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      Onset and ending of the late Palaeozoic ice age triggered by tectonically paced rock weathering

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      Nature Geoscience
      Springer Nature

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          Abstract

          The late Palaeozoic was characterized by glacial cycles. Numerical simulations suggest that increased silicate weathering due to mountain uplift and soil removal caused atmospheric CO2 to fall below the threshold for glaciation.

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          Author and article information

          Journal
          Nature Geoscience
          Nature Geosci
          Springer Nature
          1752-0894
          1752-0908
          April 10 2017
          April 10 2017
          :
          :
          Article
          10.1038/ngeo2931
          d5e69bd7-aa78-45a0-8ea3-1ec7d1d149ca
          © 2017
          History

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