Articles | Volume 16, issue 2
https://doi.org/10.5194/cp-16-555-2020
© 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-16-555-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
19 Mar 2020
Research article |
| 19 Mar 2020
| 19 Mar 2020
Changes in the high-latitude Southern Hemisphere through the Eocene–Oligocene transition: a model–data comparison
Alan T. Kennedy-Asser
CORRESPONDING AUTHOR
BRIDGE, School of Geographical Sciences, University of Bristol,
Bristol, UK
Cabot Institute for the Environment, University of Bristol, Bristol,
UK
Daniel J. Lunt
BRIDGE, School of Geographical Sciences, University of Bristol,
Bristol, UK
Cabot Institute for the Environment, University of Bristol, Bristol,
UK
Paul J. Valdes
BRIDGE, School of Geographical Sciences, University of Bristol,
Bristol, UK
Cabot Institute for the Environment, University of Bristol, Bristol,
UK
Jean-Baptiste Ladant
Department of Earth and Environmental Sciences, University of
Michigan, Ann Arbor, USA
Joost Frieling
Marine Palynology and Paleoceanography, Laboratory of Palaeobotany
and Palynology, Department of Earth Sciences, Faculty of Geosciences, Utrecht University, Princetonlaan 8a,
3584CB Utrecht, the Netherlands
Vittoria Lauretano
Cabot Institute for the Environment, University of Bristol, Bristol,
UK
Organic Geochemistry Unit, School of Chemistry, University of
Bristol, Bristol, UK
Viewed
Total article views: 2,631 (including HTML, PDF, and XML)
Cumulative views and downloads
(calculated since 06 Sep 2019)
| HTML | XML | Total | Supplement | BibTeX | EndNote | |
|---|---|---|---|---|---|---|
| 1,842 | 740 | 49 | 2,631 | 312 | 56 | 57 |
- HTML: 1,842
- PDF: 740
- XML: 49
- Total: 2,631
- Supplement: 312
- BibTeX: 56
- EndNote: 57
Total article views: 1,786 (including HTML, PDF, and XML)
Cumulative views and downloads
(calculated since 19 Mar 2020)
| HTML | XML | Total | Supplement | BibTeX | EndNote | |
|---|---|---|---|---|---|---|
| 1,290 | 451 | 45 | 1,786 | 143 | 51 | 50 |
- HTML: 1,290
- PDF: 451
- XML: 45
- Total: 1,786
- Supplement: 143
- BibTeX: 51
- EndNote: 50
Total article views: 845 (including HTML, PDF, and XML)
Cumulative views and downloads
(calculated since 06 Sep 2019)
| HTML | XML | Total | Supplement | BibTeX | EndNote | |
|---|---|---|---|---|---|---|
| 552 | 289 | 4 | 845 | 169 | 5 | 7 |
- HTML: 552
- PDF: 289
- XML: 4
- Total: 845
- Supplement: 169
- BibTeX: 5
- EndNote: 7
Viewed (geographical distribution)
Total article views: 2,631 (including HTML, PDF, and XML)
Thereof 2,273 with geography defined
and 358 with unknown origin.
Total article views: 1,786 (including HTML, PDF, and XML)
Thereof 1,550 with geography defined
and 236 with unknown origin.
Total article views: 845 (including HTML, PDF, and XML)
Thereof 723 with geography defined
and 122 with unknown origin.
| Country | # | Views | % |
|---|
| Country | # | Views | % |
|---|
| Country | # | Views | % |
|---|
| Total: | 0 |
| HTML: | 0 |
| PDF: | 0 |
| XML: | 0 |
- 1
1
| Total: | 0 |
| HTML: | 0 |
| PDF: | 0 |
| XML: | 0 |
- 1
1
| Total: | 0 |
| HTML: | 0 |
| PDF: | 0 |
| XML: | 0 |
- 1
1
Cited
15 citations as recorded by crossref.
