Bairdiacypris? sp. 4, Bradfield, 1935

Forel, Marie-Béatrice & Grădinaru, Eugen, 2020, Rhaetian (Late Triassic) ostracods (Crustacea, Ostracoda) from the offshore prolongation of the North Dobrogean Orogen into the Romanian Black Sea shelf, European Journal of Taxonomy 727, pp. 1-83 : 24

publication ID

https://doi.org/ 10.5852/ejt.2020.727.1183

publication LSID

lsid:zoobank.org:pub:85AF63D9-5E9E-4CE0-AEC6-6F7CC8C4D375

DOI

https://doi.org/10.5281/zenodo.4340795

persistent identifier

https://treatment.plazi.org/id/9F3D1275-FFFB-6424-DCCE-FD2B08324859

treatment provided by

Plazi

scientific name

Bairdiacypris? sp. 4
status

 

Bairdiacypris? sp. 4

Fig. 6 View Fig T–U

Material examined

ROMANIA • 1 complete carapace; Black Sea , Romanian Continental Shelf , borehole 817LV, sample CM31B; Rhaetian, Upper Triassic; MNHN.F. F63213 View Materials 1 complete carapace; same locality as for preceding but sample CM31A; Rhaetian, Upper Triassic; MNHN.F. F63214 View Materials 5 complete carapaces; same locality as for preceding but samples CM31A, CM31B and CM31C; Rhaetian, Upper Triassic; MNHN.F. F63345 View Materials .

Dimensions

RV: L = 327–809 µm; H = 157–326 µm; H/L = 0.38–0.48.

LV: L = 327–809 µm; H = 167–348 µm; H/L = 0.41–0.51.

Occurrence

Romanian Continental Shelf, Black Sea, Rhaetian, Upper Triassic (this paper).

Remarks

The absence of an antero-ventral offset of the overlap leads to the generic attribution to Bairdiacypris rather than Fabalicypris . However, in the absence of angulations at the dorsal margin, this identification is still tentative. Bairdiacypris ? sp. 4 is closely related to Fabalicypris ? praelonga Donze, 1966 from the Plicatulus Horizon, Hettangian, Early Jurassic, of Le Sartre, Ardèche, France ( Donze 1966). However, Bairdiacypris ? sp. 4 differs by having a more bairdiid AB with a maximum of curvature located higher and the AVB more raised dorsally. It is worth noting that the doubt in the generic attribution of Fabalicypris ? praelonga is related to Donze’s inability to observe the inner structures ( Donze 1966).

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