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Foraminifera taxon detailsLantschichites Tumanskaya, 1953 †
 721777 (urn:lsid:marinespecies.org:taxname:721777)
accepted
Genus
Codonofusiella (Lantschichites) maslennikovi Tumanskaya, 1953 † accepted as Lantschichites maslennikovi (Tumanskaya, 1953) † (type by original designation)
Codonofusiella (Lantschichites) Tumanskaya, 1953 † · unaccepted (Opinion of Rauzer-Chernousova and...)
Opinion of Rauzer-Chernousova and Rozovskaya (1955) nomen translatum Paraboultonia Skinner & Wilde, 1954 † · unaccepted (Subjective junior synonym in...)
Subjective junior synonym in opinion of Loeblich & Tappan, 1987
marine,
fossil only
masculine
(of Codonofusiella (Lantschichites) Tumanskaya, 1953 †) Tumanskaya, O. G. (1953). О верхнепермских фузулинидах Южно-Уссурийского края - About the Upper Permian fusulinids from the South Ussuri region. <em>Труды Всесоюзного научно-исследовательского геологического института (ВСЕГЕИ) - Proceedings of the All-Union Scientific Research Geological Institute (VSEGEI).</em> 1-56., available online at https://books.google.fr/books?id=ddipDwAAQBAJ
page(s): p. 20 [details]
Diagnosis Test elongate, fusiform to cylindrical, poles bluntly rounded, inner whorls with short axis of coiling, later with changed...
Diagnosis Test elongate, fusiform to cylindrical, poles bluntly rounded, inner whorls with short axis of coiling, later with changed coiling axis at a high angle to the earlier one, elongate and fusiform, final stage may enlarge rapidly, flaring and tending to become rectilinear, septa thin, strongly fluted, with cuniculi developed at the base of the septa in the outer whorls; wall thin, with tectum and diaphanotheca, chomata in first two volutions, tunnel low and erratic, disappearing in the later whorls where cuniculi are present; septal pores abundant in later whorls. M. Permian (Kungurian); USA: Texas; USSR. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2025). World Foraminifera Database. Lantschichites Tumanskaya, 1953 †. Accessed at: https://marinespecies.org/foraminifera/aphia.php?p=taxdetails&id=721777 on 2025-05-21
Date action by
original description
(of Codonofusiella (Lantschichites) Tumanskaya, 1953 †) Tumanskaya, O. G. (1953). О верхнепермских фузулинидах Южно-Уссурийского края - About the Upper Permian fusulinids from the South Ussuri region. <em>Труды Всесоюзного научно-исследовательского геологического института (ВСЕГЕИ) - Proceedings of the All-Union Scientific Research Geological Institute (VSEGEI).</em> 1-56., available online at https://books.google.fr/books?id=ddipDwAAQBAJ
page(s): p. 20 [details] original description (of Paraboultonia Skinner & Wilde, 1954 †) Skinner, J. W.; Wilde, G. L. (1954). The fusulinid subfamily Boultoniinae. <em>Journal of Paleontology.</em> 28(4): 434-444. page(s): p. 441 [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, fusiform to cylindrical, poles bluntly rounded, inner whorls with short axis of coiling, later with changed coiling axis at a high angle to the earlier one, elongate and fusiform, final stage may enlarge rapidly, flaring and tending to become rectilinear, septa thin, strongly fluted, with cuniculi developed at the base of the septa in the outer whorls; wall thin, with tectum and diaphanotheca, chomata in first two volutions, tunnel low and erratic, disappearing in the later whorls where cuniculi are present; septal pores abundant in later whorls. M. Permian (Kungurian); USA: Texas; USSR. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]
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