Articles | Volume 11, issue 11
https://doi.org/10.5194/cp-11-1527-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/cp-11-1527-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
19 Nov 2015
Research article |
| 19 Nov 2015
Quantifying molecular oxygen isotope variations during a Heinrich stadial
C. Reutenauer
CORRESPONDING AUTHOR
Centre for Ice and Climate, Niels Bohr Institute, University of Copenhagen, Copenhagen, Denmark
A. Landais
Institut Pierre Simon Laplace (IPSL), Laboratoire des Sciences de Climat et de l'Environnement (LSCE), UMR8212 (CEA-CNRS-UVSQ), CE Saclay, Orme des Merisiers, Bat. 701, 91191 Gif-sur-Yvette Cedex, France
T. Blunier
Centre for Ice and Climate, Niels Bohr Institute, University of Copenhagen, Copenhagen, Denmark
C. Bréant
Institut Pierre Simon Laplace (IPSL), Laboratoire des Sciences de Climat et de l'Environnement (LSCE), UMR8212 (CEA-CNRS-UVSQ), CE Saclay, Orme des Merisiers, Bat. 701, 91191 Gif-sur-Yvette Cedex, France
M. Kageyama
Institut Pierre Simon Laplace (IPSL), Laboratoire des Sciences de Climat et de l'Environnement (LSCE), UMR8212 (CEA-CNRS-UVSQ), CE Saclay, Orme des Merisiers, Bat. 701, 91191 Gif-sur-Yvette Cedex, France
M.-N. Woillez
Institut Pierre Simon Laplace (IPSL), Laboratoire des Sciences de Climat et de l'Environnement (LSCE), UMR8212 (CEA-CNRS-UVSQ), CE Saclay, Orme des Merisiers, Bat. 701, 91191 Gif-sur-Yvette Cedex, France
now at: IFPEN, 14 avenue de Bois Préau, 92852 Rueil-Malmaison Cedex, France
C. Risi
Laboratoire de Météorologie Dynamique UMR8539, IPSL/CNRS/UPMC, 4, place Jussieu, 75252 Paris Cedex 05, France
V. Mariotti
Institut Pierre Simon Laplace (IPSL), Laboratoire des Sciences de Climat et de l'Environnement (LSCE), UMR8212 (CEA-CNRS-UVSQ), CE Saclay, Orme des Merisiers, Bat. 701, 91191 Gif-sur-Yvette Cedex, France
P. Braconnot
Institut Pierre Simon Laplace (IPSL), Laboratoire des Sciences de Climat et de l'Environnement (LSCE), UMR8212 (CEA-CNRS-UVSQ), CE Saclay, Orme des Merisiers, Bat. 701, 91191 Gif-sur-Yvette Cedex, France
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Cited
12 citations as recorded by crossref.
- Does δ<sup>18</sup>O of O<sub>2</sub> record meridional shifts in tropical rainfall? A. Seltzer et al. 10.5194/cp-13-1323-2017
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- Determination of respiration and photosynthesis fractionation factors for atmospheric dioxygen inferred from a vegetation–soil–atmosphere analogue of the terrestrial biosphere in closed chambers C. Paul et al. 10.5194/bg-20-1047-2023
- On the use of δ18Oatm for ice core dating T. Extier et al. 10.1016/j.quascirev.2018.02.008
- Discrimination in Tree Stems O2 Uptake and the Dole Effect B. Hilman & A. Angert 10.1029/2018GB005918
- Stalagmite multi-proxy records of weak Asian summer monsoon interval during Termination III as an analogue to Termination I G. Chen et al. 10.1016/j.quascirev.2023.108112
- The Antarctic Ice Core Chronology 2023 (AICC2023) chronological framework and associated timescale for the European Project for Ice Coring in Antarctica (EPICA) Dome C ice core M. Bouchet et al. 10.5194/cp-19-2257-2023
- Unveiling the anatomy of Termination 3 using water and air isotopes in the Dome C ice core, East Antarctica C. Bréant et al. 10.1016/j.quascirev.2019.03.025
- Exceptionally high biosphere productivity at the beginning of Marine Isotopic Stage 11 M. Brandon et al. 10.1038/s41467-020-15739-2
- Phase relationships between orbital forcing and the composition of air trapped in Antarctic ice cores L. Bazin et al. 10.5194/cp-12-729-2016
- Linking environmental changes with human occupations between 900 and 400 ka in Western Europe M. Moncel et al. 10.1016/j.quaint.2016.09.065
- What do dust sinks tell us about their sources and past environmental dynamics? A case study for oxygen isotope stages 3–2 in the Middle Rhine Valley, Germany M. Vinnepand et al. 10.5194/egqsj-72-163-2023
12 citations as recorded by crossref.
- Does δ<sup>18</sup>O of O<sub>2</sub> record meridional shifts in tropical rainfall? A. Seltzer et al. 10.5194/cp-13-1323-2017
- Dole effect as a measurement of the low-latitude hydrological cycle over the past 800 ka E. Huang et al. 10.1126/sciadv.aba4823
- Determination of respiration and photosynthesis fractionation factors for atmospheric dioxygen inferred from a vegetation–soil–atmosphere analogue of the terrestrial biosphere in closed chambers C. Paul et al. 10.5194/bg-20-1047-2023
- On the use of δ18Oatm for ice core dating T. Extier et al. 10.1016/j.quascirev.2018.02.008
- Discrimination in Tree Stems O2 Uptake and the Dole Effect B. Hilman & A. Angert 10.1029/2018GB005918
- Stalagmite multi-proxy records of weak Asian summer monsoon interval during Termination III as an analogue to Termination I G. Chen et al. 10.1016/j.quascirev.2023.108112
- The Antarctic Ice Core Chronology 2023 (AICC2023) chronological framework and associated timescale for the European Project for Ice Coring in Antarctica (EPICA) Dome C ice core M. Bouchet et al. 10.5194/cp-19-2257-2023
- Unveiling the anatomy of Termination 3 using water and air isotopes in the Dome C ice core, East Antarctica C. Bréant et al. 10.1016/j.quascirev.2019.03.025
- Exceptionally high biosphere productivity at the beginning of Marine Isotopic Stage 11 M. Brandon et al. 10.1038/s41467-020-15739-2
- Phase relationships between orbital forcing and the composition of air trapped in Antarctic ice cores L. Bazin et al. 10.5194/cp-12-729-2016
- Linking environmental changes with human occupations between 900 and 400 ka in Western Europe M. Moncel et al. 10.1016/j.quaint.2016.09.065
- What do dust sinks tell us about their sources and past environmental dynamics? A case study for oxygen isotope stages 3–2 in the Middle Rhine Valley, Germany M. Vinnepand et al. 10.5194/egqsj-72-163-2023
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Latest update: 23 Nov 2024
Short summary
Isotopes of atmospheric O2 undergo millennial-scale variations during the last glacial period, and systematically increase during Heinrich stadials.
Such variations are mostly due to vegetation and water cycle processes.
Our modeling approach reproduces the main observed features of Heinrich stadials in terms of climate, vegetation and rainfall.
It highlights the strong role of hydrology on O2 isotopes, which can be seen as a global integrator of precipitation changes over vegetated areas.
Isotopes of atmospheric O2 undergo millennial-scale variations during the last glacial period,...
