WoRMS taxon details
Crateritinae Saidova, 1981
marine, fresh, terrestrial
recent + fossil
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 
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Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2025). World Foraminifera Database. Crateritinae Saidova, 1981. Accessed through: World Register of Marine Species at: https://www.marinespecies.org/aphia.php?p=taxdetails&id=721178 on 2025-03-22
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Nomenclature
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]
basis of record 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]basis of record 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]From editor or global species database
Diagnosis Test club-shaped, attached by a basal expansion, then narrowing slightly in a trunklike region of ten to twelve superimposed layers of polygonal chamberlets that are formed by numerous small vertical partitions, chamberlets increasing in number as the test gradually expands into a subglobular upper portion; wall calcareous, imperforate, porcelaneous?; aperture consisting of numerous rounded openings over the convex upper surface of the test that open into the small chamberlets, those of preceding layers remaining as intercameral foramina. Holocene; Lord Howe Island, South Pacific. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]
