Foraminifera taxon details
Pseudonodosinella Saidova, 1970
491733 (urn:lsid:marinespecies.org:taxname:491733)
accepted
Genus
Reophax nodulosa Brady, 1879 accepted as Reophax nodulosus Brady, 1879 accepted as Pseudonodosinella nodulosa (Brady, 1879) (type by original designation)
- Species Pseudonodosinella antarctica Saidova, 1975
- Species Pseudonodosinella elongata (Grzybowski, 1898)
- Species Pseudonodosinella hirsuta Saidova, 1975
- Species Pseudonodosinella nodulosa (Brady, 1879)
- Species Pseudonodosinella parvula (Huss, 1966) †
- Species Pseudonodosinella rubra Saidova, 1975
- Species Pseudonodosinella troyeri (Tappan, 1960) †
- Species Pseudonodosinella bacillaris (Brady, 1881) accepted as Hormosina bacillaris (Brady, 1881) (unaccepted > superseded combination)
- Species Pseudonodosinella margaritaria (Rhumbler, 1931) accepted as Reophax margaritarius Rhumbler, 1931
marine, brackish, fresh, terrestrial
feminine
Saidova, K. M. (1970). Бентосные Фораминиферы раыона курило-Камчатского желоба - Benthic foraminifera of the Kurile-Kamchatka Trench based on the data of the 39th cruise of the R/V "Vityaz.". <em>Труды Институт океанологии-Trudy Institut Oceanology.</em> 86: 134-161. [details]
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2021). World Foraminifera Database. Pseudonodosinella Saidova, 1970. Accessed at: http://www.marinespecies.org/foraminifera./aphia.php?p=taxdetails&id=491733 on 2024-04-23
Date
action
by
original description
Saidova, K. M. (1970). Бентосные Фораминиферы раыона курило-Камчатского желоба - Benthic foraminifera of the Kurile-Kamchatka Trench based on the data of the 39th cruise of the R/V "Vityaz.". <em>Труды Институт океанологии-Trudy Institut Oceanology.</em> 86: 134-161. [details]
From editor or global species database
Diagnosis Test elongate, uniserial, chambers ovate to subpyriform, each successive chamber overlapping the aperture and much of the breadth of that preceding; wall firmly agglutinated, thin but of many grains, both exterior and interior smoothly finished; aperture terminal, at the center of the somewhat thickened wall of the produced terminal face. Holocene; S. Atlantic, N. and S. Pacific, from 2,800 m to 4,000 m; Gulf of Mexico at 694 m to 1,460 m. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]
