Patterns of maximum body size evolution in Cenozoic land mammals: eco-evolutionary processes and abiotic forcing

Juha J Saarinen1, Alison G Boyer, James H Brown

  • 1Department of Geosciences and Geography, University of Helsinki, , Helsinki, Finland, Department of Ecology and Evolutionary Biology, University of Tennessee, , Knoxville, TN, USA, Department of Biology, University of New Mexico, , Albuquerque, NM, USA, Department of Anthropology, University of New Mexico, , Albuquerque, NM, USA, Department of Ecology and Evolutionary Biology, University of California, , Santa Cruz, CA, USA, Department of Biology and the Ecology Center, Utah State University, , Logan, UT, USA, School of Biological Sciences, Monash University, , Victoria, Australia, Odum School of Ecology, University of Georgia, , Athens, GA, USA, Santa Fe Institute, , Santa Fe, NM, USA, Department of Paleobiology, Smithsonian Institution, , Washington, DC, USA, School of Earth and Space Exploration, Arizona State University, , Tempe, Arizona, USA, School of Biological Sciences, University of Reading, , Reading, UK, Department of Biological Sciences, University of Calgary, , Calgary, Alberta, Canada, Department of Atmospheric, Oceanic and Earth Sciences, George Mason University, , Fairfax, VA, USA.

Summary

Macroevolutionary patterns in Cenozoic mammal evolution show global similarities. Maximum mammal size across orders peaked in the Eocene, Oligocene, and Plio-Pleistocene, influenced by climate and niche dynamics.

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