WoRMS taxon details
Cribromiliolinella Saidova, 1981
465873 (urn:lsid:marinespecies.org:taxname:465873)
accepted
Genus
Triloculina subvalvularis Parr, 1950 accepted as Cribromiliolinella subvalvularis (Parr, 1950) (type by original designation)
marine, brackish, fresh, terrestrial
Saidova, K. M. (1981). О современном состоянии системы надвидовых таксонов кайнозойских бентосных фораминифер - [On an up-to-date system of supraspecific taxonomy of Cenozoic benthonic foraminifera]. <em>Akademiya Nauk SSSR.</em> 1-73., available online at https://books.google.pt/books?id=h-jxnSjjmhQC [details] Available for editors 
[request]
[request]
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2024). World Foraminifera Database. Cribromiliolinella Saidova, 1981. Accessed through: World Register of Marine Species at: https://www.marinespecies.org/aphia.php?p=taxdetails&id=465873 on 2024-05-23
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The webpage text is licensed under a Creative Commons Attribution 4.0 License
original description
Saidova, K. M. (1981). О современном состоянии системы надвидовых таксонов кайнозойских бентосных фораминифер - [On an up-to-date system of supraspecific taxonomy of Cenozoic benthonic foraminifera]. <em>Akademiya Nauk SSSR.</em> 1-73., available online at https://books.google.pt/books?id=h-jxnSjjmhQC [details] Available for editors [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 [request]
[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
[request] 
Present Inaccurate Introduced: alien Containing type locality
From editor or global species database
Diagnosis Test ovate in outline, rounded to subtriangular in section, cryptoquinqueloculine, chambers one-half coil in length and added 144¡ apart but sufficiently overlapping so that only three chambers are visible from the exterior; wall calcareous, imperforate, porcelaneous, surface may be finely striate; aperture terminal, with a miliolinelline flap, the opening extending around the flap and up the chamber as an irregularly triradiate opening, the rays of the opening also secondarily bifurcating in well-developed specimens. Holocene; Antarctic: Weddell Sea at 193 m to 456 m; Pacific: Northeast New Zealand at 2,200 m; Caribbean, at 780 m. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]
