4.7 Article

First appearance of Grevy's zebra (Equus grevyi), from the Middle Pleistocene Kapthurin Formation, Kenya, sheds light on the evolution and paleoecology of large zebras

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QUATERNARY SCIENCE REVIEWS
卷 256, 期 -, 页码 -

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PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.quascirev.2021.106835

关键词

Baringo basin; Biogeography; Eastern Africa; Equidae; Paleoclimate; Paleodistributions

资金

  1. University of Utah Global Change and Sustainability Center Graduate Research Grant
  2. National Science Foundation [BCS-0118345]
  3. Wenner-Gren Foundation for Anthropological Research
  4. Leakey Foundation
  5. University of Connecticut Research Foundation
  6. Bill Bishop Memorial Trust

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A study describes a nearly complete skull of a large mare from the Kapthurin Formation in Kenya, indicating the first definitive appearance of E. grevyi at 547.0-392.6 ka, morphologically distinct from other zebras. The new specimen sheds light on the complex evolutionary history of large zebras and the mechanisms underlying the expanded range of Grevy's zebra during the Pleistocene.
Grevy's zebra (Equus grevyi) has been reported from fossil sites spanning the past 2.3 Myr and covering a wide geographic range. However, no currently published reports dating to >200 ka can be confidently attributed to E. grevyi, with most specimens better allocated to another taxon or lacking diagnostic characteristics aligning them with E. grevyi to the exclusion of other large Equus species such as E. oldowayensis. This leaves the origin of Grevy's zebra unresolved. Here, we describe a largely complete cranium of a large mare from the Kapthurin Formation in Kenya's Baringo Basin that represents the first definitive appearance of E. grevyi at 547.0-392.6 ka. This cranium falls within the range of variation for recent E. grevyi and is morphologically distinct from all other fossil and extant zebras. The new Kapthurin specimen has implications for the complex evolutionary history of large zebras. Furthermore, it provides insights into the mechanisms underpinning the expanded range of Grevy's zebra during the Pleistocene. Based on species distribution modeling and a multivariate analysis of its climate niche, we argue that the wide fossil distribution of E. grevyi may have had little to do with Pleistocene aridity as previously argued. Instead, the range contraction of Grevy's zebra may have been driven by competition with plains zebra (E. quagga) after the northward expansion of the latter species. (C) 2021 Elsevier Ltd. All rights reserved.

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