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Updated: Feb 20, 2026

A CO2 Concentration Gradient Facility for Testing CO2 Enrichment and Soil Effects on Grassland Ecosystem Function
Published on: November 21, 2015
Low N Deposition Coupled With Climate Warming Promote Soil Asymbiotic N Fixation via Increasing Microbial Specialists
Ke Zhang1, Yaoming Li1, Ran Zhang1
1School of Grassland Science, Beijing Forestry University, Beijing, China.
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 (NL), high-level N deposition (NH), combination of climate warming and low-level N deposition (WNL) and the control (CK). BNF rate was measured by 15N2 isotope discrimination. We found that NL significantly stimulated BNF by 112%, contrasting sharply with the complete suppression under NH. Climate warming alone increased the BNF rate by 123%, while the WNL amplified this effect, stimulating BNF by 234%. Structural equation modeling revealed that WNL 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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