-
nized species of Merica.
This paper describes three new Recent species ot
Merica, one from Soudi Africa and two from the Phil-
ippines. The assignment of Cancellaria oblonga Sower-
bv, 1825, to the genus Merica is reaffirmed, and the spe-
cies is illustrated for comparative purposes. Holofypes of
the new species are housed in the collections of the Na-
tal Museum (NM), Pietermaritzburg, Repubhc of South
Africa, and the National Museum of Natural History
(USNM)
USA.
Smithsonian Institution, Washington, DC,
SYSTEMATICS
Family Cancellariidae Forbes and Hanley, 1851
Subfamily Cancellariinae Forbes and Hanley, 1851
Genus Merica H. and A. Adams, 1854
Merica H. and A. Adams, 1854:277. Tvpe species: Cancellaria
melanostoma Sowerbv, 1849, by subsequent designation of
Cossmann, 1899.
Diagnosis: Shell with conical spire, large body whorl,
paucispiral protoconch weakly to strongly deflected from
teleoconch axis, prominent suture, generally weak si-
phonal fasciole, narrow pseudo-umbihcus, and large,
ovate aperture. Columella short, thick, weakly concave,
with 2 sharply keeled columellar folds and strong si-
phonal fold. Columellar Up with pustules and secondary
folds. Parietal callus generally present. Emargination
along outer lip at base of siphonal canal poorly defined
or absent.
Remarks: Merica appears to be the Indo-Pacific stem
group for the genus Cancellaria, which is hmited to the
eastern Pacific and the western Adantic. Merica differs
in lacking a pronounced emargination along the outer
lip of the shell as well as a heavy, bifurcated posterior
R. E. Petit and M. G. Harasewvch, 2000
Page 143
columellar fold, both characteristic of CanccUnria. ('oss-
inann (1899: 13) accorded generic status to Mcrica, and
most authors have followed this.
Kuroda and Habe (1971: 310, 202) proposed the ge-
nus Momocbora based primarily on the presence of a
strongly dexiated protoconch in its tvpe species, Can-
ccllaria sinensis Reeve, 1856. Mouiorhora has been con-
sidered a spionxTii of Mcrica by most subsecjuent au-
thors (Garrard, 1975: 3; Verhecken, 1986a: 44).
Mcrica oblonga (Sowerbv, 1825)
(Figures 1, 5, 6)
Cancellaria oblonga Sowerby, 1825: Appendix: 15; 1S32: fig.
19.
Cancellaria bifasciata Deshayes, 1830: 181; Lobbecke, 1885:
30, pi. 9, figs. 1,2.
Cancellaria oblonga Sowerby: Kieiier, 1841: 6, pi. 3, fig. 3; Ab-
bott and Dance, 1982: 225; Springsteen and Leobrera,
1986: 78, pi. 18, fig. 26.
Cancellaria (Merica) oblonga Kiener [sic]: Chenu, 1859: 277,
fig. 1847.
Not Cancellaria (Merica) bifasciata Deshayes: Chenu, 1858:
277, fig. 1845 [?=M. sinensis (Reeve, 1856)].
Not Cancellaria bifasciata Deshayes: Bamard, 1959: 13-14;
Kenslev, 1973: 194, fig. 749 [ = M. hissii new species].
Merica bifasciata (Deshayes): Habe, 1961: pi. 24, fig. 27.
Cancellaria (Merica) bifasciata Deshayes: Oyama and Take-
mura, 1963: Cancellaria plate, fig. 6.
Merica oblonga (Sowerbv): Petit, 1974: 112, fig. 5; Verhecken,
1986a: 41, figs. 7-8; Verhecken and Wranik, 1991: 60; Ver-
hecken, 1997; 308, fig. 37.
Momoebora bifasciata (Deshayes): Higo. 1973: 179.
Momocbora oblonga (Sowerby): Higo and Goto, 1993: 276;
Higoe/fl/., 1999: 294.
Remarks: For many years there was confusion about
priority of the names apphed to this species, with Can-
cellaria bifasciata Deshayes, 1830, generally given pre-
cedence over Cancellaria oblonga Sowerby, 1825. These
two available names were correctly dated by Perit
(1974). Merica oblonga (as Merica bifasciata) was attri-
buted to the genus Momoebora by Higo (1973:179), and
this placement remained unchanged in the two later re-
visions and enlargements of that work (Higo and Goto,
1993; Higo et al, 1999). As M. oblonga has a protoconch
that is not strongly deflected from the coihng axis of the
teleoconch (Figs. 5,6), we see bttle justification for the
usage of Momoebora.
There were, and to a lesser degree still remain, ques-
tions about the geographic range of this species. Its oc-
currence in Panama, as reported by Kiener (1841), was
shown to be incorrect by Keen (1971:649). Verhecken
(1997:309) gave the distribution of Merica oblonga as
"Japan to Indonesia; Northern Indian Ocean to Aden;
Eastern South Africa (?)." His query regarchng the South
African records is appropriate, as the South African
specimens previously identified as Mcrica bifasciata rep-
resent a new species, described herein as Merica hissii.
There are no verifiable Japanese records for Mcrica
oblonga (Kazunori Hasegawa, personal communication).
The figme of M. oblonga pubUshed by Habe (1961) and
ri'produced b\' Petit (1974) is of a specimen from Taiwan
that was inchulcd b\' Habe for comparison with Merica
asprella [sic] Lamarck. The specimen figured by Oyama
and Takemura (1963) is also from Taiwan. Verhecken's
(1986a: 41) record for Japan is based on Habe's usage.
Records of M. oblonga are noticeably absent in most
standard Japanese compendia and fists. Its inclusion in
the exhaustive faunal fists of Higo (1973), Higo and Goto
(1993) and Higo, Callomon and Goto (1999) was based
on a Japanese publication of uncertain authorship.
Mcrica oblonga ranges as far north as Taiwan. It is
uncommon in the Phifippines. Springsteen and Leobrera
(1986: 78) record this species as "sporadically found
throughout the Philippines in limited quantity-." The col-
or figure in Abbott and Dance (1982:225) is of a Phil-
ippine specimen taken from over 30 m depth in tangle
nets (Petit collection). Verhecken and Wranik (1991: 60)
state that M. oblonga 'seems to have its distribution cen-
ter in the eastern Inthan Ocean (Gulf of Bengal). ' While
this species is uncommon in other areas, it appears to
be common in India. We have seen commercial lots
from India containing hundreds of specimens of M. ob-
longa.
Merica litssii new species
(Figures 2, 7, 8)
Description: Shell (figure 2) to 35 mm, thin, biconic,
elongate. Spire high (spire angle 53-55°) comprising
one-half of total shell length. Protoconch (figures 7, 8)
paucispiral, nearly coaxial with teleoconch (deviated
from coifing axis by up to 4°), increasing in diameter
from 300 p,m to 2.15 mm in 2% elongated whorls. Tran-
sition to teleoconch marked by onset of spiral then axial
sculpture. Teleoconch of about 5 evenly rounded whorls.
Shoulder rounded. Suture broadly impressed, forming
conspicuous canal. Axial sculpture of 30-34 very weak,
rounded, sfightly prosocline ribs, as broad as inter\'ening
spaces. Axial ribs become prominent, irregular, crowded
on final V4 of body whorl. Spiral sculpture more pro-
nounced than axial, of regularly spaced, flat, primary
cords (8-10 on penultimate whorl, 2.5-32 on body whorl)
with weaker secondaiy cords present irregularly, but
most often on posterior portion of whorls. Aperture
large, broadly ovate, deflected from coifing axis by 16-
17°. Outer lip thin, weakly flared outwarcUv, without cfis-
cemable emargination. Inner fip smooth or with weak
spiral firae reflecting spiral cords, especially in the an-
terior portion. Inner lip with 2 columellar, 1 siphonal
fold. Siphonal fold flat, bifid on holot^pe but sharp on
other specimens. Columellar lip thick, forming induc-
tural shield that obscures chink-fike umbificus. Siphonal
canal short, broad, inconspicuous. Base color fight yel-
low-brown, irregularly marked with white and various
shades or redcfish brown. Two bands of brown some-
times present, visible inside aperture. Wider band just
below shoulder, narrower band just posterior to base of
Page 144
THE NAUTILUS, Vol. 114, No. 4
R. E. Petit and M. G. Harasewvch, 2000
Page 145
siphonal canal. Axial flammules of browii, \t>ll()\v, white,
irregular in outline and intensity
Tjpe locality: Off Park Rviiie, about SO km S ol Dur-
ban, on the KwaZulu-Natal south coast. South Africa,
appro>dmatelv 30°17' S, 3()°45' E, dredged in 150 ni on
nibble and sponge substrate.
Type material: Holot\pe, NM ¥7648/11312, height
34.4 mm; Paratvpe 1, Marcus Lussi Collection, both
from the t\pe locality-; Paratope 2, Dawni Brink Collec-
tion, near type localit\' in 140 m, nibble and sponge bot-
tom; Paratvpe 3, NM E8794, Zululand, off Matigulu
River mouth, 29°21.4' S, 3r56.5' E, in 145 m, mud,
shell rubble, NMDP 16 Apr 1989, station ZR7.
Etymology: Named for Mr. Markus Lussi of Durban
North, SoutJi Africa, who has made numerous contri-
butions to the Uterature on South African Mollusca, and
who provided specimens for study.
