Xu Jianjun, Liu Hao, Xu Xiaoni, Liu Xiang, Zhou Shurong, Nie Ming
State Key Laboratory of Wetland Conservation and Restoration, National Observations and Research Station for Wetland Ecosystems of the Yangtze Estuary, Ministry of Education Key Laboratory for Biodiversity Science and Ecological Engineering, and Institute of Eco-Chongming, School of Life Sciences, Fudan University, No. 2005, Songhu Road, Yangpu District, Shanghai, China.
State Key Laboratory of Herbage Improvement and Grassland Agro-Ecosystems, College of Ecology, Lanzhou University, Lanzhou, China.
Environ Microbiome. 2025 Mar 25;20(1):35. doi: 10.1186/s40793-025-00693-7.
The diversity of bacteria and fungi is linked to distinct ecosystem functions, and divergent responses to global changes in these two kingdoms affect the relative contributions of the kingdoms to the soil carbon and nutrient cycles. Climate warming and nitrogen (N) enrichment, which are projected to increase concurrently through modelling efforts, are considered the main drivers of biodiversity loss. However, it is unclear how bacterial and fungal diversity respond differently to the simultaneous occurrence of climate warming and nitrogen enrichment, and the underlying mechanisms involved remain unknown. Using a 9-yr warming and N enrichment experiment in an alpine permafrost area of the Tibetan Plateau, we demonstrated the contrasting response of bacterial and fungal diversity to combined warming and N enrichment, showing a reduction in bacterial richness (8.8%) and an increase in fungal diversity (33.6%). Furthermore, the negative effects of warming on fungal richness were reversed by N enrichment, and the negative effects of nitrogen enrichment on bacteria were amplified by warming. Our results also demonstrated that both biotic interactions, such as bacterial-fungal antagonism, and abiotic factors, primarily the soil C/N ratio and pH, play crucial roles in shaping microbial biodiversity. Our findings suggest that fungal diversity is expected to greatly increase in a warmer and more nitrogen-enriched world, potentially leading to the enhancement of ecosystem functions driven by fungi.
细菌和真菌的多样性与不同的生态系统功能相关联,这两个王国对全球变化的不同反应影响了它们对土壤碳和养分循环的相对贡献。通过模型预测,气候变暖和氮(N)富集预计将同时增加,它们被认为是生物多样性丧失的主要驱动因素。然而,目前尚不清楚细菌和真菌多样性如何对气候变暖和氮富集同时发生做出不同反应,其背后的机制仍然未知。在青藏高原高寒冻土区进行了为期9年的变暖和氮富集实验,我们证明了细菌和真菌多样性对变暖和氮富集组合的对比反应,细菌丰富度降低了8.8%,而真菌多样性增加了33.6%。此外,氮富集逆转了变暖对真菌丰富度的负面影响,而变暖放大了氮富集对细菌的负面影响。我们的结果还表明,生物相互作用,如细菌 - 真菌拮抗作用,以及非生物因素,主要是土壤碳氮比和pH值,在塑造微生物多样性方面都起着关键作用。我们的研究结果表明,在一个更温暖、氮含量更高的世界中,真菌多样性预计将大幅增加,这可能会导致由真菌驱动的生态系统功能增强。