| Intro | | About | | Wiki | | Search traits | | Data explorer | | Literature | | Definitions | | Sources | | Webservices | | Statistics | | Feedback | | Editors | | Log in |
Foraminifera taxon detailsQuasilituotuba Brazhnikova, 1983 †
 721340 (urn:lsid:marinespecies.org:taxname:721340)
accepted
Genus
Quasilituotuba subplana Brazhnikova, 1983 † (type by original designation)
marine,
fossil only
feminine
Brazhnikova, N. E.; Vdovenko, M. V. (1983). фораминиферы - Foraminifera. In Aizenverg, D.E.; Astakhova, T.V.et al.: Верхнесерпуховский подъярус Донецкого бассейна - The Upper Serpukhovian substage in the Donets basin. <em>Киев: Наукова думка - Kiev, Naukova Dumka.</em> 42-67.
page(s): p. 45 [details] Available for editors  [request]
Diagnosis Proloculus followed by tubular second chamber that is planispirally or slightly streptospirally enrolled, becoming uncoiled...
Diagnosis Proloculus followed by tubular second chamber that is planispirally or slightly streptospirally enrolled, becoming uncoiled and straight in the final stage, may occasionally show some constrictions due to periodic growth or possible rudimentary septation; wall calcareous, microgranular; aperture at the open end of the tube. L. Carboniferous (Serpukhovian substage); USSR: Donets Basin. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2025). World Foraminifera Database. Quasilituotuba Brazhnikova, 1983 †. Accessed at: https://www.marinespecies.org/Foraminifera/aphia.php?p=taxdetails&id=721340 on 2025-05-19
Date action by
original description
Brazhnikova, N. E.; Vdovenko, M. V. (1983). фораминиферы - Foraminifera. In Aizenverg, D.E.; Astakhova, T.V.et al.: Верхнесерпуховский подъярус Донецкого бассейна - The Upper Serpukhovian substage in the Donets basin. <em>Киев: Наукова думка - Kiev, Naukova Dumka.</em> 42-67.
page(s): p. 45 [details] Available for editors [request]taxonomy source Vachard, D.; Krainer, K. (2022). Calcareous algae and foraminifers across the Permian-Triassic boundary interval (uppermost Bellerophon Formation and basal Werfen Formation) in the Dolomites (South Tyrol – Trentino, Italy). <em>Palaeontographica Abteilung A.</em> 324(1-6): 1-173., available online at https://doi.org/10.1127/pala/2022/0128 [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 Proloculus followed by tubular second chamber that is planispirally or slightly streptospirally enrolled, becoming uncoiled and straight in the final stage, may occasionally show some constrictions due to periodic growth or possible rudimentary septation; wall calcareous, microgranular; aperture at the open end of the tube. L. Carboniferous (Serpukhovian substage); USSR: Donets Basin. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]
|
