Foraminifera taxon details

Sagrinella Saidova, 1975

480191  (urn:lsid:marinespecies.org:taxname:480191)

accepted
Genus
Sagrinella guinai Saidova, 1975 accepted as Sagrinella jugosa (Brady, 1884) (type by original designation)

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marine, brackish, fresh, terrestrial
Saidova, K. M. (1975). Бентосине фораминиферий Тихого океана-Bentosniye foraminifery Tikhogo Okeana-Benthonic Foraminifera of the Pacific Ocean. <em>Институт океанологии им. П. П. Шершова Академии наук СССР-P.P. Shirshov Institute of Oceanology, Academy of Sciences of the USSR, Moscow.</em> 3: parts.
page(s): p. 309 [details]  Available for editors  PDF available [request] 
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2024). World Foraminifera Database. Sagrinella Saidova, 1975. Accessed at: https://www.marinespecies.org/foraminifera/aphia.php?p=taxdetails&id=480191 on 2024-04-19
Date
action
by
2010-06-21 08:40:58Z
created
2013-03-08 15:09:52Z
changed
2014-05-03 09:01:20Z
changed
2014-07-22 07:06:27Z
changed
2017-05-04 16:45:08Z
changed

original description Saidova, K. M. (1975). Бентосине фораминиферий Тихого океана-Bentosniye foraminifery Tikhogo Okeana-Benthonic Foraminifera of the Pacific Ocean. <em>Институт океанологии им. П. П. Шершова Академии наук СССР-P.P. Shirshov Institute of Oceanology, Academy of Sciences of the USSR, Moscow.</em> 3: parts.
page(s): p. 309 [details]  Available for editors  PDF available [request] 

additional source 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] 
 
 Present  Inaccurate  Introduced: alien  Containing type locality 
From editor or global species database
Diagnosis Test elongate, slightly compressed and oval in section, chambers broad, low, and biserially arranged in the early stage, later becoming relatively higher, loosely biserial and finally uniserial, chambers sharply angled about onethird the distance from the basal suture, with a prominent ridge or carina at the angle resulting in a serrate outline, terminal face convex, sutures depressed, strongly oblique; wall calcareous, optically radial, chamber angle variously pustulose or carinate, perforate, with large pores in the lower part of the chambers below the carinate angle; aperture large, oval, areal to terminal, with bordering lip and a hemicylindrical toothplate that changes orientation about 180¡ in successive chambers. Holocene; tropical and subtropical Atlantic; Pacific; Timor Sea. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]