WoRMS taxon details

Chilostomellina Cushman, 1926

722315  (urn:lsid:marinespecies.org:taxname:722315)

accepted
Genus
Chilostomellina fimbriata Cushman, 1926 (type by original designation)
marine
Cushman, J. A. (1926). The Genus Chilostomella and Related Genera. <em>Contributions from the Cushman laboratory for foraminiferal research.</em> 1(4): 73-80., available online at https://cushmanfoundation.allenpress.com/Portals/_default/files/pubarchive/cclfr/1cclfr4.pdf
page(s): p. 78 [details]  Available for editors  PDF available [request] 
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2023). World Foraminifera Database. Chilostomellina Cushman, 1926. Accessed through: World Register of Marine Species at: https://www.marinespecies.org/aphia.php?p=taxdetails&id=722315 on 2023-10-01
Date
action
by
2013-03-08 13:53:47Z
created
2014-05-15 08:44:24Z
changed
2019-03-11 11:54:33Z
changed

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original description Cushman, J. A. (1926). The Genus Chilostomella and Related Genera. <em>Contributions from the Cushman laboratory for foraminiferal research.</em> 1(4): 73-80., available online at https://cushmanfoundation.allenpress.com/Portals/_default/files/pubarchive/cclfr/1cclfr4.pdf
page(s): p. 78 [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 inflated to subglobular, planispiral, and involute, chambers enlarging rapidly, strongly overlapping, basal margin of apertural face and sides of final chamber digitate, sutures curved, flush to slightly depressed, periphery broadly rounded; wall calcareous, optically granular, surface smooth, other than the fingerlike projections of the chamber margin; aperture a low interiomarginal arch, small supplementary openings present between the fingerlike projections along the base of the final chamber. Holocene; Pacific, at 2,560 m; Bering Sea. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]