J Plant Ecol ›› Advance articles     DOI:10.1093/jpe/rtag131

• Research Article •     Next Articles

Drivers of asymbiotic nitrogen fixation across alpine grasslands

Wenyin Wang1#, Wenyan Li1#, A. Allan Degen2, Lingyan Qi1, Mei Huang1, Chunyan Wang1, Tianyun Qi1, Yaling Lu3, Zhixiang Gao3, Zhanhuan Shang1*   

  1. 1. State Key Laboratory of Herbage Improvement and Grassland Agro-ecosystems, College of Ecology, Lanzhou University, Lanzhou 730000, China.
    2. Desert Animal Adaptations and Husbandry, Wyler Department of Dryland Agriculture, Blaustein Institutes for Desert Research, Ben-Gurion University of the Negev, Beer Sheva 8410500, Israel.
    3. Qinghai Grassland Improvement Experiment Station, Xining, 810007, China
    *Corresponding author, E-mail: shangzhh@lzu.edu.cn
    # the authors contributed equally to this study
  • Received:2025-10-16 Accepted:2026-03-20 Published:2026-06-13
  • Supported by:
    This work was supported by the Natural Science Foundation of China (32301397, U21A20183), Chief Scientist Program of Qinghai Province (2024-SF-101), the Science-based Advisory Program of The Alliance of National and International Science Organizations for the Belt and Road Regions (ANSO-SBA-2023-02), the Second Tibetan Plateau Expedition (2019QZKK0302), the Gansu Province Science and Technology Program (24JRRA526), the China Post-doctoral Science Foundation (2024M751262).

高寒草地非共生固氮的驱动因素

Abstract: Alpine grasslands are cold and hypoxic, typically lacking symbiotic nitrogen fixation. Nonetheless, they often maintain high nitrogen stocks, which suggests an important role for asymbiotic nitrogen fixation (ANF). However, the ANF rates of soil or plant leaves and their driving factors in alpine grasslands remain unclear. We quantified the ANF rates in soil and plant leaves, the soil stoichiometry and the nifH based community composition and abundance across alpine grasslands (swamp meadow, alpine meadow, and alpine steppe) along an altitudinal gradient between 3100 and 4300 m above sea level (a. s. l). The ANF rates in swamp and alpine meadows were faster than in alpine steppe. Diazotroph communities were dominated by Proteobacteria (85%) and Actinobacteria (12%), and 72 nifH OTUs assigned to Cluster II (anfH/vnfH-like) suggested the potential presence of alternative nitrogenase-related homologs. Specialist taxa in soil ANF bacteria were influenced mainly by stochastic processes and exhibited faster transition rates than generalists. Random forest analyses identified soil pH, nifH diversity and composition, soil stoichiometry, and molybdenum as key predictors of soil ANF. Estimated annual nitrogen inputs were 4.0, 3.1, and 0.5 kg N ha-1 yr-1 in alpine meadow, swamp meadow, and alpine steppe, respectively. Our results indicate that ANF represents a significant nitrogen input pathway in alpine grasslands and should be incorporated into nitrogen cycling and regional nitrogen budgets.

Asymbiotic nitrogen fixation provides an important nitrogen input in alpine grasslands. Its rates vary among grassland types and are mainly regulated by soil chemistry, molybdenum availability, and diazotroph community structure.

Key words: alpine grasslands, asymbiotic nitrogen fixation, niche breadth, nifH gene, stoichiometry

摘要:
高寒草地环境寒冷且低氧,通常缺乏共生固氮作用。尽管如此,这类生态系统往往仍维持较高的氮储量,这表明非共生固氮可能发挥着重要作用。然而,高寒草地中土壤或植物叶片的非共生固氮速率及其驱动因素仍不清楚。对不同海拔(3100 m–4300 m)高寒草地(沼泽草甸、高山草甸和高寒草原)土壤和植物叶片的非共生固氮速率(ANF)、土壤化学计量以及基于nifH 基因的微生物群落组成和丰度进行了定量分析。结果表明,沼泽草甸和高寒草甸的非共生固氮速率高于高寒草原。固氮微生物群落以变形菌门(Proteobacteria, 85%)和放线菌门(Actinobacteria, 12%)为主。72个OTUs被归类为Cluster II(anfH/vnfH-like),表明高寒草地生态系统中存在其他与nifH基因相关的同源基因。基于非共生固氮菌生态位与组装过程研究,土壤非共生固氮菌中特化种主要受随机过程驱动,并且其转换速率快于泛化种。随机森林进一步分析表明,土壤pH、nifH多样性及其群落组成、土壤化学计量比以及钼含量是影响土壤非共生固氮的重要预测因子。通过估算高寒草甸、沼泽草甸和高寒草原非共生固氮输入量分别为4.0、3.1和0.5 kg N ha–1 yr–1。研究结果表明,非共生固氮是高寒草地中一个重要的氮输入途径,应被纳入氮循环研究和区域氮收支评估中。

关键词: 高寒草地, 非共生固氮, 生态位宽度, nifH基因, 化学计量学