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Foraminifera taxon detailsCushmanella Palmer & Bermúdez, 1936
 415259 (urn:lsid:marinespecies.org:taxname:415259)
accepted
Genus
Nonionina brownii d'Orbigny, 1839 accepted as Cushmanella brownii (d'Orbigny, 1839) (type by original designation)
marine,
Palmer, D. K.; Bermúdez, P. J. (1936). Late Tertiary foraminifera from the Matanzas Bay region, Cuba. <em>Memorias de la Sociedad. Cubana de Historia Natural ''Felipe Poey".</em> v. 9, p. 237–257., available online at http://www.redciencia.cu/geobiblio/paper/1936_PJBermudez__Late%20terc%20foram%20matanzas%20Cuba.pdf
page(s): pp. 252-253 [details] Available for editors  [request]
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2021). World Foraminifera Database. Cushmanella Palmer & Bermúdez, 1936. Accessed at: http://marinespecies.org/foraminifera/aphia.php?p=taxdetails&id=415259 on 2024-07-12
Date action by 2009-09-23 14:01:30Z created db_admin
original description
Palmer, D. K.; Bermúdez, P. J. (1936). Late Tertiary foraminifera from the Matanzas Bay region, Cuba. <em>Memorias de la Sociedad. Cubana de Historia Natural ''Felipe Poey".</em> v. 9, p. 237–257., available online at http://www.redciencia.cu/geobiblio/paper/1936_PJBermudez__Late%20terc%20foram%20matanzas%20Cuba.pdf
page(s): pp. 252-253 [details] Available for editors [request] 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 [request] From editor or global species database
Diagnosis Test nearly planispiral, involute, somewhat compressed, rapidly enlarging chambers result in an auriculate outline, one or more small supplementary chambers at the umbilical end of each chamber on both sides of the test, tubular internal partition attached to the inside wall at the upper and lateral margins of the areal aperture, free edges of the partition infolded at each side of the lower rim of the aperture, with branches from the tubular partition opening at the lateral accessory aperture, external sutures gently curved, depressed; wall calcareous, finely perforate except for a clear oval imperforate equatorial area just above the aperture on the apertural face; aperture consists of an areal slit and an interiomarginal equatorial opening, with supplementary sutural slitlike openings on both sides of test opening into the supplementary chambers. Holocene; Caribbean. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]
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