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Foraminifera taxon detailsGlyphostomella Cushman & Waters, 1928 †
 721392 (urn:lsid:marinespecies.org:taxname:721392)
accepted
Genus
Ammochilostoma triloculina Cushman & Waters, 1927 † accepted as Glyphostomella triloculina (Cushman & Waters, 1927) † accepted as Glyphostomella hodenvillensis (Harlton, 1927) † (type by original designation)
marine,
fossil only
feminine
Cushman, J. A.; Waters, J. A. (1928). Some Foraminifera from the Pennsylvanian and Permian of Texas. <em>Contributions from the Cushman Laboratory for Foraminiferal Research.</em> 4(2): 31-55., available online at https://cushmanfoundation.allenpress.com/Portals/_default/files/pubarchive/cclfr/4cclfr2.pdf
page(s): p. 53 [details] Available for editors  [request]
Diagnosis Test enrolled, planispiral, and involute, commonly three rapidly enlarging chambers per whorl, triangular septal...
Diagnosis Test enrolled, planispiral, and involute, commonly three rapidly enlarging chambers per whorl, triangular septal chamberlets formed by septa} lamellae or partitions as in Bradyina; wall calcareous, granular, with outer tectum and inner part alveolar to keriothecal and perforate; aperture basal in the early stage, later areal and multiple with a few horizontal slits, and finally consisting of elongate slits up the apertural face as well as horizontal slits at the position of the internal septal lamellae or partitions, sutural openings as in Bradyina but much larger vertical slits perpendicular to the septa. U. Carboniferous (Westphalian to Stephanian) to Permian; USA: Oklahoma, Colorado, Texas; USSR: Russian Platform, Urals, central Asia; Egypt. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2025). World Foraminifera Database. Glyphostomella Cushman & Waters, 1928 †. Accessed at: https://www.marinespecies.org/Foraminifera/aphia.php?p=taxdetails&id=721392 on 2025-05-19
Date action by
original description
Cushman, J. A.; Waters, J. A. (1928). Some Foraminifera from the Pennsylvanian and Permian of Texas. <em>Contributions from the Cushman Laboratory for Foraminiferal Research.</em> 4(2): 31-55., available online at https://cushmanfoundation.allenpress.com/Portals/_default/files/pubarchive/cclfr/4cclfr2.pdf
page(s): p. 53 [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]From editor or global species database
Diagnosis Test enrolled, planispiral, and involute, commonly three rapidly enlarging chambers per whorl, triangular septal chamberlets formed by septa} lamellae or partitions as in Bradyina; wall calcareous, granular, with outer tectum and inner part alveolar to keriothecal and perforate; aperture basal in the early stage, later areal and multiple with a few horizontal slits, and finally consisting of elongate slits up the apertural face as well as horizontal slits at the position of the internal septal lamellae or partitions, sutural openings as in Bradyina but much larger vertical slits perpendicular to the septa. U. Carboniferous (Westphalian to Stephanian) to Permian; USA: Oklahoma, Colorado, Texas; USSR: Russian Platform, Urals, central Asia; Egypt. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]
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