Foraminifera taxon details
Eotextularia Mamet, 1970 †
721677 (urn:lsid:marinespecies.org:taxname:721677)
accepted
Genus
Palaeotextularia diversa Chernysheva, 1948 † accepted as Eotextularia diversa (Chernysheva, 1948) † (type by original designation)
marine, brackish, fresh, terrestrial
fossil only
feminine
Mamet, B., Mikhailoff, N., and Mortelmans G. (1970). La stratigraphie du Tournaisien et du Viséen inférieur de Landelies. Comparaison avec les coupes du Tournaisis et du bord nord du synclinal de Namur. <em>Mémoires de la Société belge de Géologie, de Paléontologie et d'Hydrologie.</em> série 8, 9: 1–81.
page(s): p. 21 [details] Available for editors
[request]
page(s): p. 21 [details] Available for editors
[request]
Description Diagnosis: Test initially shortly coiled, then biseriate. Chambers mstinioid in the coiled part. Wall brownish, with...
Diagnosis Proloculus followed by a small enrolled stage of one or two irregularly coiled whorls of teardroplike chambers, later...
Description Diagnosis: Test initially shortly coiled, then biseriate. Chambers mstinioid in the coiled part. Wall brownish, with agglutinated clear calcareous particles. Aperture terminal simple.
Occurrence: Late Tournaisian-middle Visean (MFZ6-MFZ11 fide Devuyst, 2006, text-fig. 1.6, p. 16). Palaeotethys, Urals and Perigondwana (Iran, Devuyst, 2006; Afghanistan, Vachard, 1980). Rare in Siberia, Asia and northern America.
(Vachard and Hance in Hance et al. (2011)). [details]
Occurrence: Late Tournaisian-middle Visean (MFZ6-MFZ11 fide Devuyst, 2006, text-fig. 1.6, p. 16). Palaeotethys, Urals and Perigondwana (Iran, Devuyst, 2006; Afghanistan, Vachard, 1980). Rare in Siberia, Asia and northern America.
(Vachard and Hance in Hance et al. (2011)). [details]
Diagnosis Proloculus followed by a small enrolled stage of one or two irregularly coiled whorls of teardroplike chambers, later...
Diagnosis Proloculus followed by a small enrolled stage of one or two irregularly coiled whorls of teardroplike chambers, later uncoiled with a few pair of biserial chambers; wall thick and coarsely granular with numerous calcite inclusions and may have a thin dark microgranular inner layer; aperture simple, a basal slit. L. Carboniferous (U. Tournaisian to M. Visean); USSR; Belgium; Denmark. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2025). World Foraminifera Database. Eotextularia Mamet, 1970 †. Accessed at: https://www.marinespecies.org/foraminifera/aphia.php?p=taxdetails&id=721677 on 2026-01-11
Date
action
by
original description
Mamet, B., Mikhailoff, N., and Mortelmans G. (1970). La stratigraphie du Tournaisien et du Viséen inférieur de Landelies. Comparaison avec les coupes du Tournaisis et du bord nord du synclinal de Namur. <em>Mémoires de la Société belge de Géologie, de Paléontologie et d'Hydrologie.</em> série 8, 9: 1–81.
page(s): p. 21 [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]
page(s): p. 21 [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]From editor or global species database
Description Diagnosis: Test initially shortly coiled, then biseriate. Chambers mstinioid in the coiled part. Wall brownish, with agglutinated clear calcareous particles. Aperture terminal simple.Occurrence: Late Tournaisian-middle Visean (MFZ6-MFZ11 fide Devuyst, 2006, text-fig. 1.6, p. 16). Palaeotethys, Urals and Perigondwana (Iran, Devuyst, 2006; Afghanistan, Vachard, 1980). Rare in Siberia, Asia and northern America.
(Vachard and Hance in Hance et al. (2011)). [details]
Diagnosis Proloculus followed by a small enrolled stage of one or two irregularly coiled whorls of teardroplike chambers, later uncoiled with a few pair of biserial chambers; wall thick and coarsely granular with numerous calcite inclusions and may have a thin dark microgranular inner layer; aperture simple, a basal slit. L. Carboniferous (U. Tournaisian to M. Visean); USSR; Belgium; Denmark. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]
From editor or global species database
Image from typetaxon
Image from typetaxon