Paracypris sp. 1, Sars, 1866
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.4340718 |
persistent identifier |
https://treatment.plazi.org/id/9F3D1275-FFDC-6402-DFD7-FA980C994F2D |
treatment provided by |
Plazi |
scientific name |
Paracypris sp. 1 |
status |
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Paracypris cf. Paracypris sp. 1 in Lord & Lambourne 1991
Fig. 10O View Fig
Material examined
ROMANIA • 1 complete carapace; Black Sea, Romanian Continental Shelf, borehole 817LV, sample CM31A; Rhaetian, Upper Triassic; MNHN.F. F63274 View Materials .
Dimensions
L = 404 µm; H = 135 µm; H/L = 0.41.
Occurrence
Romanian Continental Shelf, Black Sea, Rhaetian, Upper Triassic (this paper).
Remarks
The present species shares very close morphological proximity with Paracypris sp. 1 in Lord & Lambourne 1991 from the Pliensbachian, Early Jurassic, of the Western Pontides, Turkey ( Lord & Lambourne 1991): similar H/L ratio (0.41), low anterior maximum of curvature pointing downward, pointed PB at venter, oral concavity long, poorly expressed, located in anterior half of L max. The two specimens might be conspecific, but the Rhaetian specimen is smaller than the Jurassic one (L = 700 µm;
H = 289 µm) and might represent an immature stage. These two hypotheses can only be tested by more sampling in the two areas.
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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