Foraminifera taxon details
Fusulinellinae Staff & Wedekind, 1910 †
721137 (urn:lsid:marinespecies.org:taxname:721137)
accepted
Subfamily
- Genus Anulofusulinella Wilde, 2006 †
- Genus Fusulinella Möller, 1877 †
- Genus Hidaella Fujimoto & Igo, 1955 †
- Genus Nipperella Solovieva, 1984 †
- Genus Obsoletes Kireeva, 1950 †
- Genus Plectofusulina Stewart, 1958 †
- Genus Praefusulinella Akbaş in Akbaş & Okuyucu, 2022 †
- Genus Praeobsoletes Remizova, 1992 †
- Genus Protriticites Putrya, 1948 †
- Genus Uralofusulinella Chuvashov, 1980 †
- Genus Zellerella Wilde, 2006 †
marine, fresh, terrestrial
fossil only
Staff, H. von; Wedekind, R. (1910). Der oberkarbone Foraminiferensapropelit Spitzbergens. <em>Bulletin of the Geological Institution of the University of Uppsala.</em> 10: 81–123. [details] 
Description A fusulinellid subfamily characterized by inflated fusiform tests with narrow to moderately broad tunnel and moderate to...
Diagnosis Septa flat to slightly fluted; wall of three to four layers, with diaphanotheca and generally pronounced outer tectorium, may...
Description A fusulinellid subfamily characterized by inflated fusiform tests with narrow to moderately broad tunnel and moderate to strong chomata of various forms. Wall diaphanothecal, rarely porous.
Occurrence. Moscovian, cosmopolitan: Spain, Croatia, Carnic Alps, Donbass, Russia (from Moscow Basin to Primorye), North Africa, Near East, Middle East, China, Japan, SE Asia, Canadian Arctic, USA, and Greenland.
(Vachard et al. 2013)).
[details]
Occurrence. Moscovian, cosmopolitan: Spain, Croatia, Carnic Alps, Donbass, Russia (from Moscow Basin to Primorye), North Africa, Near East, Middle East, China, Japan, SE Asia, Canadian Arctic, USA, and Greenland.
(Vachard et al. 2013)).
[details]
Diagnosis Septa flat to slightly fluted; wall of three to four layers, with diaphanotheca and generally pronounced outer tectorium, may...
Diagnosis Septa flat to slightly fluted; wall of three to four layers, with diaphanotheca and generally pronounced outer tectorium, may be perforate, chomata prominent. U. Carboniferous (Moscovian) to U. Permian (Murgabian). (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2021). World Foraminifera Database. Fusulinellinae Staff & Wedekind, 1910 †. Accessed at: http://www.marinespecies.org/foraminifera/aphia.php?p=taxdetails&id=721137 on 2025-05-21
Date
action
by
original description
Staff, H. von; Wedekind, R. (1910). Der oberkarbone Foraminiferensapropelit Spitzbergens. <em>Bulletin of the Geological Institution of the University of Uppsala.</em> 10: 81–123. [details]
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
[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
[request]From editor or global species database
Description A fusulinellid subfamily characterized by inflated fusiform tests with narrow to moderately broad tunnel and moderate to strong chomata of various forms. Wall diaphanothecal, rarely porous.Occurrence. Moscovian, cosmopolitan: Spain, Croatia, Carnic Alps, Donbass, Russia (from Moscow Basin to Primorye), North Africa, Near East, Middle East, China, Japan, SE Asia, Canadian Arctic, USA, and Greenland.
(Vachard et al. 2013)).
[details]
Diagnosis Septa flat to slightly fluted; wall of three to four layers, with diaphanotheca and generally pronounced outer tectorium, may be perforate, chomata prominent. U. Carboniferous (Moscovian) to U. Permian (Murgabian). (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]
