N 2 O changes from the Last Glacial Maximum to the preindustrial – Part 1: Quantitative reconstruction of terrestrial and marine emissions using N 2 O stable isotopes in ice cores
Using high-precision and centennial-resolution ice core information on atmospheric nitrous oxide concentrations and its stable nitrogen and oxygen isotopic composition, we quantitatively reconstruct changes in the terrestrial and marine N 2 O emissions over the last 21 000 years. Our reconstruction...
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ftdoajarticles:oai:doaj.org/article:57094c02806a45bb9bda7beb976d17de 2023-05-15T16:39:23+02:00 N 2 O changes from the Last Glacial Maximum to the preindustrial – Part 1: Quantitative reconstruction of terrestrial and marine emissions using N 2 O stable isotopes in ice cores H. Fischer J. Schmitt M. Bock B. Seth F. Joos R. Spahni S. Lienert G. Battaglia B. D. Stocker A. Schilt E. J. Brook 2019-10-01T00:00:00Z https://doi.org/10.5194/bg-16-3997-2019 https://doaj.org/article/57094c02806a45bb9bda7beb976d17de EN eng Copernicus Publications https://www.biogeosciences.net/16/3997/2019/bg-16-3997-2019.pdf https://doaj.org/toc/1726-4170 https://doaj.org/toc/1726-4189 doi:10.5194/bg-16-3997-2019 1726-4170 1726-4189 https://doaj.org/article/57094c02806a45bb9bda7beb976d17de Biogeosciences, Vol 16, Pp 3997-4021 (2019) Ecology QH540-549.5 Life QH501-531 Geology QE1-996.5 article 2019 ftdoajarticles https://doi.org/10.5194/bg-16-3997-2019 2022-12-31T01:50:15Z Using high-precision and centennial-resolution ice core information on atmospheric nitrous oxide concentrations and its stable nitrogen and oxygen isotopic composition, we quantitatively reconstruct changes in the terrestrial and marine N 2 O emissions over the last 21 000 years. Our reconstruction indicates that N 2 O emissions from land and ocean increased over the deglaciation largely in parallel by 1.7±0.3 and 0.7±0.3 TgN yr −1 , respectively, relative to the Last Glacial Maximum level. However, during the abrupt Northern Hemisphere warmings at the onset of the Bølling–Allerød warming and the end of the Younger Dryas, terrestrial emissions respond more rapidly to the northward shift in the Intertropical Convergence Zone connected to the resumption of the Atlantic Meridional Overturning Circulation. About 90 % of these large step increases were realized within 2 centuries at maximum. In contrast, marine emissions start to slowly increase already many centuries before the rapid warmings, possibly connected to a re-equilibration of subsurface oxygen in response to previous changes. Marine emissions decreased, concomitantly with changes in atmospheric CO 2 and δ 13 C(CO 2 ) , at the onset of the termination and remained minimal during the early phase of Heinrich Stadial 1. During the early Holocene a slow decline in marine N 2 O emission of 0.4 TgN yr −1 is reconstructed, which suggests an improvement of subsurface water ventilation in line with slowly increasing Atlantic overturning circulation. In the second half of the Holocene total emissions remain on a relatively constant level, but with significant millennial variability. The latter is still difficult to attribute to marine or terrestrial sources. Our N 2 O emission records provide important quantitative benchmarks for ocean and terrestrial nitrogen cycle models to study the influence of climate on nitrogen turnover on timescales from several decades to glacial–interglacial changes. Article in Journal/Newspaper ice core Directory of Open Access Journals: DOAJ Articles Biogeosciences 16 20 3997 4021 |
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Open Polar |
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Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
Ecology QH540-549.5 Life QH501-531 Geology QE1-996.5 |
spellingShingle |
Ecology QH540-549.5 Life QH501-531 Geology QE1-996.5 H. Fischer J. Schmitt M. Bock B. Seth F. Joos R. Spahni S. Lienert G. Battaglia B. D. Stocker A. Schilt E. J. Brook N 2 O changes from the Last Glacial Maximum to the preindustrial – Part 1: Quantitative reconstruction of terrestrial and marine emissions using N 2 O stable isotopes in ice cores |
topic_facet |
Ecology QH540-549.5 Life QH501-531 Geology QE1-996.5 |
description |
