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Blancan
Pliocene Paleoenvironments in the Meade Basin, Southwest Kansas, U.S.A.
Age of a Pliocene basin fill along the Sevier River, southwestern Utah, U.S.A., based on fossil rodents
Pedogenic carbonate stable isotope record of environmental change during the Neogene in the southern Great Plains, southwest Kansas, USA: Oxygen isotopes and paleoclimate during the evolution of C 4 -dominated grasslands
Pedogenic carbonate stable isotope record of environmental change during the Neogene in the southern Great Plains, southwest Kansas, USA: Carbon isotopes and the evolution of C 4 -dominated grasslands
BLANCAN CAMELIDS FROM SAN MIGUEL DE ALLENDE, GUANAJUATO, CENTRAL MÉXICO
THE FIRST MID-BLANCAN OCCURRENCE OF AGRIOTHERIUM (URSIDAE) IN NORTH AMERICA: A RECORD FROM HAGERMAN FOSSIL BEDS NATIONAL MONUMENT, IDAHO
The Hunter Creek Sandstone of the Verdi Basin, Nevada, yielded a succession of superposed continental faunal assemblages ranging in age from the late Clarendonian (late Miocene) through the late Blancan (late Pliocene) in the North American land mammal age framework, or ca. 10.5–2.5 Ma. We describe two new local faunas from the Hunter Creek Sandstone: the East Verdi local fauna, of late-medial to late Clarendonian age, which includes Dinohippus cf. D. leardi , Camelidae, ?Antilocapridae, and Mammutidae or Gomphotheriidae; and the Mogul local fauna, of Hemphillian age, which includes Dinohippus sp., Rhinocerotidae, Camelidae (at least two species), Mammut sp., and possibly Gomphotheriidae. A third unnamed assemblage, of latest Hemphillian or earliest Blancan age, is represented by a small sample of fossils from W.M. Keck Museum locality P-105. The only taxa recovered from this locality are cf. Megatylopus and Gomphotheriidae or Mammutidae. A single late Blancan locality, the Byland locality, yielded Equus idahoensis . The recognition of this faunal succession provides a biostratigraphic framework for the Hunter Creek Sandstone that corroborates and is consistent with the previous chronostratigraphy based on radioisotopic and tephrochronologic dating methods.