MolluscaBase name details
Anodonta nordenskjoldi Steinmann & Wilckens, 1908 †
1517679 (urn:lsid:marinespecies.org:taxname:1517679)
unaccepted > superseded combination
Species
fossil only
Steinmann, G.; Wilckens, O. (1908). Kreide- und Tertiärfossilien aus den Magellansländern, gesammelt von der schwedischen Expedition 1895-1897. <em>Arkiv för zoologi.</em> 4(6): 1-118., available online at https://www.biodiversitylibrary.org/page/6399962
page(s): 35-36, textfig. 1 (p. 98) [details]
page(s): 35-36, textfig. 1 (p. 98) [details]
Type locality contained in Magellanes
, Note Type locality uncertain: "Höchst...
type locality contained in Magellanes [details]
From editor or global species database
Type locality Type locality uncertain: "Höchst wahrscheinlich Kohlenminen am Rio Condor, Westseite der Hauptinsel" [most likely from the coal mines at Rio Condor, west side of the main island]. According to Parodiz (1969) this concerns Río Cóndor, south of Bahía Inútil and across from Dawson Island, Tierra del Fuego, Chile. [details]
Fossil range Parodiz (1969) suggested an Oligocene age based on correlation with the Navidad Formation. However, that formation is...
Fossil range Parodiz (1969) suggested an Oligocene age based on correlation with the Navidad Formation. However, that formation is presently considered to be of Early-Middle Miocene age. [details]
MolluscaBase eds. (2025). MolluscaBase. Anodonta nordenskjoldi Steinmann & Wilckens, 1908 †. Accessed at: https://www.molluscabase.org/aphia.php?p=taxdetails&id=1517679 on 2025-09-10
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original description
Steinmann, G.; Wilckens, O. (1908). Kreide- und Tertiärfossilien aus den Magellansländern, gesammelt von der schwedischen Expedition 1895-1897. <em>Arkiv för zoologi.</em> 4(6): 1-118., available online at https://www.biodiversitylibrary.org/page/6399962
page(s): 35-36, textfig. 1 (p. 98) [details]
page(s): 35-36, textfig. 1 (p. 98) [details]
Present Inaccurate Introduced: alien Containing type locality
From editor or global species database
Fossil range Parodiz (1969) suggested an Oligocene age based on correlation with the Navidad Formation. However, that formation is presently considered to be of Early-Middle Miocene age. [details]Type locality Type locality uncertain: "Höchst wahrscheinlich Kohlenminen am Rio Condor, Westseite der Hauptinsel" [most likely from the coal mines at Rio Condor, west side of the main island]. According to Parodiz (1969) this concerns Río Cóndor, south of Bahía Inútil and across from Dawson Island, Tierra del Fuego, Chile. [details]
