Costoanachis sp.

Sacchetti, Claudia, Landau, Bernard & Ávila, Sérgio P., 2023, The Lower Pliocene marine gastropods of Santa Maria Island, Azores: Taxonomy and palaeobiogeographic implications, Zootaxa 5295 (1), pp. 1-150 : 67-68

publication ID

https://doi.org/ 10.11646/zootaxa.5295.1.1

publication LSID

lsid:zoobank.org:pub:F3A52660-70B8-439F-A7A0-F45ADC975EA5

DOI

https://doi.org/10.5281/zenodo.7975937

persistent identifier

https://treatment.plazi.org/id/03CF879C-2C50-0906-FF1D-F8AEFBF6761F

treatment provided by

Plazi

scientific name

Costoanachis sp.
status

 

Costoanachis sp.

Plate 4 J View PLATE 4

Santa Maria material examined. Maximum height 2.7 mm, width 1.6 mm. DBUA-F 1059 (1), Baía do Raposo, Santa Maria Island, Azores, Touril Complex , Lower Pliocene .

Description. Shell small, broadly fusiform. Protoconch missing. Teleoconch of three convex whorls, separated by deeply impressed, undulating suture. Sculpture on spire whorls of strong orthocline axial ribs, 11 on last whorl, roughly equals into space, extending slightly adapically, crenulating suture. Last whorl globose, evenly rounded, strongly constricted at base, with 16 broad weakly opisthocline ribs and fine spirals cords restricted to the base and siphonal fasciole. Aperture obscured by matrix, outer lip and siphonal canal incomplete.

Discussion. The species is represented by a single incomplete juvenile specimen from Baía do Raposo. It is characterised by the strong axial ribs and spiral sculpture that is restricted to the base and the siphonal fasciole on the last whorl. Costoanachis arpula ( Michelotti, 1840) and C. turbinellus ( Sacco, 1890) are both more evenly fusiform with spiral sculpture throughout. The last two species are better placed in Zafrona Iredale, 1916 (Landau et al. 2019a: 150). The Azorean specimen is more closely similar to C. rectecosta ( Sacco, 1890) (syntype illustrated in Ferrero Mortara et al. 1981: pl. 58, fig. 3) from the upper Miocene of Italy, that also has strong ribs and spiral sculpture restrict to the base. The preservation of the Azorean specimen does not allow further identification.

Distribution. Lower Pliocene: Atlantic, Santa Maria Island, Azores (this paper).

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