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Vulnerability of carbon in Cryosols – substrate-microorganisms-aggregate interactions

Subject Area Soil Sciences
Term from 2019 to 2024
Project identifier Deutsche Forschungsgemeinschaft (DFG) - Project number 431968700
 
Final Report Year 2025

Final Report Abstract

The bilateral project CryoVulcan dealt with the consequences of thawing permafrost and its effects on the stability and microbial turnover of soil organic matter (SOM) under different soil hydrological conditions. Year-round monitoring of the redox potential in the soil was accompanied by physico-chemical analyses, stable isotope studies and microbiological analyses at DNA, RNA and metatranscriptome level. Organic carbon (OC) stocks were 60-75% lower in soil profiles of degraded sites, regardless of whether soils were wet or well-drained. Processes such as anaerobic inhibition of microbial decomposition or formation of highly reactive pedogenic mineral phases and pronounced aggregation appeared to stabilize only a small proportion of the organic matter formerly stored in the permafrost in the long term. Losses of OC were mainly detected in the subsoils, while topsoils apparently showed no significant losses due to increased input of plant litter. Hydromorphic subsoils were less anaerobic than assumed, and showed like their well-drained counterparts quite high root density in the subsoil. Laboratory experiments demonstrated an accelerated decomposition of complex organic compounds by root exudates, which are assumed to be released in higher quantities in the degraded soils regardless of their hydrological regime. In-situ incubation experiments with 13C-labeled litter in the soil further indicated a high translocation of organic substances. The results of the Cryo- Vulcan project show that in degrading permafrost soils the effect of alternative stabilization mechanisms is limited and SOM is mobilized, mainly via mineralization, but partly also via translocation in dissolved form. Further research should shed more light on translocation and transformation of SOM in whole degrading permafrost soil landscapes, especially at the interface with the hydrosphere.

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