Foraminifera taxon details
Lituotubellidae Miklukho-Maklay, 1963 nom. translat. Lipina, 1989 †
1054909 (urn:lsid:marinespecies.org:taxname:1054909)
accepted
Family
- Genus Alticonilites Hance, Hou & Vachard, 2011 †
- Genus Lituotubella Rauzer-Chernousova, 1948 †
- Genus Pseudolituotubella Vdovenko, 1967 †
- Genus Bogushella Conil & Lys, 1977 † accepted as Lituotubella Rauzer-Chernousova, 1948 † (Subjective junior synonym Opinion of Hance, Hou and Vachard (2011))
- Genus Conilites Vdovenko, 1970 † accepted as Alticonilites Hance, Hou & Vachard, 2011 † (Preoccupied by Conilites Schlotheim, 1820 Mollusca)
- Genus Cribrella Lipina, 1989 † accepted as Cribroaperturata Lipina, 1990 † accepted as Lituotubella Rauzer-Chernousova, 1948 † (Junior homonym)
- Genus Cribroaperturata Lipina, 1990 † accepted as Lituotubella Rauzer-Chernousova, 1948 † (Subjective junior synonym Opinion of Hance et al. (2011) [probable juvenile?])
- Genus Eocribrella Lipina, 1989 † accepted as Lituotubella Rauzer-Chernousova, 1948 † (unaccepted > junior subjective synonym, Subjective junior synonym in opinion of Hance et al. (2011))
- Subfamily Lituotubellinae Miklukho-Maklay, 1963 † (unnecessay rank)
- Genus Mstiniella Conil & Lys, 1977 † accepted as Pseudolituotubella Vdovenko, 1967 † (unaccepted > junior subjective synonym, Subjective junior synonym in opinion of Hance et al. (2011))
marine, fresh, terrestrial
fossil only
Miklukho-Maklay, A. D. (1963). Верхний палеозой Средней Азии - Upper Paleozoic of Central Asia. <em>Ленинградский государственный университет им. А.А. Жданова - Leningrad State University. A.A. Zhdanov.</em> 1-330., available online at https://books.google.pt/books?id=kh1fDwAAQBAJ
page(s): p. 183 [details] Available for editors
[request]
page(s): p. 183 [details] Available for editors
[request]
Description Tests streptospirally coiled becoming uncoiled. Complete septa in all whorls. Chambers characteristically teardrop-shaped....
Description Tests streptospirally coiled becoming uncoiled. Complete septa in all whorls. Chambers characteristically teardrop-shaped. Rare supplementary deposits. Wall dark and simple, with rare agglutinated calcareous particles in some representatives. Aperture terminal simple.
Occurrence. Late Tournaisian–late Serpukhovian; Palaeotethyan and Uralian shelves (Hance et al. 2011). LAD probably located in the late Asbian (Cózar & Somerville 2004, 2005) or early Brigantian (Somerville & Cózar 2005); but the genus has been mentioned up to the top of Visean: Mamet 1974a, p. 395; Fewtrell et al. 1989, p. 56; Somerville & Cózar 2005, text-fig. 3 p. 133; Wu et al. 2009, p. 29) or to Protvian (Kulagina 1988, p. 26).
(Vachard and Le Coze (2022)).
[details]
Occurrence. Late Tournaisian–late Serpukhovian; Palaeotethyan and Uralian shelves (Hance et al. 2011). LAD probably located in the late Asbian (Cózar & Somerville 2004, 2005) or early Brigantian (Somerville & Cózar 2005); but the genus has been mentioned up to the top of Visean: Mamet 1974a, p. 395; Fewtrell et al. 1989, p. 56; Somerville & Cózar 2005, text-fig. 3 p. 133; Wu et al. 2009, p. 29) or to Protvian (Kulagina 1988, p. 26).
(Vachard and Le Coze (2022)).
[details]
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2024). World Foraminifera Database. Lituotubellidae Miklukho-Maklay, 1963 nom. translat. Lipina, 1989 †. Accessed at: https://www.marinespecies.org/foraminifera/aphia.php?p=taxdetails&id=1054909 on 2024-04-19
Date
action
by
original description
Miklukho-Maklay, A. D. (1963). Верхний палеозой Средней Азии - Upper Paleozoic of Central Asia. <em>Ленинградский государственный университет им. А.А. Жданова - Leningrad State University. A.A. Zhdanov.</em> 1-330., available online at https://books.google.pt/books?id=kh1fDwAAQBAJ
page(s): p. 183 [details] Available for editors [request]
page(s): p. 183 [details] Available for editors
[request] From editor or global species database
Description Tests streptospirally coiled becoming uncoiled. Complete septa in all whorls. Chambers characteristically teardrop-shaped. Rare supplementary deposits. Wall dark and simple, with rare agglutinated calcareous particles in some representatives. Aperture terminal simple. Occurrence. Late Tournaisian–late Serpukhovian; Palaeotethyan and Uralian shelves (Hance et al. 2011). LAD probably located in the late Asbian (Cózar & Somerville 2004, 2005) or early Brigantian (Somerville & Cózar 2005); but the genus has been mentioned up to the top of Visean: Mamet 1974a, p. 395; Fewtrell et al. 1989, p. 56; Somerville & Cózar 2005, text-fig. 3 p. 133; Wu et al. 2009, p. 29) or to Protvian (Kulagina 1988, p. 26).
(Vachard and Le Coze (2022)).
[details]