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Foraminifera taxon detailsEscornebovina Butt, 1966 †
 722332 (urn:lsid:marinespecies.org:taxname:722332)
accepted
Genus
Rotalia cuvillieri Poignant, 1965 † accepted as Escornebovina cuvillieri (Poignant, 1965) † (type by original designation)
Falsipatellina D. Haman & Huddleston, 1981 † · unaccepted (Subjective junior synonym in...)
Subjective junior synonym in opinion of Loeblich and Tappan (1987) Pseudopatellina Kenawy & Nyírő, 1967 † · unaccepted (junior homonym of Pseudopatellina...)
junior homonym of Pseudopatellina Haque, 1960
marine,
fossil only
feminine
Butt, A. A. (1966). Late Oligocene Foraminifera from Escornebeou, SW France. <em>Utrecht: Schotanus & Jens.</em> 1-124.
page(s): p. 56 [details]
Diagnosis Test small, about 0.3 mm to 0.4 mm in diameter, low trochospiral coil, planoconvex, spiral side evolute, gently convex,...
Diagnosis Test small, about 0.3 mm to 0.4 mm in diameter, low trochospiral coil, planoconvex, spiral side evolute, gently convex, about three and a half to four very slowly enlarging whorls of numerous narrow chambers, about twelve to twenty-six in the final whorl, chambers distinctly inflated at their base against the previous suture and erroneously appearing to represent limbate sutures, whereas the true sutures are straight, radia1, and depressed, umbilical side flat to slightly excavated centrally, sutures straight and radial toward the umbilicus but curve proximally at the periphery, broad umbilicus occupying about one-third of the test diameter and filled with a solid central plug or button of shell material, periphery angular; wall calcareous, optically granular, no perforations visible on the spiral side at magnifications up to X 20,000, surface appearing leathery at x 5,000; aperture a narrow interiomarginal slit extending from near the periphery toward the umbilicus, with small pustules on the lower apertural face and area below the aperture. M. Oligocene (Stampian) to M. Miocene (Vindobonian); France; Spain; Italy; Germany; Hungary. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2024). World Foraminifera Database. Escornebovina Butt, 1966 †. Accessed at: https://www.marinespecies.org/foraminifera/aphia.php?p=taxdetails&id=722332 on 2024-10-14
Date action by
original description
Butt, A. A. (1966). Late Oligocene Foraminifera from Escornebeou, SW France. <em>Utrecht: Schotanus & Jens.</em> 1-124.
page(s): p. 56 [details] original description (of Pseudopatellina Kenawy & Nyírő, 1967 †) Kenawy, A. I.; Nyírő, R. M. (1967). Zwei neue Foraminiferen aus dem Oberoligozan in Eger (Nordungarn). <em>Annales Historico Naturales Musei Nationalis Hungarici.</em> 59: 103-107., available online at http://publication.nhmus.hu/pdf/annHNHM/Annals_HNHM_1967_Vol_59_103.pdf page(s): p. 104 [details] Available for editors  [request] original description (of Falsipatellina D. Haman & Huddleston, 1981 †) Haman, D.; Huddleston, R. (1981). Falsipatellina, a new name for Pseudopatellina Kenawy and Nyiro, non Haque (Foraminiferida). <em>Proceedings of The Biological Society of Washington.</em> 94: 378-379., available online at https://biostor.org/reference/82301 page(s): p. 378 [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 small, about 0.3 mm to 0.4 mm in diameter, low trochospiral coil, planoconvex, spiral side evolute, gently convex, about three and a half to four very slowly enlarging whorls of numerous narrow chambers, about twelve to twenty-six in the final whorl, chambers distinctly inflated at their base against the previous suture and erroneously appearing to represent limbate sutures, whereas the true sutures are straight, radia1, and depressed, umbilical side flat to slightly excavated centrally, sutures straight and radial toward the umbilicus but curve proximally at the periphery, broad umbilicus occupying about one-third of the test diameter and filled with a solid central plug or button of shell material, periphery angular; wall calcareous, optically granular, no perforations visible on the spiral side at magnifications up to X 20,000, surface appearing leathery at x 5,000; aperture a narrow interiomarginal slit extending from near the periphery toward the umbilicus, with small pustules on the lower apertural face and area below the aperture. M. Oligocene (Stampian) to M. Miocene (Vindobonian); France; Spain; Italy; Germany; Hungary. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]
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