Comparative remarks: Merica lussii differs from M.
ohlonga in having a broader shell with a stepped spire,
a proportioniilly shorter but broader aperture, and a
deeply impressed sutural canal. Merica lussii lacks the
closely packed strong axial ribs that produce the finely
beaded surface characteristic of M. ohlonga. Barnard
(1959: 14) and Verhecken (1986a: 42) have previously
suggested that South African records of M. bifasciata ( =
M. oblonga) might represent a distinct species.
Merica detjnzeri new species
(Figures 3, 9, 10)
Description: Shell (figure 3) to 35 mm, thick, biconic,
weakly pseudo-umbilicate. Spire high (spire angle 55-
58°). Protoconch (figures 9, 10) paucispiral, deviated
from coiling a.xis by about 14°, increasing in diameter
from 300 jim to 2.15 mm in 2V4 evenly rounded, glassy
whorls. Transition to teleoconch marked by onset of spi-
ral cords followed almost immediately by axial ribs. Te-
leoconch of up to 6 whorls. Shoulder inconspicuous. Su-
ture deeply impressed, forming narrow canal. Axial
sculpture of 27-33 low, evenly spaced, prosochne ribs,
rounded in profile, as wide as intervening spaces. Peri-
odic internal varices (see Harasewych and Petit, 1982:
111) barely discernable on outer surface of shell by
thickened axial rib slightly expanded along edge of su-
tural canal followed closely by thin axial rib and slightly
reflected fip, begin after about 2% whorls, continue at
intervals of about 240° thereafter. Spiral sculpture of
strong, broad cords (20-26 on body whorl, 8-9 on pen-
ultiiriatc whorl) that are narrower, more closely spaced
near suture and siphcjn. Spiral cords overlav axial ribs to
produce a cancellate surface on early whorls. Single, sec-
ondarv' cords occur between primary cords along central
region of whorls. Axial ribs Iteconie progressivi'ly broad-
er, irregular, more widely spaced on last half of body
whorl, obscuring cancellate appearance. Aperture large,
broad, nearl\' hemi-elliptical, deflecteil from coifing axis
by 14-15°. Outer lip weakly recurved in profile, with
finely .serrated edge, lacking emargination. Inner surface
of outer Up with 16 recessed spiral Urae that diminish 1/
3 whorl into the aperture. Inner Up with 2 columellar, 1
siphonal fold, columellar lip nearly covering pseudo-um-
bificus. Posterior columellar fold strongest, overlying
weak siphonal fasciole. Anterior columellar fold extends
to edge of columellar fip. Spiral ridge parallels anterior
columellar ff)ld adapically, but is confined to the colu-
mellar hp without extending into aperture. Surface of
siphonal fold with single pustule in some specimens. Si-
phonal canal short, narrow, axial. Color uniform yellow-
brown, sometimes with narrow darker bands above and
below mid-whorl. Portions of spire whorls intficate that
juveniles may be mottled.
Type locality: Off Baficasag Island, Bohol, Phifip-
pines. Taken in tangle nets at approximately 200 meters.
Type material: Holotvpe, USNM 880645, height 35.2
mm; Paratype 1, R. Petit Collection 2465, both from the
type locahty; Paratypes 2-A, USNM 242316, off Pt. Du-
murug, Ma.sbate, Philippines (12°00'30" N, 124°05'.36"
E), dredged in 280 m, green mud, USES Albatross, sta.
5394, l3'Mar 1909; Paratvpes 5-8, USNM 242321, off
Adyagan Island, E Masbate, PhiUppines (12°12'35" N,
124°02'48" E), dredged in 247 m, green mud, sand.
USES Albatross, sta. 5392, 13 Mar 1909; Paratype 9,
USNM 277485, off Sibugav Island, E of Masbate, Phil-
ippines (12°04'15" N, 124°()4'36" E) in 198 m, grav sand,
mud, 15.5°C. USES Albatross, sta. 5212, 20 Apr'l908.
Etymology: We take pleasure in naming this species
for Mr. Al Deynzer of Sanibel, Elorida, who obtained
these and other uncommon Cancellariidae in the Phil-
ippines and made them available for study.
Comparative remarks: This new species is distinc-
tive in having a well-developed sutural margin strongly
rounded to form a deeply impressed sutural canal. Mer-
ica deynzeri is similar to, but stockier and broader than
M. oblonga, from which it can also be distinguished by
its much stronger and coarser axial and spiral sculpture,
and by its more rounded aperture. A notable feature of
<-
Figures 1—4. Apertural, lateral and dorsal views of the shells of. 1. Merica oblonga (Sowerby, 1825), USNM 845168, taken by
fishing trawler in Manila Bay, Luzon, Philippines, 1969 2. Merica lussii new species, holotype, NM V7648Ari.312, off Park Ryiiie,
about 80 km south of Durban on the KwaZulu-Natal south coast. South Africa, approximately 30°17'S, .30°45'E, dredged in 150
meters, rubble and sponge substrate. 3. Merica deijnzeri new species, holotype, USNM 880645. off Balicasag Island, Bohol, Phil-
ippines, taken in tangle nets from about 200 meters. 4. Merica ekti/phos new species, holotype, USNM 880646, Off Balicasag
Island, Bohol, Philippines, taken in tangle nets from about 200 meters. Scale bar = 2 cm for all figures.
Page 146
THE NAUTILUS, Vol. 114, No. 4
Figures 5-12. Scanning Electron Micrographs of a\ial and lateral aspects ot pnitcicDnclis nt spcnini-ns iii figures 1—4. 5-6. Merica
oblonga (Sowerby, 1825). 7-8. Merica lussii new species. 9-10. Merica detjnzeri new species. 11-12. Merica ekttjphos new species.
Arrowheads indicate transition from protoconch to teleoconch. Scale bar = 1 mm for all figures.
R. E. Petit and M. G. Harasewvch, 2000
Page 147
Merica deynzeri is the lack of color bands that arc char-
acteristic of most species of Merica.
Merica ektyphos new species
(Figures 4, 11, 12)
Description: Shell (figure 4) to 33 mm, very thick,
globose, pseudo-umbilicate. Spire relatively low (spire
angle 63°). Protoconch (figures 11, 12) paucispiral, de-
viated from coiling ;L\is by about 8°, increasing in di-
ameter from 400 |xm to 2.10 nun in 2y2 low, evenlv
rounded whorls. Transition to teleoconch marked by on-
set of axial ribs followed by overlying spiral cords. Te-
leoconch of up to 6 rounded whorls. Suture impressed,
forming deep, narrow sutural canal. A.\ial sculpture of
prominent, prosocline ribs (31 on body whorl, 31 on
penultimate whorl). Ribs become smaller, more densely
spaced in narrow bands spaced every Vi to % whorl, in-
dicating position of internal varices. Spiral sculpture of
strong, flattened cords (15-16 on bodv whorl, 6 on pen-
ultimate whorl) that form nodes at intersections with ax-
ial ribs. Nodes especially pronounced at margin of su-
tural canal, forming serrated ridge. Finer secondaiy
threads present between adjacent cords above suture
line. Aperture large, deflected from coifing axis by 12°,
with broadly elfiptical outer lip, sharp, 48° angle between
columella and parietal wall. Outer fip prosocline, sfightly
crenate, with 12-13 strong, sfightly recessed firae that
become reduced, disappearing about V4 whorl within the
aperture. Outer lip with emargination discernible only
by touch as shallow depression. Columella with 2 colu-
mellar, 1 siphonal fold. Posteriormost fold strongest,
overlving conspicuous siphonal fasciole, does not reach
edge of columellar lip as anterior and siphonal folds do.
Columellar fip thick, rounded, nearly covering pseudo-
umbificus. Four weak, short spiral ridges run along col-
umellar fip parallel to and posterior to anterior colu-
mellar fold, but do not extend into aperture. Siphonal
canal short, narrow, well demarcated, deflected from
axis. Color whitish, with ginger brown bands along su-
ture (darkest), above mid-whorl (broadest), below mid-
whorl (narrowest) and along siphonal fasciole. Gaps in
coloration of sutural band correlate with internal varices.
Type locality: Off Baficasag Island, Bohol, Phifip-
pines. Taken in tangle nets at appro.ximately 200 meters.
Type material: Holotype, USNM 880646, 32.3 mm;
Paratypes 1-4, R. Petit Collection 2472; Paratypes 5-7,
Deynizer Collection, all from tyjie locafity.
Etymology: Gr ektyphos. puffed up. Named for its
inflated shefl.
Comparative remarks: This new species can be dis-
tinguished from all known species of Merica by the
thickness of its shell and the strength of its sculpture. In
outfine it is closest to the Australian M. wcstralis (Gar-
rard, 1975), from which it differs in having much coarser
axial and spiral sculpture, a straighter columella with
Tabic 1. Merica deynzeri new species. Measurements of shell
characters. Linear measiirpnients in mm. n = 5. ° n = 3 for
no. whorls, protoconch.
(;!iaractcr
Mean
SU
Range
Shell length (SL)
.35.0
2.6
.34.9-38.6
Aperture length (AL)
22.1
1.7
19.6-24.3
AIVSL
0.629
0.003
0.624-0.632
No. whorls, protoconch"
1.5
0
2.5-2.5
No. whorls, tcleoconcii
5.53
0.14
5..33-5.67
.Spire angle
56.7°
1..3°
5.5-58°
stronger folds, and a body whorl that is niuch less con-
stricted beliind the siphonal fasciole.
ACKNOWLEDGMENTS
We thank Marcus Lussi and Dawn Brink of South Africa
for making specimens of Merica lussii available for this
study. While on visits to the Phifippines Al Deynzer
made special efforts to obtain specimens for this study.
We are grateful to Paul Callomon of Osaka and Dr. Ka-
zunori Hasegawa of Ibaraki for information about the
Japanese records of M. ohlonga.
LITERATURE CITED
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E. P Dntton. New York, x -I- 411 pp.
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Chenu, J. C. 1859-62. Manuel de conch\liologie et de paleon-
tologie conchyliologique. Librarie Victor Masson, Paris. 2
vols. [l:i-vii, 1-508, 18.59; 2:1-327, 1862].
Cossmann, M. 1899. Essais de Paleoconchologie Comparee.
Troisieme hvraison. Paris. 201 p., 8 pis.
Deshayes, G. P. 1830. Encyclopedic Methodique. Histoire na-
turelle des vers 2(l):l-256, Paris.
Forbes, E. and S. Hanley 1848-1853. A history of British Mob
lusca and their shells. London. 4 volumes. [Published in
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Garrard, T. A. 1975. A revision of the Australian Cancellariidae
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Habe, T. 1961. Description of four new cancellariid species,
with a list of the Japanese species of the familv Cancel-
lariidae. Venus 21:431-441. pis. 2:3-24,
Harasewvch, M. G. and R, E, Petit. 1982. Notes on the mor-
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iidae). The Nautilus 96:104-113.
Higo, S. 1973. A catalogue of molluscan faima of the Japanese
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Islands and the adjacent area. S. Higo. Isahaya, Japan. (58)
+ 397 + 61 pp.
Higo, S. and Y. Goto. 1993. A systematic list of molluscan shells
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ration, Osaka, Japan,3 + 22 + 693 + 13 + 149 pp.
Higo, S., Callomon, P. and Y. Goto. 1999. Catalogue and bib-
liography of the marine shell-bearing Mollusca of Japan.
