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

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

Permafrost and Periglacial Processes, 2024, vol. 35, issue 3, 278-293

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

Date: 2024
References: Add references at CitEc
Citations:

Downloads: (external link)
https://doi.org/10.1002/ppp.2230

Related works:
This item may be available elsewhere in EconPapers: Search for items with the same title.

Export reference: BibTeX RIS (EndNote, ProCite, RefMan) HTML/Text

Persistent link: https://EconPapers.repec.org/RePEc:wly:perpro:v:35:y:2024:i:3:p:278-293

Access Statistics for this article

More articles in Permafrost and Periglacial Processes from John Wiley & Sons
Bibliographic data for series maintained by Wiley Content Delivery ().