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作者单位: | 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; School of Earth and Environment, University of Leeds, Leeds, LS2 9JT, United Kingdom; GeoZentrum Nordbayern, Friedrich-Alexander-Universität Erlangen-Nürnberg, Erlangen, 91054, Germany; London Geochemistry and Isotope Centre, Institute of Earth and Planetary Sciences, University College London and Birkbeck, University of London, Gower Street, London, WC1E 6BT, United Kingdom; Institute of Geosciences, Johannes Gutenberg University Mainz, Mainz, 55128, Germany; State Key Laboratory of Marine Environmental Science, Xiamen University, Xiamen, 361102, China; State Key Laboratory for Mineral Deposits Research, School of Earth Sciences and Engineering, Nanjing University, Nanjing, 210093, China; Department of Earth and Planetary Sciences, University of California–Davis, Davis, CA 95616, United States; State Key Laboratories of Biogeology and Environmental Geology and Geological Processes and Mineral Resources, China University of Geosciences, Wuhan, 430074, China; Department of Geology, University of Cincinnati, Cincinnati, OH 45221-0013, United States
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| Recommended Citation: | |
Chen B.,Chen J.,Qie W.,et al. Was climatic cooling during the earliest Carboniferous driven by expansion of seed plants?[J]. Earth and Planetary Science Letters,2021-01-01,565
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