Elle Scientific Publications, Osaka, 49 pp.
Janssen, A. W. 1984. An account of the Cancellariidae (Gastro-
poda) of Winterswijk-Mi.ste (Miocene, Henimoorian),The
Netherlands. Scripta Geologica 68; 1-39, pis. 1-6.
Keen, A. M. 1971. Sea shells of tropical West America. Second
edition. Stanford University Press, Stanford, xiv -t- 1064
pp., 22 pis.
KensJey, B. 1973. Sea-Shells of southern Africa, Gastropods.
Maskew Miller Ltd., Cape Town, 236 pp.
Kiener, L. C. 1841. Genre Cancellaire. Species general et icon-
ographic des coquiUes vivantes. Paris, 44p., 9 pis.
Kuroda, T. and T. Habe. 1971. [Descriptions of species] In:
Kuroda, Habe and Oyama, The sea shells of Sagami Bay.
Manizen Co., Tokyo. Pp. i-xix, 1-741 (Japanese), 121 pis.,
1-489 (English), 1-51 (index).
Ladd, H. S. 1982. Cenozoic fossil mollusks from Western Pa-
cific Islands; gastropods (Eulimidae and Volutidae through
Terebridae). United States Geological Suwey Professional
Paper 1171:1-100, pis. 1-41.
Lobbecke, T. 1881-1887a. Das genus Cancellaiia. Systema-
tisches Conchylien-cabinet von Martini und Chemnitz 4:
1-96, pis. 1-23 [issued in parts; pt. .309; 1-16, pis. 1-5,
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11-15, 1886; pt. 343;5780, pis. 16-20, 1886; pt. .346;81-
96, pis. 21-23, 1887.]
Matsukiuua, A. 1998. Index and collation of The Molluscan
Shells by Katura Oyama and Yoshio Takemura (1957-
1963). The Yuriyagai 6;91-122.
Noda, H. 1980. Molluscan fossils from the Ryukyu Islands,
southwestern Japan. Part 1. Gastropoda and Pelecypoda
from the Shinzato Fomiation in southeastern part of Old-
nawa-jinia. Science Reports of the Institute of Geoscience,
University of Tsuk-uba, SecHon B, l;l-95, pis. 1-12.
Oyama, K. and Y. Takemura. 1963. The Molluscan Shells. Pt.
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ing, Kallaroo, 370 pp.
I
THE NAUTILUS 114(4):149-154, 2000
Page 149
Systematics of the genus Infundihulum Montfort, 1810
(Gastropoda: Trochidae)
Bruce A. Marshall
Museum of New Zealand Te Papa
Tongarewa
P.O. Box 467, Wellington
NEW ZEALAND
brucem@tepapa.govt.nz
Two Recent Infundibtiluin species are recognized: /.
concaviiin (Gnielin, 1791) (type species) and /. tonilini
(Fulton, 1930). Their shells are convergent on those of
calyptraeid limpets of the genus Trochita Schumacher,
1817, having the most widely excavated bases and the
most strongly tangential apertures of any living Trochini.
They Hve firmly attached to rocks on highly e.xposed
shores from low tide level to several meters depth in
tropical seas. Reliable records of /. concavum are from
Reunion and Mauritius. All Recent specimens of /. tom-
lini seen were from old collections, and most have either
minimal, often dubious locality data, or none at all,
though it would seem that /. tomlini has a patchy chs-
tribution in the tropical southwest Pacific.
Additional key words: Mollusca, Trochoidea, fossils.
Pleistocene, Kermadec Islands.
INTRODUCTION
The present contribution was initiated some years ago
when I recognized a species oi Infundihulum among
Pleistocene fossils from Raoul Island, Kermadec Islands,
northeast of New Zealand. A search of the literature re-
vealed that Infundihulum species are sui"prisingly poorly
known. Moreover, inquiries revealed that most of the
few specimens of Infundihulum species in museum col-
lections were acquired during the nineteenth century,
and have broad, often dubious locality data, or none at
all. The fossils from Raoul Island prove to be the little
known species /. tomlini (Fulton, 1930), which is rep-
resented in old collections labeled as originating vari-
ously from Penang (Pinang, Malaysia), Australia, Upolu
(Western Samoa), Lifou (Loyalty Islands) or the New
Hebrides (Vanuatu). Of these locality records, only Upo-
lu, Lifou, and Vanuatu seem hkely to be correct. Mu-
seum specimens of the type species (Trochus concavus
Gmehn, 1791) are labeled as having originated from lo-
calities in the Indian Ocean, as well as the Red Sea and
Cochin China (southern Vietnam), though the only re-
hably locaUzed specimens seen during the present study
were from Reunion. An explanation for the poor rep-
resentation of /. concavum (and presumably /. tomlini)
in collections is suggested by the fact that specimens
collected ahve were cryptic at and below low tide, at-
tached to exposed, wave-swept volcanic rocks, which
tend to receive far less attention from collectors than
more congenial and species-rich coral reef and lagoon
environments, where they have never been recorded. In-
stitutional acronyms: ANSP, Academy of Natural Scienc-
es, Philadelphia; AMS, Australian Museum, Sydney;
RMNH, The Natural Histoiy Museum, London; LACM,
Los Angeles County Museum of Natural History;
MNHN, Museum National d'Histoire Naturelle, Paris;
NMNZ, Museum of New Zealand, Welfington; NMP,
Natal Museum, Pietermaritzburg; USNM, National Mu-
seum of Natural History, Washington, DC.
SYSTEMATICS
Superfamily Trochoidea Rafinesque, 1815
Family Trochidae Rafinesque, 1815
Subfamily Trochinae Rafinesque, 1815
Tribe Trochini Rafinesque, 1815
Genus Infundihulum Montfort, 1810
Infundibuluiii Montfort, ISIO: 167. Type species (by original
designation): Infundihulum tijpus Montfort, 1810 = Tro-
cluis concavus Gmelin, 1791; Recent, Rennion.
Carinidea Swainson, 1S40: .350. T^pe species (by nionotypy):
Trochus concavus Gnielin, 1791.
Description: Shell up to 54 mm in diameter, stout,
base excavate, umbilicus narrow; aperture very strongly
tangential, as wide as shell; periphery sharply angulate,
not stellate at any stage of growth, almost flush against
a flat surface. Spire sculptured with strong, close, round-
ed spiral cords and a.xial costae, intersections finely and
bluntly nodular Base weakly convex, evenly curving into
narrow umbilicus, excavated from periphery. ColumeUar
lip adapicallv with strong, rounded denticle, sharply re-
tracted to insertion within umbilicus. Foot (/. concavum)
very large, epipothum very well developed, edge finely
fringed, well developed epipodial flaps beside epipodial
Page 150
THE NAUTILUS. Vol. 114, No. 4
insertion; cephalic lappets large, papillate. Radula (/.
concavum, figure 9) with the formula ii + .5+l+5 + n,
very similar to that in Trochiis (scnsu stricto).
Remarks: Infundibiilum species are referable to sub-
family Trochinae, tribe Trochini because of similaritv' to
species oiTrochtis Linnaeus, 175S, and Tectiis Montfort,
1810, in shell and radular morphology, and external anat-
omy. External anatomy is close to that of Tcctiis fenes-
trattis (Gniehn, 1791) (Hickman and McLean, 1990: fig.
55b). lufiindibtihtm species differ irom Trochiis and Tcc-
tus in the combination of low, evenly conical spire, weak-
ly convex whorls, low sculpture, lack of peripheral nod-
ules at any stage of growth, and widely excavated base,
which fits almost flush with a flat surface. All of these
character states (apomoq^hies) evidentlv enhance attach-
ment to rocks exposed to strong wave action. Infundib-
iilum concavum (Gmehn, 1791) and /. tomlini (Fulton,
19.30) have the most strongly tangential apertures and
the most widely excavated bases of any li\ing Trochini,
and they resemble limpets in ventral view when the foot
is fully extended (shdes of aquarium specimens of 7. con-
coviim provided by D. G. Herbert). Gross shell mor-
phology strikingly parallels calyptraeid fimpets of the ge-
nus Trochita Schumacher, 1817.
Whereas Infiindibulum has been interpreted as a sub-
genus of Trochus by many authors, I prefer to treat In-
fiindibulum as a distinct genus because of current lack
of clear exddence for degrees of relatedness.
Trochus hochii Phihppi, 1844, from Oman (figures 8,
10) has a similar shape and sculpture to Infundibiihtm
species, but differs in having the base considerably less
excavated, and a much more weaklv tangential aperture
(and thus presumably a more weakly expanding foot).
The relationships of this species are unclear, and I refer
it to Trochus, subgenus Infundibidops Pilsbry, 1889 (type
species Trochus cri/thracus Brocchi, 1821) with some
hesitation.
Inftindibiihim concavum (Gmelin, 1791)
(Figures 1-.3, 9)
Trochus ptjramidalis rarissimus . . . Chemnitz, 1781: 86, pi.
168, figs. 1620, 1621 (not binominal).
Trochus concavus Gmelin, 1791: .3.570 (refers to Chemnitz,
1781. figs. 1620, 1621); Dillw>ii. 1817: 763; Blaimille.
1825: 425. pi. .32 bis. fig. 1; Wood. 1825:134. pi. 28. fig.
7; Sganzin. 1843: 22; Philippi. 1848: .38. pi. 8. figs. 7. 8;
Deshayes. 1863: 71; Fischer. 1876: 105. pi. 33, fig. 2;
Kaicher. 1979: card 2087.
Infundibulum tijpus Montfort, 1810: 167, text fig.
Carinidea concavus: Swainson, 1840: .350.
Pohjdonta (Carinidea) concavus: Chenu. 1859: 357. fig. 2646
Trochus (Pohjdonta) concavus: Martens. 1880: 295.
Trochus (Infundibulum) concavus: Pilsbry, 1889: 40, pi. 43, fig.
13; VVenz, 1938: 311, fig. 693.
Infundibulum concavum: Cossmann. 1918: 188. text fig. 65.
Tectus concavus: Dri\'as and Jay. 1988. pi. 2, fig. 3.
Not Poh/donta (Infundibulum) concava: MeMlI and Standen,
1895: 125 = /. tomUni.
