WoRMS taxon details
Neofusulina Miklukho-Maklay, 1963 †
721815 (urn:lsid:marinespecies.org:taxname:721815)
accepted
Genus
Eofusulina (Paraeofusulina) subtilissima Putrya, 1956 † accepted as Neofusulina subtilissima (Putrya, 1956) † (type by original designation)
marine, brackish, fresh, terrestrial
fossil only
feminine
Miklukho-Maklay, A. D. (1963). Верхний палеозой Средней Азии - Upper Paleozoic of Central Asia. <em>Ленинградский государственный университет им. А.А. Жданова - Leningrad State University. A.A. Zhdanov.</em> 1-330., available online at https://books.google.pt/books?id=kh1fDwAAQBAJ
page(s): p. 221 [details] Available for editors
[request]
page(s): p. 221 [details] Available for editors
[request]
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2025). World Foraminifera Database. Neofusulina Miklukho-Maklay, 1963 †. Accessed through: World Register of Marine Species at: https://www.marinespecies.org/aphia.php?p=taxdetails&id=721815 on 2025-05-12
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Nomenclature
original description
Miklukho-Maklay, A. D. (1963). Верхний палеозой Средней Азии - Upper Paleozoic of Central Asia. <em>Ленинградский государственный университет им. А.А. Жданова - Leningrad State University. A.A. Zhdanov.</em> 1-330., available online at https://books.google.pt/books?id=kh1fDwAAQBAJ
page(s): p. 221 [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]
page(s): p. 221 [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 large, subcylindrical, elongate, septa intensely and regularly folded, forming cuniculi; wall thin, protheca may be differentiated in places, outer whorls with weakly developed diaphanotheca and inner tectorium, small chomata in earliest whorls only, well-developed axial deposits fill the central area from the proloculus to the poles. U. Carboniferous (U. Moscovian); USSR: Donets Basin, central Asia. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]
