Research School of Earth Sciences, The Australian National University, Canberra, ACT, Australia; State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi’an, China; Climate Change Research Centre, University of New South Wales, Sydney, NSW, Australia; CAS Center for Excellence in Quaternary Science and Global Change, Xi’an, China; Open Studio for Oceanic–Continental Climate and Environment Changes, Qingdao National Laboratory for Marine Science and Technology, Qingdao, China; Lamont–Doherty Earth Observatory, Columbia University, New York, NY, United States; State Key Laboratory of Marine Geology, Tongji University, Shanghai, China; Department of Earth Sciences, University of Cambridge, Cambridge, United Kingdom; Ocean and Earth Science, National Oceanography Centre, University of Southampton, Southampton, United Kingdom; Centro de Investigación Mariña, GEOMA, Palaeoclimatology Lab, Universidade de Vigo, Vigo, Spain
Recommended Citation:
Yu J.,Menviel L.,Jin Z.D.,et al. Last glacial atmospheric CO2 decline due to widespread Pacific deep-water expansion[J]. Nature Geoscience,2020-01-01,13(9)