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Mid-Pleistocene climate transition triggered by Antarctic Ice Sheet growth

Zhisheng An1,2,3, Weijian Zhou1,2,3, Zeke Zhang1,2,4

  • 1State Key Laboratory of Loess Science, Institute of Earth Environment, Chinese Academy of Sciences, Xi'an 710061, China.

Science (New York, N.Y.)
|August 1, 2024
PubMed
Summary

The Mid-Pleistocene Transition was triggered by Antarctic Ice Sheet growth, which cooled the Northern Hemisphere. This finding is crucial for understanding current global warming and bipolar ice melt.

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