MolluscaBase name details

Pyramidula lecontei Stearns, 1902 †

1338524  (urn:lsid:marinespecies.org:taxname:1338524)

 unaccepted > superseded combination
Species
marine, brackish, fresh, terrestrial
fossil only
Stearns, R. E. C. (1902). Fossil shells of the John Day Region. <em>Science, new series.</em> 15(369): 153-154.
page(s): 154 [details]  OpenAccess publication 
Note "The North Fork of John Day River, Oregon, at...  
From editor or global species database
Type locality "The North Fork of John Day River, Oregon, at the angle of the big bend, longitude 119° 40', latitude 44° 50" (referring to the "same general locality" as in Stearns 1900, who in turn referred to White 1885, p. 174) [details]
Fossil range Exact age uncertain. Claimed to be from the "John Day group" (today John Day Formation), which roughly ranges in age from...  
Fossil range Exact age uncertain. Claimed to be from the "John Day group" (today John Day Formation), which roughly ranges in age from the Bartonian (late Eocene) to the Burdigalian (early Miocene). [details]
MolluscaBase eds. (2021). MolluscaBase. Pyramidula lecontei Stearns, 1902 †. Accessed at: https://www.molluscabase.org/aphia.php?p=taxdetails&id=1338524 on 2024-03-28
Date
action
by
2019-04-03 07:16:03Z
created
2022-08-30 07:32:28Z
changed

Creative Commons License The webpage text is licensed under a Creative Commons Attribution 4.0 License


original description Stearns, R. E. C. (1902). Fossil shells of the John Day Region. <em>Science, new series.</em> 15(369): 153-154.
page(s): 154 [details]  OpenAccess publication 

basis of record Pilsbry, H. A. (1948). Land Mollusca of North America (north of Mexico). Volume II Part 2. <em>The Academy of Natural Sciences of Philadelphia Monographs.</em> 3: i-xlvii, 521-1113. Philadelphia [19 March].
page(s): 599 [details]  Available for editors  PDF available [request] 
 
 Present  Inaccurate  Introduced: alien  Containing type locality 
   

From editor or global species database
Fossil range Exact age uncertain. Claimed to be from the "John Day group" (today John Day Formation), which roughly ranges in age from the Bartonian (late Eocene) to the Burdigalian (early Miocene). [details]

Type locality "The North Fork of John Day River, Oregon, at the angle of the big bend, longitude 119° 40', latitude 44° 50" (referring to the "same general locality" as in Stearns 1900, who in turn referred to White 1885, p. 174) [details]

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