7.3 The Palaeoproterozoic Perturbation of the Global Carbon Cycle: The Lomagundi-Jatuli Isotopic Event

  • Victor A. Melezhik
  • Anthony E. Fallick
  • Adam P. Martin
  • Daniel J. Condon
  • Lee R. Kump
  • Alex T. Brasier
  • Paula E. Salminen
Part of the Frontiers in Earth Sciences book series (FRONTIERS)


On Earth, carbon cycles through the land, ocean, atmosphere, living and dead biomass and the planet’s interior. The global carbon cycle can be divided into the tectonically driven geological cycle and the biological/physicochemical cycles. The former operates over millions of years, whereas the latter operate over much shorter time scales (days to thousands of years). Within the geological cycle, atmospheric carbon dioxide concentration is controlled by the balance between weathering, biological drawdown, size of sedimentary reservoir, subduction, metamorphism and volcanism over time periods of hundreds of millions of years.


Carbon Isotope Detrital Zircon Greenstone Belt Global Carbon Cycle Sedimentary Formation 
These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.


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Copyright information

© Springer-Verlag Berlin Heidelberg 2013

Authors and Affiliations

  • Victor A. Melezhik
    • 1
    • 2
  • Anthony E. Fallick
    • 3
  • Adam P. Martin
    • 4
  • Daniel J. Condon
    • 4
  • Lee R. Kump
    • 5
  • Alex T. Brasier
    • 3
  • Paula E. Salminen
    • 6
  1. 1.Geological Survey of NorwayTrondheimNorway
  2. 2.Centre for GeobiologyUniversity of BergenBergenNorway
  3. 3.Scottish Universities Environmental Research CentreGlasgowScotland, UK
  4. 4.NERC Isotope Geosciences Laboratory (NIGL)NottinghamUK
  5. 5.Department of GeosciencesPennsylvanian State UniversityUniversity ParkUSA
  6. 6.Department of Geosciences and GeographyUniversity of HelsinkiHelsinkiFinland

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