Lhasa Plateau Ecosystem Research Station, Key Laboratory of Ecosystem Network Observation and Modeling, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China.
Lhasa Plateau Ecosystem Research Station, Key Laboratory of Ecosystem Network Observation and Modeling, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China; University of Chinese Academy of Sciences, Beijing 100049, China.
Sci Total Environ. 2024 Dec 10;955:176961. doi: 10.1016/j.scitotenv.2024.176961. Epub 2024 Oct 16.
Soil microorganisms act as the primary decomposers in global terrestrial ecosystems. Whether climate warming will lead to the convergence of the temperature sensitivity of soil microbial community structure and the convergence of the responses of soil microbial community structure to warming remains controversial. This study explored how warming amplitude affected the temperature sensitivity of soil bacteria and fungi community structures, and how it influenced the responses of soil bacteria and fungi community structures to warming on the Qinghai-Tibet Plateau based on meta-analysis and a single-site warming experiment. The temperature sensitivity of soil microbial community structure did not consistently decline with increasing warming magnitude; instead, it even rose, which might be associated with the nonlinear relationships of the warming magnitude with the temperature sensitivity of ecological processes of soil microbial community assembly or the topological parameters of species co-occurrence network. Meta-analysis indicated that responses of soil microbial community to warming were independent of warming amplitude. However, the single-site warming experiment demonstrated that responses of soil microbial community to warming varied with warming amplitude. These inconsistent results might be attributed to distinct spatial scales, grassland types, climatic conditions and warming magnitudes between the single-site experiment and the meta-analysis. Therefore, the temperature sensitivity of soil microbial community and its response to climate warming cannot be simply characterized as monotonically decreasing or increasing in relation to increasing warming magnitude.
土壤微生物是全球陆地生态系统中主要的分解者。气候变暖是否会导致土壤微生物群落结构的温度敏感性趋同以及土壤微生物群落结构对变暖的响应趋同,这一问题仍存在争议。本研究通过荟萃分析和单站点增温实验,探讨了增温幅度如何影响青藏高原土壤细菌和真菌群落结构的温度敏感性,以及如何影响土壤细菌和真菌群落结构对变暖的响应。土壤微生物群落结构的温度敏感性并未随增温幅度的增加而一致下降,甚至有所上升,这可能与增温幅度与土壤微生物群落组装的生态过程的温度敏感性或物种共存网络的拓扑参数之间的非线性关系有关。荟萃分析表明,土壤微生物群落对变暖的响应与增温幅度无关。然而,单站点增温实验表明,土壤微生物群落对变暖的响应随增温幅度而变化。这些不一致的结果可能归因于单站点实验和荟萃分析之间在空间尺度、草地类型、气候条件和增温幅度上的差异。因此,土壤微生物群落的温度敏感性及其对气候变暖的响应不能简单地用与增温幅度增加相关的单调减少或增加来描述。