State Key Laboratory for Mineral Deposits Research, School of Earth Sciences and Engineering, Nanjing University, Nanjing, 210023, China; Centre for Research and Education on Biological Evolution and Environment, Nanjing University, Nanjing, 210023, China; Department of Earth and Planetary Sciences, Yale University, New Haven, CT, United States; School of Earth and Environment, University of Leeds, Leeds, United Kingdom; State Key Laboratory of Palaeobiology and Stratigraphy & Center for Excellence in Life and Paleoenvironment, Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, Nanjing, 210008, China; Department of Geological Sciences, Stanford University, Stanford, CA 94305, United States; School of Earth and Atmospheric Sciences, Georgia Institute of Technology, Atlanta, GA, United States
Recommended Citation:
Wei G.-Y.,Planavsky N.J.,He T.,et al. Global marine redox evolution from the late Neoproterozoic to the early Paleozoic constrained by the integration of Mo and U isotope records[J]. Earth Science Reviews,2021-01-01,214