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Article
Permafrost carbon cycle and its dynamics on the Tibetan Plateau
Our knowledge on permafrost carbon (C) cycle is crucial for understanding its feedback to climate warming and develo** nature-based solutions for mitigating climate change. To understand the characteristics ...
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Article
Open AccessDivergent changes in particulate and mineral-associated organic carbon upon permafrost thaw
Permafrost thaw can stimulate microbial decomposition and induce soil carbon (C) loss, potentially triggering a positive C-climate feedback. However, earlier observations have concentrated on bulk soil C dynam...
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Article
Open AccessNitrogen availability regulates topsoil carbon dynamics after permafrost thaw by altering microbial metabolic efficiency
Input of labile carbon may accelerate the decomposition of existing soil organic matter (priming effect), with the priming intensity depending on changes in soil nitrogen availability after permafrost thaw. Ho...
