Foraminifera taxon details
Polarisella Mamet & Pinard, 1992 †
1052959 (urn:lsid:marinespecies.org:taxname:1052959)
accepted
Genus
Polarisella blindensis Mamet & Pinard, 1992 † (type by original designation)
- Species Polarisella blindensis Mamet & Pinard, 1992 †
- Species Polarisella curta (Zheng & Lin, 1978) † (accepted > unreplaced junior homonym, Primary junior homonym of Nodosaria (Dentalina) curta Paalzow, 1917)
- Species Polarisella elabugae (Cherdynzev, 1914) †
- Species Polarisella globosa Nestell & Nestell in Nestell et al., 2006 †
- Species Polarisella hoae (Trifonova, 1967) †
- Species Polarisella lanceolata (Zheng & Lin, 1978) † (accepted > unreplaced junior homonym, Primary junior homonym of Nodosaria (Dentalina) lanceolata Herrmann, 1917)
- Species Polarisella lingulae Nestell & Nestell, 2006 †
- Species Polarisella nigra (Luperto, 1966) †
- Species Polarisella ordinata (Trifonova, 1965) †
- Species Polarisella piricamerata (Efimova, 1974) †
- Species Polarisella potentina (Luperto, 1966) †
- Species Polarisella spathulata (Luperto, 1966) †
- Species Polarisella transcaucasica (Vuks in Kotlyar et al., 1984) †
- Species Polarisella armeniensis (Efimova, 1961) † (unaccepted > nomen nudum)
- Species Polarisella cubanica (Miklukho-Maklay, 1954) † accepted as Nodosinelloides cubanicus (Miklukho-Maklay, 1954) †
- Species Polarisella sagitta (Miklukho-Maklay, 1954) † accepted as Protonodosaria sagitta (Miklukho-Maklay, 1954) †
marine, brackish, fresh, terrestrial
fossil only
feminine
Mamet, B.; Pinard, S. (1992). Note sur la taxonomie des petits foraminifères du Paléozoïque supérieur - A taxonomic note on upper Paleozoic smaller foraminifera. <em>Bulletin de la Société belge de Géologie.</em> 99[1990]: 373-398., available online at http://biblio.naturalsciences.be/rbins-publications/bulletin-de-la-societe-belge-de-geologie/099%20-%201990/bsbg_nr99_1990_373-397.pdf
page(s): p. 377 [details] Available for editors
[request]
page(s): p. 377 [details] Available for editors
Description Emended diagnosis: See Mamet & Pinard (1992: 377) and add the following characters: In sagittal axial sections, the palmate...
Description Emended diagnosis: See Mamet & Pinard (1992: 377) and add the following characters: In sagittal axial sections, the palmate chambers are only high in the central part, then very low in the upper part. They communicate probably with the exterior by a lateral connection (sutural pores or gutters).
Range and distribution: Early Permian (Mamet & Pinard 1992) to Middle Triassic (Anisian), cosmopolitan (Gaillot & Vachard 2007); and up to the Jurassic of Germany (see the “Frondicularia” of Flügel (2004: pl. 69, fig. 11)).
(Vachard and Krainer (2022)). [details]
Range and distribution: Early Permian (Mamet & Pinard 1992) to Middle Triassic (Anisian), cosmopolitan (Gaillot & Vachard 2007); and up to the Jurassic of Germany (see the “Frondicularia” of Flügel (2004: pl. 69, fig. 11)).
(Vachard and Krainer (2022)). [details]
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2025). World Foraminifera Database. Polarisella Mamet & Pinard, 1992 †. Accessed at: https://www.marinespecies.org/Foraminifera/aphia.php?p=taxdetails&id=1052959 on 2026-07-12
Date
action
by
original description
Mamet, B.; Pinard, S. (1992). Note sur la taxonomie des petits foraminifères du Paléozoïque supérieur - A taxonomic note on upper Paleozoic smaller foraminifera. <em>Bulletin de la Société belge de Géologie.</em> 99[1990]: 373-398., available online at http://biblio.naturalsciences.be/rbins-publications/bulletin-de-la-societe-belge-de-geologie/099%20-%201990/bsbg_nr99_1990_373-397.pdf
page(s): p. 377 [details] Available for editors
[request]
page(s): p. 377 [details] Available for editors
From editor or global species database
Description Emended diagnosis: See Mamet & Pinard (1992: 377) and add the following characters: In sagittal axial sections, the palmate chambers are only high in the central part, then very low in the upper part. They communicate probably with the exterior by a lateral connection (sutural pores or gutters).Range and distribution: Early Permian (Mamet & Pinard 1992) to Middle Triassic (Anisian), cosmopolitan (Gaillot & Vachard 2007); and up to the Jurassic of Germany (see the “Frondicularia” of Flügel (2004: pl. 69, fig. 11)).
(Vachard and Krainer (2022)). [details]