Foraminifera taxon details

Chubbina Robinson, 1968 †

722009  (urn:lsid:marinespecies.org:taxname:722009)

accepted
Genus
Chubbina jamaicensis Robinson, 1968 † (type by original designation)

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marine, brackish, fresh, terrestrial
fossil only
feminine
Robinson, E. (1968). Chubbina, a new Cretaceous alveolinid genus from Jamaica and Mexico. <em>Palaeontology.</em> 11: 526-534., available online at https://www.palass.org/sites/default/files/media/publications/palaeontology/volume_11/vol11_part4_pp526-534.pdf
page(s): p. 527 [details]  Available for editors  PDF available [request] 
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2024). World Foraminifera Database. Chubbina Robinson, 1968 †. Accessed at: https://www.marinespecies.org/foraminifera/aphia.php?p=taxdetails&id=722009 on 2024-05-01
Date
action
by
2013-03-08 13:53:47Z
created
2017-12-17 11:25:48Z
changed
2019-11-27 15:12:28Z
changed

original description Robinson, E. (1968). Chubbina, a new Cretaceous alveolinid genus from Jamaica and Mexico. <em>Palaeontology.</em> 11: 526-534., available online at https://www.palass.org/sites/default/files/media/publications/palaeontology/volume_11/vol11_part4_pp526-534.pdf
page(s): p. 527 [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, up to 8 mm in diameter and about 1.5 mm in thickness, globular or lenticular in early stage, later flaring and peneropline, spherical megalospheric proloculus followed by single undivided tubular chamber, microspheric early stage milioline, later with numerous whorls, at first streptospiral, later planispiral with the number of chambers per whorl increasing to about fifteen, chambers increase rapidly in height as added so that the adult test is uncoiled and flabelliform, interior subdivided by numerous primary and secondary axially aligned septula, central thickening and numerous residual pillars present in the preseptal space as in Rhapydionina; wall calcareous, porcelaneous; aperture multiple, with openings scattered uniformly over the apertural face of the final chamber, previous foramina connecting successive chamberlets. U. Cretaceous (Campanian to Maastrichtian); Jamaica; Mexico; Cuba; USA: Florida. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]