Foraminifera name details

Corrigotubella Ganelina, 1966 †

721722  (urn:lsid:marinespecies.org:taxname:721722)

 unaccepted (Subjective junior synonym Opinion of Hance et al. (2011))
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marine, brackish, fresh, terrestrial
fossil only
feminine
Ganelina, R. A. (1966). Фораминиферы турнейских и нижневизейских отложений некоторых районов Камско-Кинельской впадины-Foraminifera of the Tournaisian and Lower Visean deposits of some areas of the Kamsko-Kinel Basin. <em>Микрофауна CCCR, Microfauna of the USSR, Proceedings of the Oil Research Geological Institute (ВНИГРИ-VNIGRI).</em> Col. 14, 250: 64-175., available online at https://books.google.pt/books?id=vzbXlMVkgIEC&dq
page(s): p. 98 [details]  Available for editors  PDF available [request] 
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2021). World Foraminifera Database. Corrigotubella Ganelina, 1966 †. Accessed at: http://marinespecies.org/foraminifera/aphia.php?p=taxdetails&id=721722 on 2024-04-24
Date
action
by
2013-03-08 13:53:47Z
created
2017-05-08 09:24:30Z
changed
2017-05-19 15:29:36Z
changed
2018-01-29 10:22:33Z
changed

original description Ganelina, R. A. (1966). Фораминиферы турнейских и нижневизейских отложений некоторых районов Камско-Кинельской впадины-Foraminifera of the Tournaisian and Lower Visean deposits of some areas of the Kamsko-Kinel Basin. <em>Микрофауна CCCR, Microfauna of the USSR, Proceedings of the Oil Research Geological Institute (ВНИГРИ-VNIGRI).</em> Col. 14, 250: 64-175., available online at https://books.google.pt/books?id=vzbXlMVkgIEC&dq
page(s): p. 98 [details]  Available for editors  PDF available [request] 

basis of record Loeblich, A. R.; Tappan, H. (1987). Foraminiferal Genera and their Classification. Van Nostrand Reinhold Company, New York. 970pp., available online at https://books.google.pt/books?id=n_BqCQAAQBAJ [details]  Available for editors  PDF available [request] 
From editor or global species database
Diagnosis Test large, robust, up to 1.08 mm in length, early stage streptospiral, later planispiral, about five to six chambers in the last whorl, finally with a few short, broad, uncoiled, and rectilinear chambers, septa in the enrolled stage short, continuing the curvature of the outer wall and equal to it in thickness, septa of the rectilinear portion horizontal and thicker than the outer wall; wall calcareous, microgranular, with some inclusions; aperture simple and basal in the coiled stage, terminal in the rectilinear portion, with a double opening in at least the final chamber. L. Carboniferous (U. Toumaisian to L. Visean); USSR: Urals. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]