Li-yuan Zheng , Yong Zhang , Lei Tang , Chao Lu , Bo Tan , Lai Jiang , Jin-meng Tang , Cheng-bang An
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Warming promotes soil carbon sequestration in the Tianshan Mountains
Alpine ecosystems are critical components of the global carbon cycle, not only because they store substantial organic carbon, but also due to their high sensitivity to climate change, which has garnered considerable scientific interest. However, under ongoing climate warming, the dynamics and underlying mechanisms of alpine soil organic carbon (SOC) are not yet quantified, thereby introducing uncertainties in predictions of carbon–climate feedbacks. To elucidate the response mechanisms of soil carbon dynamics in alpine ecosystems, this study focuses on the Tianshan Mountains—a representative alpine system in the arid region of Central Asia—through an integrated approach combining field surveys and published data. The results showed that SOC content exhibited a clear altitude-dependent pattern across different vegetation types, and that climate warming generally promoted SOC sequestration in alpine soils. Linear mixed-effects analysis indicated that SOC sequestration may be enhanced via two key mechanisms: (1) warming promotes the accumulation of plant-derived microbial-transformed carbon; and (2) warming promotes carbon stabilization through soil weathering processes. These findings advance our mechanistic understanding of altitudinal SOC dynamics under climate change and provide quantitative evidence that alpine ecosystems act as persistent carbon sinks, which has significant potential for global climate regulation.
期刊介绍:
The objective of the journal Global and Planetary Change is to provide a multi-disciplinary overview of the processes taking place in the Earth System and involved in planetary change over time. The journal focuses on records of the past and current state of the earth system, and future scenarios , and their link to global environmental change. Regional or process-oriented studies are welcome if they discuss global implications. Topics include, but are not limited to, changes in the dynamics and composition of the atmosphere, oceans and cryosphere, as well as climate change, sea level variation, observations/modelling of Earth processes from deep to (near-)surface and their coupling, global ecology, biogeography and the resilience/thresholds in ecosystems.
Key criteria for the consideration of manuscripts are (a) the relevance for the global scientific community and/or (b) the wider implications for global scale problems, preferably combined with (c) having a significance beyond a single discipline. A clear focus on key processes associated with planetary scale change is strongly encouraged.
Manuscripts can be submitted as either research contributions or as a review article. Every effort should be made towards the presentation of research outcomes in an understandable way for a broad readership.