Guangdong Provincial Key Laboratory of Microbial Safety and Health, State Key Laboratory of Applied Microbiology Southern China, Key Laboratory of Agricultural Microbiomics and Precision Application, Ministry of Agriculture and Rural Affairs, Institute of Microbiology, Guangdong Academy of Sciences, Xianlie Road 100#, Guangzhou, 510070, China.
South China Botanical Garden, Chinese Academy of Sciences, Guangzhou, 510650, China.
Microb Ecol. 2023 Jul;86(1):521-535. doi: 10.1007/s00248-022-02092-8. Epub 2022 Aug 4.
Increased nitrogen deposition (N factor) and changes in precipitation patterns (W factor) can greatly impact soil microbial communities in tropical/subtropical forests. Although knowledge about the effects of a single factor on soil microbial communities is growing rapidly, little is understood about the interactive effects of these two environmental change factors. In this study, we investigated the responses of soil bacterial and fungal communities to the short-term simulated environmental changes (nitrogen addition, precipitation seasonality change, and their combination) in a subtropical forest in South China. The interaction between N and W factors was detected significant for affecting some soil physicochemical properties (such as pH, soil water, and NO contents). Fungi were more susceptible to treatment than bacteria in a variety of community traits (alpha, beta diversity, and network topological features). The N and W factors act antagonistically to affect fungal alpha diversity, and the interaction effect was detected significant for the dry season. The topological features of the meta-community (containing both bacteria and fungi) network overrode the alpha and beta diversity of bacterial or fungal communities in explaining the variation of soil enzyme activities. The associations between Ascomycota fungi and Gammaproteobacteria or Alphaproteobacteria might be important in mediating the inter-kingdom interactions. In summary, our results suggested that fungal communities were more sensitive to N and W factors (and their interaction) than bacterial communities, and the treatments' effects were more prominent in the dry season, which may have great consequences in soil processes and ecosystem functions in subtropical forests.
氮沉降(N 因子)增加和降水格局变化(W 因子)会极大地影响热带/亚热带森林的土壤微生物群落。尽管关于单一因素对土壤微生物群落影响的知识正在迅速增加,但对这两个环境变化因素的交互作用知之甚少。在这项研究中,我们调查了亚热带森林中短期模拟环境变化(氮添加、降水季节性变化及其组合)对土壤细菌和真菌群落的响应。N 和 W 因子之间的相互作用对一些土壤理化性质(如 pH 值、土壤水分和 NO 含量)的影响是显著的。与细菌相比,真菌在多种群落特征(α、β多样性和网络拓扑特征)上对处理更敏感。N 和 W 因子对抗地影响真菌的 α 多样性,并且在旱季检测到显著的互作效应。包含细菌和真菌的元群落网络的拓扑特征在解释土壤酶活性变化方面超过了细菌或真菌群落的α和β多样性。子囊菌真菌与γ变形菌或α变形菌之间的关联可能在调节种间相互作用方面很重要。总之,我们的结果表明,真菌群落对 N 和 W 因素(及其相互作用)比细菌群落更敏感,并且在旱季处理效果更为显著,这可能对亚热带森林的土壤过程和生态系统功能产生重大影响。