Foraminifera taxon details
Janischewskinidae Reitlinger in Rauzer-Chernousova et al., 1996 †
1055911 (urn:lsid:marinespecies.org:taxname:1055911)
accepted
Family
- Genus Bibradya Strank, 1983 †
- Genus Cribrospira Möller, 1878 †
- Genus Janischewskina Mikhailov, 1939 †
- Genus Parajanischewskina Cózar & Somerville, 2006 †
- Genus Groessensella Strank in Somerville & Strank, 1984 † accepted as Bibradya Strank, 1983 † (unaccepted > junior subjective synonym, Subjective junior synonym Opinion of Vachard and Cózar in Liu et al. (2023))
- Genus Rhodesina Conil & Longerstaey, 1980 † accepted as Rhodesinella Conil & Longerstaey, 1980 † accepted as Cribrospira Möller, 1878 † (Junior homonym)
- Genus Rhodesinella Conil & Longerstaey, 1980 † accepted as Cribrospira Möller, 1878 † (unaccepted > junior subjective synonym, Subjective junior synonym Opinion of Vachard and Cózar in Liu et al. (2023))
- Genus Samarina Rauzer-Chernousova & Reitlinger, 1940 † accepted as Janischewskina Mikhailov, 1939 † (Subjective junior synonym in opinion of Loeblich & Tappan, 1987)
marine, fresh, terrestrial
fossil only
Rauzer-Chernousova, D.M., Bensh, F.R., Vdovenko, M.V., Gibshman, N.B., Leven, E.Ya., Lipina, O.A. Reitlinger, E.A., Solovieva, M.N. and Chediya, I.O. (1996). Справочник по систематике фораминифер палеозоя (эндотироиды, фузулиноиды) - Handbook on taxonomy of Paleozoic foraminifera (endotyroids, fusulinoids). <em>Nauka.</em> 1-205., available online at https://books.google.com/books?id=z9FGBQAAQBAJ
page(s): p. 60 [details] Available for editors
[request]
page(s): p. 60 [details] Available for editors
[request]
Description Test free, nautiloid to compressed laterally, with a juvenarium endothyroid passing to a planispiral final coiling. Coiling...
Description Test free, nautiloid to compressed laterally, with a juvenarium endothyroid passing to a planispiral final coiling. Coiling follows a progressive increase of the spire with a common rapid increase of the final whorl, in species trending to the uncoiling.
Secondary deposits absent. The most common septa are simple, curved backward, but also furrowed, blunt, swollen, and bifurcated. Cribrate aperture in the final whorl, rarely present in the penultimate chambers. Wall microgranular to granular with some agglutinated grains in the more ancestral forms, or with a porous tectum.
(Liu et al. (2023)).
Occurrence. Late Visean–early Bashkirian; Palaeotethys and Urals shelves. Rare in NW Washington, U.S.A. (Liszak & Ross 1997) but testifying probably of a Cathaysian, exotic, tectonostratigraphic terrane.
(Vachard and Le Coze (2022)). [details]
Secondary deposits absent. The most common septa are simple, curved backward, but also furrowed, blunt, swollen, and bifurcated. Cribrate aperture in the final whorl, rarely present in the penultimate chambers. Wall microgranular to granular with some agglutinated grains in the more ancestral forms, or with a porous tectum.
(Liu et al. (2023)).
Occurrence. Late Visean–early Bashkirian; Palaeotethys and Urals shelves. Rare in NW Washington, U.S.A. (Liszak & Ross 1997) but testifying probably of a Cathaysian, exotic, tectonostratigraphic terrane.
(Vachard and Le Coze (2022)). [details]
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2024). World Foraminifera Database. Janischewskinidae Reitlinger in Rauzer-Chernousova et al., 1996 †. Accessed at: https://www.marinespecies.org/foraminifera/aphia.php?p=taxdetails&id=1055911 on 2024-04-18
Date
action
by
original description
Rauzer-Chernousova, D.M., Bensh, F.R., Vdovenko, M.V., Gibshman, N.B., Leven, E.Ya., Lipina, O.A. Reitlinger, E.A., Solovieva, M.N. and Chediya, I.O. (1996). Справочник по систематике фораминифер палеозоя (эндотироиды, фузулиноиды) - Handbook on taxonomy of Paleozoic foraminifera (endotyroids, fusulinoids). <em>Nauka.</em> 1-205., available online at https://books.google.com/books?id=z9FGBQAAQBAJ
page(s): p. 60 [details] Available for editors [request]
page(s): p. 60 [details] Available for editors
[request] From editor or global species database
Description Test free, nautiloid to compressed laterally, with a juvenarium endothyroid passing to a planispiral final coiling. Coiling follows a progressive increase of the spire with a common rapid increase of the final whorl, in species trending to the uncoiling.Secondary deposits absent. The most common septa are simple, curved backward, but also furrowed, blunt, swollen, and bifurcated. Cribrate aperture in the final whorl, rarely present in the penultimate chambers. Wall microgranular to granular with some agglutinated grains in the more ancestral forms, or with a porous tectum.
(Liu et al. (2023)).
Occurrence. Late Visean–early Bashkirian; Palaeotethys and Urals shelves. Rare in NW Washington, U.S.A. (Liszak & Ross 1997) but testifying probably of a Cathaysian, exotic, tectonostratigraphic terrane.
(Vachard and Le Coze (2022)). [details]