增温对干旱区土壤微生物多样性及固碳功能的影响OA北大核心CSTPCD
Effects of warming on soil microbial diversity and carbon sequestration in drylands
干旱区约占全球陆地面积41%,是典型生态脆弱区,对气候变化敏感.土壤微生物在干旱区陆地生态系统结构与功能维持方面起着关键作用,如碳氮生物地球化学循环等.然而,气候变暖对干旱区土壤微生物群落影响的研究结果存在较大差异.本文梳理了增温对干旱区土壤微生物多样性与群落结构影响的研究进展,总结了不同研究结果存在差异的原因,并深入分析了增温如何影响微生物调控土壤碳循环的功能.在此基础上提出了未来需要深入研究的方向,如加强增温与多个全球变化因子交互作用的研究;开展不同增温幅度和增温时长对不同生态系统土壤微生物群落功能影响的研究;利用多组学分析方法深入探究微生物在碳固持和矿化过程中的作用,为干旱区生态系统可持续发展提供科学基础.
Drylands,which cover about 41%of the Earth's land area,are typical ecologically fragile areas and sensitive to climate change.Soil microbial community plays a crucial role in maintaining ecosystem structure and function in drylands,such as carbon and nitrogen cycling.However,the findings regarding the impacts of climate warming on soil microbial communities in drylands exhibit considerable variation across different studies.Here,we reviewed the responses of soil microbial(bacteria and fungi)diversity and community structure to climate warming,elucidated the underlying reasons for the observed disparities,and conducted a thorough analysis of how warming affects soil microbial functions in regulating soil carbon cycling.Finally,we proposed future development direc-tions:(1)monitoring dynamics of soil microbial communities in various ecosystems at large spatial scale involving the interaction of multiple global change factors in drylands;(2)expanding the studies of microbial community at different warming extents and ecosystems for long period;and(3)thoroughly investigating the roles of soil microor-ganisms in carbon sequestration and mineralization in drylands,by employing multi-omics analytical methods.These efforts will provide a scientific foundation for the sustainable management of dryland ecosystems.
张韶阳;樊丹丹;孔维栋
中国科学院青藏高原研究所,青藏高原地球系统与资源环境国家重点实验室,北京 100101||中国科学院大学资源与环境学院,北京 101408
土壤微生物群落干旱区增温固碳功能
soil microbial communitydrylandclimate warmingcarbon sequestration
《生态学杂志》 2024 (006)
1817-1823 / 7
国家自然科学基金项目(42177101和32161123004)和国家重点研发计划项目(2022YFE0114000)资助.
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