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Foraminifera taxon detailsVerbeekina Staff, 1909 †
 721883 (urn:lsid:marinespecies.org:taxname:721883)
accepted
Genus
Fusulina verbeeki Geinitz, 1876 † accepted as Schwagerina verbeeki (Geinitz, 1876) † accepted as Verbeekina verbeeki (Geinitz, 1876) † (type by original designation)
Doliolina (Verbeekina) Ozawa, 1925 † · unaccepted (Opinion of Loeblich & Tappan,...)
Opinion of Loeblich & Tappan, 1987 Nomen translatum Neoverbeekina Zhang & Dong in Xiao et al., 1986 † · unaccepted > junior subjective synonym (Subjective junior synonym Opinion...)
Subjective junior synonym Opinion of Rauzer-Chernousova et al. (1996), Vachard (2022) pers. comm. Schwagerina (Verbeekina) Staff, 1909 † · unaccepted (Opinion of Loeblich & Tappan,...)
Opinion of Loeblich & Tappan, 1987 Nomen translatum Verbeekina (Paraverbeekina) F.Kahler & G. Kahler, 1966 † · unaccepted (Opinion of Loeblich & Tappan,...)
Opinion of Loeblich & Tappan, 1987 Nomen translatum
marine,
fossil only
feminine
Staff, H. von. (1909). Beiträge zur Kenntnis der Fusuliniden. <em>Neues Jahrbuch für Mineralogie, Geologie und Paläontologie, Beilage-Band.</em> 27: 461–508.
page(s): p. 68 footnote 506 [details] (of Schwagerina (Verbeekina) Staff, 1909 †) Staff, H. von. (1909). Beiträge zur Kenntnis der Fusuliniden. <em>Neues Jahrbuch für Mineralogie, Geologie und Paläontologie, Beilage-Band.</em> 27: 461–508. page(s): p. 468, 476 [details]
Diagnosis Test subspherical, up to about 14 mm in length, tiny proloculus followed by irregularly coiled or endothyroid juvenarium,...
Diagnosis Test subspherical, up to about 14 mm in length, tiny proloculus followed by irregularly coiled or endothyroid juvenarium, succeeding whorl of sharply increased diameter, then with up to twenty slowly enlarging planispiral whorls, septa formed by downward deflection of the tectum and keriotheca, angled forward, unfluted; wall of tectum and thin, extremely fine alveolar keriotheca, inner and outer surfaces of the wall and both sides of the septa may be coated with dense calcite resembling parachomata in structure, and the more extensive coatings at the poles may nearly fill the chambers, parachomata absent or rudimentary in early whorls but well developed between the foramina of the outer whorls, project forward from the septa, and may join those of the succeeding chamber and form nearly continuous ridges for a short distance, no tunnel, numerous elliptical basal foramina, as many as a hundred in later whorls. M. Permian (U. Artinskian) to U. Permian (L. Tatarian); Sumatra; Viet Nam; Java; China; Japan; Turkey; Yugoslavia; Greece; Sicily; Afghanistan; USSR: Turkestan, Crimea, Caucasus, Pamir; USA: Washington. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2025). World Foraminifera Database. Verbeekina Staff, 1909 †. Accessed at: https://marinespecies.org/foraminifera/aphia.php?p=taxdetails&id=721883 on 2025-05-19
Date action by
original description
Staff, H. von. (1909). Beiträge zur Kenntnis der Fusuliniden. <em>Neues Jahrbuch für Mineralogie, Geologie und Paläontologie, Beilage-Band.</em> 27: 461–508.
page(s): p. 68 footnote 506 [details] original description (of Verbeekina (Paraverbeekina) F.Kahler & G. Kahler, 1966 †) Kahler, F.; Kahler, G. (1966). Fusulinida (Foraminiferida): Teil 1. <em>Fossilium Catalogus: I: Animalia.</em> 111: 1-254. page(s): p. 72 [details] Available for editors  [request]original description (of Schwagerina (Verbeekina) Staff, 1909 †) Staff, H. von. (1909). Beiträge zur Kenntnis der Fusuliniden. <em>Neues Jahrbuch für Mineralogie, Geologie und Paläontologie, Beilage-Band.</em> 27: 461–508. page(s): p. 468, 476 [details] original description (of Doliolina (Verbeekina) Ozawa, 1925 †) Ozawa, Y. (1925). Paleontological and Stratigraphical Studies on the Permo-Carboniferous Limestone of Nagato. Part 2. Paleontology. <em>Journal of the College of Science, Imperial University of Tokyo.</em> 45 (art. 6): 1-90., available online at http://hdl.handle.net/2261/32945 [details] Available for editors [request]original description (of Neoverbeekina Zhang & Dong in Xiao et al., 1986 †) Xiao, W.; Wang, H.; Zhang, L.; Dong, W. L. (1986). 贵州南部早二叠世地层及其生物群 - Early Permian stratigraphy and fauna in southern Guizhou. <em>贵阳 : 贵州人民出版社 - Guiyang: The People's Publishing House of Guizhou.</em> 1-364. page(s): p. 142 [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 subspherical, up to about 14 mm in length, tiny proloculus followed by irregularly coiled or endothyroid juvenarium, succeeding whorl of sharply increased diameter, then with up to twenty slowly enlarging planispiral whorls, septa formed by downward deflection of the tectum and keriotheca, angled forward, unfluted; wall of tectum and thin, extremely fine alveolar keriotheca, inner and outer surfaces of the wall and both sides of the septa may be coated with dense calcite resembling parachomata in structure, and the more extensive coatings at the poles may nearly fill the chambers, parachomata absent or rudimentary in early whorls but well developed between the foramina of the outer whorls, project forward from the septa, and may join those of the succeeding chamber and form nearly continuous ridges for a short distance, no tunnel, numerous elliptical basal foramina, as many as a hundred in later whorls. M. Permian (U. Artinskian) to U. Permian (L. Tatarian); Sumatra; Viet Nam; Java; China; Japan; Turkey; Yugoslavia; Greece; Sicily; Afghanistan; USSR: Turkestan, Crimea, Caucasus, Pamir; USA: Washington. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]
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