MolluscaBase taxon details
Physa bullatula C. A. White, 1886 †
1260720 (urn:lsid:marinespecies.org:taxname:1260720)
accepted
Species
fossil only
White, C.A. (1886). On the relation of the Laramie molluscan fauna to that of the succeeding fresh-water Eocene and other groups. <em>United States Geological Survey Bulletin.</em> 34: 391-442.
page(s): 25, pl. 3, figs 14-17 [details]
page(s): 25, pl. 3, figs 14-17 [details]
Note Reported by White (1886) as "Wasatch strata,...
From editor or global species database
Type locality Reported by White (1886) as "Wasatch strata, near Wales, Utah; and also at several other localities in equivalent strata in the Wasatch Mountains, east of San Pete Valley". However, according to La Rocque (1960), there are no lacustrine deposits at this locality. After Spieker (1946), the fossils reported by White variably derive from Price River, North Horn and Flagstaff formations (Campanian-Paleocene). [details]
MolluscaBase eds. (2024). MolluscaBase. Physa bullatula C. A. White, 1886 †. Accessed at: https://molluscabase.org/aphia.php?p=taxdetails&id=1260720 on 2024-04-19
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original description
White, C.A. (1886). On the relation of the Laramie molluscan fauna to that of the succeeding fresh-water Eocene and other groups. <em>United States Geological Survey Bulletin.</em> 34: 391-442.
page(s): 25, pl. 3, figs 14-17 [details]
basis of record Henderson, J. (1935). Fossil non-marine Mollusca of North America. <em>Geological Society of America Special Papers.</em> 3: 1-313.
page(s): 258 [details] Available for editors
[request]
page(s): 25, pl. 3, figs 14-17 [details]
basis of record Henderson, J. (1935). Fossil non-marine Mollusca of North America. <em>Geological Society of America Special Papers.</em> 3: 1-313.
page(s): 258 [details] Available for editors
[request] From editor or global species database
Spelling Obviously misspelt as "bullata" in species heading (White compared his species with P. bullata Gould). [details]Type locality Reported by White (1886) as "Wasatch strata, near Wales, Utah; and also at several other localities in equivalent strata in the Wasatch Mountains, east of San Pete Valley". However, according to La Rocque (1960), there are no lacustrine deposits at this locality. After Spieker (1946), the fossils reported by White variably derive from Price River, North Horn and Flagstaff formations (Campanian-Paleocene). [details]
