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Appy Sluijs and Gerald R. Dickens Assessing offsets between the δ13C of sedimentary components and the global exogenic carbon pool across early Paleogene carbon cycle perturbations Global Biogeochemical Cycles 26

Version of Record online: 18 OCT 2012 | DOI: 10.1029/2011GB004224

Key Points

  • The d13C changes in sediment records are described in three simple equations
  • Increasing marine organic matter contribution during the PETM enhances the CIE
  • No d13C record precisely records the evolution of global exogenic d13C

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