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Responses of soil C pools to combined warming and altered precipitation regimes: A meta-analysis |
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| Authors: | Xinyu Wei,Koenraad Van Meerbeek,Kai Yue,Xiangyin Ni,Ellen Desie,Petr Heděnec,Jing Yang,Fuzhong Wu |
| Affiliation: | 1. Key Laboratory for Humid Subtropical Eco-Geographical Processes of the Ministry of Education, School of Geographical Sciences, Fujian Normal University, Fuzhou, China Department of Earth and Environmental Sciences, KU Leuven, Leuven, Belgium;2. Department of Earth and Environmental Sciences, KU Leuven, Leuven, Belgium KU Leuven Plant Institute, KU Leuven, Leuven, Belgium;3. Key Laboratory for Humid Subtropical Eco-Geographical Processes of the Ministry of Education, School of Geographical Sciences, Fujian Normal University, Fuzhou, China;4. Department of Earth and Environmental Sciences, KU Leuven Campus Geel, Geel, Belgium;5. Institute of Tropical Biodiversity and Sustainable Development, University Malaysia Terengganu, Kuala Nerus, Malaysia |
| Abstract: | AimGlobal warming and altered precipitation substantially affect soil carbon (C) pools and can, in turn, feed back into climate change. However, how soil C pools respond to the combined effects of warming and altered precipitation remains unclear.LocationGlobal.Time period1996–2021.Major taxa studiedSoil organic C pools.MethodA meta-analysis was performed using 657 observations obtained from 34 published articles that focused on both individual and combined effects of warming and altered precipitation on soil organic C (SOC), dissolved organic C (DOC) and microbial biomass C (MBC) to quantify the responses of soil C pools.ResultsAcross all combined warming and increased precipitation experiments, SOC and MBC increased by an average of 4.0% and 15.4%, respectively. In contrast, warming combined with decreased precipitation led to a substantial decline in SOC and MBC by an average of 8.2% and 12.3%, respectively. The responses of DOC to combined warming and altered precipitation were marginal. The direction and magnitude of the responses to the combined treatment were more similar to those in the individual altered precipitation treatment than to those in the individual warming treatment. Furthermore, these combined effects were substantially influenced by altered precipitation magnitudes. Combined warming and altered precipitation had greater impacts on soil C pools than their individual treatments but were not substantially different from the sum of their respective individual effects, showing overall additive effects. The responses of soil C pools to combined warming and altered precipitation were observed to be more pronounced in grasslands than in forests.Main conclusionThe results demonstrated that altered precipitation regimes often dominated over warming in regulating soil C pools under combined warming and altered precipitation and improved our understanding of soil C cycles under climate change scenarios. |
| Keywords: | dissolved organic carbon global climate change interactive effect meta-analyses microbial biomass carbon soil organic carbon |