TY - JOUR
T1 - Successive climate crises in the deep past drove the early evolution and radiation of reptiles
AU - Simões, Tiago R.
AU - Kammerer, Christian F.
AU - Caldwell, Michael W.
AU - Pierce, Stephanie E.
N1 - Publisher Copyright:
Copyright © 2022 The Authors, some rights reserved.
PY - 2022/8/19
Y1 - 2022/8/19
N2 - Climate change–induced mass extinctions provide unique opportunities to explore the impacts of global environmental disturbances on organismal evolution. However, their influence on terrestrial ecosystems remains poorly understood. Here, we provide a new time tree for the early evolution of reptiles and their closest relatives to reconstruct how the Permian-Triassic climatic crises shaped their long-term evolutionary trajectory. By combining rates of phenotypic evolution, mode of selection, body size, and global temperature data, we reveal an intimate association between reptile evolutionary dynamics and climate change in the deep past. We show that the origin and phenotypic radiation of reptiles was not solely driven by ecological opportunity following the end-Permian extinction as previously thought but also the result of multiple adaptive responses to climatic shifts spanning 57 million years.
AB - Climate change–induced mass extinctions provide unique opportunities to explore the impacts of global environmental disturbances on organismal evolution. However, their influence on terrestrial ecosystems remains poorly understood. Here, we provide a new time tree for the early evolution of reptiles and their closest relatives to reconstruct how the Permian-Triassic climatic crises shaped their long-term evolutionary trajectory. By combining rates of phenotypic evolution, mode of selection, body size, and global temperature data, we reveal an intimate association between reptile evolutionary dynamics and climate change in the deep past. We show that the origin and phenotypic radiation of reptiles was not solely driven by ecological opportunity following the end-Permian extinction as previously thought but also the result of multiple adaptive responses to climatic shifts spanning 57 million years.
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U2 - 10.1126/sciadv.abq1898
DO - 10.1126/sciadv.abq1898
M3 - Article
C2 - 35984885
AN - SCOPUS:85136170011
SN - 2375-2548
VL - 8
JO - Science Advances
JF - Science Advances
IS - 33
M1 - eabq1898
ER -