Perisphinctes (Dichotomosphinctes), 1926
publication ID |
https://doi.org/ 10.5281/zenodo.4651042 |
persistent identifier |
https://treatment.plazi.org/id/6A5FC813-3762-BD03-FD55-FA8AC740FCF6 |
treatment provided by |
Felipe |
scientific name |
Perisphinctes (Dichotomosphinctes) |
status |
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Perisphinctes (Dichotomosphinctes) gr. antecedens ? Salfeld, 1914 ( Fig. 5C View FIG )
MATERIAL EXAMINED. — MI3 9/3, MI3 9/10.
STRATIGRAPHIC DISTRIBUTION. — Bed 9 of section Castello Inici, which has been assigned to the Middle Oxfordian Plicatilis Zone.
DESCRIPTION
The two incomplete specimens correspond to evolute shells; the largest one probably reached the
diameter of 12 cm. The whorl section is rectangular to subtrapezoidal, characterized by a relatively large venter, flat to gently round flanks, a well developed rounded umbilical margin and a flat to oblique umbilical wall. Ribs are strong and gently prorsiradiate. The two fragments only show biplicate ribs whose point of branching is located on the upper fourth of the flank.
DISCUSSION
The preservation of the studied specimens is too poor to allow a reliable identification. The ribbing and the general features of the shell suggest affinities with the group of P. antecedens . The specimens from Castello Inici bear a wider whorl section than the one developed by the type specimens studied by Arkell (1937) and by specimens from the Jura Mountains and from Beauvoisin ( France), respectively described by Enay (1966) and Bourseau (1977). However, Enay (1966: 473) mentions that some specimens have flanks that converge towards the venter.
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