MolluscaBase name details
Trigonioides laotiae Hoffet, 1937 †
1533979 (urn:lsid:marinespecies.org:taxname:1533979)
unaccepted (subjective synonym)
Species
fossil only
Hoffet, J.-H. (1937). Les lamellibranches saumatres du Sénonien de Muong Phalane (Bas-Laos). <em>Bulletin du Service géologique de l'Indochine.</em> 24(1): 4-25.
page(s): 12-13, pl. 2, figs 1-5 [details] Available for editors
[request]
page(s): 12-13, pl. 2, figs 1-5 [details] Available for editors
[request]
Type locality contained in Laos
type locality contained in Laos [details]
MolluscaBase eds. (2021). MolluscaBase. Trigonioides laotiae Hoffet, 1937 †. Accessed at: https://www.molluscabase.org/aphia.php?p=taxdetails&id=1533979 on 2024-04-25
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The webpage text is licensed under a Creative Commons Attribution 4.0 License
original description
Hoffet, J.-H. (1937). Les lamellibranches saumatres du Sénonien de Muong Phalane (Bas-Laos). <em>Bulletin du Service géologique de l'Indochine.</em> 24(1): 4-25.
page(s): 12-13, pl. 2, figs 1-5 [details] Available for editors [request]
source of synonymy Sha, J. (2007). Cretaceous trigonioidid (non-marine Bivalvia) assemblages and biostratigraphy in Asia with special remarks on the classification of Trigonioidacea. <em>Journal of Asian Earth Sciences.</em> 29(1): 62-83., available online at https://doi.org/10.1016/j.jseaes.2006.01.003
page(s): 72 [details] Available for editors [request]
page(s): 12-13, pl. 2, figs 1-5 [details] Available for editors
[request] source of synonymy Sha, J. (2007). Cretaceous trigonioidid (non-marine Bivalvia) assemblages and biostratigraphy in Asia with special remarks on the classification of Trigonioidacea. <em>Journal of Asian Earth Sciences.</em> 29(1): 62-83., available online at https://doi.org/10.1016/j.jseaes.2006.01.003
page(s): 72 [details] Available for editors
[request] 
Present Inaccurate Introduced: alien Containing type locality
From editor or global species database
Synonymy Sha (2007) considered the three species Trigonioides kobayashi, T. laotiae and T. trigonus, all described by Hoffet (1937), as conspecific, since they "continuously vary in outline, and sometimes occur in the same formation and site." [details]
