Foraminifera taxon details
Endothyranopsinae Reitlinger, 1958 †
721130 (urn:lsid:marinespecies.org:taxname:721130)
accepted
Subfamily
- Genus Cribranopsis Conil & Longerstaey, 1980 †
- Genus Endothyranopsis Cummings, 1955 †
- Genus Granuliferella Zeller, 1957 †
- Genus Latiendothyranopsis Lipina, 1977 †
- Genus Plectogyranopsis Vachard, 1977 †
- Genus Rectocribranopsis Vachard & Kobayashi in Kobayashi & Vachard, 2022 †
- Genus Latiendothyra Lipina, 1963 † accepted as Granuliferella Zeller, 1957 † (Subjective junior synonym Opinion of Hance, Hou and Vachard (2011))
marine, fresh, terrestrial
fossil only
Reitlinger. E. A. (1958). К вопросу систематики и филогении надсемейства Endothyridea - On the question of the systematics and phylogeny of the superfamily Endothyridea. <em>Voprosy Mikropaleontologii.</em> 2: 53-73., available online at http://www.ginras.ru/library/pdf/02_1958_voprosy_mikropaleontologii.pdf
page(s): p. 57 [details] Available for editors
[request]
page(s): p. 57 [details] Available for editors
[request]
Description Bradyinoids small to medium in size, planispiral involute and generally nautiloid. Moderate number of whorls and chambers....
Diagnosis Test large, planispiral, and involute, rarely uncoiling in the adult; septa thick and massive; wall coarsely microgranular,...
Description Bradyinoids small to medium in size, planispiral involute and generally nautiloid. Moderate number of whorls and chambers. Septa truncated at the base. Supplementary deposits absent or represented by a terminal hook and some pseudochomata. Wall dark simple, relatively thick and generally calcareously agglutinated. A fine pseudokeriotheca exists in the most advanced Endothyranopsis. Wall terminal, simple, basal.
(Vachard and Le Coze (2024)). [details]
(Vachard and Le Coze (2024)). [details]
Diagnosis Test large, planispiral, and involute, rarely uncoiling in the adult; septa thick and massive; wall coarsely microgranular,...
Diagnosis Test large, planispiral, and involute, rarely uncoiling in the adult; septa thick and massive; wall coarsely microgranular, with a tendency to recrystallize, thick and finely perforate in geologically later forms, supplementary deposits as chomata and parachomata; aperture simple, basal, rarely cribrate. L. Carboniferous (Visean) to U. Carboniferous (Stephanian). (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2025). World Foraminifera Database. Endothyranopsinae Reitlinger, 1958 †. Accessed at: https://marinespecies.org/foraminifera/aphia.php?p=taxdetails&id=721130 on 2025-05-19
Date
action
by
original description
Reitlinger. E. A. (1958). К вопросу систематики и филогении надсемейства Endothyridea - On the question of the systematics and phylogeny of the superfamily Endothyridea. <em>Voprosy Mikropaleontologii.</em> 2: 53-73., available online at http://www.ginras.ru/library/pdf/02_1958_voprosy_mikropaleontologii.pdf
page(s): p. 57 [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. 57 [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 Bradyinoids small to medium in size, planispiral involute and generally nautiloid. Moderate number of whorls and chambers. Septa truncated at the base. Supplementary deposits absent or represented by a terminal hook and some pseudochomata. Wall dark simple, relatively thick and generally calcareously agglutinated. A fine pseudokeriotheca exists in the most advanced Endothyranopsis. Wall terminal, simple, basal.(Vachard and Le Coze (2024)). [details]
Diagnosis Test large, planispiral, and involute, rarely uncoiling in the adult; septa thick and massive; wall coarsely microgranular, with a tendency to recrystallize, thick and finely perforate in geologically later forms, supplementary deposits as chomata and parachomata; aperture simple, basal, rarely cribrate. L. Carboniferous (Visean) to U. Carboniferous (Stephanian). (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]