Description: Shell (figures 1-3) up to 56 mm in di-
ameter, stout, broadly conical, wider than high, weakly
cyrtoconoid, base excavate; aperture strongly tangential,
as wide as shell; peripherv sharplv angulate, almost flush
against a flat sin4ace, narrow umbihcus. Spire dull green
with subsutur;il band of irregular, duU, red and white
maculations, last few whorls pinkish milky green. Base
white, inner half with porcellanous glaze. Protoconch
and first few teleoconch whorls unknown (eroded). Spire
whorls moderately convex at first, becoming weakly con-
vex, sculptured with low, rounded spiral cords and op-
isthocline, non-coUabral axial costae, interspaces narrow-
er; intersections with strong, bluntlv rounded nodules;
axial costae on last 2 or .3 whorls traversing rounded axial
folds that are broader than the costae and tend to be
more strongly opisthochne. Spiral cords 7, strong and
similar on early whorls, weakening after shell attains
about 8 mm diameter, obsolete on last 2 or 3 adult
whorls. Excavate base convex, smoothly cuning into nar-
row umbihcus. Outer part of base with 6 or 7 smooth,
simflar spiral cords, becoming obsolete on last whorl at
maturit\'; inner (porceUanous) part of base with 6 or 7
spiral cords that become obscured bv indiictura at ma-
turity. Aperture ovate. Basal Mp strongly tluckened,
smoothly continuous with columellar lip, which is
stronglv thickened adapicallv then sharplv retracted to
insertion within umbihcus.
Animal (retracted, ex ethanol). Foot extremely large
and spreachng. Epipodium very weU developed, edge
finely fringed throughout; inner surface finely papillate,
tapered macropapillae over posterior half neck lobes
convoluted, finely fringed, left lobe considerably larger
and more deeply convoluted than right. Epipodial ten-
tacles slender, narrowly tapering, 4 pairs. Epipodial flaps
well-developed, bases close to epipodial insertion, edges
finely fringed, 5 on right, 5 or 6 on left. Cephahc ten-
tacles slender, narrowly tapered, subcyhndrical. right
tentacle base adjacent to tip of left tentacle due to
obhque asymmetry of head. Eye stalks large, dorsoven-
trally flattened, well developed eyes in tips. Cephahc lap-
pets well developed, edge and adjacent ventral surface
Figures 1-10. Infundibulum and Trochus (Infiindibulops) species. 1-3. /. concavum (Gmelin. 1791). St. Paul Bav. Reunion, .56
X 40 mm (NMNZ M. 270521). 4-6. I tomlini (Fulton. 19.30). s\Titype, locality unhiown (possibly Western Samoa or Vanuatu).
19.0 X 26.6 mm (BMNH 19.30.4.2.3). 7. 7 tomlini. Boat Cove. Raoul Island. Kemiadec Islands (Pleistocene). 25.5 X .33 (est.) mm
(NMNZ M.214580); 8, 10. Trochus (Infundibidops) kochii (Philippi. 1844). SW coast of As Sawda. Juzor Al Halaaniyaat. Oman,
32 X ,38 mm (Zoological Museum, Amsterdam). 9. Radula of 7 concavum. north of Cap la Houssaye, St. Paul Bav. Reunion (NMP
K4898).
B. A. Marshall, 2000
Page 151
Page 152
THE NAUTILUS, Vol. 114, No. 4
papillate. Cephalic tentacles blackish brown, sides of
foot darker, elsewhere cream.
Radula (figure 9) with the formula n+5+1+5+n,
very similar to that in Trochtis {scnsit stricto) (Hickman
and McLean, 1990: fig. 57D).
Type data: Holotype, the specimen illustrated by
Chemnitz (1781: figs. 1620, 1621), ex Spengler collec-
tion, in Zoological Museum, Copenhagen (T. Schi0tte,
pers. comm.); "k-uste von Coromandel".
Material examined: North of Cap la Houssaye, St.
Paul Ba\-, Reunion, exposed rocky shore, extreme low
tide to 2 m, 24 September 1988, R. N. Kilbum and D.
G, Herbert (3, NMP); St Paul Bay, Reunion, breaker
zone on exposed rock-\' shore at low tide, M. Jay, 1994
(.3 NMNZ); St Paul, Reunion, M. Jav, 1985 (3 ANSP);
"Zanzibar" (8 in 3 lots, MNHN): Seychelles (4, MNHN);
"Seychelles [and] Madagascar", H. Cuming collection (2,
BMNH); "Madagascar(?)", M. Larrey, 1874 (1, MNHN);
"Madagascar", M. Ballot (1, MNHN); "Madagascar" (1,
MNHN); "Indian Ocean", H. Fischer (1, MNHN); "In-
dian Ocean", Staadt colln (2 MNHN); "Ceylon", ex-
Gould coUn (1 USNM); "Cochin China", M. Harmand,
1876 (2, MNHN); "Penang (?)", ex Marie and Sowerby
collections (7, BMNH); "Penang" (2, LACM); "Austra-
lia". Steams colln (1, USNM).
Distribution: Reunion and (based on Sganzin, 1843)
Mauritius. Living on faces of lava rock and boulders ex-
posed to tlie open sea from low tide to 2 m depth (M.
Jay, pers. comm.). Records from Madagascar and the
Seychelles require confirmation. Specimens in old col-
lections reputedly from Zanzibar, Coromandel Coast,
Ceylon (Sri Lanka) are of uncertain provenance, whereas
Penang, Cochin China (southern Vietnam) and Austrafia
are extremely doubtful.
Remarks: The shell oi Infundibuhim concavum is dis-
tinctive among Trochoidea in the combination of broadly
conical, weakly cyrtoconoid spire; flat, inwardly sloping
base, conical umbilicus, and very strongly prosocline out-
er Up. Among trochid animals examined or that have
been recorded in the literature, the external anatomy of
this species seems most similar to that of Tcctiis fcncs-
tratiis (Gmehn, 1791) (Hickman and McLean, 1990: fig.
55A).
Infundibulum tomlini (Fulton, 1930)
(Figures 4-7)
Pobjdonta {Infundibidum) concava: MeMl and Standen, 1895:
125 (not Gmelin, 1791).
Trochtts (Infundibulum) tomlini Fulton, 19.30: 16, pi. .3, fig. 5.
Trochus tomlini: Kaicher, 1979: card 2162.
Trochus mnculatus: Marshall, 1979: 535; Marshall, 1981: 90
(not Linnaeus, 1758).
Trochus (Infundibulum) sp.: Brook, 1998: 256.
Description: Shell (figures 4-7) up to 36.0 mm wide,
stout, broadly conical, wider than high, weakly cyrtocon-
oid, base excavate; aperture strongly tangential, as wide
as shell, narrow umbilicus; periphery sharply angulate,
not stellate, almost flush against a flat surface. Proto-
conch white. First 3.5 teleoconch whorls CTeen with red
spiral bands; 2 or 3 continuous median bands and 1 su-
prasutural band on 1st 2 whorls; spiral cords spotted and
streaked with red on 3rd whorl. Subsequent spire whorls
deep duU greenish or reddish grey with subsutural band
of white spots or streaks. Base considerably paler than
spire, inner third (approximately) porcelain-white. Pro-
toconch 200 fjLm wide, tip narrowly tapered, sculpture
unknown (eroded). Teleoconch of up to 7.5 whorls. Ear-
ly spire whorls moderately convex, later whorls moder-
ately or weakly convex; sculptured with rounded spiral
cords and rounded, prosocUne, non-coUabral axial cos-
tae, interspaces narrower; intersections with strong,
bluntly rounded nodules; fine, crowded coUabral growth
lines throughout. Spiral cords numbering 7 per spire
whorl; adapical spiral broadest in most specimens, al-
most fusing with adjacent spiral in some specimens; pe-
ripheral and adjacent spiral narrowest, similar; other spi-
rals similar, peripheral spiral partly covered by succeed-
ing whorls. Excavated base broad, weakly convex, evenly
curving into narrow steep-sided umbilicus, base of which
is fiUed with callus. Basal spirals much finer than spire
spirals; outer (pigmented) part of base of most speci-
mens with 7 or 8 weakly nodular spirals, typically 1 sec-
ondary spiral in each interspace, some interspaces in
some specimens with 2 secondary spirals; 6-8 smooth
spirals on inner (white) part of base, smooth, similar.
Aperture ovate-trapezoidal. Columellar and basal fips
smoothly continuous, thickened adapicaUy, sharply re-
tracted to insertion within umbilicus. Rounded spiral
ridge at base of outer lip.
Animal unk-nown.
Type data: Originally figured syntype BMNH
1930.4.2.3 (height 19.0 mm, diameter 26.6 mm); syntype
National Museum of Wales Cardiff (Trew, 1984). Fulton
(1930) stated that he had seen five specimens and did
not segregate a holotype. The specimens could not be
locahzed and evidently originated from somewhere in
the tropical southwest Pacific.
Other material examined: Titi Knob (Trig Sentinel),
Boat Cove, Raoul Island, Kermadec Islands, cemented
tuffaceous conglomerate (Pleistocene), W. R. B. Oliver
(1, NMNZ); DavTell Islet. Raoul Island, hard sandy tuff
(Pleistocene), F.'j. Brook, June 1991 (2, Auckland Insti-
tute and Museum); Upolu, Western Samoa, R. W Tate
(7, NMNZ); Lifou, Loyalty- Islands, J. Brazier, 1873 (4,
BMNH); Vanuatu, C. Bertie, 1895 (1, AMS); Erroman-
go, Vanuatu, H. A. Robertson, 1898 (3 in 2 lots, AMS);
"Red Sea", E. C. Freeman collection (3, BMNH); "Red
Sea" (4, LACM); "Penang" (1, NMNZ); "Penang, ex
Sowerby" (1, NMP).
Distribution: Raoul Island, Kermadec Islands (Pleis-
tocene): Upolu, Western Samoa (record plausible be-
cause R.W. Tate coUected extensively there); Aneiteum
and Erromango, Vanuatu (records plausible because
B. A. Marshall. 2000
Page 153
there are extensive stretches of exposed rockv' shore),
and possibly Lifou. Specimens in old collections reput-
edl\ from the Red Sea and Penang are of extremely
doubtful provenance.
Remarks: Compared with Infundihiiliim concamiin. I.
tonilini differs in attaining smaller size (nia.\imum di-
ameter 36.0 mm instead of 56.0 nnn). in being more
broadly conical, in ha\'ing more strongly convex whorls,
and in having much stronger axial costae and nodules on
the spire, especially after the shell is about 6 mm wide.
