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WoRMS taxon detailsLaterostomella de Klasz & Rérat, 1962
526513 (urn:lsid:marinespecies.org:taxname:526513)
accepted
Genus
Laterostomella guembeliniformis de Klasz & Rérat, 1962 † (type by original designation)
Pseudoheterohelix Aliyulla, 1977 · unaccepted (Opinion of Loeblich & Tappan, 1987)
marine,
recent + fossil
feminine
Klasz, I. de; Rérat, D. (1962). Quelques nouveaux foraminifères du Crétacé et du Tertiaire du Gabon (Afrique Équatoriale). <em>Revue de Micropaléontologie.</em> 4: 175-189.
page(s): p. 177 [details]
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2025). World Foraminifera Database. Laterostomella de Klasz & Rérat, 1962. Accessed through: World Register of Marine Species at: https://www.marinespecies.org/aphia.php?p=taxdetails&id=526513 on 2025-05-14
Date action by
Nomenclatureoriginal description
Klasz, I. de; Rérat, D. (1962). Quelques nouveaux foraminifères du Crétacé et du Tertiaire du Gabon (Afrique Équatoriale). <em>Revue de Micropaléontologie.</em> 4: 175-189.
page(s): p. 177 [details] original description (of Pseudoheterohelix Aliyulla, 1977) Aliyulla, Kh. (1977). Верхний мел и развитие фораминифер Малого Кавказа (Азербайджан) - Upper Cretaceous and development of foraminifera of the Lesser Caucasus (Azerbaijan). <em>Баку - Baku.</em> 1-237., available online at http://www.geokniga.org/books/13422 page(s): p. 205 [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 elongate, tapering, chambers inflated, biserial, sutures depressed, slightly oblique; wall calcareous, finely perforate, although pores may become enlarged by dissolution, surface commonly granulate, pustulate, or finely cancellate, pustules of earlier chambers may fuse into longitudinal ridges; aperture a slightly eccentric high arch at the base of the last chamber, rarely with a lower and more symmetrical aperture that may divide into two openings, collarlike apertural border has one margin turned inward as an internal plate that connects with the proximal margin of the collar of the previous aperture. ?Paleocene, U. Eocene to Holocene; Pacific Ocean; USSR: Caucasus; Indian Ocean; Red Sea; Atlantic Ocean; Gabon; Sierra Leone; Gulf of Mexico; Cuba. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]
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