Articles | Volume 15, issue 4
https://doi.org/10.5194/cp-15-1463-2019
© Author(s) 2019. 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-15-1463-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
05 Aug 2019
Research article |
| 05 Aug 2019
| 05 Aug 2019
Simulating the climate response to atmospheric oxygen variability in the Phanerozoic: a focus on the Holocene, Cretaceous and Permian
David C. Wade
CORRESPONDING AUTHOR
Department of Chemistry, Centre for Atmospheric Science, Cambridge, UK
Nathan Luke Abraham
Department of Chemistry, Centre for Atmospheric Science, Cambridge, UK
Department of Chemistry, National Centre for Atmospheric Science, Cambridge, UK
Alexander Farnsworth
School of Geographical Sciences, University of Bristol, Bristol, UK
Paul J. Valdes
School of Geographical Sciences, University of Bristol, Bristol, UK
Fran Bragg
School of Geographical Sciences, University of Bristol, Bristol, UK
Department of Chemistry, Centre for Atmospheric Science, Cambridge, UK
Department of Chemistry, National Centre for Atmospheric Science, Cambridge, UK
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19 citations as recorded by crossref.
- The oxygen cycle and a habitable Earth J. Huang et al. 10.1007/s11430-020-9747-1
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- A Systems Approach to Understanding How Plants Transformed Earth's Environment in Deep Time W. Matthaeus et al. 10.1146/annurev-earth-080222-082017
- Persistence of flare-driven atmospheric chemistry on rocky habitable zone worlds H. Chen et al. 10.1038/s41550-020-01264-1
- Evolution and driving mechanisms of water circulation during the late Paleozoic to early Mesozoic H. Song et al. 10.1360/TB-2022-0896
- Using carbon isotopes and organic composition to decipher climate and tectonics in the Early Cretaceous: An example from the Hailar Basin, Inner Mongolia, China T. Moore et al. 10.1016/j.cretres.2020.104674
- Oxygenation of the Baltoscandian shelf linked to Ordovician biodiversification A. Lindskog et al. 10.1038/s41561-023-01287-z
- Palaeoecology and palaeoclimate of an Early Cretaceous peat mire in East Laurasia (Hailar Basin, Inner Mongolia, China) A. Wheeler et al. 10.1016/j.palaeo.2022.111050
- Lower Cretaceous Hailar amber: The oldest-known amber from China Y. Li et al. 10.1016/j.cretres.2022.105472
- Stratospheric dynamics modulates ozone layer response to molecular oxygen variations I. Józefiak et al. 10.3389/feart.2023.1239325
- Climate change is an important predictor of extinction risk on macroevolutionary timescales C. Malanoski et al. 10.1126/science.adj5763
- Toward a Cenozoic history of atmospheric CO 2 B. Hönisch et al. 10.1126/science.adi5177
- Glacial‐Interglacial Controls on Ocean Circulation and Temperature During the Permo‐Carboniferous S. Macarewich & C. Poulsen 10.1029/2022PA004417
- Amber and the Cretaceous Resinous Interval X. Delclòs et al. 10.1016/j.earscirev.2023.104486
- Diagnosing the controls on desert dust emissions through the Phanerozoic Y. Xie et al. 10.5194/cp-20-2561-2024
- Oxygen bounty for Earth-like exoplanets: spectra of Earth through the Phanerozoic R. Payne & L. Kaltenegger 10.1093/mnrasl/slad147
- Role of the stratospheric chemistry–climate interactions in the hot climate conditions of the Eocene S. Szopa et al. 10.5194/cp-15-1187-2019
- On the Sensitivity of the Devonian Climate to Continental Configuration, Vegetation Cover, Orbital Configuration, CO 2 Concentration, and Insolation J. Brugger et al. 10.1029/2019PA003562
17 citations as recorded by crossref.
- The oxygen cycle and a habitable Earth J. Huang et al. 10.1007/s11430-020-9747-1
- Induced Power Scaling Alone Cannot Explain Griffenfly Gigantism O. Ellers et al. 10.1093/icb/icae046
- Effects of ozone levels on climate through Earth history R. Deitrick & C. Goldblatt 10.5194/cp-19-1201-2023
- A Systems Approach to Understanding How Plants Transformed Earth's Environment in Deep Time W. Matthaeus et al. 10.1146/annurev-earth-080222-082017
- Persistence of flare-driven atmospheric chemistry on rocky habitable zone worlds H. Chen et al. 10.1038/s41550-020-01264-1
- Evolution and driving mechanisms of water circulation during the late Paleozoic to early Mesozoic H. Song et al. 10.1360/TB-2022-0896
- Using carbon isotopes and organic composition to decipher climate and tectonics in the Early Cretaceous: An example from the Hailar Basin, Inner Mongolia, China T. Moore et al. 10.1016/j.cretres.2020.104674
- Oxygenation of the Baltoscandian shelf linked to Ordovician biodiversification A. Lindskog et al. 10.1038/s41561-023-01287-z
- Palaeoecology and palaeoclimate of an Early Cretaceous peat mire in East Laurasia (Hailar Basin, Inner Mongolia, China) A. Wheeler et al. 10.1016/j.palaeo.2022.111050
- Lower Cretaceous Hailar amber: The oldest-known amber from China Y. Li et al. 10.1016/j.cretres.2022.105472
- Stratospheric dynamics modulates ozone layer response to molecular oxygen variations I. Józefiak et al. 10.3389/feart.2023.1239325
- Climate change is an important predictor of extinction risk on macroevolutionary timescales C. Malanoski et al. 10.1126/science.adj5763
- Toward a Cenozoic history of atmospheric CO 2 B. Hönisch et al. 10.1126/science.adi5177
- Glacial‐Interglacial Controls on Ocean Circulation and Temperature During the Permo‐Carboniferous S. Macarewich & C. Poulsen 10.1029/2022PA004417
- Amber and the Cretaceous Resinous Interval X. Delclòs et al. 10.1016/j.earscirev.2023.104486
- Diagnosing the controls on desert dust emissions through the Phanerozoic Y. Xie et al. 10.5194/cp-20-2561-2024
- Oxygen bounty for Earth-like exoplanets: spectra of Earth through the Phanerozoic R. Payne & L. Kaltenegger 10.1093/mnrasl/slad147
2 citations as recorded by crossref.
- Role of the stratospheric chemistry–climate interactions in the hot climate conditions of the Eocene S. Szopa et al. 10.5194/cp-15-1187-2019
- On the Sensitivity of the Devonian Climate to Continental Configuration, Vegetation Cover, Orbital Configuration, CO 2 Concentration, and Insolation J. Brugger et al. 10.1029/2019PA003562
Latest update: 14 Dec 2024
Short summary
The amount of O2 in the atmosphere may have varied from as little as 10 % to as much as 35 % during the last 541 Myr. These changes are large enough to have led to changes in atmospheric mass, which may alter the radiative budget of the atmosphere. We present the first fully 3-D numerical model simulations to investigate the climate impacts of changes in O2 during different climate states. We identify a complex new mechanism causing increases in surface temperature when O2 levels were higher.
The amount of O2 in the atmosphere may have varied from as little as 10 % to as much as 35 %...
