Acratia nagyvisnyoensis? Forel, 2013

Zazzali, Sindbad, Crasquin, Sylvie, Deconinck, Jean-François & Feng, Qinglai, 2015, Biodiversity across the Guadalupian-Lopingian Boundary: first results on the ostracod (Crustacea) fauna, Chaotian section (Sichuan Province, South China), Geodiversitas 37 (3), pp. 283-313 : 292

publication ID	https://doi.org/ 10.5252/g2015n3a1
publication LSID	urn:lsid:zoobank.org:pub:5F708564-E50F-4452-ACF4-06157C83A841
DOI	https://doi.org/10.5281/zenodo.4535682
persistent identifier	https://treatment.plazi.org/id/133D87A1-FFD2-2732-FEA9-BBCFFD3DFD2E
treatment provided by	Felipe
scientific name	Acratia nagyvisnyoensis? Forel, 2013
status

Treatment

( Fig. 5A, B View FIG )

Acratia nagyvisnyoensis Forel in Forel et al., 2013: 204, fig. 10K-O.

MATERIAL EXAMINED. — Four complete carapaces and two broken carapaces.

DIMENSIONS. — L= 629-682 µm; H= 308-373 µm.

OCCURRENCES. — Bükk Mountains , Hungary, Late Permian ( Forel et al. 2013) ;? Chaotian section, Sichuan Province, China. Wujiaping Formation , basal Wuchiapingian, Late Permian (this study, samples: 11 CHAO81 , 11 CHAO84 , see Table 1) .

REMARKS Our specimens are very similar to A. nagyvisnyoensis Forel, 2013 from the Late Permian of Hungary ( Forel et al. 2013) but differ in having longer carapaces and a less arched DB.