MolluscaBase taxon details
Kinerkaella elongata Khalfin, 1950 †
1645018 (urn:lsid:marinespecies.org:taxname:1645018)
accepted
Species
Kinerkaella balakhonskiensis var. elongata Khalfin, 1950 † · unaccepted > superseded rank
fossil only
(of Kinerkaella balakhonskiensis var. elongata Khalfin, 1950 †) Khalfin L.L. (1950). The lamellibranchiate mollusks of the coal-bearing deposits of Kuzbass [= Пластинчатожаберные моллюски угленосных отложений Кузбасса]. <em>Trudy Gorno-Geologicheskogo Instituta Zapadno-Sibirskogo Filiala AN SSSR.</em> 9: 1-159. [In Russian].
page(s): 52, pl. 2, figs 14-17 [details] Available for editors
[request]
page(s): 52, pl. 2, figs 14-17 [details] Available for editors

Type locality contained in West Siberia
type locality contained in West Siberia [from synonym] [view taxon] [details]
MolluscaBase eds. (2025). MolluscaBase. Kinerkaella elongata Khalfin, 1950 †. Accessed at: https://www.molluscabase.org/aphia.php?p=taxdetails&id=1645018 on 2025-04-27
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original description
(of Kinerkaella balakhonskiensis var. elongata Khalfin, 1950 †) Khalfin L.L. (1950). The lamellibranchiate mollusks of the coal-bearing deposits of Kuzbass [= Пластинчатожаберные моллюски угленосных отложений Кузбасса]. <em>Trudy Gorno-Geologicheskogo Instituta Zapadno-Sibirskogo Filiala AN SSSR.</em> 9: 1-159. [In Russian].
page(s): 52, pl. 2, figs 14-17 [details] Available for editors
[request]
basis of record Betekhtina, O. A. (1966). Verkhnepaleozoiskie nemorskie peletsipody (dvustvorki) Sibiri i vostochnogo Kazakhstana [Upper Paleozoic non-marine Pelecypoda (bivalves) of Siberia and eastern Kazakhstan]. Nauka, Moskva, 220 pp.
page(s): 152, 153, pl. 4, figs 9, 10 [details] Available for editors
[request]
page(s): 52, pl. 2, figs 14-17 [details] Available for editors

basis of record Betekhtina, O. A. (1966). Verkhnepaleozoiskie nemorskie peletsipody (dvustvorki) Sibiri i vostochnogo Kazakhstana [Upper Paleozoic non-marine Pelecypoda (bivalves) of Siberia and eastern Kazakhstan]. Nauka, Moskva, 220 pp.
page(s): 152, 153, pl. 4, figs 9, 10 [details] Available for editors




