Conus
aemulator (Brown & Pilsbry, 1911)
Conus
aemulator manzanillaensis (Mansfield, 1925)
Conus aemulator michoacanensis (Perrilliat,
1992)
Descrizione e caratteristiche:
Occurrence (4).
—Conus aemulator was described from excavations for the Gatun locks,
which Woodring (1970, p. 351) characterized as middle
Gatun Formation. Woodring (1970) reported the species as spanning the Gatun
Formation. Additional records presented by Woodring (1970) for C. aemulator
come from Neogene localities throughout tropical America, including the Darién
and Bocas del Toro areas of Panama, Ecuador, the Dominican Republic, Haiti, the
Grenadine Islands, and Colombia; these all require confirmation (4).
Very recently, Landau et al.
(2016) reported the species from the lower–middle Miocene Cantaure Formation of
Venezuela (4).
Description (4).
—Maximum shell size: medium. Largest observed specimen
(UF 270973) has SL 43.7 mm. Typical shell size of specimens from UF locality
YN020: medium (32.3 mm; N=29). Last whorl.—Shape conical to broadly conical (RD
0.64–0.73, x= 0:68; PMD 0.86–0.91, x= 0:88; N=17); outline convex on posterior
half, nearly straight on anterior half, resulting in a slightly convex profile.
Shoulder carinate and forming a posteriorpointing ridge. Widest part of shell
below shoulder. Aperture slightly wider at base than shoulder. Siphonal notch
absent. Slightly wavy spiral threads or cords present, usually restricted to
the anterior half, but in rare cases extend past the midline or are absent
altogether. Some specimens (e.g., UF 259739, UF 270980) show evidence of weakly
beaded spiral threads. Spire whorls.—Spire low to moderate (RSH 0.05–0.19, x=
0:11; N=17); outline concave to slightly sigmoidal. Early spire whorls stepped.
Protoconch unknown. Ornamentation of early postnuclear whorls unknown. Sutural
ramp slightly convex
to flat on early whorls, concave
or sigmoidal in later whorls, with 3–6 (typically four) spiral grooves that
separate threads. Subsutural flexure asymmetrical to strongly asymmetrical (ASSF 0.2–0.7, x =0:4, N= 4), depth typically
slightly greater than width (DWSSF 0.9–1.7,
x=1:3, N=4) (Fig. 6.6) (4).
Coloration pattern (4).
—One pattern present. Pattern
usually consists of three rows of discontinuous spiral bands. The elements
within the bands are complex, including sub-rectangular blotches (e.g., Fig.
6.7), diagonal streaks (e.g., Fig. 6.8), subtriangular markings (e.g., Fig.
6.11, 6.13), irregular blotches (Fig. 6.14), or closely spaced axial streaks
(Fig. 6.15); in one observed specimen (Fig. 6.16), the spiral elements form
nearly continuous bands. Sutural ramp with occasional blotches (4).
Materials (4).
—ANSP 1691 (holotype, Fig.
6.1–6.3); USNM 645744 (one specimen, figured by Woodring, 1970; Fig. 6.4, 6.5);
56 additional observed specimens, all from UF locality YN020, which are listed
in Supplementary Data Set 1 (4).
Remarks (4).
—This species was described from the Gatun Formation on the basis of a
single calcitic cast (holotype, ANSP 1691; Fig. 6.1–6.3). This poorly preserved
specimen has a conical last whorl (RD 0.66, PMD 0.86) and a moderately high
spire (RSH 0.14); there is evidence of several spiral threads on the sutural
ramp and on the anterior half of the last whorl. Despite the poor preservation
of the holotype, the characteristics preserved allow it to be recognized as a
valid taxon. Shells of Conus aemulator are very similar to those of C.
molis and the possibility that specimens of C. aemulator are in fact
juvenile C. molis was carefully considered. Both taxa have shells that are
similar in overall shape, are widest below the shoulder, have raised spiral
ornamentation on the anterior half of the last whorl, and possess spiral
ornamentation (4).
Distribuzione temporale: Oligocene
Superiore – Miocene Medio
Distribuzione geografica: Colombia,
Venezuela, Ecuador, Panama, Lesser Antilles,
Grenadine Island
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Conus aemulator (1) - ( Brown & Pilsbry,
1911 ) mm. 22,5 x 12,8 Panama |
Conus cf. aemulator (3) - ( Brown & Pilsbry, 1911
) mm. 45,1 x 26,4 Carriacou Island |
Conus aemulator
manzanillaensis (Mansfield, 1925) Trinidad |
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Conus aemulator (1) - ( Brown & Pilsbry,
1911 ) mm. 45 x 28 Panama |
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Conus aemulator (3) mm. 22,7 x 12,8 |
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Panama |
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Conus aemulator - ( Brown & Pilsbry,
1911 ) mm 39,1 x 24,6 – Miocene - Gatun Fm. [AZFC N. 507-01] |
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Conus cf. aemulator (3) mm. 45,1 x 26,4 Carriacou Island |
Conus aemulator (1) (4) USNM 645744 Woodring (1970, pl. 56, figs. 4, 8) mm. 45,2 x 28,7 Panama |
Conus aemulator mm. 39,1 x 24,6 Miocene - Gatun Fm. [AZFC N. 507-01] |
Conus aemulator (3) mm. 22,7 x 12,8 |
Conus aemulator (1) mm. 22,5 x 12,8 Panama |
Bibliografia Consultata
· (2) - Peter Jung - Fossil Mollusk from Carriacou, West Indies
· (3) - Woodring – Geology and Paleontology of Canal Zone and Adjoining Parts of Panama