Hiatobairdia sp. 2, Kristan-Tollmann, 1970

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 : 31

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.4340813

persistent identifier

https://treatment.plazi.org/id/9F3D1275-FFF2-642D-DCC1-FE920EF64A29

treatment provided by

Plazi

scientific name

Hiatobairdia sp. 2
status

 

Hiatobairdia sp. 2

Fig. 8 View Fig C–E

Material examined

ROMANIA • 1 complete carapace; Black Sea , Romanian Continental Shelf , borehole 817LV, sample CM31B; Rhaetian, Upper Triassic; MNHN.F. F63230 View Materials 1 LV; same collection data as for preceding; Rhaetian, Upper Triassic; MNHN.F. F63231 View Materials 2 LV; same collection data as for preceding; Rhaetian, Upper Triassic; MNHN.F. F63349 View Materials .

Dimensions

RV: L = 1068 µm; H = 644 µm; H/L = 0.6.

LV: L = 838–1068 µm; H = 520–695 µm; H/L = 0.62–0.63.

Occurrence

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

Remarks

Hiatobairdia sp. 2 is characterized by its very high and nearly symmetrical AB and PB, which clearly relates it to Hiatobairdia arcuata Kristan-Tollmann in Kristan-Tollmann et al., 1980 from the Rhaetian of Iran ( Kristan-Tollmann et al. 1980). However, Hiatobairdia sp. 2 is differentiated from it by having the lateral surface not overhanging the ventral margin, absence of postero-ventral thickening and less pronounced antero-dorsal and postero-dorsal concavities. Hiatobairdia sp. 2 is undeniably a new species, but we lack enough material to define its diagnostic characters.

Kingdom

Animalia

Phylum

Arthropoda

Class

Ostracoda

Order

Podocopida

SuperFamily

Bairdioidea

Family

Bairdiidae

SubFamily

Bairdiinae

Genus

Hiatobairdia

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