In /. concaium the spiral cords and nodules progres-
sivelyweaken and become obsolete when the shell is 12-
15 mm wide, while in /, touiliui the spiral cords pro-
gressively enlarge throughout.
One lot (NMP) labelled "Penang, ex Sowerby", sug-
gests origin from the London shell dealers Messrs. Sow-
erby and Fulton, who advertised Trochus concavus in
their 1908 price list. Other "Penang" specimens of I.
coucavtiin and /. totulini in old collections mav well have
originated from this source.
The Pleistocene specimens from Raoul Island (figure
7) are indistinguishable from the syntype (figures 4-6)
and other Recent specimens. /. tomlini is absent from
the Recent fauna of the Kermadec Islands (Brook and
Marshall, 1998).
ACKNOWLEDGMENTS
For loan or gift of specimens I thank Philippe Bouchet
(Museum National d'Histoire Naturelle, Paris), Dai Her-
bert (Natal Museum, Pietermaritzburg), Maurice Jay (La
Reunion), Alan Kabat (National Museum of Natural His-
tory, Washington D.C.), Ian Loch (Australian Museum,
Sydney), Jim McLean (Los Angeles County Museum of
Natural History), Robert Moolenbeek (Zoological Mu-
seum, Amsterdam), David Reid and Kathie Way (The
Natural Historv^ Museum, London), and Gary Rosenberg
(Academy of Natural Sciences of Philadelphia). Thanks
to Dai Herbert and Jim McLean for comments on the
manuscript, Norman Heke (Museum of New Zealand)
for the photography, and to Robert Thompson (Victoria
Universitv', Wellington) for access to the scanning elec-
tron microscope.
LITERATURE CITED
Blainville, H. M. D. de 1825-1827. Manuel de malacologie et
de conchy liologie. . , LevTaiilt, Strasbourg, 664 pp.
Brook, F. J. 199S. Stratigraphy and Paleontology of Pleistocene
submarine volcanic-sedimentarv sequences at the north-
em Kermadec Islands. Journal of the Royal Society of
New Zealand 2S;235-257.
Brook, F. J. and B. A. Marshall. 1998. Checklist of benthic
coastal marine Mollusca from the northern Kermadec Is-
lands, pp. 210-233 (Appendix) In: Brook, F. J. The coastal
molluscan fauna of northern Keniiadec Islands, southwest
Pacific Ocean. Journal of the Royal Society of New Zea-
land 28:185-2.33.
Chemnitz, J. H. 1781. Neues Systematisches Conchylien Cab-
inet 5. Raspe, Nuniberg, 324 pp.
Chenu, J. C. 1859. Manuel de conchvliologie et de paleonto-
logie conchyliologique 1. Masson, Paris, 508 pp.
Cossmann, M. 1918. Essais de paleoconchologie comparee 11.
Cossmann, Paris, 388 pp.
Deshayes, G. P. 1863. Catalogue des Mollusques de I'ile de la
Reunion (Bourbon) 7m. Maillard, L. (ed.) Notes sur I'ile
de la Reunion. Annexe E, Dentu, Paris, pp. 1-144.
Dillwyn, L. W. 1817. A descriptive catalogue of Recent shells,
arranged according to the Linnaean method 2. Arch, Lon-
don, pp. 581-1092.
Drivas. J. and M. Jay, 1988. Coquillages de la Reunion et de
I'ile Maurice. Delachaux et Niestle, Paris, 159 pp.
Fi.scher, P. 1875-1880. Species general et Iconographie des co-
quilles vivantes, comprenant la collection du Museum
d'Histoire naturelle de Paris, la collection Lamarck, celle
du Prince Massena. .11. Bailliere, Paris, 480 pp.
Fulton, H. C. 1930. Descriptions of new species of Fiisinus.
Biplex, Trochus. and Biisliia. Proceedings of the Malaco-
logical Society of London 19:16-17.
Gmelin, J. F. 1791. Caroli a Linne . . . Systema naturae per
regna tria naturae, secundum classes . . . Editio decima
tertia, aucta, reformata. 1 (6). Vermes testacea. Beer, Lip-
siae, pp. .'3021-4120.
Kaicher, S. D. 1979. Card catalogue of world-wide shells. Pack
21. Trochidae 1. Kaicher, St. Petersburg, Florida, cards
2072-2177.
Keen, A. M. and L. R. Cox. 1960. 7/i. Moore, R. C. (ed) Trea-
tise on invertebrate paleontology. Part 1. Mollusca 1. Geo-
logical Society of America and University of Kansa.s,
Lawrence, pp. 246-275.
Marshall, B. A. 1979. The Trochidae and Turbinidae of the
Kermadec Ridge. New Zealand Journal of Zoology 6:521-
552.
Marshall, B. A. 1981. Boat Cove Formation: macrofossils hi:
Lloyd, E. F. and S. Nathan (eds.) Geology and Tephro-
chronology of Raoul Island, Kemiadec Group, New Zea-
land. New Zealand Geological Sur\'ey Bulletin 95, pp. 90-
91.
Martens, E. von 1880. Die Mollusken der Maskarenen und
Seychellen auf Gniud der von Professor Karl Mohius ges-
ammelten Mollusken In: Mohius, K. (ed.) Beitriige zur
Meeresfauna der Insel Mauritius und der Seychellen.
Gutmann'schen, Berlin, pp. 179-.343.
Melvill, J. C. and R. Standen 1895. Notes on a collection of
shells from Lifu and Uvea, Loyalt)' Islands, formed by the
Rev. James and Mrs. Hadfield, with list of species. Journal
of Conchology 8:84-1.32.
Montfbrt, D. de 1810. Conchyliologie systematique, et classifica-
tion mediodique des coquilles. . . 2. Schoell, Paris, 676 pp.
Oliver, W. R. B. 1915. The Mollusca of the Kermadec Islands.
Transactions of the New Zealand Institute 47:509-568.
Philippi, R. A. 1846-1855. Systematisches Conchylien-Cabinet
von Martini und Chemnitz. Neu herausgegeben von ver-
voUstaeudigt \on H. C. Kuester (iiach dessen Tode fort-
gesetzt von W. Kobelt) 2 (3). Bauer and Raspe, Nurem-
berg, 372 pp.
Pilsbry, H. A. 1889-1890. Manual of Conchology; structural
and systematic. With illustrations of the species. Volume
11. Academy of Natural Sciences, Philadelphia, 519 pp.
Sganzin, V. 1843. Catalogue des cotjuilles troiuees aux ties de
France, de Bourbon et de Madagascar Memoires de la
Societe d'Histoire Naturelle de Strasbourg 3 (2):l-.'30.
Swainson, W. 1840. A treatise on malacology, or shells and
Page 154 THE NAUTILUS, Vol. 114, No. 4
shellfish. Longman, Omie, Brown. Green, Longmans and Prosobranchia. In: Schindewolf, O. H. (ed.) Handbuch
Taylor, London, 419 pp. der Palaozoologie 6. Bonitraeger, Berlin, pp. 24-^80.
Thiele, J. 1929. Handbuch der Systematischen Weichtierkunde Wood, W. 1825. Index testaceologicus; or a catalogue of shells,
1(1). Fischer, Jena, pp. 1-.376. British and foreign, arranged according to the Linnean
Trew, A. 1984. The Melvill-Tomlin Collection. Part 30. Tro- system; with the Latin and Enghsh names, references to
chacea. Handlists of the moUuscan collections in the De- authors, and places where found. Illustrated with 2300
partment of Zoology, National Museum of Wales, 94 pp. figures. Taylor, London, 188 pp.
Wenz, W 1938. Gastropoda. Teil 1 (2): Allgemeiner Tell und
THE NAUTILUS 114(4):155-160, 2000
Page 155
On the tcLxononiic placement of Uiiio ochraceus Say, 1817 in the
genus Ligumia (Bivalvia: Unionidae)
Douglas G. Smith
Department of Bi()log^ and
Graduate Program in Organisniic and
Exolutionan' BioloijN
Uni\ersitv of Massachusetts
Amherst,' MA 01003-5810 USA
d<rsmith@bio. imiass.edu
ABSTRACT
Since 1975, the freshwater unionid mussel orig;inally described
as Vnio ochraceus Sav, 1S17, has been \ariouslv assigned to the
genera LampsiUs or Leptodca. The taxonomic stabilit\' of tliis
species has been comphcated h\ incomplete biowledge of cer-
tain features of its anatomy. Study of the mantle of this taxon
leads to the conclusion that V. ochraceus does not belong to
either Lampsilis or Leptodea. The species is assigned to the
genus Ligumia according to established taxonomic criteria to
differentiate lampsiline genera that include characters of the
anatomy and lar\a. The mantle edge contains distinct, regular
papillae along an luiinternipted, lamellate border and the glo-
chidia are of the large t\pe.
Additional kiij words: LampsiUs, Leptodea. Unionoidea, fresh-
water nuissels, new combination.
INTRODUCTION
The unionid mu.ssel originally described as Unio ochra-
ceus Sav, 1817, is discontinuouslv distributed east of the
Appalachian divide in drainages veiy near the Atlantic
coast of North America. The northernmost populations
are found in Nova Scotia (Atheam and Clarke, 1962) and
the southernmost in Georgia (Johnson, 1947).
The generic position of this species has remained an
open question since Morrison (1975) and Bereza and
Fuller (1975) challenged the placement of U. ochraceus
in Lampsilis. The present paper attempts to resoK'e the
issue in light of widely accepted anatomical definitions
of the various genera comprising the Lanipsihnae (sen.su
Heard and Guckert, 1971) or Lampsihni (sensu Davis
and Fuller, 19S1). It is proposed that the species be
placed in the genus Ligumia and is treated as such in
the remaining portion of the paper.
HISTORY OF THE PROBLEM
The question of generic allocation of this species was
raised by Morrison (1975) and Bereza and Fuller (1975).
