Aglaiocypris ” sp., 1947
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.4340815 |
persistent identifier |
https://treatment.plazi.org/id/9F3D1275-FFC1-641C-DCC1-FC8E08344C24 |
treatment provided by |
Plazi |
scientific name |
Aglaiocypris ” sp. |
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“ Aglaiocypris ” sp. View in CoL
Fig. 10 View Fig F–G
Material examined
ROMANIA • 1 complete carapace; Black Sea , Romanian Continental Shelf , borehole 817LV, sample CM31A; Rhaetian, Upper Triassic; MNHN.F. F63266 View Materials • 1 complete carapace; same locality as for preceding but sample CM31C; Rhaetian, Upper Triassic; MNHN.F. F63267 View Materials • 2 complete carapaces; same locality as for preceding but sample CM31B; Rhaetian, Upper Triassic; MNHN.F. F63357 View Materials .
Dimensions
RV: L = 333–482 µm; H = 162–243 µm; H/L = 0.46–0.49.
LV: L = 333–482 µm; H = 162–243 µm; H/L = 0.48–0.5.
Occurrence
Romanian Continental Shelf, Black Sea, Rhaetian, Upper Triassic (this paper).
Remarks
The present species is close to Aglaiocypris ? sp. from the Ladinian, Middle Triassic, of Spain ( Kozur et al. 1974). This species is morphologically similar to Fabalicypris ? sp. A in Ainsworth 1990 from the Hettangian, Early Jurassic, from Ireland ( Ainsworth 1990), but the carapace of the present species is thinner, with H max located more anteriorly, shorter and more rounded ADB, and AB more rounded and less bairdiid. These characters are closer to those of Aglaiocypris as described in Kozur et al. (1974).
No known copyright restrictions apply. See Agosti, D., Egloff, W., 2009. Taxonomic information exchange and copyright: the Plazi approach. BMC Research Notes 2009, 2:53 for further explanation.
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