MolluscaBase name details
Cuneopsis humilioris [sic] †
1556169 (urn:lsid:marinespecies.org:taxname:1556169)
unaccepted > misspelling - incorrect subsequent spelling
Species
fossil only
(of Unio humilior Lindholm, 1932 †) Lindholm, W. A. (1932). Presnovodnyye mollyuski iz pliotsenovykh otlozheniy po r. Irtyshu (Yugo-Zapadnaya Sibir') [Freshwater mollusks from the Pliocene deposits of the Irtysh River (SW Siberia)]. <em>Trudy Vsesoyuznogo geologo-razvedochnogo ob'edineniya NKTP SSSR.</em> 239: 3–27.
page(s): 19, pl. VI, fig. 4-6 [details] Available for editors
[request]
page(s): 19, pl. VI, fig. 4-6 [details] Available for editors

MolluscaBase eds. (2025). MolluscaBase. Cuneopsis humilioris [sic] †. Accessed at: https://molluscabase.org/aphia.php?p=taxdetails&id=1556169 on 2025-09-10
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original description
(of Unio humilior Lindholm, 1932 †) Lindholm, W. A. (1932). Presnovodnyye mollyuski iz pliotsenovykh otlozheniy po r. Irtyshu (Yugo-Zapadnaya Sibir') [Freshwater mollusks from the Pliocene deposits of the Irtysh River (SW Siberia)]. <em>Trudy Vsesoyuznogo geologo-razvedochnogo ob'edineniya NKTP SSSR.</em> 239: 3–27.
page(s): 19, pl. VI, fig. 4-6 [details] Available for editors
[request]
basis of record Maderni U.N. (1990). Mollusks of the continental Cenozoic of the Turgai Depression and adjacent areas [= Моллюски континентального кайнозоя Тургайского прогиба и смежных регионов]. <em>Trudy VSEGEI.</em> 345: 1-191. [In Russian]., available online at http://ashipunov.me/shipunov/school/books/moll_kontin_kajnoz_turgajskogo_progiba_1990.djvu
page(s): 53-54, pl. 15, fig. 4 [details]
page(s): 19, pl. VI, fig. 4-6 [details] Available for editors

basis of record Maderni U.N. (1990). Mollusks of the continental Cenozoic of the Turgai Depression and adjacent areas [= Моллюски континентального кайнозоя Тургайского прогиба и смежных регионов]. <em>Trudy VSEGEI.</em> 345: 1-191. [In Russian]., available online at http://ashipunov.me/shipunov/school/books/moll_kontin_kajnoz_turgajskogo_progiba_1990.djvu
page(s): 53-54, pl. 15, fig. 4 [details]