Foraminifera taxon details

Pseudonodosinella Saidova, 1970

491733  (urn:lsid:marinespecies.org:taxname:491733)

accepted
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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] 
Diagnosis Test elongate, uniserial, chambers ovate to subpyriform, each successive chamber overlapping the aperture and much of the...  
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]
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 2026-01-16
Date
action
by
2010-07-21 07:48:58Z
created
2012-01-20 07:56:03Z
changed
2013-08-18 10:23:22Z
changed
2014-03-02 09:07:43Z
changed
2017-09-29 19:54:05Z
changed

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]
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