Conus trailli (Hutton, 1873)
Conus huttoni (Tate,
1890)
Conospirus
bimutatus (Finlay, 1924)
Conus ornatus
(Hutton, 1873)
Description.
69. C.
ornatus, sp. nov. Whorls smooth, with a row of small nodules on the keel, crossed
by two or three spiral lines ; a few spiral stria: at the anterior end of
the body whorl. Axis, .8 ; breadth, .3.
Localities.-
Awamoa (2).
70. C.
trailli, sp. nov. Spire whorls smooth, angled; body whorl faintly
distantly irregularly spirally striated. Axis, .9 ; breadth, .43.
Localities.-Awamoa
(2).
Hutton (1873. p. 10) gave brief
diagnoses (without illustrations) of two species of fossil cones (Conus
ornatus and Conus trailli) from "Awamoa". a locality-that refers to the Altonian siltstones and shell
beds exposed along the banks and, on occasion, at the mouth of Awamoa Crek,
North Otago.
Tate (1890, p. 189) noted that Conus trailli Hutton was
preoccupied by "C. Traillii Adams", and proposed the
replacement name Conus huttoni, but since this nomenclatural change was
included in a paper on Australian Cenozoic mollusks, it was overlooked by New
Zealand workers for nearly 40 years.
In the meantime. Suter (1914. p. 31) redescribed both species and figured the type specimens, using rather idealised pencil drawings originally
made by John Buchanan under the
direction of Sir James Hector. He referred ornatus to Conospira (as
a subgenus of Conus) and trailli to
Hemiconus, noting that there was a prior Conus ornatus Michelotti,
but since he considered Michelotti's species lo be a Hemiconus he
thought Hutton's name could stand.
Somewhat later Suter had occasion
to examine some cones collected by James Park from Pukeuri, North Otago
(Altonian), and on the basis of the variation in strength of the peripheral
nodules concluded that C. ornatus and C. trailli were synonyms
(Suter 1917, p. 84). Suter decided to use the name ornatus, which has
page priority, and—apparently overlooking his earlier statement about Conus
ornatus Michelotti— referred Hutton's species to Hemiconus.
Finlay (1924a, p. 105) pointed out
that since Conus ornatus Button is preocuppied by Michelotti's name, C.
trailli should be used instead, assuming that the two Mutton names refer to
the same species. Shortly afterwards Finlay (!924b, p. 498, footnote)
discovered that Conus trailli Hutton was preoccupied by C. trailli A.
Adams, 1855, and therefore introduced the new replacement name Conospira (misspelt Cenospira) bimutata.
In yet
another paper, Finlay
(1927, p. 518-19) drew attention to Tale's much earlier replacement name for Conus
trailli Hutton and transferred it to genus Conospira. Later workers
have changed the generic name to Conospirus (Marwick 1931. p. 132) and Conilithes
(Fleming 1966a, p. 70), but for some 45 years the specific epithet huttoni
has been used, in one combination or the other, for the rather elegant
cone that is so characteristic of Altonian faunas in North Otago and South
Canterbury.
My own work suggests that (1):
(a)
Conus
ornatus Hutton and C.
trailli Hutton are distinct taxa;
(b)
C.
trailli (= C. huttoni)
is so far known only from the holotype; (c) since both Conus huttoni and
Conospira bimutata were proposed as replacement names for C. trailli,
the common 'Awamoan' cone is without a name
Conus
ornatus (4)
Conus
(Conospira) ornatus
Hutton. Plate II, fig. 14 ; Plate XVII, fig, 7. 1873.
Conus ornatus
Htitton, Cat. Tert. Moll., p. 10. 1887. „ „ Hutton, P.L.S. N.S.W. (2), vol. i,
p. 212.
Shell
small, biconic, spire elevated, with small nodules on the keels, the greater
part of the body-whorl smooth. Sculpture : Protoconch smooth, the following whorls
with a broad shoulder, the keel below the middle of the whorl, ornamented with numerous
small nodules, crossed by a few spiral linear grooves ; body-whorl with
about 8 oblique cinguli. Spire conical, about half the length of the aperture,
angle about 65°.
Protoconch
subulate, consisting of 3 convex whorls. Whorls 8 to 9, slowly increasing, the
shoulder slightly concave ; body-whorl an inverted cone. Suture but little
impressed. Aperture high and narrow, oblique, the margins parallel, truncated
at the base. Outer lip almost straight, sharp, angled above. Columella oblique,
very slightly convex, with a distinct spiral groove above.
Height,
20 mm. ; diameter, 8 mm. (type).
Type in
the collection of the New Zealand Geological Survey.
Loc. —
Awamoa, South Island. Miocene.
Remarks.
— There is a Conus ornatus Michelotti, which, however, belongs to the
genus Hemiconus Cossmann, 1889.
