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Foraminifera taxon detailsPraerhapydionina van Wessem, 1943 †
 722031 (urn:lsid:marinespecies.org:taxname:722031)
accepted
Genus
Praerhapydionina cubana van Wessem, 1943 † (type by original designation)
marine,
fossil only
feminine
Wessem, A. van. (1943). Geology and Paleontology of Central Camaguey, Cuba. <em>Utrecht Rijks-Universiteit, Geographische en Geologische Mededelingen, Physiographisch-Geologische Reeks.</em> 2(5): 1-91.
page(s): p. 43 [details]
Diagnosis Test elongate, subconical, up to about 1 mm in length, circular in section, early stage planispirally enrolled, later...
Diagnosis Test elongate, subconical, up to about 1 mm in length, circular in section, early stage planispirally enrolled, later uncoiled and rectilinear, chambers low and arched centrally, interior subdivided by a few inward projecting radial septula; wall calcareous, porcelaneous; aperture:; terminal, central. Eocene (Lutetian) to Oligocene; Cuba; Iraq; Iran; Spain. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2025). World Foraminifera Database. Praerhapydionina van Wessem, 1943 †. Accessed at: https://www.marinespecies.org/Foraminifera/aphia.php?p=taxdetails&id=722031 on 2025-05-22
Date action by
original description
Wessem, A. van. (1943). Geology and Paleontology of Central Camaguey, Cuba. <em>Utrecht Rijks-Universiteit, Geographische en Geologische Mededelingen, Physiographisch-Geologische Reeks.</em> 2(5): 1-91.
page(s): p. 43 [details] 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 page(s): p. 377 pl. 409 fig. 5-13; note: Rather of Eocene in age than Upper Cretaceous as originally reported. [details] Available for editors  [request]From editor or global species database
Diagnosis Test elongate, subconical, up to about 1 mm in length, circular in section, early stage planispirally enrolled, later uncoiled and rectilinear, chambers low and arched centrally, interior subdivided by a few inward projecting radial septula; wall calcareous, porcelaneous; aperture:; terminal, central. Eocene (Lutetian) to Oligocene; Cuba; Iraq; Iran; Spain. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]
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