Foraminifera taxon details

Crespinina Wade, 1955 †

722411  (urn:lsid:marinespecies.org:taxname:722411)

accepted
Genus
Crespinina kingscotensis Wade, 1955 † (type by original designation)

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marine, brackish, fresh, terrestrial
fossil only
feminine
Wade, M. (1955), A new genus of the Chapmanininae from southem Australia, Contributions from the Cushman Foundation for Foraminiferal Research 6:45-49. , available online at https://cushmanfoundation.allenpress.com/portals/_default/files/pubarchive/CCFFR/06ccffr1.pdf
page(s): p. 45 [details]  Available for editors  PDF available [request] 
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2021). World Foraminifera Database. Crespinina Wade, 1955 †. Accessed at: http://www.marinespecies.org/foraminifera/aphia.php?p=taxdetails&id=722411 on 2024-08-30
Date
action
by
2013-03-08 13:53:47Z
created
2018-01-07 21:36:51Z
changed
2019-12-04 15:56:56Z
changed

original description Wade, M. (1955), A new genus of the Chapmanininae from southem Australia, Contributions from the Cushman Foundation for Foraminiferal Research 6:45-49. , available online at https://cushmanfoundation.allenpress.com/portals/_default/files/pubarchive/CCFFR/06ccffr1.pdf
page(s): p. 45 [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 Low conical test, bilocular megalospheric embryo of spherical protoconch and reniform deuteroconch, followed by a few annular and undivided chambers and later by broadly saucer-shaped rectilinear chambers, microspheric form with early planispiral coil followed by embracing and finally annular chambers, annular and saucer-shaped chambers divided by the imperforate radial partitions formed by infolding of the outer wall, interior with hollow pillars extending from one septum to the next and similarly formed by infolding of the basal wall, neither partitions nor pillars aligned in successive chambers; wall calcareous, lamellar, convex surface and pillars perforate, ventral surface of the test partially imperforate and radial partitions imperforate; aperture consists of the large pores that open into the hollow pillars. U. Eocene to L. Oligocene; South Australia. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]
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