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SoilMicrobial Controls Jointly Regulate Elevational Patterns of Free-Living Nitrogen Fixation RateIts Temperature Sensitivity
时间:2026-06-30
作  者:Zhang XM, Deng MF*, Wu YT, Gao YX, Luo J, Pan SN, Liu LL*
影响因子:12.0
刊物名称:Global Change Biology
出版年份:2026
卷:32  期:5  页码:e70897

论文摘要:

Free-living nitrogen fixation (FLNF), like any enzyme-mediated process, is inherently temperature dependent. As FLNF contributes nearly half of global biological nitrogen fixation in natural ecosystems, its response to warming is crucial for predicting how ecosystems will cope with nutrient limitations under climate warming. However, current model studies on climate change often rely on simplified representations of biological nitrogen fixation based on empirical proxies, overlooking microbial thermal acclimationcommunity shifts across climate gradients. To address this gap, we quantified FLNF ratestheir temperature sensitivity (Q10) along a 1500 m elevational gradient in the eastern Himalayas to evaluate how climate, soil propertiesdiazotrophic (nitrogen-fixing) microbial communities jointly regulate FLNF. Our results showed that soil FLNF rates at site-specific MAT exhibited a unimodal pattern, peaking at mid-elevations, rather than following the expected monotonic increase with temperature. This pattern was jointly regulated by soil nutrient conditionsshifts in diazotrophic community composition. In contrast, the Q10 of soil FLNF rates increased with the elevation, being more than twofold higher at the coldest sites. This pattern was primarily driven by elevation-induced shifts in diazotrophic community composition, with Q10 closely associated with community structurepositively related to the relative abundance of Thermodesulfobacteriota. Together, these findings reveal a dual regulatory mechanism: soil nutrient availability constrains the baseline of FLNF rates both directlyindirectly via its effects on diazotrophic community composition, whereas community composition predominantly governs the magnitude of temperature sensitivity. The higher Q10 in colder zones also suggests that warming may have a more profound impact on N inputs in nutrient-limited high-elevationhigh-latitude ecosystems, although this effect is likely contingent on soil resource availability. We emphasize the importance of incorporating diazotrophic community structurethermal traitsglobal biogeochemical models to improve predictions of future nitrogen budgets.

全文链接:https://onlinelibrary.wiley.com/doi/10.1111/gcb.70897