The Omo Mursi Formation

A window into the East African Pliocene

Michelle S M Drapeau, René Bobe, Jonathan G. Wynn, Christopher Campisano, Laurence Dumouchel, Denis Geraads

Research output: Contribution to journalArticle

11 Citations (Scopus)

Abstract

Dating to more than four million years ago (Ma), the Mursi Formation is among the oldest of the Plio-Pleistocene Omo Group deposits in the lower Omo Valley of southwestern Ethiopia. The sedimentary sequence is exposed along a strip ~35km by 4km, but it has received relatively little attention due to the difficult access to this area. Although expeditions to the lower Omo Valley between 1968 and 1973 focused primarily on the Usno and Shungura Formations, survey of the Mursi Formation produced a faunal collection of about 250 specimens deriving exclusively from the Yellow Sands area at the southern extent of the exposures. In 2009, we reinitiated an investigation of the formation by focusing on the most northern exposures, and a new fossil site, Cholo, was identified. Cholo is depositionally similar to the lowermost exposures at the Yellow Sands, although no stratigraphic correlation between the two localities has yet been made. The fossiliferous sediments at Cholo are capped by a prominent vitric tuff that is compositionally distinct from any other known tephra preserved in East African rift basins, including the only known vitric tuff at the Yellow Sands. The faunal assemblage of the Yellow Sands area presents interesting characteristics: the fossils generally show little weathering and include a large proportion of suids (44% of the mammalian fauna) and a small proportion of bovids (14%) compared with other Pliocene African sites. The sample is also unusual in the high frequency of deinotheres (7%). Taxon-specific stable carbon isotopic composition of the Mursi mammals tends to show generally higher proportions of C3 diets compared with other Pliocene sites in East Africa and Chad. This and the particular faunal proportions suggest that the environments represented by the Mursi Formation were more closed than those of other Pliocene sites.

Original languageEnglish (US)
Pages (from-to)64-79
Number of pages16
JournalJournal of Human Evolution
Volume75
DOIs
StatePublished - Oct 1 2014

Fingerprint

Pliocene
sand
tuff
Chad
valleys
fossils
East Africa
fossil
Ethiopia
tephra
valley
stratigraphic correlation
Eastern Africa
sedimentary sequence
weathering
isotopic composition
mammal
fauna
Pleistocene
mammals

Keywords

  • Cholo
  • Omo Group
  • Paleoenvironment
  • Stable isotopes
  • Suidae
  • Yellow Sands

ASJC Scopus subject areas

  • Ecology, Evolution, Behavior and Systematics
  • Arts and Humanities (miscellaneous)
  • Education

Cite this

The Omo Mursi Formation : A window into the East African Pliocene. / Drapeau, Michelle S M; Bobe, René; Wynn, Jonathan G.; Campisano, Christopher; Dumouchel, Laurence; Geraads, Denis.

In: Journal of Human Evolution, Vol. 75, 01.10.2014, p. 64-79.

Research output: Contribution to journalArticle

Drapeau, Michelle S M ; Bobe, René ; Wynn, Jonathan G. ; Campisano, Christopher ; Dumouchel, Laurence ; Geraads, Denis. / The Omo Mursi Formation : A window into the East African Pliocene. In: Journal of Human Evolution. 2014 ; Vol. 75. pp. 64-79.
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