Climate warming promotes deterministic assembly of arbuscular mycorrhizal fungal communities

全球变暖 植物群落 生态学 气候变化 微生物种群生物学 降水 群落结构 农学 环境科学 生态系统 丛枝菌根真菌 土壤水分 嵌套 土壤碳 社区 全球变化 生物 全球变暖的影响 生长季节 球囊菌门 陆地生态系统 扰动(地质) 营养物 环境变化 乡土植物 农林复合经营 资源(消歧) 植物生态学 生物多样性 生产力
作者
Xinyu Xu,Yunpeng Qiu,Kangcheng Zhang,Fei Yang,Mengfei Chen,Xi Luo,Xuebin Yan,Peng Wang,Yi Zhang,Huaihai Chen,Hui Guo,Lin Jiang,Shuijin Hu
出处
期刊:Global Change Biology [Wiley]
卷期号:28 (3): 1147-1161 被引量:92
标识
DOI:10.1111/gcb.15945
摘要

Abstract Arbuscular mycorrhizal fungi (AMF) significantly contribute to plant resource acquisition and play important roles in mediating plant interactions and soil carbon (C) dynamics. However, it remains unclear how AMF communities respond to climate change. We assessed impacts of warming and precipitation alterations (30% increase or decrease) on soil AMF communities, and examined major ecological processes shaping the AMF community assemblage in a Tibetan alpine meadow. Our results showed that warming significantly increased root biomass, and available nitrogen (N) and phosphorus (P) in soil. While precipitation alterations increased AMF abundances, they did not significantly affect the composition or diversity of AMF communities. In contrast, warming altered the composition of AMF communities and reduced their Shannon–Wiener index and Pielou's evenness. In particular, warming shifted the AMF community composition in favor of Diversisporaceae over Glomeraceae, likely through its impact on soil N and P availability. In addition, AMF communities were phylogenetically random in the unwarmed control but clustered in warming plots, implying more deterministic community assembly under climate warming. Warming enhancement of root growth, N and P availability likely reduced plant C‐allocation to AMF, imposing stronger environmental filtering on AMF communities. We further proposed a conceptual framework that integrates biological and geochemical processes into a mechanistic understanding of warming and precipitation changes’ effects on AMF. Taken together, these results suggest that soil AMF communities may be more sensitive to warming than expected, highlighting the need to monitor their community structure and associated functional consequences on plant communities and soil C dynamics under the future warmer climate.
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