Foraminifera taxon details

Paravervilleina Vachard in Krainer, Vachard & Schaffhauser, 2019 †

1397921  (urn:lsid:marinespecies.org:taxname:1397921)

accepted
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marine, brackish, fresh, terrestrial
fossil only
feminine
Krainer, K.; Vachard, D.; Schaffhauser, M. (2019). Early Permian (Yakhtashian; Artinskian - Early Kungurian) foraminifers and microproblematica from the Carnic Alps. <em>Abhandlungen der Geologischen Bundesanstalt.</em> 73:1-247., available online at https://opac.geologie.ac.at/wwwopacx/wwwopac.ashx?command=getcontent&server=images&value=Abh_0073.pdf
page(s): p. 111 [details] Available for editors  PDF available [request]
Original description Test uniseriate subcylindrical slightly curved. Proloculus not prominent followed by a series of chambers developed with...  
Original description Test uniseriate subcylindrical slightly curved. Proloculus not prominent followed by a series of chambers developed with complete septa and sutured connexions. Wall structure two-layered with a thin inner, dark microgranular, and an external, hyaline, evolved, fibrous layer. Aperture terminal, areal, simple.
Occurrence: Early–Middle–?Late Permian; Paleotethys, South China, and Primorye.
(Krainer et al. (2019)). [details]
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2025). World Foraminifera Database. Paravervilleina Vachard in Krainer, Vachard & Schaffhauser, 2019 †. Accessed at: https://www.marinespecies.org/foraminifera/aphia.php?p=taxdetails&id=1397921 on 2025-05-14
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2020-01-07 18:14:08Z
created

original description Krainer, K.; Vachard, D.; Schaffhauser, M. (2019). Early Permian (Yakhtashian; Artinskian - Early Kungurian) foraminifers and microproblematica from the Carnic Alps. <em>Abhandlungen der Geologischen Bundesanstalt.</em> 73:1-247., available online at https://opac.geologie.ac.at/wwwopacx/wwwopac.ashx?command=getcontent&server=images&value=Abh_0073.pdf
page(s): p. 111 [details] Available for editors  PDF available [request]
From editor or global species database
Original description Test uniseriate subcylindrical slightly curved. Proloculus not prominent followed by a series of chambers developed with complete septa and sutured connexions. Wall structure two-layered with a thin inner, dark microgranular, and an external, hyaline, evolved, fibrous layer. Aperture terminal, areal, simple.
Occurrence: Early–Middle–?Late Permian; Paleotethys, South China, and Primorye.
(Krainer et al. (2019)). [details]
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