Low N Deposition Coupled With Climate Warming Promote Soil Asymbiotic N Fixation via Increasing Microbial Specialists in Alpine Grassland

Biological nitrogen fixation (BNF) is a vital process for introducing new N into natural ecosystems, and this process has been demonstrated to be suppressed by high N deposition. However, the net ecological effect and underlying mechanisms of BNF under chronic low-level N deposition, characteristic of terrestrial ecosystems, remain highly uncertain. Given that climate warming is a key environmental change factor concurrent with N deposition, it is important to investigate whether climate warming can change BNF activity and alter the effects of N deposition on BNF. To fill these knowledge gaps, we implemented a decade-long-term manipulation experiment in an alpine grassland ecosystem with 5 treatments, that is, experimental warming (W), low-level N deposition (N<sub>L</sub>), high-level N deposition (N<sub>H</sub>), combination of climate warming and low-level N deposition (WN<sub>L</sub>) and the control (CK). BNF rate was measured by <sup>15</sup>N<sub>2</sub> isotope discrimination. We found that N<sub>L</sub> significantly stimulated BNF by 112%, contrasting sharply with the complete suppression under N<sub>H</sub>. Climate warming alone increased the BNF rate by 123%, while the WN<sub>L</sub> amplified this effect, stimulating BNF by 234%. Structural equation modeling revealed that WN<sub>L</sub> selectively favored specific diazotrophic groups (Desulfovibrio), whose proliferation directly drove the observed BNF shifts. In this N-limited alpine grassland, low-level chronic N deposition, especially when combined with warming, fundamentally shifts the diazotrophic community structure by driving a process of niche contraction. This selection process functionally enriches specialized diazotrophs, resulting in a dramatic, positive feedback that significantly promotes the overall biological nitrogen input. Our findings highlight the potential for increased N inputs under realistic future climate scenarios and provide a scientific basis for precision N management in alpine grasslands, both on the Qinghai-Tibetan Plateau and worldwide.

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Publication Details

Journal
Global Change Biology
Published
2026-02-01
DOI
https://doi.org/10.1111/gcb.70751
Primary Topic
Soil Carbon and Nitrogen Dynamics
Type
article
Field-Weighted Citation Impact
0.00

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article

Low N Deposition Coupled With Climate Warming Promote Soil Asymbiotic N Fixation via Increasing Microbial Specialists in Alpine Grassland

Yaoming Li, Huaiying YAO, Ran Zhang, Hang Shi et al.
Global Change Biology
Soil Carbon and Nitrogen Dynamics
article

Low N Deposition Coupled With Climate Warming Promote Soil Asymbiotic N Fixation via Increasing Microbial Specialists in Alpine Grassland

Yaoming Li, Huaiying YAO, Ran Zhang, Hang Shi, Juejie Yang, Wenli Ding, Shikui Dong, Anna Du, Ke Zhang, Hao Shen, Zuyan Ma, Richard D. Bardgett
article en

Abstract

Biological nitrogen fixation (BNF) is a vital process for introducing new N into natural ecosystems, and this process has been demonstrated to be suppressed by high N deposition. However, the net ecological effect and underlying mechanisms of BNF under chronic low-level N deposition, characteristic of terrestrial ecosystems, remain highly uncertain. Given that climate warming is a key environmental change factor concurrent with N deposition, it is important to investigate whether climate warming can change BNF activity and alter the effects of N deposition on BNF. To fill these knowledge gaps, we implemented a decade-long-term manipulation experiment in an alpine grassland ecosystem with 5 treatments, that is, experimental warming (W), low-level N deposition (N<sub>L</sub>), high-level N deposition (N<sub>H</sub>), combination of climate warming and low-level N deposition (WN<sub>L</sub>) and the control (CK). BNF rate was measured by <sup>15</sup>N<sub>2</sub> isotope discrimination. We found that N<sub>L</sub> significantly stimulated BNF by 112%, contrasting sharply with the complete suppression under N<sub>H</sub>. Climate warming alone increased the BNF rate by 123%, while the WN<sub>L</sub> amplified this effect, stimulating BNF by 234%. Structural equation modeling revealed that WN<sub>L</sub> selectively favored specific diazotrophic groups (Desulfovibrio), whose proliferation directly drove the observed BNF shifts. In this N-limited alpine grassland, low-level chronic N deposition, especially when combined with warming, fundamentally shifts the diazotrophic community structure by driving a process of niche contraction. This selection process functionally enriches specialized diazotrophs, resulting in a dramatic, positive feedback that significantly promotes the overall biological nitrogen input. Our findings highlight the potential for increased N inputs under realistic future climate scenarios and provide a scientific basis for precision N management in alpine grasslands, both on the Qinghai-Tibetan Plateau and worldwide.

Global Change BiologyVol. 32(2)
University of Manchester (GB), Beijing Forestry University (CN), Wuhan Institute of Technology (CN)
National Natural Science Foundation of China, National Key Research and Development Program of China
Openalex Percentile: Top 51%
Soil Carbon and Nitrogen Dynamics
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