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Foraminifera taxon detailsBaituganella Lipina, 1955 †
 721348 (urn:lsid:marinespecies.org:taxname:721348)
accepted
Genus
Baituganella chernyshinensis Lipina, 1955 † (type by original designation)
marine,
fossil only
feminine
Lipina, O. A. (1955). Фораминиферы турнейского яруса и верхней части девона Волго-Уральской области и западного склона среднего Урала - The foraminifera of the Tournaisian stage and the upper part of the Devonian of the Volga-Ural region and the western slope of the middle Urals. <em>Труды ИГН Ан СССР - Reports Geological Institute Academy of sciences USSR.</em> 163(70): 1-96., available online at https://books.google.pt/books/about?id=nulPDwAAQBAJ
page(s): p. 19 [details] Available for editors  [request]
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2024). World Foraminifera Database. Baituganella Lipina, 1955 †. Accessed at: https://www.marinespecies.org/foraminifera/aphia.php?p=taxdetails&id=721348 on 2024-07-13
Date action by
original description
Lipina, O. A. (1955). Фораминиферы турнейского яруса и верхней части девона Волго-Уральской области и западного склона среднего Урала - The foraminifera of the Tournaisian stage and the upper part of the Devonian of the Volga-Ural region and the western slope of the middle Urals. <em>Труды ИГН Ан СССР - Reports Geological Institute Academy of sciences USSR.</em> 163(70): 1-96., available online at https://books.google.pt/books/about?id=nulPDwAAQBAJ
page(s): p. 19 [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 irregular in form, with proloculus followed by irregularly tubular chamber that appears to coil about the proloculus in the early stage, partially subdivided by incipient septa that project inward from the wall at irregular intervals but do not completely cross the chamber lumen; wall calcareous, microgranular, reported to have some included agglutinated particles; aperture not seen in the sections observed, probably at the end of the tubular chamber. L. Carboniferous (Tournaisian); USSR. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]
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