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Foraminifera taxon detailsPfenderina Henson, 1948 †
 739316 (urn:lsid:marinespecies.org:taxname:739316)
accepted
Genus
Eorupertia neocomiensis Pfender, 1938 † accepted as Pfenderina neocomiensis (Pfender, 1938) † (type by original designation)
marine,
fossil only
feminine
Henson, F. R. S. (1948). New Trochamminidæ and Verneuilinidæ from the Middle East. <em>Journal of Natural History Series 11.</em> 14(117)[1947]: 605-630., available online at https://doi.org/10.1080/00222934708654671
page(s): p. 609 [details] Available for editors  [request]
Diagnosis Test a high trochospiral, chambers numerous, surrounding an axial region of thickened shell material, septa perpendicular...
Diagnosis Test a high trochospiral, chambers numerous, surrounding an axial region of thickened shell material, septa perpendicular to the spiral axis, and oblique to the test axis; wall microgranular in structure, imperforate; aperture consisting of numerous pores in the center of the apertural face, with secondary intercameral foramina about equidistant from the ends of the chambers, appearing along the central solid column as a spiral groove or subcameral tunnel. U. Jurassic to U. Cretaceous (Cenomanian); Europe; SW Asia. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2025). World Foraminifera Database. Pfenderina Henson, 1948 †. Accessed at: https://www.marinespecies.org/foraminifera/aphia.php?p=taxdetails&id=739316 on 2025-05-22
Date action by
original description
Henson, F. R. S. (1948). New Trochamminidæ and Verneuilinidæ from the Middle East. <em>Journal of Natural History Series 11.</em> 14(117)[1947]: 605-630., available online at https://doi.org/10.1080/00222934708654671
page(s): p. 609 [details] Available for editors [request]From editor or global species database
Diagnosis Test a high trochospiral, chambers numerous, surrounding an axial region of thickened shell material, septa perpendicular to the spiral axis, and oblique to the test axis; wall microgranular in structure, imperforate; aperture consisting of numerous pores in the center of the apertural face, with secondary intercameral foramina about equidistant from the ends of the chambers, appearing along the central solid column as a spiral groove or subcameral tunnel. U. Jurassic to U. Cretaceous (Cenomanian); Europe; SW Asia. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]
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