Foraminifera taxon details

Vanderbeekia Brönnimann & Wirz, 1962 †

722358  (urn:lsid:marinespecies.org:taxname:722358)

accepted
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marine, brackish, fresh, terrestrial
fossil only
feminine
Brönnimann, P.; Wirz, A. (1962). New Maastrichtian rotaliids from Iran and Libya. <em>Eclogae Geologicae Helvetiae.</em> 55: 519-528., available online at http://Link: http://doi.org/10.5169/seals-162935
page(s): p. 526 [details]  Available for editors  PDF available [request] 
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2024). World Foraminifera Database. Vanderbeekia Brönnimann & Wirz, 1962 †. Accessed at: https://www.marinespecies.org/Foraminifera/aphia.php?p=taxdetails&id=722358 on 2024-05-16
Date
action
by
2013-03-08 13:53:47Z
created
2018-01-10 13:52:53Z
changed
2020-01-19 17:09:06Z
changed

original description Brönnimann, P.; Wirz, A. (1962). New Maastrichtian rotaliids from Iran and Libya. <em>Eclogae Geologicae Helvetiae.</em> 55: 519-528., available online at http://Link: http://doi.org/10.5169/seals-162935
page(s): p. 526 [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] 

additional source Rahaghi, A. (1992). Remarks on the genera Sirtina, Vanderbeekia, Iranites and Neumannites (Foraminifera) from the Upper Cretaceous of Iran with suggestion of a new subfamily Neumannitinae. <em>Revista Española de Micropaleontologia 24, 2, 119-129.</em>  [details]  Available for editors  PDF available [request] 
From editor or global species database
Diagnosis Test rotaloid and trochospiral as in Sirtina, diameter of holotype 1.27 mm, on the ventral side spiral chambers surround an umbilical mass of tightly packed pillars with intercalated vertical canals, dorsal side has many layers of lateral chambers inserted between the pillars, both lateral chambers and pillars of the dorsal side being separated from the spiral chambers and umbilical mass of the ventral side by a single layer of small thick-walled equatorial chambers whose plane of growth forms a broad inverted cone. U. Cretaceous (L. Maastrichtian); Iran. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]
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