MolluscaBase name details
Discus (Gonyodiscus) marmorensis H. B. Baker, 1932
1365107 (urn:lsid:marinespecies.org:taxname:1365107)
alternative representation
Species
Baker, H. B. (1932). New land snails from Idaho and eastern Oregon. <em>The Nautilus.</em> 45(3): 82-87, pl. 5., available online at https://www.biodiversitylibrary.org/page/8527913
page(s): 84-85, pl. 5, figs. 1-3 [details]
page(s): 84-85, pl. 5, figs. 1-3 [details]
Type locality contained in USA
, Note "about 116° 20' W. Long., 45° 35' N. Lat.,...
type locality contained in USA (origin: native) [details]
Type locality "about 116° 20' W. Long., 45° 35' N. Lat., elevation near 3,000 feet; quite infrequent in steep, north facing, mossy talus slope, shaded by fairly open stand of mesophytes (dominated by grand fir and large yew), below cliffs of white, crystalline marble that tends to crumble into angular gravel and sand, about 2 miles up middle fork of John Day Creek canyon, which opens into Salmon River canyon near southeast corner of section 14, T. 26. 26 N., R. 1 E. (Boise Meridian), Idaho County, Idaho" [details]
MolluscaBase eds. (2025). MolluscaBase. Discus (Gonyodiscus) marmorensis H. B. Baker, 1932. Accessed at: https://www.molluscabase.org/aphia.php?p=taxdetails&id=1365107 on 2025-09-11
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Attribution 4.0 License
original description
Baker, H. B. (1932). New land snails from Idaho and eastern Oregon. <em>The Nautilus.</em> 45(3): 82-87, pl. 5., available online at https://www.biodiversitylibrary.org/page/8527913
page(s): 84-85, pl. 5, figs. 1-3 [details]
basis of record InvertEBase. (2018). Authority files of U.S. and Canadian land and freshwater mollusks developed for the InvertEBase (InvertEBase.org) project. [details]
page(s): 84-85, pl. 5, figs. 1-3 [details]
basis of record InvertEBase. (2018). Authority files of U.S. and Canadian land and freshwater mollusks developed for the InvertEBase (InvertEBase.org) project. [details]




From editor or global species database
Type locality "about 116° 20' W. Long., 45° 35' N. Lat., elevation near 3,000 feet; quite infrequent in steep, north facing, mossy talus slope, shaded by fairly open stand of mesophytes (dominated by grand fir and large yew), below cliffs of white, crystalline marble that tends to crumble into angular gravel and sand, about 2 miles up middle fork of John Day Creek canyon, which opens into Salmon River canyon near southeast corner of section 14, T. 26. 26 N., R. 1 E. (Boise Meridian), Idaho County, Idaho" [details]