Foraminifera taxon details
Ogbinella Chediya in Kotlyar, Zakharov, Kropacheva, Pronina, Chediya & Burago, 1989 †
1059397 (urn:lsid:marinespecies.org:taxname:1059397)
accepted
Genus
Boultonia avushensis Chediya in Kotlyar et al., 1984 † accepted as Ogbinella avushensis (Chediya in Kotlyar et al., 1984) † (type by original designation)
- Species Ogbinella ardaglensis (Chediya in Kotlyar et al., 1984) †
- Species Ogbinella avushensis (Chediya in Kotlyar et al., 1984) †
- Species Ogbinella erki (Skinner, 1969) †
- Species Ogbinella guadalupensis (Skinner & Wilde, 1954) †
- Species Ogbinella ogbinensis (Chediya in Kotlyar et al., 1984) †
- Species Ogbinella plata Orlov-Labkovsky, 2004 †
- Species Ogbinella yukonensis (Ross, 1967) †
- Species Ogbinella cascadensis (Thompson, Wheeler & Danner, 1950) † accepted as Dunbarula cascadensis (Thompson, Wheeler & Danner, 1950) † (unaccepted > superseded combination)
marine, brackish, fresh, terrestrial
fossil only
feminine
Kotlyar, G. V.; Zakharov, Y. D.; Kropacheva, G. S.; Pronina, G. P.; Chediya, I. O.; Burago, V. I. (1989). Позднепермский этап эволюции органического мира: мидийский ярус СССР - Evolution of the latest Permian biota, Midian regional stage in the USSR. <em>Nauka, Leningrad.</em> 1-177., available online at https://www2.ekeng.am/files/library/1/15256780882746.pdf
page(s): p. 100 [details] Available for editors
[request]
page(s): p. 100 [details] Available for editors
[request]
Description Р. маленькая, от вздуто- до вытянуто- веретеновидной формы; нач. к....
Description Р. маленькая, от вздуто- до вытянуто- веретеновидной формы; нач. к. маленькая; первые 1,5-2 об. навиты под углом к последующим; число об. 4-6; ст. р. тонкая, двухслойная; складчатость септ преимущественно на боках и у полюсов, равномерная, невысокая; хоматы непостоянные; доп. отл. слабые - на септах и в приустьевой части; туннель отчетливый. 7 видов. В. пермь, мургабский-джульфинский ярусы; Закавказье, Турция, С. Ам. От псевдодунбарул и парадунбарул отличаются более вытянутой р., от последних - вдвое меньшими размерами.
(Rauzer-Chernousova et al. (1996)).
Test small, from inflated- to elongated-fusiform; proloculus small; the first 1.5-2 whorls are coiled at an angle to the subsequent ones; whorl number 4-6; wall thin, two-layered; the folding of the septa is predominantly on the sides and at the poles, uniform, not high; chomata are inconstant; additional deposits are weak - on the septa and in the peak part; the tunnel is distinct. 7 species. Upper Permian, Murgabian-Dzhulfinian; Transcaucasia, Turkey, North America. Differs from Pseudodunbarula and Paradunbarula in a more elongated test, from the latter in half its size. [details]
(Rauzer-Chernousova et al. (1996)).
Test small, from inflated- to elongated-fusiform; proloculus small; the first 1.5-2 whorls are coiled at an angle to the subsequent ones; whorl number 4-6; wall thin, two-layered; the folding of the septa is predominantly on the sides and at the poles, uniform, not high; chomata are inconstant; additional deposits are weak - on the septa and in the peak part; the tunnel is distinct. 7 species. Upper Permian, Murgabian-Dzhulfinian; Transcaucasia, Turkey, North America. Differs from Pseudodunbarula and Paradunbarula in a more elongated test, from the latter in half its size. [details]
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2025). World Foraminifera Database. Ogbinella Chediya in Kotlyar, Zakharov, Kropacheva, Pronina, Chediya & Burago, 1989 †. Accessed at: https://www.marinespecies.org/foraminifera/aphia.php?p=taxdetails&id=1059397 on 2026-04-17
Date
action
by
original description
Kotlyar, G. V.; Zakharov, Y. D.; Kropacheva, G. S.; Pronina, G. P.; Chediya, I. O.; Burago, V. I. (1989). Позднепермский этап эволюции органического мира: мидийский ярус СССР - Evolution of the latest Permian biota, Midian regional stage in the USSR. <em>Nauka, Leningrad.</em> 1-177., available online at https://www2.ekeng.am/files/library/1/15256780882746.pdf
page(s): p. 100 [details] Available for editors [request]
page(s): p. 100 [details] Available for editors
[request]From editor or global species database
Description Р. маленькая, от вздуто- до вытянуто- веретеновидной формы; нач. к. маленькая; первые 1,5-2 об. навиты под углом к последующим; число об. 4-6; ст. р. тонкая, двухслойная; складчатость септ преимущественно на боках и у полюсов, равномерная, невысокая; хоматы непостоянные; доп. отл. слабые - на септах и в приустьевой части; туннель отчетливый. 7 видов. В. пермь, мургабский-джульфинский ярусы; Закавказье, Турция, С. Ам. От псевдодунбарул и парадунбарул отличаются более вытянутой р., от последних - вдвое меньшими размерами.(Rauzer-Chernousova et al. (1996)).
Test small, from inflated- to elongated-fusiform; proloculus small; the first 1.5-2 whorls are coiled at an angle to the subsequent ones; whorl number 4-6; wall thin, two-layered; the folding of the septa is predominantly on the sides and at the poles, uniform, not high; chomata are inconstant; additional deposits are weak - on the septa and in the peak part; the tunnel is distinct. 7 species. Upper Permian, Murgabian-Dzhulfinian; Transcaucasia, Turkey, North America. Differs from Pseudodunbarula and Paradunbarula in a more elongated test, from the latter in half its size. [details]
From editor or global species database
Image from typetaxon