Traits name details

Palaeomutela (Palaeanodonta) tersiensis (Fedotov, 1937) †

1725900  (urn:lsid:marinespecies.org:taxname:1725900)

alternative representation
Species
Palaeanodonta tersiensis Fedotov, 1937 † · unaccepted > superseded combination
marine, fresh, terrestrial
fossil only
(of Palaeanodonta tersiensis Fedotov, 1937 †) Fedotov, D. M. (1937). Plastinchatozhabernyye mollyuski uglenosnykh otlozheniy Kuz­netskogo basseyna [The Pelecypoda from the coal-bearing deposits of the Kuznetsk basin]. In: Paleontologiya i stratigrafiya Kuzbassa (XVII mezhdunarodnogo geologicheskogo kongressu) [Paleontology and stratigraphy of Kuzbass (17th International Geological Congress)]. <em>Trudy Tsentral'nogo nauchno-issledovatel'skogo geologo-razvedochnogo instituta.</em> 97: 5–96.
page(s): 42-43, 83-84, pl. 8, figs 4-9v, pl. 9, figs 1, 2 [details] Available for editors  PDF available
MolluscaBase eds. (2024). MolluscaBase. Palaeomutela (Palaeanodonta) tersiensis (Fedotov, 1937) †. Accessed through: Marine Species Traits editorial board (2024) Marine Species Traits at: https://www.marinespecies.org/traits./aphia.php?p=taxdetails&id=1725900 on 2024-11-05
Marine Species Traits editorial board (2024). Marine Species Traits. Palaeomutela (Palaeanodonta) tersiensis (Fedotov, 1937) †. Accessed at: https://marinespecies.org/traits/aphia.php?p=taxdetails&id=1725900 on 2024-11-05
Date
action
by
2023-12-29 14:02:07Z
created

original description (of Palaeanodonta tersiensis Fedotov, 1937 †) Fedotov, D. M. (1937). Plastinchatozhabernyye mollyuski uglenosnykh otlozheniy Kuz­netskogo basseyna [The Pelecypoda from the coal-bearing deposits of the Kuznetsk basin]. In: Paleontologiya i stratigrafiya Kuzbassa (XVII mezhdunarodnogo geologicheskogo kongressu) [Paleontology and stratigraphy of Kuzbass (17th International Geological Congress)]. <em>Trudy Tsentral'nogo nauchno-issledovatel'skogo geologo-razvedochnogo instituta.</em> 97: 5–96.
page(s): 42-43, 83-84, pl. 8, figs 4-9v, pl. 9, figs 1, 2 [details] Available for editors  PDF available
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