Abstract
Microbial-driven processes, particularly denitrification and anaerobic ammonium oxidation (anammox), convert inorganic nitrogen (N) in soils into gaseous forms, causing substantial N losses. However, their responses to global change across ecosystem types remain unclear. Here, we synthesized global data on denitrification and anammox from experiments examining major global change factors (GCFs), including elevated CO2, N addition, warming, and altered precipitation. Our analysis shows that N addition markedly stimulated both processes, and warming enhanced denitrification. On average, multiple GCFs exerted stronger effects on N-loss processes than single or two GCFs. These effects are ecosystem dependent, with croplands being the most affected, particularly under N addition. Furthermore, the sensitivity of N-loss processes to each GCF varies greatly among ecosystems and is largely explained by local climate and soil conditions. Our findings reveal accelerated soil N losses under multifactor global change and offer insights for improving future N-cycle predictions and sustainable N management.
Data availability
The datasets64 generated during this study are available at https://doi.org/10.6084/m9.figshare.29367797.
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Acknowledgements
This work was funded by the National Natural Science Foundation of China (32301369 and U24A20641) and Hubei Provincial Natural Science Foundation of China (2024AFD214).
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B.D., Q.Z., and W.L. developed the original idea of the analyses presented in the manuscript. B.D., D.X., and S.W. collected and analyzed the data. B.D., Q.Z., and W.L. wrote the original draft. Q.Z. and W.L. contributed significantly to improve subsequent drafts.
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Ding, B., Xu, D., Wang, S. et al. Multiple global change factors amplify nitrogen loss and croplands are at the highest risk.
Commun Earth Environ (2026). https://doi.org/10.1038/s43247-026-03316-2
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DOI: https://doi.org/10.1038/s43247-026-03316-2
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