Foraminifera taxon details
Nestellorella Gaillot & Vachard, 2007 †
1052956 (urn:lsid:marinespecies.org:taxname:1052956)
accepted
Genus
Pseudolangella pulchra Pronina in Kotlyar et al., 1989 † accepted as Nestellorella pulchra (Pronina in Kotlyar et al., 1989) † (type by original designation)
- Species Nestellorella acus (G. Pronina, 1989) †
- Species Nestellorella doraschamensis (G. Pronina, 1989) †
- Species Nestellorella dzhagadzurensis (Pronina in Kotlyar et al., 1989) †
- Species Nestellorella fabaeformis (Pronina in Kotlyar et al., 1989) †
- Species Nestellorella filumiformis (Pronina in Kotlyar et al., 1989) †
- Species Nestellorella geranossensis (Pronina in Kotlyar et al., 1989) †
- Species Nestellorella lepida (Wang, 1982) †
- Species Nestellorella pulchra (Pronina in Kotlyar et al., 1989) †
- Species Nestellorella vachardi Le Coze, Altıner, Arefifard, Aretz, Bucur, Cózar, Fassihi, Gaillot, Ghazzay-Souli, Haig, Hance, Izart, Krainer, Kulagina, Lucas, Martini, Rettori, Somerville, Yarahmadzahi, Zandkarimi & Zaninetti, 2025 †
- Species Nestellorella parva (Lipina, 1949) † accepted as Nestellorella vachardi Le Coze, Altıner, Arefifard, Aretz, Bucur, Cózar, Fassihi, Gaillot, Ghazzay-Souli, Haig, Hance, Izart, Krainer, Kulagina, Lucas, Martini, Rettori, Somerville, Yarahmadzahi, Zandkarimi & Zaninetti, 2025 † (unaccepted > junior homonym, Primary junior homonym of Nodosaria simoniana var. parva Franke, 1936)
marine, brackish, fresh, terrestrial
fossil only
feminine
Gaillot, J.; Vachard, D. (2007). The Khuff Formation (Middle East) and time-equivalents in Turkey and South China: biostratigraphy from Capitanian to Changhsingian times (Permian), new foraminiferal taxa, and palaeogeographical implications. <em>Coloquios de Paleontologia.</em> 57: 37-223., available online at https://hal.archives-ouvertes.fr/hal-00310245
page(s): p. 118 [details] Available for editors
[request]
page(s): p. 118 [details] Available for editors
[request]
Diagnosis Diagnosis: Test small to medium-sized (H.= 0.100-0.440 mm), tapering to cylindrical. Chambers reniform. Septa curvated to...
Diagnosis Diagnosis: Test small to medium-sized (H.= 0.100-0.440 mm), tapering to cylindrical. Chambers reniform. Septa curvated to angular and similar to the angulatus stage of the archaediscid foraminifers, i.e. evolute with suture marked along all the base of the chamber wall. Wall hyaline only present. Aperture absent in the first chamber, then of Protonodosaria type, and finally very large, with faint inner and outer thickening of the wall.
Occurrence: Wordian? of southern Oman (ANGIOLINI et al., 2004). Midian-late Changhsingian of Transcaucasia (PRONINA, 1988a, 1989; KOTLYAR et al., 1989). Midian of Rushan-Pshart Pamir (DRONOV, 2004). Late Midian of Hazro. Lopingian of Zagros.
(Gaillot and Vachard (2007)).
Range and distribution: Wordian? of southern Oman (Angiolini et al. 2004) – late Changhsingian of Transcaucasia (Pronina 1988a; Kotlyar et al. 1989; Pronina 1989). Midian of Rushan-Pshart, Pamir (Dronov 2004). Late Midian of Hazro. Lopingian of Zagros. Discovered in the latest Permian of the northwestern Dolomites (South Tyrol, Italy).
(Vachard and Krainer (2022)). [details]
Occurrence: Wordian? of southern Oman (ANGIOLINI et al., 2004). Midian-late Changhsingian of Transcaucasia (PRONINA, 1988a, 1989; KOTLYAR et al., 1989). Midian of Rushan-Pshart Pamir (DRONOV, 2004). Late Midian of Hazro. Lopingian of Zagros.
(Gaillot and Vachard (2007)).
Range and distribution: Wordian? of southern Oman (Angiolini et al. 2004) – late Changhsingian of Transcaucasia (Pronina 1988a; Kotlyar et al. 1989; Pronina 1989). Midian of Rushan-Pshart, Pamir (Dronov 2004). Late Midian of Hazro. Lopingian of Zagros. Discovered in the latest Permian of the northwestern Dolomites (South Tyrol, Italy).
(Vachard and Krainer (2022)). [details]
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2025). World Foraminifera Database. Nestellorella Gaillot & Vachard, 2007 †. Accessed at: https://www.marinespecies.org/Foraminifera/aphia.php?p=taxdetails&id=1052956 on 2026-07-01
Date
action
by
original description
Gaillot, J.; Vachard, D. (2007). The Khuff Formation (Middle East) and time-equivalents in Turkey and South China: biostratigraphy from Capitanian to Changhsingian times (Permian), new foraminiferal taxa, and palaeogeographical implications. <em>Coloquios de Paleontologia.</em> 57: 37-223., available online at https://hal.archives-ouvertes.fr/hal-00310245
page(s): p. 118 [details] Available for editors [request]
page(s): p. 118 [details] Available for editors
[request]From editor or global species database
Diagnosis Diagnosis: Test small to medium-sized (H.= 0.100-0.440 mm), tapering to cylindrical. Chambers reniform. Septa curvated to angular and similar to the angulatus stage of the archaediscid foraminifers, i.e. evolute with suture marked along all the base of the chamber wall. Wall hyaline only present. Aperture absent in the first chamber, then of Protonodosaria type, and finally very large, with faint inner and outer thickening of the wall.Occurrence: Wordian? of southern Oman (ANGIOLINI et al., 2004). Midian-late Changhsingian of Transcaucasia (PRONINA, 1988a, 1989; KOTLYAR et al., 1989). Midian of Rushan-Pshart Pamir (DRONOV, 2004). Late Midian of Hazro. Lopingian of Zagros.
(Gaillot and Vachard (2007)).
Range and distribution: Wordian? of southern Oman (Angiolini et al. 2004) – late Changhsingian of Transcaucasia (Pronina 1988a; Kotlyar et al. 1989; Pronina 1989). Midian of Rushan-Pshart, Pamir (Dronov 2004). Late Midian of Hazro. Lopingian of Zagros. Discovered in the latest Permian of the northwestern Dolomites (South Tyrol, Italy).
(Vachard and Krainer (2022)). [details]
From editor or global species database
Image from typetaxon