Foraminifera taxon details

Gublerina Kikoïne, 1948 †

722439  (urn:lsid:marinespecies.org:taxname:722439)

accepted
Genus
Gublerina cuvillieri Kikoïne, 1948 † (type by original designation)

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marine, brackish, fresh, terrestrial
fossil only
feminine
Kikoïne, J. (1948). Les Heterohelicidae du Crétacé supérieur pyrénéen. <em>Bulletin de la Société Géologique de France.</em> ser. 5, 18(1-3): 15-35.
page(s): p. 26 [details] 
Diagnosis Test compressed, flabelliform, early stage planispiral, later biserial and increasing rapidly in breadth, the two series of...  
Diagnosis Test compressed, flabelliform, early stage planispiral, later biserial and increasing rapidly in breadth, the two series of chambers diverging to leave a broad nonseptate central area that later is partially occupied by chamber proliferation, sutures depressed; wall calcareous, finely perforate, ornamented with longitudinal costae and nodes, most prominently in the early stage; aperture an arch at the base of the final chamber. U. Cretaceous (Santonian to Maastrichtian); cosmopolitan. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2025). World Foraminifera Database. Gublerina Kikoïne, 1948 †. Accessed at: https://www.marinespecies.org/foraminifera/aphia.php?p=taxdetails&id=722439 on 2025-05-11
Date
action
by
2013-03-08 13:53:47Z
created
2017-09-07 10:06:04Z
changed
2024-03-07 10:40:37Z
changed
2024-03-15 09:37:40Z
changed

original description Kikoïne, J. (1948). Les Heterohelicidae du Crétacé supérieur pyrénéen. <em>Bulletin de la Société Géologique de France.</em> ser. 5, 18(1-3): 15-35.
page(s): p. 26 [details] 

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 compressed, flabelliform, early stage planispiral, later biserial and increasing rapidly in breadth, the two series of chambers diverging to leave a broad nonseptate central area that later is partially occupied by chamber proliferation, sutures depressed; wall calcareous, finely perforate, ornamented with longitudinal costae and nodes, most prominently in the early stage; aperture an arch at the base of the final chamber. U. Cretaceous (Santonian to Maastrichtian); cosmopolitan. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]
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