Conus
trailli (4)
Hemiconus
trailli (Hutton). Plate II, fig. 15, a, b. , 1873.
Conus trailli Hutton, Cat. Tert. MoU., p. 10. 1887. „ „ Hutton, P.L.S. N.S.W. (2), vol. i, p. 212.
Shell small, biconic, with raised scalar spire, subnodose keels, and irregular spiral grooves on the body-whorl. Sculpture : Protoconch smooth, succeeding whorls with curved retrocurrent growth-lines upon the shoulder, which are obliquely slightly ante-current on the body-whorl ; the keels are subnodulous, there are a few spiral lines below, and the suture is plicated below ; body-whorl with distant, irregular, and but slightly impressed spiral grooves, deeper and closer together upon the base. Spire conoidal, outlines scalar, straight, its height a little more than one-third the height of the aperture, angle about 65°. Protoconch small, obtuse. Whorls about 8, regularly and slowly increasing, the body-whorl large, inverted conical ; spire-whorls with a broad shoulder, which is but very little concave, and the distinct keel is at the lower third of the whorls. Suture but little impressed. Aperture long and narrow, the margins subparallel, angled above. Outer lip lightly convex, angled above, with a shallow sinus at the shoulder, sharp. Columella oblilque, straight above, slightly twisted below ; there is no distinct groove below the suture.
Height, 21 mm. ; diameter, 11 mm. (imperfect type specimen).
Height, 41 mm. ; diameter, 17 mm. (perfect specimen).
Type in the collection of the New Zealand Geological Survey.
Loc. — Awamoa, South Island. Miocene.
Hutton,
1873 (2) |
Conus trailli |
|
|
There are traces of weak peripheral nodules on the early spire whorls,
but not on later whorls, giving the shell a superficial resemblance to the
smooth-shouldered cones here considered to be variants of C. wollastoni.
It differs from both forms of C. wollastoni in having distinct spiral
grooves over the whole of the last whorl below the shoulder. |
Conus trailli
(Hutton, 1873) and Conus ornatus (Hutton, 1873) are two different
species |
|
Hutton, 1873 (2) |
Holotype TM 5465 Altoniano
(Lower Miocene) New Zealand
Stage Altonian
(17.5 - 16.5) |
|
|
|
|
|
Tate,
1890 |
= Conus trailli Holotype
Altoniano
(Lower Miocene) |
|
|
The
name Conus trailli (Hutton) is replaced by Conus huttoni |
Conus
trailli Hutton was preoccupied
by "C. Traillii Adams" |
|
Suter,
1914 |
|
|
|
Conus
trailli became
Hemiconus trailli Conus
ornatus became Conospira ornatus |
|
|
Suter,
1917 |
|
|
|
Conus
ornatus synonym of Conus trailli Both
named Conus ornatus |
|
|
Finlay,
1924a |
|
|
|
Conus
ornatus preocuppied by Michelotti's name, so Both
named Conus trailli |
|
|
Finlay,
1924b |
Conospirus bimutatus |
|
|
Conus trailli Hutton was
preoccupied by C. trailli A. Adams, so named both Conospirus
bimutatus |
|
|
Finlay,
1926 |
Conus
rivertonensis |
|
|
Finlay (1926, p. 255) distinguished C.
rivertonensis from Conospira
bimutata Finlay (Le., Conilithes wollaston i) by its
"longer and more exsert spire and narrower shell". Judging by Finlay's
illustration of the holotype (the only known specimen) the shoulder is
situated much higher up on later spire whorls than in any specimen of C.
wollastoni. |
|
|
Marwick,
1931 |
Conus
oliveri |
|
|
The protoconch is considerably larger and
more narrowly conical in C. oliveri than in C. wollastoni. |
|
|
Conus
wollastoni Plate 22 V GS95000, J41/f8028 Excavation for Oamaru Borough Council
septic tank South Oamaru – Altonian New Zealand Stage: Altonian (17.5
- 16.5 My) |
|
|
Conus
trailli = Conus
huttoni (v. Tate, 1890) |
Conus
ornatus now is without a name |
|
|
= Conus trailli Holotype
Altoniano
(Lower Miocene) Awamoa
– N. Ottago |
|
|
|
Holotype TM 5465 Altoniano
(Lower Miocene) New Zealand
Stage Altonian (17.5 - 16.5) |
Holotype TM 5447 Altoniano
(Lower Miocene) New Zealand
Stage Altonian (17.5 - 16.5) |
Hypotype TM 5477 Altoniano (Lower
Miocene) New Zealand
Stage Altonian (17.5 - 16.5) |
|
|
Conus huttoni
Auckland Museum MA48381 |
|
Middle Miocene (Balcomian 9-12 Ma) Fyansford Formation Australian Portland Cement Limited Quarry Batesford, Victoria, Australia [Andrea
Petri] |
Bibliografia Consultata