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  • The AA. investigated the potential effect of permafrost thawing by the analysis of the physical-chemical soil properties of permafrost versus non-permafrost sites. Specifically, they 1) quantified the SOM stocks at such sites, 2) characterised SOM
  • was verified) were investigated in detail. It is confirmed that different decomposition processes occur between permafrost and non-permafrost sites. The results suggest that a warmer climate may not necessarily lead to an increased CO2 release from SOM