Soil Microbes as Key Drivers of Global Carbon Cycling in the Context of Climatic Change
DOI:
https://doi.org/10.58445/rars.3742Keywords:
soil ecology, global carbon cycle, climate change, carbon cycling, microbiology, global warming, microbial metabolism, terrestrial ecosystems, metagenomics, metatranscriptomics, nutrient cyclingAbstract
Soil microbial communities function as key regulators of the global carbon cycle, controlling the largest carbon pool found in terrestrial ecosystems. Ongoing climate change, particularly rising temperatures and increased atmospheric carbon dioxide, influences these communities through both direct effects on microbial metabolism and indirect interactions mediated by plants. Evidence gathered in this review indicates that long term warming commonly promotes an “oligotrophic shift,” where microbial assemblages become dominated by organisms adapted to nutrient-poor conditions and more complex, resistant carbon substrates. In contrast, elevated carbon dioxide enhances plant root activity and increases the release of organic compounds into the soil, leading to rhizosphere driven processes that can stimulate the decomposition of previously stable soil organic matter through priming effects.
A key conceptual advance highlighted here is the understanding that the persistence of soil organic matter is not determined solely by its chemical composition, but instead emerges from ecosystem-level controls, including microbial accessibility and physical protection within the soil matrix. Despite recent progress, a major challenge remains in connecting fine-scale microbial mechanisms with large scale Earth system models. Integrating detailed process-based information such as functional gene activity and microbial carbon use efficiency will be essential to move beyond simplified modeling approaches and improve predictions of climate carbon feedbacks. Overall, this review underscores the fundamental role of soil microbial processes in shaping the future stability of global carbon reserves.
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