Foraminifera taxon details

Mikhailovella Ganelina, 1956 †

721726  (urn:lsid:marinespecies.org:taxname:721726)

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marine, brackish, fresh, terrestrial
fossil only
feminine
Ganelina, R. A. (1956). Фораминиферы визейских отложений северо-западных районов Подмосковной котловины - Foraminifera of the Visean deposits of the northwest region of the lower Moscow basin. <em>Микрофауна СССР - Mikrofauna SSSR, Trudy Vsesoyuznogo Nauchno-Issledovatel'skogo Geologorazvedochnogo Instituta VNIGRI.</em> 98(8): 61-159., available online at https://books.google.pt/books?id=CMV0ZQE5TBkC
page(s): p. 100 [details] Available for editors  PDF available [request]
Description Diagnosis: Test endothyroid followed by uncoiled uniseriate chambers. Wall microgranular. Aperture simple, terminal, basal...  
Description Diagnosis: Test endothyroid followed by uncoiled uniseriate chambers. Wall microgranular. Aperture simple, terminal, basal in the endothyroid stage, and cribrate in the terminal stage.
Occurrence: Tulsky-Mikhailovsky, Venevsky of Russian Platform, Urals and Southern Timan. C1 vg (B8 limestone) of Donets Basin. Late Arundian-Asbian of England (latest Asbian-early Brigantian and doubtful in late Brigantian of Northern England). Asbian-Brigantian of southwestern Spain. Late Asbian of Ireland and Germany. Early-late Brigantian of central Morocco (Saïd, 2005, p. 181, 185) where it is very rare. Ichinotani Fm, Hina Limestone, and Akiyoshi Group of Japan. ?Asbian-early Serpukhovian of Windsor Group (SE Canada). Latest Visean of South China.
(Vachard and Hance in Hance et al. (2011)). [details]

Diagnosis Test streptospirally enrolled in the early stage, later uncoiled and rectilinear, chambers inflated, septa arched forward,...  
Diagnosis Test streptospirally enrolled in the early stage, later uncoiled and rectilinear, chambers inflated, septa arched forward, sutures depressed; wall calcareous, microgranular, dark and homogeneous, thin and of constant thickness throughout; aperture basal, low, and slitlike in the early enrolled part, becoming terminal and cribrate in the later enrolled chambers or only in the uncoiled stage. L. Carboniferous (M. Visean); USSR: Moscow Basin; USA: Idaho, Utah. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]

Fossil range Occurrence: Tulskian-Mikhailovian, Venevian of Russian Platform, Urals and southern Timan. C1vg (limestone B8) of Donets...  
Fossil range Occurrence: Tulskian-Mikhailovian, Venevian of Russian Platform, Urals and southern Timan. C1vg (limestone B8) of Donets Basin. Late Arundian–Asbian of England (latest Asbian–early Brigantian and doubtful in late Brigantian of northern England). Asbian–Brigantian of southwestern Spain. Late Asbian of Ireland and Germany. Early–late Brigantian of central Morocco. Ichinotani Fm. and Akiyoshi Limestone Group of Japan. ?Asbian–early Serpukhovian of Windsor Group (SE Canada). Late Visean–early Serpukhovian of the Montagne Noire.
(Vachard and Cózar in Vachard et al. (2016)).

Occurrence: Tulian-Mikhailovian, and rare in early Venevian of Russian Platform, Urals and Southern Timan (Ganelina, 1956; Durkina, 1959; Fomina, 1960; Rozovskaya, 1963; Shlykova & Ganelina, 1974; Gibshman, 2003). C1 vg (B8 limestone) of Donets Basin (Vdovenko, 2001). Late Arundian-Asbian of England (latest Asbian-early Brigantian and doubtful in late Brigantian of Northern England; Conil et al., 1980). MFZ14 = Cf6γ of Poland (Skompski et al., 1989). Asbian-Brigantian of southwestern Spain (Cózar, 2001). Latest Asbian-early Serpukhovian of southern France (Montagne Noire: Pille, 2008). Early-late Brigantian of central Morocco (Saïd, 2005, pp. 181, 185) where it is very rare. Asbian?-early Serpukhovian of Windsor Group (SE Canada; Mamet, 1970). Ichinotani Fm (Adachi, 1985), Hina Limestone (Mizuno & Ueno, 1997), and Akiyoshi Limestone Group (Matsusue, 1986) of Japan.
(Kobayashi and Vachard (2022)). [details]
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2025). World Foraminifera Database. Mikhailovella Ganelina, 1956 †. Accessed at: https://www.marinespecies.org/Foraminifera/aphia.php?p=taxdetails&id=721726 on 2026-01-24
Date
action
by
2013-03-08 13:53:47Z
created
2017-12-10 11:22:52Z
changed
2018-01-28 16:40:36Z
changed
2019-02-20 09:57:36Z
changed

