Foraminifera taxon details

Conicorbitolina Schroeder, 1973 †

739375  (urn:lsid:marinespecies.org:taxname:739375)

accepted
Genus
Orbitolina (Conicorbitolina) Schroeder, 1973 † · unaccepted (Opinion of Loeblich &Tappan...)  
Opinion of Loeblich &Tappan (1987) nomen translatum

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marine, brackish, fresh, terrestrial
fossil only
feminine
(of Orbitolina (Conicorbitolina) Schroeder, 1973 †) Schroeder, R., 1973, EI Corte de Aulet (Prov. de Huesca). Evolución de las Orbitolinas en el limite del Cretácico inferior-superior, in XIII Coloquio Europeo de Micropaleontología España 1973. Madrid: Comisión Nacional de Geologia (CNG) and Empresa Nacional Aderode Investigaciones Mineras, S. A. (ENADIMSA), pp. 141-149.
page(s): p. 143 [details]   
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2024). World Foraminifera Database. Conicorbitolina Schroeder, 1973 †. Accessed at: https://marinespecies.org/foraminifera/aphia.php?p=taxdetails&id=739375 on 2024-04-19
Date
action
by
2013-09-04 09:28:16Z
created
2017-11-28 10:46:52Z
changed

original description  (of Orbitolina (Conicorbitolina) Schroeder, 1973 †) Schroeder, R., 1973, EI Corte de Aulet (Prov. de Huesca). Evolución de las Orbitolinas en el limite del Cretácico inferior-superior, in XIII Coloquio Europeo de Micropaleontología España 1973. Madrid: Comisión Nacional de Geologia (CNG) and Empresa Nacional Aderode Investigaciones Mineras, S. A. (ENADIMSA), pp. 141-149.
page(s): p. 143 [details]   

original description  (of Neorbitolina Bilotte, Moullade & Vial, 1974 †) Bilotte, M.; Moullade, M.; Vial, J. (1974). Description et signification phylogénétique d'un nouvel Orbitolinide découvert dans le Cénomanien des Corbières (France), Neorbitolina cenomana, n. gen. n. sp. <em>Archives des Sciences, Genève.</em> 27: 93-98., available online at https://www.e-periodica.ch/digbib/view?pid=ads-002%3A1974%3A27%3A%3A4#114
page(s): p. 94 [details]   
From editor or global species database
Diagnosis Test large, a low cone up to 10 mm in diameter, with pointed apex and flat to concave base, proloculus divided into protoconch and deuteroconch, the succeeding subembryonal zone already subdivided by radial plates, postembryonal chambers subdivided into a strongly differentiated outermost marginal zone with radial beams of three orders and horizontal rafters of two orders between the septa, a median radial zone occupied by the first order vertical radial beams that extend farther inward and become undulating and triangular in section, and a central reticular zone in which the radial beams are more regular in thickness rather than triangular in section, and showing a somewhat cellular structure of large cavities, commonly including quartz fragments. L. Cretaceous (Vraconnian) to U. Cretaceous (Cenomanian); France; Spain. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]