Foraminifera taxon details

Colomia Cushman & Bermúdez, 1948 †

721317  (urn:lsid:marinespecies.org:taxname:721317)

accepted
Genus
Colomia cretacea Cushman & Bermúdez, 1948 † (type by original designation)

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marine, brackish, fresh, terrestrial
fossil only
feminine
Cushman, J.A.; Bermúdez, P.J. 1948. Colomia, a new genus from the Upper Cretaceous of Cuba. Contr. Cushman Lab. Foram. Res. 24: 12, 13. , available online at https://cushmanfoundation.allenpress.com/Portals/_default/files/pubarchive/cclfr/24cclfr1.pdf
page(s): p. 12 [details]  Available for editors  PDF available [request] 
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2021). World Foraminifera Database. Colomia Cushman & Bermúdez, 1948 †. Accessed at: http://www.marinespecies.org/Foraminifera/aphia.php?p=taxdetails&id=721317 on 2024-05-23
Date
action
by
2013-03-08 13:53:47Z
created
2017-12-23 15:19:12Z
changed
2020-01-21 16:29:21Z
changed

original description Cushman, J.A.; Bermúdez, P.J. 1948. Colomia, a new genus from the Upper Cretaceous of Cuba. Contr. Cushman Lab. Foram. Res. 24: 12, 13. , available online at https://cushmanfoundation.allenpress.com/Portals/_default/files/pubarchive/cclfr/24cclfr1.pdf
page(s): p. 12 [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 elongate, conical in the early stage or throughout, or later stage may have nearly parallel sides, microspheric generation with a whorl of three chambers, then biserial, and finally uniserial for the major part of the test, megalospheric test with much reduced early stage of a few biserial chambers, and then uniserial, commonly with numerous low dishlike chambers, but in some species the later chambers are higher and slightly inflated, sutures in the uniserial stage straight and horizontal and may be incised, flush, or elevated; wall calcareous, aragonitic, hyaline, relatively thick, finely perforate, surface smooth to finely hispid; aperture in the early stage as in Conorboides, becoming an arcuate slit in the uniserial chambers, those of successive chambers changing about 65¡ in orientation, reflecting the earlier trochospiral coiling, internally a scroll-shaped tooth plate extends from one margin of the slitlike aperture across the chamber lumen to the preceding septum. U. Cretaceous (Turonian to Maastrichtian); Germany; Austria; USA: California; Cuba; Australia: Victoria. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]
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