PRELIMINARY ASSESSMENT OF THE FAUNA OF THE UPPER MIOCENE HUMBOLDT FORMATION EXPOSED IN ELKO COUNTY, NEVADA FROM FIELD AND MUSEUM COLLECTIONS
The Humboldt Formation contains alluvial fan, fluvial, and lacustrine terrestrial deposits with abundant interbedded volcaniclastic intervals. The Humboldt Basin was formed initially by continued gravitational collapse of the Nevadaplano, and subsequently by regional detachment faulting and resulting adjacent accommodation space.
Previous studies have identified horses, camelids, and potential antilocaprids. We confirm and add to these taxa including: Suidae, Camelidae, Equiidae (cf. Neohipparion sp.), Rhinocerotidae (cf. Teleoceras sp.), cf. Mustelidae, Feliformes (cf. Machairodus), Proboscidea (Gomphotheriidae). The presence of the horse taxon Neohipparion is instructive biostratigraphically as this morph is known only from Upper Miocene strata of Clarendonian-Hemphillian North American Land Mammal Ages (13-5 Ma). Continued survey of new sites and museum collections will greatly expand this list and provide for regional stratigraphic refinement of faunal distributions. Further work planned includes chronostratigraphy, and microvertebrate processing of matrix from these sites.