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Abstract
The causes of Mid-Pleistocene Transition global cooling 1 million years ago are still unknown. Here, the authors find the subarctic North Pacific became stratified during these glaciations due to closure of the Bering Strait, which would have removed CO2 from the atmosphere and caused global cooling.
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1 Camborne School of Mines, University of Exeter, Penryn Campus, Penryn, Cornwall, UK; NERC Isotope Geosciences Facilities, British Geological Survey, Keyworth, Nottingham, UK
2 University of California, Santa Cruz, CA, USA
3 Centre for Environmental Geochemistry, School of Geography, University of Nottingham, University Park, Nottingham, UK
4 NERC Isotope Geosciences Facilities, British Geological Survey, Keyworth, Nottingham, UK; Centre for Environmental Geochemistry, School of Biosciences, University of Nottingham, Sutton Bonington Campus, Loughborough, UK
5 Center for Advanced Marine Core Research, Kochi University, Nankoku, Kochi, Japan
6 Department of Geosciences, State Museum of Natural History, Karlsruhe, Germany
7 Department of Geoscience, Aarhus University, Aarhus C, Denmark
8 Moss Landing Marine Laboratories, Moss Landing, CA, USA
9 School of Earth and Ocean Sciences, Cardiff University, Cardiff, UK