Morrison's (1975) discussion was the most comprehen-
sive of the two; he argued that the taxon Mijtilus fluvia-
tihs Gmelin, 1791, took precedence over Unio ochraceus
and that M. fluviatilis, for which he elected a neotype,
belonged in Leptodea because of its "smaller glochidia,
and a complete lack of 'mantle flaps' or papillae on the
mantle margins of the females ". Although his conclusion
regarding the generic placement of U. ochracea has
been widely adopted, his argument for M. fluviatilis has
not gained acceptance. One major issue regarding the
position of L. ochracea concerns the lack of the "mantle
flap " (Morrison, 1975), a character included in the pre-
vailing definition of Lampsilis (sensu stricto), the genus
to which the species has been assigned bv manv authors
(e.g.. Ortmann, 1919; Reardon, 1929; Johnson, 1947,
1970; Burch, 1973). Ortmann (1912) reassessed the
characters defining lampsiline genera. This author used
primarily anatomical and lanal characters in the diag-
nosis of the various genera, including: ( 1 ) features of the
mantle margin anterior to the inhalant aperture, (2) the
size and shape of the glochidia, (3) the nature of the
marsupial portion of the female gill (four "types"), and
(4) the degree of attachment of the inner gill to the
abdomen. Ortmann (1912) defined the mantle flap, a
feature of Lampsilis, as a highly pigmented free lobe
extending from the mantle margin anterior to the inhal-
ant aperture with a 'lacerated appearance. " Papillae are
not present in this region of die mantle. The mantle flap
is best represented in the female, reduced in the male.
Ortmann (1912) was apparentlv unable to examine an-
atomical material of Ligumia ochracea and consequentlv
omitted the species in his discussion. Later, Ortmann
(1919), still unfamiliar with the anatomv, placed the spe-
cies in Lampsilis, presumably on the basis of shefl char-
acters. Subsequent study (Bereza and Fuller, 1975; Mor-
rison, 1975; Kat, 19S3; Smith, 1995) has shown that Lig-
umia ochracea clearly does not possess a mantle flap.
Nevertheless, L. ochracea continued to be included in
Lampsilis, at least proxdsionallv, by several in\'estigators
(Fuller, 1977; Johnson, 19S0; Clarke, 1981a; Kat, 1983;
Porter, 1985; Strayer, 1987). Certainly part of the reason
Page 156
THE NAUTILUS, Vol. 114, No. 4
for maintaining L. ochracca in Lampsilis has been the
strong resemblance of its shell to other .species oi Lamp-
silis sensii stiicto and conservatism in the absence of a
definitive description of the species.
Otherwise, following the suggestion of Morrison
(1975), the species has been placed within Lcpfodea (D.
Stan.sberrv', in Porter, 1985; Smith, 1991; Stiven and Al-
derman, 1992; Strayer and Jirka, 1997; Turgeon ct al.,
1998). Ortmann (1912) stated that the mande margin of
Paraptcra (= Lepiodea), based on the type, L. fragilis,
was lamellate with at most marginal crenulations, but
without papillae or a flap. There were little or no ob-
served differences behveen the sexes. The glochidia
were described as "very small" and "suboval."
Descriptions of the mantle o{ Ligumia ochracca from
North Carohna and Nova Scotia (Porter, 1985, and Kat,
1983, respectively) have clearly shown, in conjunction
with characters discussed below, that L. ochracca does
not belong within Leptodea either. Porter (1985) noticed
in his studv of this species the occurrence of some pa-
pillae along the margin of the mantle of females and
males. Whereas Lea (1863), Reardon (1929), Bereza and
Fuller (1975) and Morrison (1975) did not report these
papillae, Kat (1983) mentioned observing a few papillae.
At various jimctures, and with apparent awareness of
the difficulties regarding the placement of Ligumia
ochracca, both Fuller (1977) and Clarke (in Porter,
1985) indicated that a new genus name was forthcoming.
To date, however, no such name has been pubhshed.
Figure 1. Mantle region of an adult female Ligumia ochra-
cca posterior to the foot. Arrows denote papillae along inner
margin. F = foot, lA = inhalant aperture, M = mantle. Scale
line = 15 mm.
MATERIALS AND METHODS
Materia] cited in the discussion of Ligumia ochracca is
cataloged in the Museum of Zoology, In\ertebrate Di-
vision, University of Massachusetts at Amherst. The cat-
alog numbers are as follows:
Leptodea fragilis (Rafinesque, 1820) UMA MO. 1270, 1.381,
1.38.3, Vermont;
Lioionia nasuta (Say. 1817) UMA MO. 769, 8.32, 1129, 1810,
1849, 1904, Connecticut, Massachusetts, New York;
Lioimia ochracea (Say, 1817) UMA MO. 1053, 1234, 1241,
1809, 1822, 1823, 1850 Connecticut, Maine, Massachu-
setts, and North Carolina;
Ligumia recta (Lamarck, 1819) UMA MO. 1137. 1379. 1902.
\'ermont. New York;
Ligumia subrostrata (Say 1831) UMA MO. 1903, Illinois.
Specific locahHes wiU be furnished upon request.
All specimens used in this studv were prepared fol-
lowing the method described by Smith (1996). For his-
tological studies, a portion of the mantle edge measuring
appro.ximatelv 5 mm- was excised, cleared, and infiltrat-
ed with paraplast®. Embedded specimens v\'ere sec-
tioned at 5 (xm inten'als and stained with hematoxvhn
and eosin. Bright field micrography was accomphshed
with a Wild M20 microscope. Glochidia were either
whole mounted on slides or mounted on Cambridge
SEM stubs and sputter-coated with gold. SEM microg-
raphy used a JEOL JSM-5200 scanning electron micro-
scope.
RESULTS
Close examination of the mantle margin of carefully re-
la.\ed preserved male and female specimens of L. ochra-
cca revealed a row of small but regular papillae extend-
ing along the mantle margin from the base of the in-
halant aperture anteriorlv to the gape of the foot. The
papillae are regularlv arranged (figure I), rather closelv
set, and average about 100 (jim in length (figures 2, 3).
They are less developed than those of Ligumia nasuta,
L. subrostrata, or L. recta, which mav reach >1 mm in
length. The mantle edge bearing these papillae is slightly
lamellate and there is no indication of a flap or lacera-
tions, as is also the case with L. nasuta, L. subrostrata,
and L. recta. The papillae of L. ochracea appear at a
young age, about two years as evidenced by prominent
grov\4h marks on shells of 20-25 mm in length. At this
age (shell size), the papillae are not as closeK- set as in
the adult and there is no evidence of crenulation, a flap,
or a "lacerated" structure (sensu Ortmann, 1912).
The mantle edge of L. ochracca is pigmented with a
cream, orange-ochre, or hght-grev background and var-
iegated with darker grev. Although most of the darker
pigment is distributed near the posterior portion of the
mantle edge (figure 1), no specific pattern is e\ident. In
this regard, L. ochracea is intermediate between L. na-
suta, which has verv dark pigment throughout and a dis-
cernible pattern, and L recta and L. subrostrata. in
D. G. Smith, 2000
Page 157
3f^'
Figure 2. Section of mantle edge of female Lii^iimia ocJira-
cca (sliell lengtli = 55 mm) from the Connecticut Ri\er, Con-
necticut. Scale line = 50 ni.
Figure 3. Same as figure 2, different specimen (shell length
= 72 mm). Scale hne = 50 ni.
Figure 4. Glochidia of Liotania ochracea (left) and Leptoclea
Jrajiilis (right). Scale line = 200 m.
which the mantle edge is a siightK" variegated, pattern-
less, light- to dark-gray. The mantle margins o( Ligiimia
subrosirata and L. recta differ in that the inner edge of
the mantle of L. suhrostrata has a very dark-brown bor-
der, a feature absent in L. recta. Both species possess a
densely pigmented "eye spot" at the base of the inhahint
aperture. In L. recta, the spot is small and not swollen;
in L. suhrostrata, however, the spot is actually a shghtly
thickened pad, almost lobe-like in a few specimens. The
function of these spots is as yet unclear, although it is
supposed that thev act as some sort of light rece]itor. No
such spots are appari'Ht externalK in either L iiasulti or
L. ochracea.
E.\aniined specimens ol Leptodea fragiUs comply with
Ortmann's (1912) (hagnosis for the most part. In one
female, a few small papillae extend slightly anteriorly
from the inhalant apertural papillae but subsequently
disappear completely. In the remaining specimens, no
extra-apertural papillae are evident. The crenulation re-
ported by Ortmann (1912) is actually no more than a
shght sinuation of the margin, the edge being uninter-
rupted whatsoever for the length of the mantle. The
mantle margin is slightly more lamellate in the female
than in the male, but there is httle difference between
the sexes. Although the specimens have been in alcohol
for several years, there is no indication of concentration
of pigment in the posterior region <jf the mantle, and no
specific pattern was observed during the original prep-
aration of the specimens (D. G. Smith, unpublished ob-
servations).
The glocliidia of L. ochracea are over twice the size
of those of Leptodea fragiUs (figiu-e 4) (see also Porter,
1985). The glochidia of L. fragilis from Vermont mea-
sure on the average 7.3 |xm (length) by 94 fim (height)
and possess a narrow hinge. This compares well with
observations on glochicha of this species by Surber
(1912). Glochidia of L. ochracea from Massachusetts
have a mean length ot 222 fxm and a mean height of
287 (xm (see Porter and Horn, 1980, for similar values
of North Carohna populations). These values are: shghtly
smaller than those for glochidia from L. nasuta from
Massachusetts and New York, which have a combined
mean length of 256 ^xm and mean height of .318 |xm;
shghtlv larger than L. suhrostrata v\'ith a mean length of
205 fjLm and mean height of 261 [xm; and nearest to
values reported for L. recta, with mean values of 220
|xm by 270 (xm (Ortmann, 1912; Baker, 1928). The ratio
of glochidia length:height among the species is rather
consistent, 0.77 for Ligumia ochracea, 0.78 for L. recta
and L. suhrostrata. and 0.80 for L. na.suta. The ratio of
glochidial length:height in Leptodea fragihs is similar,
0.78, however, as noted above, the glochidia of this spe-
cies are less than one third the size of Ligumia ochracea.
The glochidia of L. ochracea (figure 5) are most similar
to those of L. suhrostrata. which also has a narrow hinge:
those of L. nasuta (figure 7) possess a wider hinge. The
surfaces of the glochidial shell of each species are pro-
vided with minute pores less than 5 |xni in diameter
(figures 6, 8) and the margin opposite the hinge is evenly
cur\'ed and smooth.
