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Foraminifera taxon detailsGlomalveolina Hottinger, 1960 †
 721285 (urn:lsid:marinespecies.org:taxname:721285)
accepted
Genus
Alveolina dachelensis Schwager, 1883 † accepted as Glomalveolina dachelensis (Schwager, 1883) † (type by original designation)
Alveolina (Glomalveolina) Hottinger, 1960 † · unaccepted (Opinion of Loeblich & Tappan,...)
Opinion of Loeblich & Tappan, 1987 Nomen translatum Fasciolites (Glomalveolina) Reichel in Loeblich & Tappan, 1964 † · unaccepted (Opinion of Loeblich & Tappan,...)
Opinion of Loeblich & Tappan, 1987 Nomen translatum
marine,
fossil only
feminine
(of Alveolina (Glomalveolina) Hottinger, 1960 †) Hottinger, L. (1960). Recherches sur les Alvéolines du Paléocène et de l'Éocène. <em>Mémoires Suisses de Paléontologie.</em> 75-76: 1-243.
page(s): pp. 44, 54; note: The date of publication is said to be 1962 in Loeblich and Tappan (1987). 1962 is never used neither for Alveolina (Glomalveolina) nor for the species described then by Hottinger in any further public... The date of publication is said to be 1962 in Loeblich and Tappan (1987). 1962 is never used neither for Alveolina (Glomalveolina) nor for the species described then by Hottinger in any further publication.
 [request]
Diagnosis Test small, globular to slightly ovate, dimorphism evident only in the juvenile, both generations with tiny proloculus...
Diagnosis Test small, globular to slightly ovate, dimorphism evident only in the juvenile, both generations with tiny proloculus followed by early streptospiral coiling, adult planispiral, numerous septula resulting in small chamberlets that alternate in position in successive chambers; wall and septula are thicker in the geologically older middle Paleocene species, but thinner with more reduced chamber lumina in upper Paleocene and Eocene species, thickness of basal layer about half the height of the whorl, not flosculinized; aperture multiple, a row of openings at the base of the apertural face, with smaller openings intercalated between these. M. Paleocene to M. Eocene; France; Spain; Italy; Greece; Libya; Egypt; Somalia; Turkey; Syria; Pakistan. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2025). World Foraminifera Database. Glomalveolina Hottinger, 1960 †. Accessed at: https://www.marinespecies.org/foraminifera/aphia.php?p=taxdetails&id=721285 on 2025-05-28
Date action by
original description
(of Alveolina (Glomalveolina) Hottinger, 1960 †) Hottinger, L. (1960). Recherches sur les Alvéolines du Paléocène et de l'Éocène. <em>Mémoires Suisses de Paléontologie.</em> 75-76: 1-243.
page(s): pp. 44, 54; note: The date of publication is said to be 1962 in Loeblich and Tappan (1987). 1962 is never used neither for Alveolina (Glomalveolina) nor for the species described then by Hottinger in any further public... The date of publication is said to be 1962 in Loeblich and Tappan (1987). 1962 is never used neither for Alveolina (Glomalveolina) nor for the species described then by Hottinger in any further publication.
[request]original description (of Fasciolites (Glomalveolina) Reichel in Loeblich & Tappan, 1964 †) Loeblich, A. R.; Tappan, H. (1964). Treatise on Invertebrate Paleontology, Part C: Protista 2, Sarcodina, chiefly "Thecamoebians" and Foraminiferida. <em>Geological Society of America and University of Kansas Press, Lawrence.</em> page(s): C509 [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, globular to slightly ovate, dimorphism evident only in the juvenile, both generations with tiny proloculus followed by early streptospiral coiling, adult planispiral, numerous septula resulting in small chamberlets that alternate in position in successive chambers; wall and septula are thicker in the geologically older middle Paleocene species, but thinner with more reduced chamber lumina in upper Paleocene and Eocene species, thickness of basal layer about half the height of the whorl, not flosculinized; aperture multiple, a row of openings at the base of the apertural face, with smaller openings intercalated between these. M. Paleocene to M. Eocene; France; Spain; Italy; Greece; Libya; Egypt; Somalia; Turkey; Syria; Pakistan. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]
From editor or global species database
Image from typetaxon
Image from typetaxon
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