MolluscaBase name details
Pyramidula lecontei Stearns, 1902 †
1338524 (urn:lsid:marinespecies.org:taxname:1338524)
unaccepted > superseded combination
Species
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]
page(s): 154 [details]
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 2025-09-12
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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]
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
[request]
page(s): 154 [details]
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
[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]
