Foraminifera taxon details
Rectoglomus Malakhova, 1980 †
1301225 (urn:lsid:marinespecies.org:taxname:1301225)
accepted
Genus
Rectoglomus iriclinsis Malakhova, 1980 † (type by original designation)
marine, brackish, fresh, terrestrial
fossil only
masculine
Malakhova, N. P. (1980). Комплекс мелких фораминифер среднего карбона юго-восточного Урала - A complex of smaller foraminifers of the Middle Carboniferous of southeastern Urals. <em>Preprint, Akademiya Nauk SSSR, Uralskii Nauchnyi Tsentr, Trudy Instituta Geologii i Geokhimii.</em> 1-54., available online at http://books.google.com/books/about?id=ER9xDwAAQBAJ
page(s): p. 14 [details] Available for editors
[request]
page(s): p. 14 [details] Available for editors
[request]
Original description Диагноз. Раковина прикрепленная, трубчатая. Начальная часть трубки...
Original description Диагноз. Раковина прикрепленная, трубчатая. Начальная часть трубки навивается компактно, клубкообразно, последующие обороты навиты на субстрате в одном направлении. Стенка тонкозернистая, толщина ее медленно возрастает от начальных оборотов к последнему.
Место нахождение и возраст. Восточный склон Южноrо Урала, р. Ташла; средний карбон.
(Malakhova (1980)).
Diagnosis. The shell is attached and tubular. The initial part of the tube is coiled compactly, like a ball, with subsequent whorls coiled on the substrate in a single direction. The wall is fine-grained, its thickness slowly increasing from the initial whorls to the final ones.
Location and age. Eastern slope of the Southern Urals, Tashla River; Middle Carboniferous. [details]
Место нахождение и возраст. Восточный склон Южноrо Урала, р. Ташла; средний карбон.
(Malakhova (1980)).
Diagnosis. The shell is attached and tubular. The initial part of the tube is coiled compactly, like a ball, with subsequent whorls coiled on the substrate in a single direction. The wall is fine-grained, its thickness slowly increasing from the initial whorls to the final ones.
Location and age. Eastern slope of the Southern Urals, Tashla River; Middle Carboniferous. [details]
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2025). World Foraminifera Database. Rectoglomus Malakhova, 1980 †. Accessed at: https://www.marinespecies.org/foraminifera/aphia.php?p=taxdetails&id=1301225 on 2026-06-01
Date
action
by
original description
Malakhova, N. P. (1980). Комплекс мелких фораминифер среднего карбона юго-восточного Урала - A complex of smaller foraminifers of the Middle Carboniferous of southeastern Urals. <em>Preprint, Akademiya Nauk SSSR, Uralskii Nauchnyi Tsentr, Trudy Instituta Geologii i Geokhimii.</em> 1-54., available online at http://books.google.com/books/about?id=ER9xDwAAQBAJ
page(s): p. 14 [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
note: ?Calcivertellidae. [details] Available for editors [request]
page(s): p. 14 [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
note: ?Calcivertellidae. [details] Available for editors
[request]From editor or global species database
Original description Диагноз. Раковина прикрепленная, трубчатая. Начальная часть трубки навивается компактно, клубкообразно, последующие обороты навиты на субстрате в одном направлении. Стенка тонкозернистая, толщина ее медленно возрастает от начальных оборотов к последнему.Место нахождение и возраст. Восточный склон Южноrо Урала, р. Ташла; средний карбон.
(Malakhova (1980)).
Diagnosis. The shell is attached and tubular. The initial part of the tube is coiled compactly, like a ball, with subsequent whorls coiled on the substrate in a single direction. The wall is fine-grained, its thickness slowly increasing from the initial whorls to the final ones.
Location and age. Eastern slope of the Southern Urals, Tashla River; Middle Carboniferous. [details]
From editor or global species database
Image from typetaxon