Foraminifera taxon details
Cribellopsis Arnaud-Vanneau, 1980 †
739353 (urn:lsid:marinespecies.org:taxname:739353)
accepted
Genus
Orbitolinopsis neoelongata Cherchi & Schroeder, 1978 † accepted as Cribellopsis neoelongata (Cherchi & Schroeder, 1978) † (type by original designation)
- Species Cribellopsis delicatula Schlagintweit & Yazdi-Moghadam, 2020 †
- Species Cribellopsis elongata (Dieni, Massari & Moullade, 1963) †
- Species Cribellopsis kharaibensis Schlagintweit, Steuber & Alteneiji, 2024 †
- Species Cribellopsis moulladei (Saint-Marc, 1974) †
- Species Cribellopsis neoelongata (Cherchi & Schroeder, 1978) †
- Species Cribellopsis pfenderae (Canérot & Moullade, 1971) †
- Species Cribellopsis schroederi Arnaud-Vanneau, 1980 †
- Species Cribellopsis sudari Schlagintweit & Bucur, 2021 †
- Species Cribellopsis thieuloyi Arnaud-Vanneau, 1980 †
- Species Cribellopsis arnaudae Chiocchini, 1989 † accepted as Cribellopsis moulladei (Saint-Marc, 1974) † (Subjective junior synonym Opinion of Schlagintweit (2020))
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. 593, 667 [details] Available for editors
[request]
page(s): p. 593, 667 [details] Available for editors
[request]
Diagnosis Test conical to subcylindrical, with simple embryonal apparatus followed by evolute subapical trochospire, later uncoiled...
Diagnosis Test conical to subcylindrical, with simple embryonal apparatus followed by evolute subapical trochospire, later uncoiled with uniserial discoidal chambers, with marginal zone subdivided into rectangular chamberlets by alternating longer and shorter radial beams, the longer beams continuing into the central zone and secondary ones limited to the marginal zone, beams of successive chambers in vertical alignment; apertural face flat to convex, with smooth marginal zone and central zone that may have approximately radially arranged grooves, apertural pores with small collars, forming a circlet at the junction of the marginal and central zones, as well as scattered over the surface in the central zone, either obliquely piercing the radial plates or passing vertically through the septa between the radial plates. L. Cretaceous (U. Hauterivian to L. Bedoulian); France; Switzerland; Italy: Sardinia. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2025). World Foraminifera Database. Cribellopsis Arnaud-Vanneau, 1980 †. Accessed at: https://www.marinespecies.org/Foraminifera/aphia.php?p=taxdetails&id=739353 on 2025-12-19
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. 593, 667 [details] Available for editors [request]
page(s): p. 593, 667 [details] Available for editors
[request]From editor or global species database
Diagnosis Test conical to subcylindrical, with simple embryonal apparatus followed by evolute subapical trochospire, later uncoiled with uniserial discoidal chambers, with marginal zone subdivided into rectangular chamberlets by alternating longer and shorter radial beams, the longer beams continuing into the central zone and secondary ones limited to the marginal zone, beams of successive chambers in vertical alignment; apertural face flat to convex, with smooth marginal zone and central zone that may have approximately radially arranged grooves, apertural pores with small collars, forming a circlet at the junction of the marginal and central zones, as well as scattered over the surface in the central zone, either obliquely piercing the radial plates or passing vertically through the septa between the radial plates. L. Cretaceous (U. Hauterivian to L. Bedoulian); France; Switzerland; Italy: Sardinia. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]
From editor or global species database
Image from typetaxon