Rising global temperatures reduce soil microbial diversity over the long term

全球变暖 土壤碳 环境科学 生态系统 气候变化 固碳 多样性指数 物种丰富度 全球变化 生态学 生物多样性 土壤水分 土壤科学 生物 二氧化碳
作者
Yuan Sun,Han Y. H. Chen,Xin Chen,Masumi Hisano,Han Y. H. Chen,Peter B. Reich,Xinli Chen,Peter B. Reich
出处
期刊:Proceedings of the National Academy of Sciences of the United States of America [National Academy of Sciences]
卷期号:122 (35): e2426200122-e2426200122 被引量:4
标识
DOI:10.1073/pnas.2426200122
摘要

Soil microbial diversity is crucial to sustaining ecosystem productivity and improving carbon sequestration. Global temperature continues to rise, but how climate warming affects microbial diversity and its capacity to sequester soil organic carbon (SOC) remains uncertain. Here, by conducting a global meta-analysis with 251 paired observations from 102 studies, we showed that, on average, warming reduced bacterial and fungal diversity (measured by richness and Shannon index) by 16.0 and 19.7%, respectively, and SOC by 18.1%. The negative responses of both soil bacterial and fungal diversity to warming became more pronounced with increasing warming magnitude, experimental duration, and decreasing soil nitrogen availability. Under the worst-case climate warming scenario (2010 to 2070, 3.4 increase in °C), soil bacterial diversity and fungal diversity are projected to reduce by 56% and 81%, respectively, over 60 y. Importantly, in addition to the direct impact of warming on SOC, warming-induced declines in microbial diversity also contributed to SOC losses. We highlight that prolonged warming could substantially reduce soil microbial diversity and decrease SOC sequestration, accelerating future warming and underscoring the urgent need for decisive actions to mitigate global climate change.
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