Foraminifera taxon details
Cuneolina d'Orbigny, 1839 †
585282 (urn:lsid:marinespecies.org:taxname:585282)
accepted
Genus
Cuneolina pavonia d'Orbigny, 1846 † (type by subsequent designation)
- Species Cuneolina axinoides Arnaud-Vanneau, 1980 †
- Species Cuneolina bermudezi Palmer, 1938 †
- Species Cuneolina cojimarensis Palmer, 1938 †
- Species Cuneolina compressa Schlagintweit, 1988 †
- Species Cuneolina conica d'Orbigny, 1850 †
- Species Cuneolina cylindrica Henson, 1948 †
- Species Cuneolina dominicana Bermúdez, 1949 †
- Species Cuneolina fleuriausa d'Orbigny, 1850 †
- Species Cuneolina hensoni Dalbiez, 1958 †
- Species Cuneolina immatura He, 1982 †
- Species Cuneolina ketini Inan, 1988 †
- Species Cuneolina parva Henson, 1948 †
- Species Cuneolina pavonia d'Orbigny, 1846 †
- Species Cuneolina sliteri Arnaud-Vanneau & Premoli Silva, 1995 †
- Species Cuneolina trinitensis Stead, 1951 †
- Species Cuneolina walteri Cushman & Applin, 1947 †
- Species Cuneolina angusta Cushman, 1919 accepted as Textulariella angusta (Cushman, 1919)
- Species Cuneolina camposaurii Sartoni & Crescenti, 1962 † accepted as Scythiolina camposaurii (Sartoni & Crescenti, 1962) † accepted as Vercorsella camposaurii (Sartoni & Crescenti, 1962) † (Opinion of Neagu (2000))
- Species Cuneolina elegans Rzehak, 1891 † accepted as Pseudotextularia elegans (Rzehak, 1891) †
- Species Cuneolina laurenti Sartoni & Crescenti, 1962 † accepted as Vercorsella laurenti (Sartoni & Crescenti, 1962) † (Opinion of Bucur et al. (2004))
- Species Cuneolina scarsellai De Castro, 1963 † accepted as Vercorsella scarsellai (De Castro, 1963) † (Opinion of Arnaud-Vanneau (1980))
- Species Cuneolina tenuis Velić & Gušić, 1973 † accepted as Vercorsella tenuis (Velić & Gušić, 1973) † (Opinion of Arnaud-Vanneau (1980))
marine, brackish, fresh, terrestrial
fossil only
feminine
Orbigny, A. D. d'. (1839). Foraminifères, in de la Sagra R., Histoire physique, politique et naturelle de l'ile de Cuba. <em>A. Bertrand.</em> 1-224., available online at https://books.google.pt/books?id=KpVeAAAAcAAJ&pg
page(s): p. 150 [details]
page(s): p. 150 [details]
Type locality contained in Cuban Exclusive Economic Zone
type locality contained in Cuban Exclusive Economic Zone [details]
Diagnosis Test free, compressed conical to flabelliform, early trochospire of about five chambers followed by very broad and low...
Diagnosis Test free, compressed conical to flabelliform, early trochospire of about five chambers followed by very broad and low biserially arranged chambers, commonly compressed parallel to the plane of biseriality, interior subdivided into nearly rectangular chamberlets by radial partitions arising perpendicular to the outer wall and projecting inward toward the plane of biseriality, and by horizontal partitions paralleling the septa; wall agglutinated, imperforate, with reticulate subepidermal layer; aperture a row of pores at the base of the septal face. L. Cretaceous (Valanginian) to U. Cretaceous (Coniacian); China; USA; Europe. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2024). World Foraminifera Database. Cuneolina d'Orbigny, 1839 †. Accessed at: https://www.marinespecies.org/foraminifera/aphia.php?p=taxdetails&id=585282 on 2024-12-20
Date
action
by
original description
Orbigny, A. D. d'. (1839). Foraminifères, in de la Sagra R., Histoire physique, politique et naturelle de l'ile de Cuba. <em>A. Bertrand.</em> 1-224., available online at https://books.google.pt/books?id=KpVeAAAAcAAJ&pg
page(s): p. 150 [details]
page(s): p. 150 [details]
Present Inaccurate Introduced: alien Containing type locality
From editor or global species database
Diagnosis Test free, compressed conical to flabelliform, early trochospire of about five chambers followed by very broad and low biserially arranged chambers, commonly compressed parallel to the plane of biseriality, interior subdivided into nearly rectangular chamberlets by radial partitions arising perpendicular to the outer wall and projecting inward toward the plane of biseriality, and by horizontal partitions paralleling the septa; wall agglutinated, imperforate, with reticulate subepidermal layer; aperture a row of pores at the base of the septal face. L. Cretaceous (Valanginian) to U. Cretaceous (Coniacian); China; USA; Europe. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]