original description Ganelina, R. A. (1956). Фораминиферы визейских отложений северо-западных районов Подмосковной котловины - Foraminifera of the Visean deposits of the northwest region of the lower Moscow basin. <em>Микрофауна СССР - Mikrofauna SSSR, Trudy Vsesoyuznogo Nauchno-Issledovatel'skogo Geologorazvedochnogo Instituta VNIGRI.</em> 98(8): 61-159., available online at https://books.google.pt/books?id=CMV0ZQE5TBkC
page(s): p. 100 [details] Available for editors  PDF available [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  PDF available [request]
From editor or global species database
Description Diagnosis: Test endothyroid followed by uncoiled uniseriate chambers. Wall microgranular. Aperture simple, terminal, basal in the endothyroid stage, and cribrate in the terminal stage.
Occurrence: Tulsky-Mikhailovsky, Venevsky of Russian Platform, Urals and Southern Timan. C1 vg (B8 limestone) of Donets Basin. Late Arundian-Asbian of England (latest Asbian-early Brigantian and doubtful in late Brigantian of Northern England). Asbian-Brigantian of southwestern Spain. Late Asbian of Ireland and Germany. Early-late Brigantian of central Morocco (Saïd, 2005, p. 181, 185) where it is very rare. Ichinotani Fm, Hina Limestone, and Akiyoshi Group of Japan. ?Asbian-early Serpukhovian of Windsor Group (SE Canada). Latest Visean of South China.
(Vachard and Hance in Hance et al. (2011)). [details]

Diagnosis Test streptospirally enrolled in the early stage, later uncoiled and rectilinear, chambers inflated, septa arched forward, sutures depressed; wall calcareous, microgranular, dark and homogeneous, thin and of constant thickness throughout; aperture basal, low, and slitlike in the early enrolled part, becoming terminal and cribrate in the later enrolled chambers or only in the uncoiled stage. L. Carboniferous (M. Visean); USSR: Moscow Basin; USA: Idaho, Utah. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]

Fossil range Occurrence: Tulskian-Mikhailovian, Venevian of Russian Platform, Urals and southern Timan. C1vg (limestone B8) of Donets Basin. Late Arundian–Asbian of England (latest Asbian–early Brigantian and doubtful in late Brigantian of northern England). Asbian–Brigantian of southwestern Spain. Late Asbian of Ireland and Germany. Early–late Brigantian of central Morocco. Ichinotani Fm. and Akiyoshi Limestone Group of Japan. ?Asbian–early Serpukhovian of Windsor Group (SE Canada). Late Visean–early Serpukhovian of the Montagne Noire.
(Vachard and Cózar in Vachard et al. (2016)).

Occurrence: Tulian-Mikhailovian, and rare in early Venevian of Russian Platform, Urals and Southern Timan (Ganelina, 1956; Durkina, 1959; Fomina, 1960; Rozovskaya, 1963; Shlykova & Ganelina, 1974; Gibshman, 2003). C1 vg (B8 limestone) of Donets Basin (Vdovenko, 2001). Late Arundian-Asbian of England (latest Asbian-early Brigantian and doubtful in late Brigantian of Northern England; Conil et al., 1980). MFZ14 = Cf6γ of Poland (Skompski et al., 1989). Asbian-Brigantian of southwestern Spain (Cózar, 2001). Latest Asbian-early Serpukhovian of southern France (Montagne Noire: Pille, 2008). Early-late Brigantian of central Morocco (Saïd, 2005, pp. 181, 185) where it is very rare. Asbian?-early Serpukhovian of Windsor Group (SE Canada; Mamet, 1970). Ichinotani Fm (Adachi, 1985), Hina Limestone (Mizuno & Ueno, 1997), and Akiyoshi Limestone Group (Matsusue, 1986) of Japan.
(Kobayashi and Vachard (2022)). [details]