Foraminifera taxon details
Vercorsella Arnaud-Vanneau, 1980 †
739159 (urn:lsid:marinespecies.org:taxname:739159)
accepted
Genus
Vercorsella arenata Arnaud-Vanneau, 1980 † (type by original designation)
- Species Vercorsella arenata Arnaud-Vanneau, 1980 †
- Species Vercorsella camposaurii (Sartoni & Crescenti, 1962) †
- Species Vercorsella halleinensis Schlagintweit & Gawlick, 2005 †
- Species Vercorsella laurenti (Sartoni & Crescenti, 1962) †
- Species Vercorsella scarsellai (De Castro, 1963) †
- Species Vercorsella tenuis (Velić & Gušić, 1973) †
- Species Vercorsella wintereri Arnaud-Vanneau & Sliter, 1995 †
marine, brackish, fresh, terrestrial
fossil only
feminine
Arnaud-Vanneau, A. (1980). Micropaléontologie, paléoécologie, et sédimentologie d'une plate-forme carbonatée de la marge passive de la Téthys : l'Urgonien du Vercors septentrional et de la Chartreuse (Alpes occidentales). <em>Géologie Alpine Mem.</em> 11(1-3): 1-874., available online at https://tel.archives-ouvertes.fr/tel-00662977/document
page(s): p. 518 [details] Available for editors
[request]
page(s): p. 518 [details] Available for editors
[request]
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2024). World Foraminifera Database. Vercorsella Arnaud-Vanneau, 1980 †. Accessed at: https://www.marinespecies.org/Foraminifera/aphia.php?p=taxdetails&id=739159 on 2024-04-19
Date
action
by
original description
Arnaud-Vanneau, A. (1980). Micropaléontologie, paléoécologie, et sédimentologie d'une plate-forme carbonatée de la marge passive de la Téthys : l'Urgonien du Vercors septentrional et de la Chartreuse (Alpes occidentales). <em>Géologie Alpine Mem.</em> 11(1-3): 1-874., available online at https://tel.archives-ouvertes.fr/tel-00662977/document
page(s): p. 518 [details] Available for editors [request]
page(s): p. 518 [details] Available for editors
[request] 
Present Inaccurate Introduced: alien Containing type locality
From editor or global species database
Diagnosis Test elongate and flaring, short early trochospiral stage followed by a more prominent biserial stage, laterally compressed parallel to the plane of biseriality, chamber interior subdivided by radial vertical partitions that increase in number in successive chambers, less well-developed horizontal partitions present in later chambers; wall agglutinated, with quartz and carbonate grains held in a microgranular calcareous cement, surface commonly rough; aperture a simple interiomarginal slit that extends nearly the entire breadth of the final chamber. L. Cretaceous (U. Hauterivian to Bedoulian); France; Italy; Yugoslavia. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]