DISCUSSION
As concluded earlier by Bereza and Fuller (1975), Lig-
umia ochracea can not be assigned to either Lampsilis
or Leptodea as these genera are currenth' defined. In
the case of Lampsilis, this is further supported by studies
using biochemical techniques (Kat, 1983; Stiven and Al-
Page 158
THE NAUTILUS, Vol. 114, No. 4
Figure 5. Glochidiuni of Li ffania ochracea Scale line = 100 [jliii. Figure 6. Enlargement of glochidial shell surface ofLigumia
ochracea. Scale line = 10 [j.m Figure 7. Glochidiuin of Ligiiinin nasuta. Scale line = 100 (jini. Figure 8. Enlargement of
glochidial shell surface ot Ligumia nasuta. Scale hne = 10 [jim.
derman, 1992). which lia\'e .showii that Liaumia ochra-
cea is quite distantly related to two s)inpatric species of
Lampsilis with mantle flaps. The only recognized lamp-
sihne genus to which the species ochracea can be allo-
cated is Ligtitnia. In re\aew, Ortmann (1912), defined a
large genus, Eiinjnia, which was distinguished from oth-
er lampsihne genera principally by the presence ol pa-
pillae, variously developed, along the mantle margin and
exddent in both the male and female. Glochidia of Eii-
njnia species were hsted as "subovate, oi mediimi size,
or rather large." Other characters, including the nature
of the marsupial gill (Ortmann "type 4") and degree of
attachment of the inner gill were essentially as in Lamp-
silis. The three subgenera oi Eiin/nia listed by Ortmann
(1912) [Micronuja, Canincitlina, Eiinjnia] were even-
tually raised to genus rank and their nomenclature sta-
bihzed (Ortmann and Walker, 1922). The nominotypical
genus sen.su Ortmann (1912) is Ligumia Swainson, 1840
[type-species: Unio recta Lamarck, 1819] and is defined
(Ortmann, 1912, as subgenus Etirynia) by having "quite
regular, uniform, smaller or larger papillae, reaching
about the middle of the lower margin." Ligumia ochra-
cea fits this description and, though less dex'eloped, its
papillae are similar in their external gross morjiholog)- to
those of L. nasuta, less so to L. recta, in which the pa-
pillae are somewhat crowded and slightly irregular.
At present, erection of a new genus for this species
seems unwarranted, in the absence of urgently needed
critical anatomical studies of the various nominal lamp-
sine genera.
ACKNOWLEDGMENTS
1 thank Richard I. Johnson whom, though not in com-
plete agreement with some of what has iieen presented,
provided useful comments on an earher draft of this ar-
ticle. David Strayer, Catherine Corey, Kevin Cummings,
Ethan Nedeau, and Sarah Riseman donated many spec-
imens used in this studv. The study was funded in part
by a grant from The Nature Conservancy, Connecticut
Chapter.
D. G. Smith, 2000
Page 159
Figure 9. Mantle margin of female Ligumia nasuta. Arrow
denotes papilla. Scale line = 5 mm.
Figure 10. Mantle margin of female Ligtnuiti stihrostrnta.
Arrov\' denote.s papilla. Scale line = 5 mm.
Figure 11. Mantle margin of female Ligumia recta. Arrow
denotes papilla. Scale line = 5 mm.
LITERATURE CITED
Atheani. H. D. and A. H. Clarke, Jr 1962. The freshwater
mussels of No\'a Scotia. Bulletin National Museum Can-
ada 183:11-41.
Baker F. C. 1928. The freshwater Mollnsca of Wisconsin. Part
II. Pelec\poda. Bulletin \Vi.sconsin Geological and Natural
History Survey 70:1—482.
Bereza, D. J. and S. L. H. Fuller 1975. Notes on "Lainpsilis"
ochracea (Say) (Mollusca: Bi\alvia). Association of South-
easteni Biologists Bulletin (Abstract) 22:42.
Burch, J. B. 1973. Freshwater Unionacean Clams (Mollusca:
Pelecypoda) of North America. Biota of Freshwater Eco-
systems. Identification Manual 11, United States Environ-
mental Protection Agency, Washington, D.C., 176 pp.
Clarke, A. H. 1981. The Freshwater Molluscs of Canada. Na-
tional Museum of Natural Sciences, National Museums of
Canada, Ottawa, 446 pp.
Davis, G. M. and S. L. H. Fuller 1981. Genetic relationships
among Recent Unionacea (Bivalvia) of North America.
Malacologia 20:217-253.
Fuller, S. L. H. 1977. Freshwater and terrestrial mollusks. In:
J. E. Cooper, S. S. Robin.son, J. B. Fimderbnrg (eds.) En-
dangered and Threatened Plants and Animals of Nortli
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Johnson, R. I. 1970. The .systematics and zoogeography of the
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Johnson, R. I. 1980. Zoogeography of North American Union-
acea (Mollusca: BivaKia) north of the maximum Pleisto-
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Kat, P. W. 1983. Morphologic divergence, genetics, and spe-
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Obsenations on the genus Unio 10:10-92.
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Malacologia :34:355-
Page 160 THE NAUTILUS, Vol. 114, No. 4
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THE NAUTILUS 114{4);161-163, 2000
Page 161
Latims beckijae, a new species of Fasciolariidae
(Neogastropoda) from Brazil
Martin Avery Snyder
745 Newtown Road
Villanova, PA 190S5 USA
ABSTRACT
Latirus becktjae new species is described from off Vitoria, Es-
pirito Santo State, and off Santos, Sao Paulo State, Brazil. The
new species is readily distinguished from conchologically sim-
ilar species in the same genus by its caramel color, white spiral
banding, and angular profile.
Additional key words: Southwestern Atlantic Ocean, south-
eastern Brazil, Peristeniiinae.
INTRODUCTION
In May, 1994, local .shrimpers trawling in 30-35 ni off
Vitoria, Espi'rito Santo State, and in 190 in off Santos,
Sao Paulo, Brazil, collected specimens of Latims that
were tentatively identified as Latims cf. varai Bullock,
1970. Although superficially similar to L. varai, these
specimens are readily distinguished from all other spe-
cies of western Atlantic Latims. Despite having been
collected alive, no soft parts ot the new species were
available for study, and the species is herein described
solely on the basis of shell morjihology. Institutional ab-
breviations are as follows: ANSP, The Academy of Nat-
ural Sciences, Philadelphia; IBUFRJ, Instituto de Bio-
logia, Universidade Federal do Rio Janeiro, Brazil;
MNRJ, Museu Nacional, Rio de Janeiro, Brazil; MORG,
Museu Oceanografico, Funda^iio Universidade do Rio
Grande, Brazil; UNSM, National Museum of Natural
History, Smithsonian Institution, Washington, DC.
SYSTEM ATICS
Family Fasciolariidae Gray, 1853
Subfamily Peristeniiinae Tryon, 1880
Genus Latims Montfort, 1810
Type species: Latims aurantiacus Montfort, 1810, by
monotypy [= L. gibhulus (Gmelin, 1791)].
Latims beckijac new species
(Figures 1, 2)
Description: Shell length to 54 mm. Shell broadly fu-
siform, biconic, moderately heavy, with prominent axial
and spiral sculpture. Protf)conch with 1 3/4—2 smooth.
bulbous, white, translucent whorls, with axial sculpture
and shoulder developing in last 1/4 whorl. Transition to
teleoconch abiTipt, distinguished by coarser axial sculp-
ture, onset of spiral sculpture, and by change of color
from white to orange-tan. Teleoconch with up to 8 1/2
convex, strongly sculptured whorls. Axial sculpture dom-
inant, consisting of 7-8 strong, broad ribs per whorl,
ahgned with spaces between ribs of previous whorl. Ribs
rounded on early whorls, becoming increasingly angular
with size. Growth lines forming widely spaced lamellae,
eroded on early whorls and on spiral cords, most proin-
inent along adpressed suture and between spiral cords
on body whorl. Spiral sculpture of strong, cream-colored
cords (3-5 on early whorls, 5-7 between suture and pe-
ripheiy, 6-7 between peripherv and siphonal canal, 6-9
on siphonal canal) that are most pronounced along axial
ribs. Weak threads (1-2) may be present between adja-
cent cords. Aperture ovate, with weakly developed pos-
terior canal. Golumella with 1 weak, narrow fold below
mid-aperture, and one weak, broad fold over the fasci-
ole, which may represent two partially fused folds. Outer
lip crenulated, with 12-15 irregular hrae running into
the aperture. Siphonal fasciole well developed. Pseudo-
umbilicus slit-like, prominent, open. Siphonal canal as
long as aperture, broad, open, proximal end demarcated
by tubercles on columella and outer hp. Shell color a
dense caramel-tan, with cream spiral cords and threads.
Operculum medium dark-brown, claw-like, with termi-
nal nucleus. Periostracum unknown.
Type locality:
in 30-50 m.
Off Vitoria, Espirito Santo State, Brazil,
Type material: Holotype, USNM 880231 (51.3 mm);
Parat\pe 1, USNM 880232 (48.8 mm); Paratypes 2-3,
Snyder Collection (43.2 mm and 53.4 mm); Paratypes
4-5, IBUFRJ 9121 (55.3 and 51.2 mm); Paratvi:)e 6.
MORG 39008 (50.4 mm); Paraty^ie 7, MNRJ 7696 (52.3
mm), all from the type localit}'. Paratvpe 8, ANSP (52.7
mm), off Santos, Sao Paulo State, Brazil, in 190 ni.
Etymology: The species is named for the author's el-
dest daughter, Becky.
Discussion: Latims hecki/ae resembles L. varoi (figure
3; see also Bullock, 1970) but is reachlv distinguished
Page 162
THE NAUTILUS, Vol. 114, No. 4
Figures 1-2. Latinis becktjae new species 1. Holotype, USNM 880231 (51.3 mm), 2. Paratype 1, USNM 880232 (48.8 mm),
both from off Vitoria, Espirito Santo State, Brazil, in 30-50 m.
Figure 3. Latinis varai Bullock, 1970. Holotype, MCZ 262589 (70.0 mm), from Off Gibara, Oriente Province, Cuba, in 183 m.
from it b\' its smaller, differently colored shell. Latinis
bcckyae has roughK' half as many strong spiral cords as
L varai. The axial ribs in L. heckijae are whitish whereas
in L. varai the axial ribs are light chestnut brown. Larger
(80+ mm), whitish specimens of Latinis have recently
been taken off San Salvador, Bahamas, in depths of 490
m by research submersibles (D. Dan, pers. comm.).
