Foraminifera taxon details

Pseudobroeckinella Deloffre & Hamaoui, 1969 †

721277  (urn:lsid:marinespecies.org:taxname:721277)

accepted
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marine, brackish, fresh, terrestrial
fossil only
feminine
Deloffre, R.; Hamaoui, M. (1969). Biostratigraphie des « Brèches de Soumoulou » et description de Pseudobroeckinella soumoulouensis n. gen., n. sp., foraminifère du Crétacé supérieur d'Aquitaine. <em>Bulletin du Centre de Recherches de Pau – SNPA.</em> 3(1): 5-31.
page(s): p. 8 [details]  Available for editors  PDF available [request] 
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2024). World Foraminifera Database. Pseudobroeckinella Deloffre & Hamaoui, 1969 †. Accessed at: https://www.marinespecies.org/foraminifera/aphia.php?p=taxdetails&id=721277 on 2024-03-28
Date
action
by
2013-03-08 13:53:47Z
created
2017-12-18 14:39:52Z
changed
2020-02-21 17:10:18Z
changed

original description Deloffre, R.; Hamaoui, M. (1969). Biostratigraphie des « Brèches de Soumoulou » et description de Pseudobroeckinella soumoulouensis n. gen., n. sp., foraminifère du Crétacé supérieur d'Aquitaine. <em>Bulletin du Centre de Recherches de Pau – SNPA.</em> 3(1): 5-31.
page(s): p. 8 [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, discoidal, bilaterally symmetrical, early stage planispirally coiled, chambers rapidly increasing in breadth but very little in height so that test becomes peneropliform, then reniform in outline, and apparently has cyclic chambers in the final stage, septa arched, chambers subdivided by three types of partitions, primary and secondary septula that are vertical to the septa, and transverse septula that parallel the septa, the primary septula being longer than the other partitions and all fusing in the vicinity of the outer walls; wall calcareous, microgranular, imperforate, probably originally porcelaneous; aperture of two rows of circular pores along the midregion of the final chamber face. U. Cretaceous (Santonian); France. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]