Author
Listed:
- Carla R. Reis Ely
(Oregon State University
Oak Ridge Institute for Science and Education)
- Steven S. Perakis
(United States Geological Survey)
- Cory C. Cleveland
(University of Montana)
- Duncan N. L. Menge
(Columbia University)
- Sasha C. Reed
(United States Geological Survey)
- Benton N. Taylor
(Harvard University)
- Sarah A. Batterman
(Cary Institute of Ecosystem Studies
University of Leeds
Smithsonian Institution)
- Christopher M. Clark
(US Environmental Protection Agency)
- Timothy E. Crews
(The Land Institute)
- Katherine A. Dynarski
(University of Montana)
- Maga Gei
(Association for Tropical Biology and Conservation)
- Michael J. Gundale
(Swedish University of Agricultural Sciences)
- David F. Herridge
(University of New England)
- Sarah E. Jovan
(USDA Forest Service)
- Sian Kou-Giesbrecht
(Dalhousie University)
- Mark B. Peoples
(CSIRO)
- Johannes Piipponen
(Aalto University)
- Emilio Rodríguez-Caballero
(Universidad de Almería
Max Planck Institute for Chemistry)
- Verity G. Salmon
(Oak Ridge National Laboratory)
- Fiona M. Soper
(McGill University)
- Anika P. Staccone
(Earthshot Labs)
- Bettina Weber
(Max Planck Institute for Chemistry
University of Graz)
- Christopher A. Williams
(Clark University)
- Nina Wurzburger
(University of Georgia)
Abstract
Biological nitrogen fixation (BNF) is the largest natural source of new nitrogen (N) that supports terrestrial productivity1,2, yet estimates of global terrestrial BNF remain highly uncertain3,4. Here we show that this uncertainty is partly because of sampling bias, as field BNF measurements in natural terrestrial ecosystems occur where N fixers are 17 times more prevalent than their mean abundances worldwide. To correct this bias, we develop new estimates of global terrestrial BNF by upscaling field BNF measurements using spatially explicit abundances of all major biogeochemical N-fixing niches. We find that natural biomes sustain lower BNF, 65 (52–77) Tg N yr−1, than previous empirical bottom-up estimates3,4, with most BNF occurring in tropical forests and drylands. We also find high agricultural BNF in croplands and cultivated pastures, 56 (54–58) Tg N yr−1. Agricultural BNF has increased terrestrial BNF by 64% and total terrestrial N inputs from all sources by 60% over pre-industrial levels. Our results indicate that BNF may impose stronger constraints on the carbon sink in natural terrestrial biomes and represent a larger source of agricultural N than is generally considered in analyses of the global N cycle5,6, with implications for proposed safe operating limits for N use7,8.
Suggested Citation
Carla R. Reis Ely & Steven S. Perakis & Cory C. Cleveland & Duncan N. L. Menge & Sasha C. Reed & Benton N. Taylor & Sarah A. Batterman & Christopher M. Clark & Timothy E. Crews & Katherine A. Dynarski, 2025.
"Global terrestrial nitrogen fixation and its modification by agriculture,"
Nature, Nature, vol. 643(8072), pages 705-711, July.
Handle:
RePEc:nat:nature:v:643:y:2025:i:8072:d:10.1038_s41586-025-09201-w
DOI: 10.1038/s41586-025-09201-w
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