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. 2025 Apr;36(4):1081-1090.
doi: 10.13287/j.1001-9332.202504.018.

[Ecological stoichiometric imbalance drives the responses of soil bacterial communities to nitrogen addition in an alpine meadow]

[Article in Chinese]
Affiliations

[Ecological stoichiometric imbalance drives the responses of soil bacterial communities to nitrogen addition in an alpine meadow]

[Article in Chinese]
Chen-Xing Lian et al. Ying Yong Sheng Tai Xue Bao. 2025 Apr.

Abstract

Nitrogen is the main limiting nutrient for the productivity of grassland ecosystems, and can indirectly affect the structure of microbial communities, especially bacterial communities, by altering soil properties. In this study, we conducted a field nitrogen addition experiment in the alpine meadow of Haibei in the northeastern Tibetan Plateau. Urea was used as the nitrogen source. Five nitrogen addition levels were set up: N0 (control, no nitrogen addition), N50 (50 kg N·hm-2·a-1), N100 (100 kg N·hm-2·a-1), N150 (150 kg N·hm-2·a-1), and N200 (200 kg N·hm-2·a-1). In the third year of the experiment, we collected soil samples of the surface layer to measure soil physical and chemical properties, stable isotope δ15N, and microbial biomass. The microbial stoichiometric imbalance was calculated, and bacterial community characteristics (composition, diversity, and community assembly) along the nitrogen addition levels were analyzed by 16S rRNA high-throughput sequencing. Through correlation analysis, non-metric multidimensional scaling analyses, and phylogenetic-bin-based null model analyses, we investigated the driving mechanisms of the changes in soil bacterial community composition and community assembly. The results showed that: 1) Nitrogen addition significantly altered soil bacterial community composition, but did not change the α diversity of soil bacteria. 2) Nitrogen addition significantly increased soil inorganic nitrogen content by 85.7% and reduced the stoichiometric imbalance of carbon:nitrogen by 40.6%. Soil inorganic nitrogen content and carbon:nitrogen stoichiometric imbalance were significantly correlated with bacterial community composition and the relative abundance of the dominant phylum (i.e., Bacteroidetes), indicating that bacterial taxa were significantly influenced by soil available nitrogen and stoichiometric imbalance. 3) The stochastic process (54.7%-56.8%) dominated the community assembly of soil bacteria across all treatments. Nitrogen addition had no significant effect on the community assembly of soil bacteria. In conclusion, soil available nitrogen and the resulting stoichiometric imbalance were the primary factors regulating the relative abundance of bacterial taxa under nitrogen addition. Our findings provide a scientific basis for predicting the changes of soil microbial communities in alpine meadows in the context of future environmental changes.

氮是草地生态系统生产力的主要限制性养分,可通过改变土壤性质间接作用于微生物群落结构,特别是细菌群落。本研究在青藏高原东北部的海北高寒草甸开展野外氮添加试验,以尿素为氮源,设置了5个氮添加水平:N0(对照,无氮添加)、N50(50 kg N·hm-2·a-1)、N100(100 kg N·hm-2·a-1)、N150(150 kg N·hm-2·a-1)和N200(200 kg N·hm-2·a-1)。在试验的第3年采集表层土壤样品,测定其理化性质、稳定同位素δ15N和微生物生物量,计算微生物化学计量不平衡性,并通过16S rRNA高通量测序分析细菌群落特征(组成、多样性和群落构建)沿氮添加水平的变化。通过相关性分析、非度量多维尺度分析以及基于系统发育的二元零模型分析,探究土壤细菌群落变化的驱动机制和群落构建过程。结果表明: 1)氮添加显著影响草甸土壤细菌的群落组成,但是土壤细菌α多样性没有显著变化;2)与对照相比,氮添加使土壤无机氮含量显著增加了85.7%,碳∶氮化学计量不平衡性降低了40.6%,且其与细菌群落组成和优势菌门(拟杆菌门)的相对丰度显著相关,表明细菌类群受土壤有效氮及其引起的化学计量不平衡的显著影响;3)所有处理中细菌群落构建的随机性过程(54.7%~56.8%)均占据优势地位,但是氮添加对细菌群落构建过程无明显影响。综上,土壤有效氮及其引起的化学计量不平衡是调控氮添加下细菌类群相对丰度的主要因素,本研究为预测未来环境变化背景下高寒草地土壤微生物群落的变化提供了科学依据。.

Keywords: available nitrogen; community assembly; ecological stoichiometry; high-throughput sequencing; meadow.

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