Evolution of a deep-water ferromanganese nodule in the South China Sea in response to Pacific deep-water circulation and continental weathering during the Plio-Pleistocene
University of the Chinese Academy of Sciences, Beijing, 100049, China; Center for Marine Magnetism (CM2), Department of Ocean Science and Engineering, Southern University of Science and Technology, Shenzhen, 518055, China; Key Laboratory of Ocean and Marginal Sea Geology, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou, 510301, China; Key Laboratory of Marine Geology and Environment, Institute of Oceanology, Chinese Academy of Sciences, Qingdao, 266071, China; U.S. Geological Survey, PCMSC, 2885 Mission St., Santa Cruz, CA 95060, United States; Marine Geology Division, Geological Survey of Spain (IGME), Madrid, 28003, Spain; College of Marine Geosciences, Ocean University of China, Qingdao, 266100, China; Department of Earth Science, Sun Yat-Sen University, Guangzhou, 510275, China; MARUM-Center for Marine Environmental Sciences and Faculty of Geosciences, University of Bremen, Bremen, 128359, Germany; Key Laboratory of Marine Sedimentology and Environmental Geology, First Institute of Oceanography, Ministry of Natural Resources, Qingdao, 266061, China; Laboratory for Marine Geology, Qingdao National Oceanography Laboratory for Marine Science and Technology, Qingdao, 266061, China; Department of Earth Sciences, University of Hong Kong, Hong Kong, Hong Kong
Recommended Citation:
Zhong Y.,Chen Z.,Hein J.R.,et al. Evolution of a deep-water ferromanganese nodule in the South China Sea in response to Pacific deep-water circulation and continental weathering during the Plio-Pleistocene[J]. Quaternary Science Reviews,2020-01-01,229