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Conus omaria
Andaman Is.:
one pale surabajensis in the museum of Calcutta, sent to me for examination by Dr. Ray in 1957, it came from an old
collection, but the "A'' written originally on the base of the shell makes the correctness of indication rather probable.
Western Sumatra:
two typical walkeri collected in West Sumatra by Aurivillius in 1891, personally examined in the museum of Stockholm in 1957.
- These two areas close the gap between Lemuria and Malaysia.
North West Australia:
one shell (17 mm.) from Peak Is. in the Dampier Archipelago, collected by the Davina Expedition in 1960, presented me (coll.
Schilder No. 11862) by Ray Summers; some more specimens seem to have been collected in the Dampier Archipelago by this
expedition. Besides, walkeri has been mentioned from Nickol Bay by Brazier (1879, Journ. Conch. 2:321).
North Australia:
Yirrkala in Eastern Arnhem Land, according to Iredale (1939, Austr. Zoologist 9:299). - These two areas extend the occurrence
of walkeri to tropical Australia west of Torres Strait.
Aru Is.:
one shell (19 mm.) recalling the western walkeri has been collected by Merton in 1908, personally examined in the Senckenberg
museum in Frankfurt on Main, Germany. - This locality closes the gap between Misool (Schepman 1909, Siboga Exped. 49/2/2:133)
and Torres Strait (Brazier 1879). The indication "New South Wales'' by Iredale (1935, Austr. Zoologist 8:127) needs
confirmation, the southernmost reliable indication in East Australia seems to be Peel Is. in Moreton Bay.
Ryu-kyu Is.:
Kuroda (1960, Cat. Moll. Fauna Okinawa, p. 21) mentioned "walkeri surabajensis" from Okinawa Is.; the indication seems
correct, as P. W. Clover enumerated two specimens of walkeri from "South of Japan'' in a manuscript list of cowries preserved
in Japanese collections (communicated to the writer by Mr. Ray Summers in 1961).
Caroline Is.:
Recently Mr. C. N. Cate presented me two walkeri from Moen Is. in the Truk Is. (coll. Schilder No. 17135 and 17136); they
formerly belonged to a series of fifteen similar shells dredged by R. Willis in the harbour in January 1962. These two shells
are "pellucid" like the dead glossy cowries dredged in Honolulu harbour, and exhibit a similar white chalk in the aperture:
there, the conditions of preservation in the harbour of Moen Is. must be about equal to those in Honolulu. The specimens
undoubtedly belong to walkeri (surabajensis) and not to bregeriana: the discovery of this far-off population of walkeri in
the central Caroline Is. is not very surprising, as other typically Malayan cowry species also spread to western Micronesia,
e.g. Erronea ovum Gmelin and E. onyx Linnaeus to Palau and Guam respectively.
Northern Melanesia:
Mrs. K. Matcott of Mooloolaba, Queensland informed me by letter in March 1963, that she possesses a "surabajensis" from New
Britain; as I have never examined the shell personally, the reliability of this indication seems to need confirmation.
In land snails real sinistrality is frequent: there are families, genera, and species in which all shells are sinistral. In
some usually dextral species hereditary mutation in a population caused sinistrality of a local race: so all specimens of
Fruticicola lantzi are sinistral in one valley east of Alma Ata while this species is dextral in all other places of Central
Asia. (Schilder 1952, Biotaxonomie (Jena), p. 74, map fig. 36). In other cases, sinistral shells may be classified as rare
abnormalities: so in Helix pomatia, a large edible snail sold in large quantities chiefly in France, there is one sinistral
specimen (called "king") among 6,000 to 8,000 shells, and in the allied smaller species of Cepaea there is one sinistral
shell among 30,000 to 150,000 dextral ones (Schilder 1953, Die Banderschnecken (Jena), p. 17).
In marine gastropods sinistral shells seem to be rarer. A normally sinistral cone (Conus adversarius) from the Pliocene beds
of Florida, has been figured in the Sean Raynon Sabado (n.s.) 2:3 (February, 1960).
In cowries sinistral specimens are extremely rare, if indeed they occur at all. Among the more than 150,000 cowries which the
writer has examined personally during forty-four years special study, there was no sinistral shell. But R. J. Griffiths
(1962, Mem. Nat. Mus. Melbourne, 25:217) mentions a sinistral Notocypraea declivis which is preserved in the South Australian
Museum: its curator would oblige many malacologists if he would publish an enlarged photograph, at least of the basal view of
this curiosity.
Another case of sinistrality in cowries has been proved to be erroneous: Stoliczka (1867, Palaeont. Indica (5) 2:56, pl. 4,
fig. 6) has established a Cypraea anomala from the Cretaceous of India, believing it to be a sinistral shell. But details of
the drawing of the incomplete shell undoubtedly show that Stoliczka's specimen represents its posterior extremity, and not
its anterior extremity as the author supposed, so that anomala is a normally dextral Palaeocypraea (Schilder 1926, Rec. Geol.
Surv. India 58(4):372).
Collectors should be eager to find a really sinistral cowry among the shells which go through their hands, and if they were
happy enough to detect one, they should publish it in the Sean Raynon Sabado, accompanied by a photograph. For such a shell
would be more valuable than the rarest cowry species we know.
But I think that nobody will find a sinistral cowry.
Three small oblong cowries which have been dredged as dead shells in 80 fathoms off the Bonin Islands, have been described as
Erosaria cernica ogasawarensis Schilder 1944 (Arkiv for Zoologi 36.A.2, p. 22); their formulae i.e. length in mm., breadth
in per cent of length (in brackets [parentheses]), and number of labial and true columellar teeth (separated by a colon) are
as follows:
13(60)18:14 (a rather worn paratype), 15(57)17:15 (holotype according to Schilder 1958, Arch. Mollusk. 87:172), 16(56)19:18
(paratype in coll. Schilder No. 7433).
As these shells never have been figured before, I think it useful to publish a photograph of the last-named paratype of 16mm
because a specimen from the Bonin Is. figured by Cate (1960, Veliger 3, pl. 1, fig. 5) is a much larger and broader shell, as
its formula is 29(64)23:24.
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