Cardobairdia, van den Bold, 1960 emend. McKenzie, 1967
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.4340803 |
persistent identifier |
https://treatment.plazi.org/id/9F3D1275-FFDA-6405-DCC6-FBB2096449EB |
treatment provided by |
Plazi |
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Cardobairdia |
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Cardobairdia sp. 3
Fig. 12 View Fig D–F
Material examined
ROMANIA • 1 complete carapace; Black Sea , Romanian Continental Shelf , borehole 817LV, sample CM31C; Rhaetian, Upper Triassic; MNHN.F. F63302 View Materials • 1 RV; same collection data as for preceding; Rhaetian, Upper Triassic; MNHN.F. F63362 View Materials • 1 complete carapace; same locality as for preceding but sample CM31A; Rhaetian, Upper Triassic; MNHN.F. F63303 View Materials .
Dimensions
RV: L = 275–354 µm; H = 143–203 µm; H/L = 0.59–0.64.
LV: L = 283–299 µm; H = 168–192 µm; H/L = 0.52–0.59.
Occurrence
Romanian Continental Shelf, Black Sea, Rhaetian, Upper Triassic (this paper).
Remarks
Cardobairdia sp. 3 is very close to Cardobairdia cf. liassica (Drexler, 1958) in Monostori 2008 from the Pliensbachian of Hungary ( Monostori 2008: pl. 1, fig. 8). Cardobairdia has been attributed to the Sigilliidae , which are merodont hinge ostracods (e.g., Tabuki & Hanai 1999; Olempska 2001). Cardobairdia shows a crenulate posterior tooth, which might correspond to a merodont hingement. However, the ventral bar is not visible, so it is not possible to assess with certainty that it is crenulate or whether the lobes occur before and after the anterior and posterior teeth.
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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