Acratia nagyvisnyoensis? Forel, 2013
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 |
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Acratia nagyvisnyoensis? Forel, 2013
( Fig. 5A, B View FIG )
Acratia nagyvisnyoensis Forel in Forel et al., 2013: 204 View Cited Treatment , 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.
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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Acratia nagyvisnyoensis? Forel, 2013
Zazzali, Sindbad, Crasquin, Sylvie, Deconinck, Jean-François & Feng, Qinglai 2015 |
Acratia nagyvisnyoensis Forel
FOREL M. B. & CRASQUIN S. & HIPS K. & KERSHAW S. & COLLIN P. - Y. & HAAS J. 2013: 204 |