MolluscaBase name details
Unio gardneri Stanton, 1916 †
1501561 (urn:lsid:marinespecies.org:taxname:1501561)
unaccepted > superseded combination
Species
fossil only
Stanton, T.W. (1916). Nonmarine Cretaceous invertebrates of the San Juan Basin. <em>United States Geological Survey Professional Paper.</em> 98-R: 309-326., available online at https://pubs.usgs.gov/pp/0098r/report.pdf
page(s): 314, pl. 80, figs 10-11 [details]
page(s): 314, pl. 80, figs 10-11 [details]
Holotype USNM 32034
, Type locality contained in Colorado , Note "Sec. 19, T. 35 N., R. 8 W., Ignacio...
Holotype USNM 32034 [details]
type locality contained in Colorado [details]
Type locality "Sec. 19, T. 35 N., R. 8 W., Ignacio quadrangle, Colo. (locality 6063), about 300 feet below the top of the 'Laramie', probably in the upper part of the Fruitland formation", USA; Late Cretaceous [details]
MolluscaBase eds. (2024). MolluscaBase. Unio gardneri Stanton, 1916 †. Accessed at: https://www.molluscabase.org/aphia.php?p=taxdetails&id=1501561 on 2024-04-29
Date
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The webpage text is licensed under a Creative Commons Attribution 4.0 License
original description
Stanton, T.W. (1916). Nonmarine Cretaceous invertebrates of the San Juan Basin. <em>United States Geological Survey Professional Paper.</em> 98-R: 309-326., available online at https://pubs.usgs.gov/pp/0098r/report.pdf
page(s): 314, pl. 80, figs 10-11 [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): 82 [details] Available for editors
[request]
page(s): 314, pl. 80, figs 10-11 [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): 82 [details] Available for editors
[request] 
Present Inaccurate Introduced: alien Containing type locality
Holotype USNM 32034 [details]
From editor or global species database
Type locality "Sec. 19, T. 35 N., R. 8 W., Ignacio quadrangle, Colo. (locality 6063), about 300 feet below the top of the 'Laramie', probably in the upper part of the Fruitland formation", USA; Late Cretaceous [details]
