Foraminifera name details
Shouguania Lin, 1981 †
721764 (urn:lsid:marinespecies.org:taxname:721764)
unaccepted (Subjective junior synonym Opinion of Hance et al. (2011))
Genus
Shouguania furongshanensis Lin, 1981 † (type by original designation)
- Species Shouguania annectena Lin, 1981 †
- Species Shouguania furongshanensis Lin, 1981 †
- Species Shouguania lianxianensis Lin, 1981 †
- Species Shouguania songziensis Lin, 1984 †
- Species Shouguania bradyi (Möller, 1878) † accepted as Reitlingerina bradyi (Möller, 1878) †
marine, brackish, fresh, terrestrial
fossil only
feminine
Lin, J. (1981). The Early Carboniferous Foraminifera in Guangdong and Hunan and their stratigraphical significance. <em>Bulletin of the Yichang Institute of Geology and Mineral Resources, Special Issue.</em> 1-41.
page(s): p. 27 [details]
page(s): p. 27 [details]
Diagnosis Test small, up to 0.57 mm in diameter, lenticular, periphery angular, poles flattened to depressed, globular proloculus...
Diagnosis Test small, up to 0.57 mm in diameter, lenticular, periphery angular, poles flattened to depressed, globular proloculus followed by four to four and a half rapidly enlarging planispiral whorls, first whorl evolute, later ones involute, septa straight, no axial fillings; wall calcareous, light yellow or gray in color, with four layers, tectum, diaphanotheca, and inner and outer tectoria, chomata small but prominent, at the top of the lateral slopes, tunnel crescentic. Upper part of L. Carboniferous; China; USSR; W. Europe. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2021). World Foraminifera Database. Shouguania Lin, 1981 †. Accessed at: https://marinespecies.org/foraminifera./aphia.php?p=taxdetails&id=721764 on 2025-05-25
Date
action
by
original description
Lin, J. (1981). The Early Carboniferous Foraminifera in Guangdong and Hunan and their stratigraphical significance. <em>Bulletin of the Yichang Institute of Geology and Mineral Resources, Special Issue.</em> 1-41.
page(s): p. 27 [details]
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]
source of synonymy Hance, L.; Hou, H.; Vachard, D. (2011). Upper Famennian to Visean foraminifers and some carbonate microproblematica from South China – Hunan, Guangxi and Guizhou . <em>Beijing Geological Publishing House: Beijing.</em> 1-359.
page(s): p. 175 [details] Available for editors [request]
source of synonymy 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]
page(s): p. 27 [details]
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]source of synonymy Hance, L.; Hou, H.; Vachard, D. (2011). Upper Famennian to Visean foraminifers and some carbonate microproblematica from South China – Hunan, Guangxi and Guizhou . <em>Beijing Geological Publishing House: Beijing.</em> 1-359.
page(s): p. 175 [details] Available for editors
[request]source of synonymy 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
Diagnosis Test small, up to 0.57 mm in diameter, lenticular, periphery angular, poles flattened to depressed, globular proloculus followed by four to four and a half rapidly enlarging planispiral whorls, first whorl evolute, later ones involute, septa straight, no axial fillings; wall calcareous, light yellow or gray in color, with four layers, tectum, diaphanotheca, and inner and outer tectoria, chomata small but prominent, at the top of the lateral slopes, tunnel crescentic. Upper part of L. Carboniferous; China; USSR; W. Europe. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]
