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变暖通过调节土壤动物群相互作用来降低青藏高原草地凋落物分解。

Warming decreased plant litter decomposition by modulating soil fauna interactions in a Tibetan alpine meadow.

机构信息

Institute of Environment and Sustainable Development in Agriculture, Chinese Academy of Agricultural Sciences, Beijing 100081, China; Key Laboratory for Agro-Environment & Climate Change, Ministry of Agriculture, Beijing 100081, China.

Institute of Environment and Sustainable Development in Agriculture, Chinese Academy of Agricultural Sciences, Beijing 100081, China; Key Laboratory for Agro-Environment & Climate Change, Ministry of Agriculture, Beijing 100081, China; Institute of Plant Nutrition, Resources, and Environment, Beijing Academy of Agricultural and Forestry Sciences, Beijing 100097, China.

出版信息

Sci Total Environ. 2024 Dec 1;954:176332. doi: 10.1016/j.scitotenv.2024.176332. Epub 2024 Sep 18.

Abstract

Litter decomposition is a vital process for maintaining ecosystem carbon cycling. It is affected by soil fauna which are predators and decomposers of litter. However, how the interactions of soil fauna communities affect litter decomposition remains unclear under warming. Here, we conducted a five-year in-situ manipulative warming experiment by Open-Top Chamber (OTC) in an alpine meadow on the Tibetan Plateau to reveal how warming affects litter decomposition. The results demonstrated that warming decreased the litter decomposition rate by 29 %, the soil collembola abundance by 25 %, and the nematode abundance by 27 %. Nematode ecological indices remain stable but a shift in the decomposition of litter to the fungivores pathway under warming. The piecewise structural equation modelling result revealed that the combined reduction in soil collembola and nematodes synergistically leads to a massive decline in litter decomposition rate under warming. Our results highlight that the interactions of soil fauna can regulate litter decomposition under warming, and collembola abundance as the "speed-limiter" of litter decomposition. Therefore, the response of changes in soil fauna relationships to warming should be completely considered in future climate change modelling of the grassland carbon cycle.

摘要

凋落物分解是维持生态系统碳循环的重要过程。它受到土壤动物的影响,土壤动物既是凋落物的捕食者又是分解者。然而,在变暖的情况下,土壤动物群落的相互作用如何影响凋落物分解仍不清楚。在这里,我们通过青藏高原高寒草甸上的开顶式气室(OTC)进行了为期五年的原位控制性增温实验,以揭示增温如何影响凋落物分解。结果表明,增温使凋落物分解率降低了 29%,土壤弹尾目丰度降低了 25%,线虫丰度降低了 27%。线虫生态指数保持稳定,但在增温下,凋落物的分解向食真菌者途径转变。分段结构方程模型的结果表明,土壤弹尾目和线虫数量的综合减少协同作用导致增温下凋落物分解率的大幅下降。我们的结果强调了土壤动物的相互作用可以调节变暖下的凋落物分解,而弹尾目丰度是凋落物分解的“限速器”。因此,在未来的草地碳循环气候变化模型中,应该充分考虑土壤动物关系变化对变暖的响应。

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