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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.
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.
Area of Science:
- Paleontology
- Macroevolution
- Climate Science
Background:
- Macroevolutionary trends in mammal evolution suggest similar trajectories across continents during the Cenozoic.
- These patterns may be driven by global abiotic factors like climate or eco-evolutionary processes such as niche specialization.
Purpose of the Study:
- To investigate the temporal distribution of maximum body size within individual mammal orders globally and continentally.
- To determine if macroevolutionary patterns of size evolution are congruent across different geographic regions.
Main Methods:
- Analysis of the temporal distribution of maximum body size for mammal orders.
- Comparison of size evolution patterns on different continents and globally.
- Correlation analysis between maximum size frequency and global temperature proxies.
Main Results:
- Maximum body size in mammal orders showed congruence in timing, peaking in the Middle Eocene, Oligocene, and Plio-Pleistocene.
- The Eocene peak coincided with high global temperatures and mammal diversity, suggesting niche expansion.
- A significant correlation between maximum size frequency and global temperature was observed since the Eocene.
- The Plio-Pleistocene peak, the most robust, occurred during low temperatures and is linked to global cooling.
Conclusions:
- Macroevolutionary patterns in mammal size are shaped by an interplay between eco-evolutionary processes and abiotic forcing.
- Global climate significantly influences mammal macroevolutionary trajectories, particularly since the Eocene.
- While niche dynamics play a role, abiotic factors like temperature are key drivers of size evolution in mammals.
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