Foraminifera taxon details
Globivalvulinidae Reitlinger, 1950 †
1052754 (urn:lsid:marinespecies.org:taxname:1052754)
accepted
Family
- Subfamily Dagmaritinae Bozorgnia, 1973 †
- Genus Bidagmarita Gaillot & Vachard in Gaillot et al., 2009 †
- Genus Crescentia Ciarapica, Cirilli, Martini & Zaninetti, 1986 †
- Genus Dagmarita Reitlinger, 1965 †
- Genus Danielita Altiner & Özkan-Altiner, 2010 †
- Genus Labiodagmarita Gaillot & Vachard, 2007 †
- Genus Louisettita Altiner & Brönnimann, 1980 †
- Genus Paynita Altiner, Özkan-Altıner, Atasoy & Şahın, 2021 †
- Genus Sengoerina Altiner, 1999 †
- Subfamily Globivalvulininae Reitlinger, 1950 †
- Genus Admiranda Marfenkova, 1991 †
- Genus Biseriella Mamet in Armstrong & Mamet, 1974 †
- Genus Charliella Altiner & Özkan-Altiner, 2001 †
- Genus Dzhamansorina Marfenkova, 1991 †
- Genus Globigaetania Gennari & Rettori, 2019 †
- Genus Globivalvulina Schubert, 1921 †
- Genus Labioglobivalvulina Gaillot & Vachard, 2007 †
- Genus Lateenoglobivalvulina Filimonova, 2016 †
- Genus Parabiseriella Cózar & Somerville, 2012 †
- Genus Retroseptellina Gaillot & Vachard, 2007 †
- Genus Tenebrosella Villa & Sánchez de Posada, 1986 †
- Genus Verispira Palmieri, 1988 †
- Subfamily Paradagmaritinae Gaillot & Vachard, 2007 †
- Subfamily Paraglobivalvulininae Gaillot & Vachard, 2007 †
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 [request]
Gaillot, J.; Vachard, D. (2007). The Khuff Formation (Middle East) and time-equivalents in Turkey and South China: biostratigraphy from Capitanian to Changhsingian times (Permian), new foraminiferal taxa, and palaeogeographical implications. <em>Coloquios de Paleontologia.</em> 57: 37-223., available online at https://hal.archives-ouvertes.fr/hal-00310245
page(s): p. 49; note: Nomen translatum [details] Available for editors [request]
Gaillot, J.; Vachard, D. (2007). The Khuff Formation (Middle East) and time-equivalents in Turkey and South China: biostratigraphy from Capitanian to Changhsingian times (Permian), new foraminiferal taxa, and palaeogeographical implications. <em>Coloquios de Paleontologia.</em> 57: 37-223., available online at https://hal.archives-ouvertes.fr/hal-00310245
page(s): p. 49; note: Nomen translatum [details] Available for editors [request]
Description Test biserial, entirely planispiral or initially trochospiral, or entirely uncoiled, or trochospiral, becoming planispiral....
Description Test biserial, entirely planispiral or initially trochospiral, or entirely uncoiled, or trochospiral, becoming planispiral. Wall thin, dark, microgranular, eventually granular with inclusions of clearer carbonate particles, or differentiated into two, three or four layers; nevertheless, this differentiation does not affect all the chambers and/or corresponds to fossil diagenetic features, and is not admitted here as a generic criterion. Endoskeletal folds or partitions lead to the formation of chamberlets. Oral tongue often present, occasionally passing to a siphon. Aperture terminal simple.
Occurrence: Mississippian (latest Tournaisian)–Permian (latest Changhsingian). ?Earliest Triassic. The Pennsylvanian genera are rather cosmopolitan, whereas the Permian ones are restricted to the Tethys and Panthalassa.
(Vachard in Krainer et al. (2019), p. 58). [details]
Occurrence: Mississippian (latest Tournaisian)–Permian (latest Changhsingian). ?Earliest Triassic. The Pennsylvanian genera are rather cosmopolitan, whereas the Permian ones are restricted to the Tethys and Panthalassa.
(Vachard in Krainer et al. (2019), p. 58). [details]
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2021). World Foraminifera Database. Globivalvulinidae Reitlinger, 1950 †. Accessed at: http://marinespecies.org/foraminifera/aphia.php?p=taxdetails&id=1052754 on 2024-09-18
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]
original description Gaillot, J.; Vachard, D. (2007). The Khuff Formation (Middle East) and time-equivalents in Turkey and South China: biostratigraphy from Capitanian to Changhsingian times (Permian), new foraminiferal taxa, and palaeogeographical implications. <em>Coloquios de Paleontologia.</em> 57: 37-223., available online at https://hal.archives-ouvertes.fr/hal-00310245
page(s): p. 49; note: Nomen translatum [details] Available for editors [request]
original description Gaillot, J.; Vachard, D. (2007). The Khuff Formation (Middle East) and time-equivalents in Turkey and South China: biostratigraphy from Capitanian to Changhsingian times (Permian), new foraminiferal taxa, and palaeogeographical implications. <em>Coloquios de Paleontologia.</em> 57: 37-223., available online at https://hal.archives-ouvertes.fr/hal-00310245
page(s): p. 49; note: Nomen translatum [details] Available for editors [request]
From editor or global species database
Description Test biserial, entirely planispiral or initially trochospiral, or entirely uncoiled, or trochospiral, becoming planispiral. Wall thin, dark, microgranular, eventually granular with inclusions of clearer carbonate particles, or differentiated into two, three or four layers; nevertheless, this differentiation does not affect all the chambers and/or corresponds to fossil diagenetic features, and is not admitted here as a generic criterion. Endoskeletal folds or partitions lead to the formation of chamberlets. Oral tongue often present, occasionally passing to a siphon. Aperture terminal simple.Occurrence: Mississippian (latest Tournaisian)–Permian (latest Changhsingian). ?Earliest Triassic. The Pennsylvanian genera are rather cosmopolitan, whereas the Permian ones are restricted to the Tethys and Panthalassa.
(Vachard in Krainer et al. (2019), p. 58). [details]