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A Third of Organic Carbon Is Mineral Bound in Permafrost Sediments Exposed by the World's Largest Thaw Slump, Batagay, Siberia

Author

Listed:
  • Maxime Thomas
  • Loeka L. Jongejans
  • Jens Strauss
  • Chloé Vermylen
  • Sacha Calcus
  • Thomas Opel
  • Alexander Kizyakov
  • Sebastian Wetterich
  • Guido Grosse
  • Sophie Opfergelt

Abstract

Organic carbon (OC) in permafrost interacts with the mineral fraction of soil and sediments, representing

Suggested Citation

  • Maxime Thomas & Loeka L. Jongejans & Jens Strauss & Chloé Vermylen & Sacha Calcus & Thomas Opel & Alexander Kizyakov & Sebastian Wetterich & Guido Grosse & Sophie Opfergelt, 2024. "A Third of Organic Carbon Is Mineral Bound in Permafrost Sediments Exposed by the World's Largest Thaw Slump, Batagay, Siberia," Permafrost and Periglacial Processes, John Wiley & Sons, vol. 35(3), pages 278-293, July.
    • Handle: RePEc:wly:perpro:v:35:y:2024:i:3:p:278-293
    DOI: 10.1002/ppp.2230
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    References listed on IDEAS

    as
    1. S. V. Kokelj & T. C. Lantz & J. Kanigan & S. L. Smith & R. Coutts, 2009. "Origin and polycyclic behaviour of tundra thaw slumps, Mackenzie Delta region, Northwest Territories, Canada," Permafrost and Periglacial Processes, John Wiley & Sons, vol. 20(2), pages 173-184, April.
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