História da distribuição e controles climáticos da cronofauna do Pikermiano do Mioceno Posterior

Distribution history and climatic controls of the Late Miocene Pikermian chronofauna

Jussi T. Eronena,1, Majid Mirzaie Ataabadia, Arne Micheelsb, Aleksis Karmea, Raymond L. Bernorc,d and Mikael Forteliusa,e

+Author Affiliations

aDepartment of Geology and eInstitute of Biotechnology, FIN-00014 University of Helsinki, Finland;

bSenckenberg Forschungsinstitut und Naturmuseum, Biodiversität und Klima Forschungszentrum (BiK-F), Senckenberganlage 25, D-60325, Frankfurt am Main, Germany;

cSedimentary Geology and Paleobiology Program, Geosciences/Earth Sciences, National Science Foundation, 4201 Wilson Boulevard, Arlington, VA 22230; and

dCollege of Medicine, Department of Anatomy, Laboratory of Evolutionary Biology, Howard University, 520 W Street Northwest, Washington, D.C. 20059

Edited by David Pilbeam, Harvard University, Cambridge, MA, and approved May 12, 2009 (received for review March 9, 2009)

Abstract

The Late Miocene development of faunas and environments in western Eurasia is well known, but the climatic and environmental processes that controlled its details are incompletely understood. Here we map the rise and fall of the classic Pikermian fossil mammal chronofauna between 12 and 4.2 Ma, using genus-level faunal similarity between localities. To directly relate land mammal community evolution to environmental change, we use the hypsodonty paleoprecipitation proxy and paleoclimate modeling. The geographic distribution of faunal similarity and paleoprecipitation in successive timeslices shows the development of the open biome that favored the evolution and spread of the open-habitat adapted large mammal lineages. In the climate model run, this corresponds to a decrease in precipitation over its core area south of the Paratethys Sea. The process began in the latest Middle Miocene and climaxed in the medial Late Miocene, about 7–8 million years ago. The geographic range of the Pikermian chronofauna contracted in the latest Miocene, a time of increasing summer drought and regional differentiation of habitats in Eastern Europe and Southwestern Asia. Its demise at the Miocene-Pliocene boundary coincides with an environmental reversal toward increased humidity and forestation, changes inevitably detrimental to open-adapted, wide-ranging large mammals.

fossil mammals paleoclimate Pikermi similarity index

Footnotes


1To whom correspondence should be addressed. E-mail: jussi.t.eronen@helsinki.fi

Author contributions: J.T.E., M.M.A., R.L.B., and M.F. designed research; J.T.E., M.M.A., A.M., and M.F. performed research; J.T.E., M.M.A., and A.K. contributed new reagents/analytic tools; J.T.E., M.M.A., A.M., A.K., and M.F. analyzed data; and J.T.E., M.M.A., A.M., R.L.B., and M.F. wrote the paper.

The authors declare no conflict of interest.

This article is a PNAS Direct Submission.

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