Foraminifera taxon details

Charentia Neumann, 1965 †

738926  (urn:lsid:marinespecies.org:taxname:738926)

accepted
Genus
Charentia cuvillieri Neumann, 1965 † (type by original designation)
Tonasia Gorbachik, 1968 † · unaccepted (Subjective junior synonym in...)  
Subjective junior synonym in opinion of Loeblich and Tappan (1987)

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marine, brackish, fresh, terrestrial
fossil only
feminine
Neumann, M. (1965). Contribution à l'étude de quelques lituolidés du Cénomanien de l'Ile Madame (Charente-Maritime). <em>Revue de Micropaléontologie.</em> 8: 90-95.
page(s): p. 93 [details]  Available for editors  PDF available [request] 
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2024). World Foraminifera Database. Charentia Neumann, 1965 †. Accessed at: https://www.marinespecies.org/foraminifera/aphia.php?p=taxdetails&id=738926 on 2024-04-19
Date
action
by
2013-09-02 09:02:02Z
created
2017-11-11 10:41:59Z
changed

original description Neumann, M. (1965). Contribution à l'étude de quelques lituolidés du Cénomanien de l'Ile Madame (Charente-Maritime). <em>Revue de Micropaléontologie.</em> 8: 90-95.
page(s): p. 93 [details]  Available for editors  PDF available [request] 

original description  (of Tonasia Gorbachik, 1968 †) Gorbachik, T. N. (1968). Явление гомеоморфии у фораминифер [Yavlenie gomeomorfii u foraminifer - Some cases of homeomorphy in Foraminifera]. <em>Палеонтологический журнал [Paleontologicheskii Zhurnal - Palaeontological Journal].</em> 1968(1): 3-10.
page(s): p. 7 [details]  Available for editors  PDF available [request] 
From editor or global species database
Diagnosis Test free, early stage planispirally enrolled, biumbonate and lenticular to subglobular, with a tendency to uncoil in the last one or two chambers, rarely as many as four, laterally compressed and rectilinear, periphery subacute to rounded; wall finely agglutinated, solid in the early stage, later with wall pierced by cylindrical canaliculi that do not reach completely to either the inner or outer wall surface but give a pseudoalveolar or almost keriothecal structure, apertural face solid and noncanaliculate, the portion just beneath the aperture and against the previous whorl being distinctly thickened, in thin section appearing as small triangular projections from the spiral septum that superficially resemble fusulinacean chomata; aperture areal, an arch near the base of the face in the early stage, later becoming triangular, the upper angle of the triangle gradually lengthening to become a narrow slit up the apertural face, and becoming a terminal slit in the uncoiled chambers. Cretaceous (U. Barremian to Cenomanian); France; Spain; USSR: E. Crimea; Egypt; USA: Texas. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]