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Deep-Sea taxon detailsEpistomina Terquem, 1883 †
 248337 (urn:lsid:marinespecies.org:taxname:248337)
accepted
Genus
marine,
fossil only
Terquem, O., 1883, Sur un nouveau genre de foraminifères de Fuller's-earth de Ia Moselle, Bulletin de Ia Société Géologique de France (1882-1883), ser. 3 11:37-39. , available online at https://www.biodiversitylibrary.org/page/47193366
page(s): p. 37 [details]
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2025). World Foraminifera Database. Epistomina Terquem, 1883 †. 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=248337 on 2025-05-19
Glover, A.G.; Higgs, N.; Horton, T. (2025). World Register of Deep-Sea species (WoRDSS). Epistomina Terquem, 1883 †. Accessed at: https://marinespecies.org/DeepSea/aphia.php?p=taxdetails&id=248337 on 2025-05-19
Date action by
original description
Terquem, O., 1883, Sur un nouveau genre de foraminifères de Fuller's-earth de Ia Moselle, Bulletin de Ia Société Géologique de France (1882-1883), ser. 3 11:37-39. , available online at https://www.biodiversitylibrary.org/page/47193366
page(s): p. 37 [details] basis of record Integrated Taxonomic Information System (ITIS). , available online at http://www.itis.gov [details] 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 trochospiral, lenticular to planoconvex, chambers increasing gradually in size, internal partition slightly curved, present in all chambers or may be resorbed during later development, extending from the margin of the apertural opening nearly or completely to the base of the chamber against the previous whorl, sutures slightly curved, commonly limbate to strongly elevated, periphery angular to carinate; wall calcareous, aragonitic, finely perforate, surface smooth to strongly sculptured; aperture lateromarginal, adjacent to the peripheral keel on the umbilical side, closed with shell material as the new chamber is added, later formed intercameral foramen oblique, oval and areal or may be interiomarginal. L. Jurassic to L. Cretaceous (Albian); cosmopolitan. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]
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