Foraminifera taxon details

Cuneolinidae Saidova, 1981 †

585281  (urn:lsid:marinespecies.org:taxname:585281)

accepted
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marine, fresh, terrestrial
fossil only
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  PDF available [request]
Diagnosis Test conical to subflabelliform, trochospiral in early stage, with up to five chambers per whorl, rapidly reduced to...  
Diagnosis Test conical to subflabelliform, trochospiral in early stage, with up to five chambers per whorl, rapidly reduced to biserial; chambers subdivided by many septulae extending from the outer wall toward the junction of the two series of chambers; wall agglutinated, with imperforate outer layer and reticulate subepidermal layer; aperture simple to multiple. M. Triassic (Anisian) to U. Cretaceous (Coniacian). (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2025). World Foraminifera Database. Cuneolinidae Saidova, 1981 †. Accessed at: https://www.marinespecies.org/foraminifera/aphia.php?p=taxdetails&id=585281 on 2026-02-27
Date
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2011-11-01 20:23:24Z
created

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  PDF available [request]
From editor or global species database
Diagnosis Test conical to subflabelliform, trochospiral in early stage, with up to five chambers per whorl, rapidly reduced to biserial; chambers subdivided by many septulae extending from the outer wall toward the junction of the two series of chambers; wall agglutinated, with imperforate outer layer and reticulate subepidermal layer; aperture simple to multiple. M. Triassic (Anisian) to U. Cretaceous (Coniacian). (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]
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