Foraminifera taxon details
Paraskinnerella Bensh in Rauzer-Chernousova et al., 1996 †
1062730 (urn:lsid:marinespecies.org:taxname:1062730)
accepted
Genus
Parafusulina leonardensis Ross, 1962 † accepted as Paraskinnerella skinneri (Dunbar, 1939) † (type by original designation)
Skinnerella (Paraskinnerella) Bensh in Rauzer-Chernousova et al., 1996 † · unaccepted (Nomen translatum Opinion of...)
Nomen translatum Opinion of Vachard et al. (2000)
marine, brackish, fresh, terrestrial
fossil only
feminine
(of Skinnerella (Paraskinnerella) Bensh in Rauzer-Chernousova et al., 1996 †) Rauzer-Chernousova, D.M., Bensh, F.R., Vdovenko, M.V., Gibshman, N.B., Leven, E.Ya., Lipina, O.A. Reitlinger, E.A., Solovieva, M.N. and Chediya, I.O. (1996). Справочник по систематике фораминифер палеозоя (эндотироиды, фузулиноиды) - Handbook on taxonomy of Paleozoic foraminifera (endotyroids, fusulinoids). <em>Nauka.</em> 1-205., available online at https://books.google.com/books?id=z9FGBQAAQBAJ
page(s): p. 145 [details] Available for editors
[request]
page(s): p. 145 [details] Available for editors
[request]
Description Description: Test elongate fusiform to subcylindrical, with buntly pointed poles, and convex to flattened lateral slopes....
Description Description: Test elongate fusiform to subcylindrical, with buntly pointed poles, and convex to flattened lateral slopes. No juvenarium individualized, even if the early whorls are more fusiform and more closely coiled. Proloculus small to moderate in size. Septa strongly folded with numerous loops, irregular in size and shape. Tunnel poorly defined or absent; no chomata. Axial filling especially developed in the initial whorls, poorly represented or absent in the last whorls. Cuniculi are present in the last whorls.
Occurrence: Sarginian–Irginskian of the southern Urals, northern Timan, Spitsbergen, Croatia, Japan, Italy, Carnic Alps, Darvaz and China (compilation in Kahler, 1989). Leonardian of the USA (Bensh, 1987).
(Vachard in Krainer et al. (2019)). [details]
Occurrence: Sarginian–Irginskian of the southern Urals, northern Timan, Spitsbergen, Croatia, Japan, Italy, Carnic Alps, Darvaz and China (compilation in Kahler, 1989). Leonardian of the USA (Bensh, 1987).
(Vachard in Krainer et al. (2019)). [details]
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2025). World Foraminifera Database. Paraskinnerella Bensh in Rauzer-Chernousova et al., 1996 †. Accessed at: https://www.marinespecies.org/foraminifera/aphia.php?p=taxdetails&id=1062730 on 2026-02-23
Date
action
by
original description
(of Skinnerella (Paraskinnerella) Bensh in Rauzer-Chernousova et al., 1996 †) Rauzer-Chernousova, D.M., Bensh, F.R., Vdovenko, M.V., Gibshman, N.B., Leven, E.Ya., Lipina, O.A. Reitlinger, E.A., Solovieva, M.N. and Chediya, I.O. (1996). Справочник по систематике фораминифер палеозоя (эндотироиды, фузулиноиды) - Handbook on taxonomy of Paleozoic foraminifera (endotyroids, fusulinoids). <em>Nauka.</em> 1-205., available online at https://books.google.com/books?id=z9FGBQAAQBAJ
page(s): p. 145 [details] Available for editors [request]
new combination reference Vachard, D.; Flores de Dios, A.; Buitrón, B. E.; Grajales, M. (2000). Biostratigraphie par fusulines des calcaires carbonifères et permiens de San Salvador Patlanoaya (Puebla, Mexique). <em>Geobios.</em> 33(1): 5-33., available online at http://www.academia.edu/17117234
page(s): p. 25 [details] Available for editors [request]
page(s): p. 145 [details] Available for editors
[request]new combination reference Vachard, D.; Flores de Dios, A.; Buitrón, B. E.; Grajales, M. (2000). Biostratigraphie par fusulines des calcaires carbonifères et permiens de San Salvador Patlanoaya (Puebla, Mexique). <em>Geobios.</em> 33(1): 5-33., available online at http://www.academia.edu/17117234
page(s): p. 25 [details] Available for editors
[request]From editor or global species database
Description Description: Test elongate fusiform to subcylindrical, with buntly pointed poles, and convex to flattened lateral slopes. No juvenarium individualized, even if the early whorls are more fusiform and more closely coiled. Proloculus small to moderate in size. Septa strongly folded with numerous loops, irregular in size and shape. Tunnel poorly defined or absent; no chomata. Axial filling especially developed in the initial whorls, poorly represented or absent in the last whorls. Cuniculi are present in the last whorls.Occurrence: Sarginian–Irginskian of the southern Urals, northern Timan, Spitsbergen, Croatia, Japan, Italy, Carnic Alps, Darvaz and China (compilation in Kahler, 1989). Leonardian of the USA (Bensh, 1987).
(Vachard in Krainer et al. (2019)). [details]
From editor or global species database
Image from typetaxon