Foraminifera taxon details
Neoschwagerinoidea Dunbar & Condra, 1927 nom. transl. Solovieva, 1978 †
marine, fresh, terrestrial
fossil only
Dunbar, C. O.; Condra, G. E. (1927). The fusulinidae of the Pennsylvanian system in Nebraska. <em>Bulletin of the Nebraska Geological Survey, ser.</em> 2(2): 1-135. [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.
note: Nomen translatum [details]
[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.
note: Nomen translatum [details]
Description Test large-inflated fusiform to spherical, planispirally coiled and involute. Supplementary deposits as parachomata often...
Taxonomic remark J. Pignatti (2022) pers. comm. kindly brought to our attention that according to the principle of coordination of the ICZN...
Description Test large-inflated fusiform to spherical, planispirally coiled and involute. Supplementary deposits as parachomata often present. Numerous genera display chambers divided into chamberlets by transverse septula of first order (which connect with the parachomata in neoschwagerinids: and shorter transverse septula of second order, as well as axial septula. Wall microgranular and finely keriothecal or re-becoming apparently dark microgranular (sumatrinins). Poorly developed apertures as small foramina between the parachomata and the chamberlets.
(Vachard and Le Coze (2024)). [details]
(Vachard and Le Coze (2024)). [details]
Taxonomic remark J. Pignatti (2022) pers. comm. kindly brought to our attention that according to the principle of coordination of the ICZN...
Taxonomic remark J. Pignatti (2022) pers. comm. kindly brought to our attention that according to the principle of coordination of the ICZN (1999), Neoschwagerinoidea Dunbar & Condra, 1927 is a junior synonym of Verbeekinoidea Staff & Wedekind, 1910.
The characteristics of the superfamily are (1) the presence of a fine keriothecal wall; (2) the presence of parachomata; (3) the axial and transverse secondary septula. The two first characters are present in the three families, but the last one is only developed in the third family : Neoschwagerinidae. It is noteworthy that in a classications only based on the internal endoskeleton, Verbeekinidae and Neoschwageridae are interpreted as belonging to two different orders/superfamilies. So we consider the family Neoschwagerinidae as more characteristic of the superfamily, and we suggest to denominate it Neoschwagerinoidea. In application of the article 35.5 of the ICZN, Neoschwagerinoidea is also to be kept since it is currently in prevailing usage (see for instance Ueno (2021)). [details]
The characteristics of the superfamily are (1) the presence of a fine keriothecal wall; (2) the presence of parachomata; (3) the axial and transverse secondary septula. The two first characters are present in the three families, but the last one is only developed in the third family : Neoschwagerinidae. It is noteworthy that in a classications only based on the internal endoskeleton, Verbeekinidae and Neoschwageridae are interpreted as belonging to two different orders/superfamilies. So we consider the family Neoschwagerinidae as more characteristic of the superfamily, and we suggest to denominate it Neoschwagerinoidea. In application of the article 35.5 of the ICZN, Neoschwagerinoidea is also to be kept since it is currently in prevailing usage (see for instance Ueno (2021)). [details]
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2021). World Foraminifera Database. Neoschwagerinoidea Dunbar & Condra, 1927 nom. transl. Solovieva, 1978 †. Accessed at: http://www.marinespecies.org/foraminifera/aphia.php?p=taxdetails&id=1058811 on 2025-05-20
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original description
Dunbar, C. O.; Condra, G. E. (1927). The fusulinidae of the Pennsylvanian system in Nebraska. <em>Bulletin of the Nebraska Geological Survey, ser.</em> 2(2): 1-135. [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.
note: Nomen translatum [details]
additional source Ueno, K. (2022). Carboniferous fusuline Foraminifera: taxonomy, regional biostratigraphy, and palaeobiogeographic faunal development. <em>Geological Society, London, Special Publications.</em> 512(1): 327-496 [first online 2021]., available online at https://doi.org/10.1144/sp512-2021-107 [details] Available for editors [request]
[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.
note: Nomen translatum [details]
additional source Ueno, K. (2022). Carboniferous fusuline Foraminifera: taxonomy, regional biostratigraphy, and palaeobiogeographic faunal development. <em>Geological Society, London, Special Publications.</em> 512(1): 327-496 [first online 2021]., available online at https://doi.org/10.1144/sp512-2021-107 [details] Available for editors
[request]From editor or global species database
Description Test large-inflated fusiform to spherical, planispirally coiled and involute. Supplementary deposits as parachomata often present. Numerous genera display chambers divided into chamberlets by transverse septula of first order (which connect with the parachomata in neoschwagerinids: and shorter transverse septula of second order, as well as axial septula. Wall microgranular and finely keriothecal or re-becoming apparently dark microgranular (sumatrinins). Poorly developed apertures as small foramina between the parachomata and the chamberlets.(Vachard and Le Coze (2024)). [details]
Taxonomic remark J. Pignatti (2022) pers. comm. kindly brought to our attention that according to the principle of coordination of the ICZN (1999), Neoschwagerinoidea Dunbar & Condra, 1927 is a junior synonym of Verbeekinoidea Staff & Wedekind, 1910.
The characteristics of the superfamily are (1) the presence of a fine keriothecal wall; (2) the presence of parachomata; (3) the axial and transverse secondary septula. The two first characters are present in the three families, but the last one is only developed in the third family : Neoschwagerinidae. It is noteworthy that in a classications only based on the internal endoskeleton, Verbeekinidae and Neoschwageridae are interpreted as belonging to two different orders/superfamilies. So we consider the family Neoschwagerinidae as more characteristic of the superfamily, and we suggest to denominate it Neoschwagerinoidea. In application of the article 35.5 of the ICZN, Neoschwagerinoidea is also to be kept since it is currently in prevailing usage (see for instance Ueno (2021)). [details]
