Articles | Volume 16, issue 6
https://doi.org/10.5194/cp-16-2203-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/cp-16-2203-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| Highlight paper
| 
14 Nov 2020
Research article | Highlight paper |
| 14 Nov 2020
| 14 Nov 2020
Millennial-scale atmospheric CO2 variations during the Marine Isotope Stage 6 period (190–135 ka)
Jinhwa Shin
CNRS, Univ. Grenoble-Alpes, Institut des Géosciences de
l'Environnement (IGE), Grenoble, France
current address: Department of Earth and Atmospheric Sciences, University of Alberta, Edmonton, AB, T6G 2E3, Canada
Christoph Nehrbass-Ahles
Climate and Environmental Physics, Physics Institute, and Oeschger
Centre for Climate Change Research, University of Bern, Bern, Switzerland
Department of Earth Sciences, University of Cambridge, Cambridge, UK
Roberto Grilli
CNRS, Univ. Grenoble-Alpes, Institut des Géosciences de
l'Environnement (IGE), Grenoble, France
Jai Chowdhry Beeman
CNRS, Univ. Grenoble-Alpes, Institut des Géosciences de
l'Environnement (IGE), Grenoble, France
Frédéric Parrenin
CNRS, Univ. Grenoble-Alpes, Institut des Géosciences de
l'Environnement (IGE), Grenoble, France
Grégory Teste
CNRS, Univ. Grenoble-Alpes, Institut des Géosciences de
l'Environnement (IGE), Grenoble, France
Amaelle Landais
Laboratoire des Sciences du Climat et de l'Environnement, LSCE/IPSL, CEA-CNRS-UVSQ, Université Paris-Saclay, Gif-sur-Yvette, France
Loïc Schmidely
Climate and Environmental Physics, Physics Institute, and Oeschger
Centre for Climate Change Research, University of Bern, Bern, Switzerland
Lucas Silva
Climate and Environmental Physics, Physics Institute, and Oeschger
Centre for Climate Change Research, University of Bern, Bern, Switzerland
Jochen Schmitt
Climate and Environmental Physics, Physics Institute, and Oeschger
Centre for Climate Change Research, University of Bern, Bern, Switzerland
Bernhard Bereiter
Climate and Environmental Physics, Physics Institute, and Oeschger
Centre for Climate Change Research, University of Bern, Bern, Switzerland
Laboratory for Air Pollution/Environmental Technology, Empa,
Dübendorf, Switzerland
current address: Bruker BioSpin AG, Fällanden, Switzerland
Thomas F. Stocker
Climate and Environmental Physics, Physics Institute, and Oeschger
Centre for Climate Change Research, University of Bern, Bern, Switzerland
Hubertus Fischer
Climate and Environmental Physics, Physics Institute, and Oeschger
Centre for Climate Change Research, University of Bern, Bern, Switzerland
Jérôme Chappellaz
CORRESPONDING AUTHOR
CNRS, Univ. Grenoble-Alpes, Institut des Géosciences de
l'Environnement (IGE), Grenoble, France
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Cited
10 citations as recorded by crossref.
- Enhanced Asian hydroclimate instability during early MIS 6.5 D. Liu et al. 10.1016/j.quascirev.2023.108482
- The Dome Fuji ice core DF2021 chronology (0–207 kyr BP) I. Oyabu et al. 10.1016/j.quascirev.2022.107754
- Insolation evolution and ice volume legacies determine interglacial and glacial intensity T. Mitsui et al. 10.5194/cp-18-1983-2022
- Douglas Fir Multiproxy Tree-Ring Data Glimpse MIS 5 Environment in the U.S. Pacific Northwest I. Panyushkina et al. 10.3390/f13122161
- Marine Isotope Stage 11c: An unusual interglacial P. Tzedakis et al. 10.1016/j.quascirev.2022.107493
- The speleothem oxygen record as a proxy for thermal or moisture changes: a case study of multiproxy records from MIS 5–MIS 6 speleothems from the Demänová Cave system J. Pawlak 10.5194/cp-17-1051-2021
- An exceptional record of millennial-scale climate variability in the southern Iberian Margin during MIS 6: Impact on the formation of sapropel S6 F. Sierro & N. Andersen 10.1016/j.quascirev.2022.107527
- A 1.5-million-year record of orbital and millennial climate variability in the North Atlantic D. Hodell et al. 10.5194/cp-19-607-2023
- Millennial atmospheric CO2 changes linked to ocean ventilation modes over past 150,000 years J. Yu et al. 10.1038/s41561-023-01297-x
- Laser-induced sublimation extraction for centimeter-resolution multi-species greenhouse gas analysis on ice cores L. Mächler et al. 10.5194/amt-16-355-2023
10 citations as recorded by crossref.
- Enhanced Asian hydroclimate instability during early MIS 6.5 D. Liu et al. 10.1016/j.quascirev.2023.108482
- The Dome Fuji ice core DF2021 chronology (0–207 kyr BP) I. Oyabu et al. 10.1016/j.quascirev.2022.107754
- Insolation evolution and ice volume legacies determine interglacial and glacial intensity T. Mitsui et al. 10.5194/cp-18-1983-2022
- Douglas Fir Multiproxy Tree-Ring Data Glimpse MIS 5 Environment in the U.S. Pacific Northwest I. Panyushkina et al. 10.3390/f13122161
- Marine Isotope Stage 11c: An unusual interglacial P. Tzedakis et al. 10.1016/j.quascirev.2022.107493
- The speleothem oxygen record as a proxy for thermal or moisture changes: a case study of multiproxy records from MIS 5–MIS 6 speleothems from the Demänová Cave system J. Pawlak 10.5194/cp-17-1051-2021
- An exceptional record of millennial-scale climate variability in the southern Iberian Margin during MIS 6: Impact on the formation of sapropel S6 F. Sierro & N. Andersen 10.1016/j.quascirev.2022.107527
- A 1.5-million-year record of orbital and millennial climate variability in the North Atlantic D. Hodell et al. 10.5194/cp-19-607-2023
- Millennial atmospheric CO2 changes linked to ocean ventilation modes over past 150,000 years J. Yu et al. 10.1038/s41561-023-01297-x
- Laser-induced sublimation extraction for centimeter-resolution multi-species greenhouse gas analysis on ice cores L. Mächler et al. 10.5194/amt-16-355-2023
Latest update: 29 Jun 2024
Short summary
We reconstruct atmospheric CO2 from the EPICA Dome C ice core during Marine Isotope Stage 6 (185–135 ka) to understand carbon mechanisms under the different boundary conditions of the climate system. The amplitude of CO2 is highly determined by the Northern Hemisphere stadial duration. Carbon dioxide maxima show different lags with respect to the corresponding abrupt CH4 jumps, the latter reflecting rapid warming in the Northern Hemisphere.
We reconstruct atmospheric CO2 from the EPICA Dome C ice core during Marine Isotope Stage 6...
