Foraminifera taxon details

Taberina Keijzer, 1945 †

722034  (urn:lsid:marinespecies.org:taxname:722034)

accepted
Genus
Taberina cubana Keijzer, 1945 † (type by original designation)

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marine, brackish, fresh, terrestrial
fossil only
feminine
Keijzer, F. G. (1945). Outline of the geology of the eastern part of the province of Oriente, Cuba (E of 760 WL): with notes on the geology of other parts of the island. <em>Geographische en Geologische Mededeelingen, Utrecht.</em> v. 6: p. 1-238.
page(s): p. 200 [details]   
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2024). World Foraminifera Database. Taberina Keijzer, 1945 †. Accessed at: https://www.marinespecies.org/foraminifera/aphia.php?p=taxdetails&id=722034 on 2024-09-18
Date
action
by
2013-03-08 13:53:47Z
created
2017-12-18 14:39:52Z
changed
2019-11-07 10:46:44Z
changed

original description Keijzer, F. G. (1945). Outline of the geology of the eastern part of the province of Oriente, Cuba (E of 760 WL): with notes on the geology of other parts of the island. <em>Geographische en Geologische Mededeelingen, Utrecht.</em> v. 6: p. 1-238.
page(s): p. 200 [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] 

redescription Vicedo, V., Berlanga J.A., Serra-Kiel, J., Caus, E. (2013). Architecture and age of the foraminiferal genus taberina keijzer, 1945. <em>The Journal of Foraminiferal Research 43(2):170-181.</em> , available online at https://www.researchgate.net/publication/275838533_Architecture_and_age_of_the_foraminiferal_genus_taberina_keijzer_1945 [details]   
From editor or global species database
Diagnosis Test elongate, up to 1.3 mm in length, globular proloculus followed by two simple low chambers, and then by more numerous chambers in a large early planispiral stage, up to twenty chambers in the final whorl, coiled stage followed by a short final uncoiled stage, all chambers after the first two are subdivided by short interseptal radial partitions that project inward from the outer wall, interseptal pillars occupy the central area of the chambers; wall calcareous, imperforate; aperture cribrate, in the face of the coiled chambers, terminal in the uncoiled ones. L. Paleocene (Danian or Montian); Cuba. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]
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