Also known as Hancock Mammal Quarry; UCMP V-75203; JDNM-13; UO 2473; UWBM #C0082
Where: Wheeler County, Oregon (44.9° N, 120.2° W: paleocoordinates 46.4° N, 105.2° W)
• coordinate based on political unit
• small collection-level geographic resolution
When: uppermost Member (Clarno Formation), Middle Eocene (47.8 - 37.7 Ma)
• The Nut beds have yielded ages between 42 and 44Ma (Manchester 1994; Bestland et al. 1999) placing the locality within the Uintan NALMA. However, several authors have noted Bridgerian fauna from the Clarno vertebrate localities (Stirton 1944; Hanson 1996). Member A of the overlying John Day Formation was dated to ~39 Ma, suggesting the Clarno Formation is also younger than this. Mihlbachler and Samuels 2016 suggest that referring to the Clarno vertebrate localities in terms of NALMA ages is problematic, as Oregan biostratigraphy during the Eocene and Miocene is in need of greater study and the localities share taxa considered characteristic of multiple land mammal ages.
Environment/lithology: terrestrial; conglomerate and sandstone
Size class: macrofossils
Primary reference: C. B. Hanson. 1996. Stratigraphy and vertebrate faunas of the Bridgerian-Duchesnean Clarno Formation, north-central Oregon. In D. R. Prothero and R. J. Emry (eds.), The Terrestrial Eocene-Oligocene Transition in North America 206-239 [J. Alroy/J. Alroy/J. Marcot]more details
Purpose of describing collection: biostratigraphic analysis
PaleoDB collection 16842: authorized by John Alroy, entered by John Alroy on 30.04.1994, edited by Patricia Holroyd and Jonathan Marcot
Creative Commons license: CC BY (attribution)
Taxonomic list
122 - 128 m level in a 150 m section of the Clarno according to Retallack et al. OAS abstract; overlies Clarno Nut Bed
just below a welded tuff at the base of the John Day dated at 39.2 Ma (SCLF AA), which is not the same as the basal John Day tuff in the Painted Hills dated at 39.7 Ma; FT zircon and KA dates from the same tuff are slightly younger than the 39.2 Ma date and have considerable errors
NISP 215+
considered Duchesnean by Hanson 1989
"Hesperoceras sp." is a bovid, not a rhinocerotid contra Fremd et al. 1994; I [JA]suspect this is a lapsus or a mistaken manuscript name.
Lucas et al. 2004 reinterpret the radioisotopic data and mammalian composition to arrive at a late Uintan age.
Reptilia | |
Chelydridae sp. Swainson 1839 turtle | |
Alligatoridae indet. crocodilian | |
Mammalia | |
Rodentia indet. Bowdich 1821 rodent | |
Heptacodon sp. Marsh 1894 anthracothere | |
Diplobunops kardoula n. sp.2
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Achaenodon fremdi n. sp.4
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Haplohippus texanus McGrew 1953 horse
Epihippus gracilis Marsh 1871 horse | |
Teletaceras radinskyi n. sp.
Teletaceras radinskyi n. sp. Hanson 1989 rhinoceros see Hanson 1989: presumably includes "Caenopus sp." of Krishtalka et al. 1987
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Zaisanamynodon protheroi n. sp.3
Zaisanamynodon protheroi n. sp.3 Lucas 2006 odd-toed ungulate NISP not given; said to new, and to be congeneric with Procadurcodon orientalis by Hanson 1989; said to be an "indeterminate amynodontid" by Wall 1998 without further comment
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Hemipsalodon grandis Cope 1885 creodont mentioned by Gustafson 1986b as from "Clarno"; "H. sp." of Krishtalka et al. 1987 as well as Bryant 1993
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