Titanothere Quarry (Eocene of the United States)
Also known as Duchesneodus Quarry; Duchesne River Quarry; Uinta Quarry
DUPLICATE REF 1438 or 1439
Where: Uintah County, Utah (40.2° N, 109.9° W: paleocoordinates 42.3° N, 100.7° W)
• coordinate based on political unit
• small collection-level geographic resolution
When: Lapoint Member (Duchesne River Formation), Duchesnean (39.7 - 37.0 Ma)
Environment/lithology: terrestrial
Primary reference: R. J. Emry. 1981. New material of the Oligocene muroid rodent Nonomys, and its bearing on muroid origins. American Museum Novitates 2712:1-14 [J. Alroy/J. Alroy/P. Mannion]more details
PaleoDB collection 16861: authorized by John Alroy, entered by John Alroy on 21.09.1998
Creative Commons license: CC BY (attribution)
Taxonomic list
• this is not in Halfway Hollow, but in Twelve Mile Draw about two miles to the east
Duchesneodus Quarry is definitely the same as Titanothere Quarry because the type of D. uintensis has been put at both quarries by different authors
Duchesneodus Quarry is definitely the same as Titanothere Quarry because the type of D. uintensis has been put at both quarries by different authors
Show authors, comments, and common names
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Poabromylus kayi n. sp.3
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Hessolestes ultimus n. sp.2
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