These closely resemble L. varai, but have far fewer spi-
ral cords (R. Bullock, pers. comm.). Not enough material
is presently available to determine whether these spec-
imens represent a deep-water form of L. varai or an-
other new species of deep-water Latinis. Latinis beck-
yae is easilv differentiated from the San Salvador spec-
imens bv its smaller size, darker color, and coarser, more
prominent sculpture.
Latinis beckyae might also be confused with some
specimens of Latinis ctina Petuch, 1990, from Honduras
and east Panama (Petuch, 1990). This latter species is
usuallv bright orange or yellow and broader overall with
a proportionally shorter canal than L. bcckyae. Latinis
cuna has pairs of white cords on the body whorl and
sometimes on earher whorls as well as on the terminal
part of the body whorl. Because of these white spiral
cords, an orange-brown color form of L. cuna superfi-
cially resembles L. beckyae. Separation of the two spe-
cies is easy: L. beckyae is more elongate and angular,
with a relatively larger teleoconch than L. cuna.
There are four previously known species of Latinis
endemic to Brazil, all of which are very distinct from
Latinis becki/ae. Latinis devyanac Rios, Costa and Cal-
vo, 1994. from southeastern Brazil, has a distinctive
curved siphonal canal and grows to just 35 mm (Rios,
Costa and Calvo, 1994). Latinis lacteum Matthews-Gas-
con. Matthews and Rocha. 1991, from northern Brazil.
is glossy-white and grows to just 32 mm (Matthews-Gas-
con, Matthews and Rocha, 1991). Latinis ogum Petuch,
1979 (Petuch, 1979; Rios, 1994: pi. 42, fig. 574), from
eastern Brazil has few large smooth axial nodules and
attains 43 mm. Latinis vennciji Petuch, 19S6, from the
northern coast of Brazil, is very small with a short
stumpv canal, growing to just 26 mm (see Petuch, 1986).
There are five other Caribbean species of Latinis also
found in northern Brazil. Four of them differ in shape
and color from Latinis bcckyae: Latinis carinifer (La-
marck, 1822), (Rios, 1994: pi. 42, fig. 572), Latinis an-
giilatus (Roding, 1798) (Rios, 1994: pi. 42, fig. 572), La-
tinis infundibuhim (Gmehn, 1791) (not Rios, 1994: pi.
42, fig. 573; see Abbott, 1974: color pi. 11, fig. 2491),
and Latinis virginensis Abbott. 1958 (Rios. 1994: pi. 42.
fig. 575). Latinis beniadensis Bullock, 1974, is uniformly
light-cream-orange, a color that sets its apart from La-
tinis beckyae (see Bullock, 1974).
There are six species of Fu.sinus known from Brazil,
of which two are superficially similar to Latinis bcckyae.
The other four species that cannot possibly be confused
with L. beckyae are large Ftisiniis, all with more or less
dark browm markings. These are Fusinus brasilicnsis
(Grabau, 1904) (Rios, 1994: pi. 42, fig. 566), F closter
(Phihppi, 1850) (Rios, 1994: pi. 42, fig. 567), F mar-
moratus (Phihppi, 1846) (Rios, 1994: pi. 42, fig. 569),
M. A. Snyder, 2000
Page 163
and F. stri^atu.s (Pliilippi, 1850) (Rios, 1994: pi. 42, fig.
570). The supei-ficiallv similar species are Fusiuiis Jtart-
vigii (Shiittleworth, 1S56) (Ahl)()tt, 1974: color pi. 11, fig.
2494) and Fnsinn.s frcngiwllii (Carcelles, 1953) (Rios,
1994: pi. 42, fig. 568). Fusiiius haiivigii, a species er-
roneously placed in Latirus by Kaicher (1978: card
1816), exliibits a different color pattern and more nu-
merous ittia] ribs than Latim.s hcckijac. (Fnsinus pactcli
(Dunker, 1867) is a .s\non\in of F hartvigii named from
Brazilian material.) Finally, young specimens ol Fusinus
frcngucUii could be confused with Latinis bech/ae (the
species was originally named in the genus Lathi/ nis [ =
Latinis]). The axial ribs of this species are more nu-
merous and its coloration ranges from uniform white to
pale orange.
LITERATURE CITED
Abbott, R. T. 19.58. The nianiie niollusks of Grand Cayman
Island, British West Indies. Monographs of the Academy
of Natural Sciences of Philadelphia 11:138 pp., 5 pis., 7
figs-
Abbott, R. T. 1974. American seashells. 2nd ed. Van Nostrand-
Reinhold, New York, 663 pp., 24 pis.
Bullock, R. C. 1970. Latinis varai. a new fasciolariid gastropod
from the Caribbean. The Nautilus 83:13:3-1.3.5.
Bullock, R. C. 1974. A contribution to the systematics of some
West Indian Latinis (Gastropoda: Fasciolariidae). The
Nautilus 88:69-79.
Lamarck, J. B. P. A. 1822. Hi.stoire naturelie des animau.x .sans
vertebres . . . Vol. 7, (2), Paris, 711 pp.
Matthews-Cascon, H., H. R. Matthews and C. A. Rocha. 1991.
Nova especie de Latinis Montfort. 1810 (Mollusca:Gas-
tropoda), Boletim do Museu Nacional, no\a serie. Zool-
ogia 349:1-6, figs. 1-4.
Petuch, E. ]. 1979. New gastropods from the Abrolhos archi-
pelago and reef complex, Brazil. Proceedings of the Bio-
logical Society of Washington 92:510-526.
Petuch, E. J. 1986 New South American gastropods in the
genera Comis (Conidae) and Latinis (Fasciolariidae). Pro-
ceedings of the Biological Societ\- of Washington 99:8-14.
Petuch, E. J. 1990. A new molluscan faunule from the Carib-
bean coast of Panama. The Nautilus 104: 57-71.
Rios, E. C. 1994. Seashells of Brazil. 2nd ed. Funda^ao Cidade
[and] Funda^ao Universidade do Rio Grande, Museu
Oceanografico "Prof Eliezer de Carxalho Rios", Rio
Grande, 368 pp., 113 pis.
Rios, E. C., R M. Costa and I. S. Calvo. 1994. From off south-
em Brazil a new species of Latinis. La Conchiglia
26(273):3.3-36.
Roding, P. F. 1798. Museum Boltenianus sive Catalogus ci-
nielioruni e tribus regnis naturae quae olim collegerat.
Pars seciuida continens Conchylia sive Testacea univalvia,
bivalvia & nuiltivahia. Johan Christi Trappii, Hamburg,
viii -I- 199 pp.
THE NAUTILUS
Volume 114
2000
AUTHOR INDEX
Bennetts, R. E.
BURCH, K. W. ..
CiAiN, A. ]
Collin, R
cordeiro, ]
Darrigran, G. .
112
, 18
, 93
117
. 80
, 69
deMaintenon, M. J 14
EZCURRA DE DrAGO, 1 69
Gittenberger, a 1
GiTTENBERGER, E 1
GOUD, J 1
Harasewtch, M. G 38, 103, 142
Hakman, W. N 120
Jansen, D 112
K,WANO, T. 74
k-antor, y. i
Kim, W.
Leal, J. H
Marshall, B. A
MgLean, J. H
monteiro, w.
Pastorino, G
Penchaszadeh, p. E.
Petit, R. E
Rex, M. a
SiMONE, L. R. L
Smith, D. G
Snyder, M. A
Sparks, S. A
Yoon, S. H
103
85
59
18, 150
99
74
38, 127
127
142
93
59, 127
31, 156
162
112
85
NEW TAXA PROPOSED IN VOLUME 114 (2000)
GASTROPODA
Columbella moinensis deMaintenon, 2000, new species (Columbellidae) 15
Copulabvssia riosi Leal and Simone, 2000, new species (Pseudococculinidae) 60
Crepidula argentina Simone, Pastorino, and Penchaszadeh, 2000, new species (Ceilyptraeidae) 129
Epitonium hoeksemai A. Gittenberger and Goud, 2000, new species (Epitoniidae) 4
Epitonitim ingridae A. Gittenberger and Goud, 2000, new species (Epitoniidae) 7
Epitonium lochi A. Gittenberger and Goud. 2000, new species (Epitoniidae) 9
Epitonium twilae A. Gittenberger and Goud, 2000, new species (Epitoniidae) 10
Latinis becht/ae Sn)der, 2000, new species ( Fasciolariidae) 162
Mericn deynzeri Petit and Harasewych. 2000, new species (Cancellariidae) 145
Merica ekti/phos Petit and Harasewych, 2000. new species (Cancellariidae) 148
Merica lussii Petit and Harasewych, 2000, new species (Cancellariidae) 143
Muricopsis {Murexstd) profunda Marshall and Burch, 2000, new species (Muricidae) 24
Muricopsis (Rolandiella ) .scoff i Marshall and Burch, 2000, new species (Muricidae) 26
Obsctiranella Kantor and Harasewych, 2000, new genus (Ranellidae) 103
Ohscuranella papijrodes Kantor and Harasewych, 2000, new species (Ranellidae) 103
Perimnngelia McLean, 2000, new genus (Turridae) 101
RetidriUia McLean, 2000, new genus (Turridae) 100
Rolandiella Marshall and Burch, 2000, new subgenus (Muricidae) 25
Subniso McLean, 2000, new genus (Eulimidae) 100
Torellivelutina .McLean. 2000, new genus (Velutinidae) 99
REVIEWERS FOR VOLUME 114
L. Adamkewicz
K. Bandel
A. G. Beu
R Bouchet
H. W. Chaney
R. Collin
R. H. Cowie
K. S. Cummings
D. J. Eemisse
K. C. Emberton
C. S. Gallardo
M. G. Harasewych
G. Haszprunar
J. M. Healv
D. G. Herisert
E. Jokinen
R. N. Kilbum
C. M. Lalli
H. G. Lee
C. Lydeard
W, G. Lyons
J. H. McLean
R E. Petit
R. Robertson
B. Roth
R. R, Seapy
D. Strayer
A. Verhecken
G. T. Walters
A. Waren
J. B. Wise
Florida Department of State
Katherine Harris
Secretary of State
Florida Arts Council
Division of Cultural Affairs
This program is sponsored
in part by the State of Florida,
Florida Department of State,
Division of Cultural Affairs, and
the Florida Arts Council
't ^: W L
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