Bairdiacypris? sp. 4, Bradfield, 1935
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 |
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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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