Middle Miocene carnivorans from the Monarch Mill Formation, Nevada

Kent Smith, Nicholas Czaplewski, Richard L. Cifelli

Research output: Contribution to journalArticle

3 Citations (Scopus)

Abstract

The lowest part of the Monarch Mill Formation in the Middlegate basin, west-central Nevada, has yielded a middle Miocene (Barstovian Land Mammal Age) vertebrate assemblage, the Eastgate local fauna. Paleobotanical evidence from nearby, nearly contemporaneous fossil leaf assemblages indicates that the Middle Miocene vegetation in the area was mixed coniferous and hardwood forest and chaparral-sclerophyllous shrubland, and suggests that the area had been uplifted to 2700-2800 m paleoaltitude before dropping later to near its present elevation of 1600 m. Thus, the local fauna provides a rare glimpse at a medium- to high-altitude vertebrate community in the intermountain western interior of North America. The local fauna includes the remains of fish, amphibians, reptiles, birds, and 25 families of mammals. Carnivorans, the focus of this study, include six taxa (three of which are new) belonging to four families. Canidae are represented by the borophagine Tomarctus brevirostris and the canine Leptocyon sp. indet. The earliest record and second North American occurrence of the simocyonine ailurid Actiocyon is represented by A. parverratis sp. nov. Two new mustelids, Brevimalictis chikasha gen. et sp. nov. and Negodiaetictis rugatrulleum gen. et sp. nov., may represent Galictinae but are of uncertain subfamilial and tribal affinity. The fourth family is represented by the felid Pseudaelurus sp. indet. Tomarctus brevirostris is limited biochronologically to the Barstovian land mammal age and thus is consistent with the age indicated by other members of the Eastgate local fauna as well as by indirect tephrochronological dates previously associated with the Monarch Mill Formation. Actiocyon parverratis sp. nov. extends the temporal range of the genus Actiocyon from late Clarendonian back to the Barstovian. The Eastgate local fauna improves our understanding of mammalian successions and evolution, during and subsequent to the Mid-Miocene Climatic Optimum (∼14-17 Ma).

Original languageEnglish
Pages (from-to)231-252
Number of pages22
JournalActa Palaeontologica Polonica
Volume61
Issue number1
DOIs
StatePublished - 1 Mar 2016

Fingerprint

mill
Miocene
fauna
vertebrate
mustelid
felid
chaparral
Hypsithermal
shrubland
reptile
amphibian
mammal
fossil
bird
vegetation
fish
basin
family
land mammal

Keywords

  • Ailuridae
  • Barstovian
  • Canidae
  • Felidae
  • Mammalia
  • Miocene
  • Mustelidae
  • Nevada

Cite this

Smith, Kent ; Czaplewski, Nicholas ; Cifelli, Richard L. / Middle Miocene carnivorans from the Monarch Mill Formation, Nevada. In: Acta Palaeontologica Polonica. 2016 ; Vol. 61, No. 1. pp. 231-252.
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Middle Miocene carnivorans from the Monarch Mill Formation, Nevada. / Smith, Kent; Czaplewski, Nicholas; Cifelli, Richard L.

In: Acta Palaeontologica Polonica, Vol. 61, No. 1, 01.03.2016, p. 231-252.

Research output: Contribution to journalArticle

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