Cyclotopsis praecursor, Neubert & Damme, 2012

Neubert, Eike & Damme, Dirk van, 2012, Palaeogene continental molluscs of Oman, Contributions to Natural History 20, pp. 1-28 : 10-12

publication ID

https://doi.org/ 10.5169/seals-787080

DOI

https://doi.org/10.5281/zenodo.5838578

persistent identifier

https://treatment.plazi.org/id/B56A8789-FFED-E50B-0D02-FD6AFC6CFD21

treatment provided by

Carolina

scientific name

Cyclotopsis praecursor
status

sp. nov.

Cyclotopsis praecursor View in CoL sp. nov.

( Figs. 8–9 View Figs )

Type specimens: Holotype NMBE 5018970 View Materials ; paratypes NMBE 5018971–5018973 View Materials , MNHN/25 About MNHN , SMF 340184/25 ; paratypes Wadi Darbat , NMBE 5018974 View Materials , 5019038– 5019043 View Materials .

Type locality: Thaytiniti , Dhofar, Oman .

Stratum typicum: Paludal biomicritic limestones of the Zalumah Formation.

Age: Late Priabonian.

Material: This species is very abundant at Thaytiniti and Wadi Darbat.

Etymology: praecursor from Latin for predecessor, a noun in apposition.

Diagnosis: A fossil species of Cyclotopsis with a slightly elevated spire and an operculum with a lamella-like coiled spiral.

Description: Shell much broader than high, spire slightly elevated; protoconch relatively large, consists of 2 whorls, surface sculpture not preserved; teleoconch of 3.5–4 rapidly increasing whorls; surface sculpture of 3–5 strong spirals (only preserved on the upper whorls); last whorl only slightly descending before the aperture; aperture almost circular, with a slightly thickened lip; umbilicus very large, broad dish-like, umbilical walls very probably smooth; operculum multispiral, spiral consisting of a broad raised lamella of at least 3 whorls.

Measurements: Holotype ( Fig. 8 View Figs ): H = 6.73 mm; W = 9.18 mm; h = 4.42 mm; w = 4.25 mm; Wh = 5.5.

Remarks: Roger & al. (1994) probably refer to eroded specimens of this species as 'cf. valvata '. The preservation state of the specimens from the type locality in Thaytiniti is quite poor and mainly consists of internal casts. However, in a few cases, remains of the shells themselves are preserved, allowing reconstructing of some details of the surface sculpture. These specimens display the same teleoconch sculpture as the specimens from Wadi Darbat ( Fig. 9 View Figs ), where the preservation state is much better (but no specimen with an operculum could be traced there).

This fossil species is placed in the extant genus Cyclotopsis , because it is almost indistinguishable from the few species from India (for comparison see the syntype of Cyclostoma semistriatum SOWERBY, 1843 ( Fig. 10 View Figs ), the type species of Cyclotopsis ). It shares autapomorphic details of umbilicus and operculum together with the spiral sculpture of the teleoconch. It differs from most of the Soqotran species of Dioscopoma NEUBERT, 2009 , which usually have a reticulate surface sculpture, a more narrow umbilicus, and an operculum with a flat sutural line and not a raised spiral; also, most of the species of Dioscopoma display a spiral sculpure on the inner umbilical wall, which is very probably smooth in C. praecursor sp. nov. Today, the Dhofar area is inhabited by two species of the genus Rochebrunia BOURGUIGNAT, 1881 , but these have larger shells with a closed umbilicus and an almost smooth operculum. For a more detailed discussion of the pomatiid genera and species of the area see Neubert (2009), and for pomatiid operculum structure Wilmsmeier & Neubert (2012).

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