MolluscaBase name details

Discus (Gonyodiscus) marmorensis H. B. Baker, 1932

1365107  (urn:lsid:marinespecies.org:taxname:1365107)

alternative representation
Species
marine, brackish, fresh, terrestrial
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] 
Type locality contained in USA  
type locality contained in USA (origin: native[details]
Note "about 116° 20' W. Long., 45° 35' N. Lat.,...  
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
Date
action
by
2019-08-08 07:44:16Z
created
2022-07-24 16:50:45Z
changed

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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] 
 
 Present  Inaccurate  Introduced: alien  Containing type locality 
   

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]
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