Foraminifera taxon details
Bradyinidae Reitlinger, 1950 nom. transl. Reitlinger, 1958 †
720912 (urn:lsid:marinespecies.org:taxname:720912)
accepted
Family
marine, fresh, terrestrial
fossil only
Reitlinger, E. A. (1950). Фораминиферы среднекаменноугольных отложений центральной части Русской платформы (исключая сем. Fusulinidае) - Foraminifera of the Middle Carboniferous deposits of the central part of the Russian Platform (exclusive of family Fusulinidae). <em>Академия наук СССР Труды ИГН-Academy of Sciences USSR Proceedings Insitute of Geological Sciences.</em> 126: 1-128., available online at http://www.ginras.ru/library/pdf/ign126_1950_reitlinger_carboniferous_forams.pdf [details] Available for editors 
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Description Bradyinoidea nautiloid, planispirally coiled and involute. Whorls and chambers are not numerous. Septa are short with...
Description Bradyinoidea nautiloid, planispirally coiled and involute. Whorls and chambers are not numerous. Septa are short with additional pre- and post-septal lamellae. Alveolar wall overlain by a continuous tectum. Simple aperture becoming cribrate at the last chamber. Additional sutural pores present.
Occurrence: Late Asbian (middle part of MFZ14; Devuyst et al., 2005; Poty et al., 2006)-late Early Permian (Middle/Late Permian Bradyina must be assigned to Postendothyra Lin, 1984); Palaeotethyan in the late Mississippian; cosmopolite since the early Pennsylvanian (e.g., Mamet, 1970, p. 32).
(Hance et al. (2011)). [details]
Occurrence: Late Asbian (middle part of MFZ14; Devuyst et al., 2005; Poty et al., 2006)-late Early Permian (Middle/Late Permian Bradyina must be assigned to Postendothyra Lin, 1984); Palaeotethyan in the late Mississippian; cosmopolite since the early Pennsylvanian (e.g., Mamet, 1970, p. 32).
(Hance et al. (2011)). [details]
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2024). World Foraminifera Database. Bradyinidae Reitlinger, 1950 nom. transl. Reitlinger, 1958 †. Accessed at: https://marinespecies.org/foraminifera/aphia.php?p=taxdetails&id=720912 on 2024-04-16
Date
action
by
original description
Reitlinger, E. A. (1950). Фораминиферы среднекаменноугольных отложений центральной части Русской платформы (исключая сем. Fusulinidае) - Foraminifera of the Middle Carboniferous deposits of the central part of the Russian Platform (exclusive of family Fusulinidae). <em>Академия наук СССР Труды ИГН-Academy of Sciences USSR Proceedings Insitute of Geological Sciences.</em> 126: 1-128., available online at http://www.ginras.ru/library/pdf/ign126_1950_reitlinger_carboniferous_forams.pdf [details] Available for editors [request]
basis of record Loeblich, A. R.; Tappan, H. (1987). Foraminiferal Genera and their Classification. Van Nostrand Reinhold Company, New York. 970pp., available online at https://books.google.pt/books?id=n_BqCQAAQBAJ [details] Available for editors [request]
[request] basis of record Loeblich, A. R.; Tappan, H. (1987). Foraminiferal Genera and their Classification. Van Nostrand Reinhold Company, New York. 970pp., available online at https://books.google.pt/books?id=n_BqCQAAQBAJ [details] Available for editors
[request] From editor or global species database
Description Bradyinoidea nautiloid, planispirally coiled and involute. Whorls and chambers are not numerous. Septa are short with additional pre- and post-septal lamellae. Alveolar wall overlain by a continuous tectum. Simple aperture becoming cribrate at the last chamber. Additional sutural pores present.Occurrence: Late Asbian (middle part of MFZ14; Devuyst et al., 2005; Poty et al., 2006)-late Early Permian (Middle/Late Permian Bradyina must be assigned to Postendothyra Lin, 1984); Palaeotethyan in the late Mississippian; cosmopolite since the early Pennsylvanian (e.g., Mamet, 1970, p. 32).
(Hance et al. (2011)). [details]
Diagnosis Test planispiral and involute, or rarely enrolled biserial; few chambers per whorl; microgranular wall with tectum, alveolar with tectum, or microgranular and finely perforate; septa with septal lamellae, no basal supplementary deposits; aperture simple in early stage, cribrate in last few chambers of adult, may have sutural supplementary openings. L. Carboniferous (Visean) to L. Permian (Sakmarian). (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]