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...
Diagnosis Test planispiral and involute, or rarely enrolled biserial; few chambers per whorl; microgranular wall with tectum,...
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]
Diagnosis Test planispiral and involute, or rarely enrolled biserial; few chambers per whorl; microgranular wall with tectum,...
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]
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2025). World Foraminifera Database. Bradyinidae Reitlinger, 1950 nom. transl. Reitlinger, 1958 †. Accessed at: https://marinespecies.org/foraminifera/aphia.php?p=taxdetails&id=720912 on 2026-01-20
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]
