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Biogeosciences An interactive open-access journal of the European Geosciences Union
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Results of the first globally resolved simulations of terrestrial carbon and nitrogen (N) cycling and N2O emissions over the past 21 000 years are compared with reconstructed N2O emissions. Modelled and reconstructed emissions increased strongly during past abrupt warming events. This evidence appears consistent with a dynamic response of biological N fixation to increasing N demand by ecosystems, thereby reducing N limitation of plant productivity and supporting a land sink for atmospheric CO2.
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BG | Articles | Volume 17, issue 13
Biogeosciences, 17, 3511–3543, 2020
https://doi.org/10.5194/bg-17-3511-2020
Biogeosciences, 17, 3511–3543, 2020
https://doi.org/10.5194/bg-17-3511-2020

Research article 08 Jul 2020

Research article | 08 Jul 2020

N2O changes from the Last Glacial Maximum to the preindustrial – Part 2: terrestrial N2O emissions and carbon–nitrogen cycle interactions

Fortunat Joos et al.

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Latest update: 19 Jan 2021
Publications Copernicus
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Please read the editorial note first before accessing the article

Short summary
Results of the first globally resolved simulations of terrestrial carbon and nitrogen (N) cycling and N2O emissions over the past 21 000 years are compared with reconstructed N2O emissions. Modelled and reconstructed emissions increased strongly during past abrupt warming events. This evidence appears consistent with a dynamic response of biological N fixation to increasing N demand by ecosystems, thereby reducing N limitation of plant productivity and supporting a land sink for atmospheric CO2.
Citation
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Final-revised paper
Preprint