Using high-precision and centennial-resolution ice core information on atmospheric nitrous oxide concentrations and its stable nitrogen and oxygen isotopic composition, we quantitatively reconstruct changes in the terrestrial and marine N 2 O emissions over the last 21 000 years. Our reconstruction indicates that N 2 O emissions from land and ocean increased over the deglaciation largely in parallel by 1.7±0.3 and 0.7±0.3 TgN yr −1 , respectively, relative to the Last Glacial Maximum level. However, during the abrupt Northern Hemisphere warmings at the onset of the Bølling–Allerød warming and the end of the Younger Dryas, terrestrial emissions respond more rapidly to the northward shift in the Intertropical Convergence Zone connected to the resumption of the Atlantic Meridional Overturning Circulation. About 90 % of these large step increases were realized within 2 centuries at maximum. In contrast, marine emissions start to slowly increase already many centuries before the rapid warmings, possibly connected to a re-equilibration of subsurface oxygen in response to previous changes. Marine emissions decreased, concomitantly with changes in atmospheric CO 2 and δ 13 C(CO 2 ) , at the onset of the termination and remained minimal during the early phase of Heinrich Stadial 1. During the early Holocene a slow decline in marine N 2 O emission of 0.4 TgN yr −1 is reconstructed, which suggests an improvement of subsurface water ventilation in line with slowly increasing Atlantic overturning circulation. In the second half of the Holocene total emissions remain on a relatively constant level, but with significant millennial variability. The latter is still difficult to attribute to marine or terrestrial sources. Our N 2 O emission records provide important quantitative benchmarks for ocean and terrestrial nitrogen cycle models to study the influence of climate on nitrogen turnover on timescales from several decades to glacial–interglacial changes. |
format |
Article in Journal/Newspaper |
author |
H. Fischer J. Schmitt M. Bock B. Seth F. Joos R. Spahni S. Lienert G. Battaglia B. D. Stocker A. Schilt E. J. Brook |
author_facet |
H. Fischer J. Schmitt M. Bock B. Seth F. Joos R. Spahni S. Lienert G. Battaglia B. D. Stocker A. Schilt E. J. Brook |
author_sort |
H. Fischer |
title |
N 2 O changes from the Last Glacial Maximum to the preindustrial – Part 1: Quantitative reconstruction of terrestrial and marine emissions using N 2 O stable isotopes in ice cores |
title_short |
N 2 O changes from the Last Glacial Maximum to the preindustrial – Part 1: Quantitative reconstruction of terrestrial and marine emissions using N 2 O stable isotopes in ice cores |
title_full |
N 2 O changes from the Last Glacial Maximum to the preindustrial – Part 1: Quantitative reconstruction of terrestrial and marine emissions using N 2 O stable isotopes in ice cores |
title_fullStr |
N 2 O changes from the Last Glacial Maximum to the preindustrial – Part 1: Quantitative reconstruction of terrestrial and marine emissions using N 2 O stable isotopes in ice cores |
title_full_unstemmed |
N 2 O changes from the Last Glacial Maximum to the preindustrial – Part 1: Quantitative reconstruction of terrestrial and marine emissions using N 2 O stable isotopes in ice cores |
title_sort |
n 2 o changes from the last glacial maximum to the preindustrial – part 1: quantitative reconstruction of terrestrial and marine emissions using n 2 o stable isotopes in ice cores |
publisher |
Copernicus Publications |
publishDate |
2019 |
url |
https://doi.org/10.5194/bg-16-3997-2019 https://doaj.org/article/57094c02806a45bb9bda7beb976d17de |
genre |
ice core |
genre_facet |
ice core |
op_source |
Biogeosciences, Vol 16, Pp 3997-4021 (2019) |
op_relation |
https://www.biogeosciences.net/16/3997/2019/bg-16-3997-2019.pdf https://doaj.org/toc/1726-4170 https://doaj.org/toc/1726-4189 doi:10.5194/bg-16-3997-2019 1726-4170 1726-4189 https://doaj.org/article/57094c02806a45bb9bda7beb976d17de |
op_doi |
https://doi.org/10.5194/bg-16-3997-2019 |
container_title |
Biogeosciences |
container_volume |
16 |
container_issue |
20 |
container_start_page |
3997 |
op_container_end_page |
4021 |
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1766029720998117376 |