Deep-Sea taxon details
Cribromiliolinella Saidova, 1981
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 
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2025). World Foraminifera Database. Cribromiliolinella Saidova, 1981. Accessed through: Glover, A.G.; Higgs, N.; Horton, T. (2025) World Register of Deep-Sea species (WoRDSS) at: https://marinespecies.org/deepsea/aphia.php?p=taxdetails&id=465873 on 2025-05-19
Glover, A.G.; Higgs, N.; Horton, T. (2025). World Register of Deep-Sea species (WoRDSS). Cribromiliolinella Saidova, 1981. Accessed at: https://marinespecies.org/deepsea/aphia.php?p=taxdetails&id=465873 on 2025-05-19
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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
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
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
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]
