WoRMS taxon details
Staffelloidea Miklukho-Maklay, 1949 nom. transl. Solovieva, 1978 †
marine, fresh, terrestrial
fossil only
Miklukho-Maklay, A. D. (1949). Верхнепалеозойские фузулиниды Средней Азии - Upper Paleozoic fusulinids from Central Asia. <em>Leningrad.</em> 3-127., available online at http://paleostratmuseum.ru/files/Mikluho1949.pdf
page(s): p. 46; note: As Staffelininae (subfamily) nom. imperfectum. [details] Available for editors
[request]
Solovieva, M. N. (1978). K sisteme foraminifer (interpretatsiya biologicheskogo znacheniya osobennostey strukturnoy i prostranstvennoy organizatsii foraminifer) - On the systematics of the foraminifera (interpretation of the biological significance of structural features and spatial organization of the foraminifera). <em>Byulletin' Moskovskoe Obshchestva Ispytateley Prirody. Otdelenie Geologicheskii.</em> 53(5): 159-160. [details]
page(s): p. 46; note: As Staffelininae (subfamily) nom. imperfectum. [details] Available for editors
[request]Solovieva, M. N. (1978). K sisteme foraminifer (interpretatsiya biologicheskogo znacheniya osobennostey strukturnoy i prostranstvennoy organizatsii foraminifer) - On the systematics of the foraminifera (interpretation of the biological significance of structural features and spatial organization of the foraminifera). <em>Byulletin' Moskovskoe Obshchestva Ispytateley Prirody. Otdelenie Geologicheskii.</em> 53(5): 159-160. [details]
Description Tests planispiral, involute, lenticular or spherical, very rarely subfusiform or uncoiled. The septa remain planar during...
Description Tests planispiral, involute, lenticular or spherical, very rarely subfusiform or uncoiled. The septa remain planar during all the history of the suborder (in contrast to the other suborder, Fusulinina). Chomata are often present but poorly developed. Some structures confused with parachomata are occasionally described. Wall calcareous secreted, probably initially dark aragonitic (probably fibrous and finely perforated), then neomicrosparitized from aragonite. Aperture simple terminal basal.
(Vachard and Le Coze (2024)). [details]
(Vachard and Le Coze (2024)). [details]
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2025). World Foraminifera Database. Staffelloidea Miklukho-Maklay, 1949 nom. transl. Solovieva, 1978 †. Accessed through: World Register of Marine Species at: https://www.marinespecies.org/aphia.php?p=taxdetails&id=1058814 on 2025-05-06
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Nomenclature
original description
Miklukho-Maklay, A. D. (1949). Верхнепалеозойские фузулиниды Средней Азии - Upper Paleozoic fusulinids from Central Asia. <em>Leningrad.</em> 3-127., available online at http://paleostratmuseum.ru/files/Mikluho1949.pdf
page(s): p. 46; note: As Staffelininae (subfamily) nom. imperfectum. [details] Available for editors [request]
original description Solovieva, M. N. (1978). K sisteme foraminifer (interpretatsiya biologicheskogo znacheniya osobennostey strukturnoy i prostranstvennoy organizatsii foraminifer) - On the systematics of the foraminifera (interpretation of the biological significance of structural features and spatial organization of the foraminifera). <em>Byulletin' Moskovskoe Obshchestva Ispytateley Prirody. Otdelenie Geologicheskii.</em> 53(5): 159-160. [details]
page(s): p. 46; note: As Staffelininae (subfamily) nom. imperfectum. [details] Available for editors
[request]original description Solovieva, M. N. (1978). K sisteme foraminifer (interpretatsiya biologicheskogo znacheniya osobennostey strukturnoy i prostranstvennoy organizatsii foraminifer) - On the systematics of the foraminifera (interpretation of the biological significance of structural features and spatial organization of the foraminifera). <em>Byulletin' Moskovskoe Obshchestva Ispytateley Prirody. Otdelenie Geologicheskii.</em> 53(5): 159-160. [details]
From editor or global species database
Description Tests planispiral, involute, lenticular or spherical, very rarely subfusiform or uncoiled. The septa remain planar during all the history of the suborder (in contrast to the other suborder, Fusulinina). Chomata are often present but poorly developed. Some structures confused with parachomata are occasionally described. Wall calcareous secreted, probably initially dark aragonitic (probably fibrous and finely perforated), then neomicrosparitized from aragonite. Aperture simple terminal basal.(Vachard and Le Coze (2024)). [details]
