School of Oceanography, Shanghai Jiao Tong University, Shanghai, China; Open Studio for Ocean-Climate-Isotope Modeling, Pilot National Laboratory for Marine Science and Technology (Qingdao), Qingdao, China; Atmospheric Science Program, Department of Geography, The Ohio State University, Columbus, OH, United States; Department of Geology and Geophysics, Woods Hole Oceanographic Institution, Woods Hole, MA, United States; School of Earth and Atmospheric Sciences, Georgia Institute of Technology, Atlanta, GA, United States; Department for Atmospheric and Oceanic Sciences, Institute of Arctic and Alpine Research, University of Colorado Boulder, Boulder, CO, United States; Cooperative Institute for Climate, Ocean, and Ecosystem Studies, University of Washington, Seattle, WA, United States; NOAA Pacific Marine Environmental Laboratory, Seattle, WA, United States; National Center for Atmospheric Research, Climate and Global Dynamics Division, Boulder, CO, United States; Physical Oceanography Laboratory, Ocean University of China, Qingdao, China
Recommended Citation:
Gu S.,Liu Z.,Oppo D.W.,et al. Remineralization dominating the δ13C decrease in the mid-depth Atlantic during the last deglaciation[J]. Earth and Planetary Science Letters,2021-01-01,571