Nature-Based Global Land Surface Soil Organic Carbon
Recent studies suggest that nature-based processes are contributing to an overall increase in global land surface soil organic carbon (SOC), largely driven by climate change. As temperatures rise and precipitation patterns shift, vegetation dynamics, microbial activity, and carbon sequestration are being altered in ways that enhance carbon storage in soils. While this may appear as a positive feedback, it is closely tied to regional variability and complex interactions between soil, climate, and ecosystems. This evolving trend highlights the crucial role of soil in mitigating climate change and underscores the need for sustained monitoring and land management strategies that support soil health and carbon retention.
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