- Fates of Paleo‐Antarctic Bottom Water During the Early Eocene: Based on a Lagrangian Analysis of IPSL‐CM5A2 Climate Model Simulations Y. Zhang et al. 10.1029/2019PA003845
- The Eocene–Oligocene transition: a review of marine and terrestrial proxy data, models and model–data comparisons D. Hutchinson et al. 10.5194/cp-17-269-2021
- Evolution of Sea Surface Temperature in the Southern Mid‐latitudes From Late Oligocene Through Early Miocene J. Guitián & H. Stoll 10.1029/2020PA004199
- The middle to late Eocene greenhouse climate modelled using the CESM 1.0.5 M. Baatsen et al. 10.5194/cp-16-2573-2020
- Late Cenozoic sea-surface-temperature evolution of the South Atlantic Ocean F. Hoem et al. 10.5194/cp-19-1931-2023
- Deep water inflow slowed offshore expansion of the West Antarctic Ice Sheet at the Eocene-Oligocene transition G. Uenzelmann-Neben et al. 10.1038/s43247-022-00369-x
- Proxy‐Model Comparison for the Eocene‐Oligocene Transition in Southern High Latitudes E. Tibbett et al. 10.1029/2022PA004496
- IPSL-CM5A2 – an Earth system model designed for multi-millennial climate simulations P. Sepulchre et al. 10.5194/gmd-13-3011-2020
- Drake Passage gateway opening and Antarctic Circumpolar Current onset 31 Ma ago: The message of foraminifera and reconsideration of the Neodymium isotope record F. Hodel et al. 10.1016/j.chemgeo.2021.120171
- Evolution of continental temperature seasonality from the Eocene greenhouse to the Oligocene icehouse –a model–data comparison A. Toumoulin et al. 10.5194/cp-18-341-2022
- Eocene to Oligocene terrestrial Southern Hemisphere cooling caused by declining pCO2 V. Lauretano et al. 10.1038/s41561-021-00788-z
- Monitoring multidecadal coastline change and reconstructing tidal flat topography Y. Tsai & K. Tseng 10.1016/j.jag.2023.103260
- Resilient Antarctic monsoonal climate prevented ice growth during the Eocene M. Baatsen et al. 10.5194/cp-20-77-2024
- Eocene-Oligocene southwest Pacific Ocean paleoceanography new insights from foraminifera chemistry (DSDP site 277, Campbell Plateau) F. Hodel et al. 10.3389/feart.2022.998237
- The enigma of Oligocene climate and global surface temperature evolution C. O’Brien et al. 10.1073/pnas.2003914117
15 citations as recorded by crossref.
- Fates of Paleo‐Antarctic Bottom Water During the Early Eocene: Based on a Lagrangian Analysis of IPSL‐CM5A2 Climate Model Simulations Y. Zhang et al. 10.1029/2019PA003845
- The Eocene–Oligocene transition: a review of marine and terrestrial proxy data, models and model–data comparisons D. Hutchinson et al. 10.5194/cp-17-269-2021
- Evolution of Sea Surface Temperature in the Southern Mid‐latitudes From Late Oligocene Through Early Miocene J. Guitián & H. Stoll 10.1029/2020PA004199
- The middle to late Eocene greenhouse climate modelled using the CESM 1.0.5 M. Baatsen et al. 10.5194/cp-16-2573-2020
- Late Cenozoic sea-surface-temperature evolution of the South Atlantic Ocean F. Hoem et al. 10.5194/cp-19-1931-2023
- Deep water inflow slowed offshore expansion of the West Antarctic Ice Sheet at the Eocene-Oligocene transition G. Uenzelmann-Neben et al. 10.1038/s43247-022-00369-x
- Proxy‐Model Comparison for the Eocene‐Oligocene Transition in Southern High Latitudes E. Tibbett et al. 10.1029/2022PA004496
- IPSL-CM5A2 – an Earth system model designed for multi-millennial climate simulations P. Sepulchre et al. 10.5194/gmd-13-3011-2020
- Drake Passage gateway opening and Antarctic Circumpolar Current onset 31 Ma ago: The message of foraminifera and reconsideration of the Neodymium isotope record F. Hodel et al. 10.1016/j.chemgeo.2021.120171
- Evolution of continental temperature seasonality from the Eocene greenhouse to the Oligocene icehouse –a model–data comparison A. Toumoulin et al. 10.5194/cp-18-341-2022
- Eocene to Oligocene terrestrial Southern Hemisphere cooling caused by declining pCO2 V. Lauretano et al. 10.1038/s41561-021-00788-z
- Monitoring multidecadal coastline change and reconstructing tidal flat topography Y. Tsai & K. Tseng 10.1016/j.jag.2023.103260
- Resilient Antarctic monsoonal climate prevented ice growth during the Eocene M. Baatsen et al. 10.5194/cp-20-77-2024
- Eocene-Oligocene southwest Pacific Ocean paleoceanography new insights from foraminifera chemistry (DSDP site 277, Campbell Plateau) F. Hodel et al. 10.3389/feart.2022.998237
- The enigma of Oligocene climate and global surface temperature evolution C. O’Brien et al. 10.1073/pnas.2003914117
Latest update: 17 Apr 2024
Short summary
Global cooling and a major expansion of ice over Antarctica occurred ~ 34 million years ago at the Eocene–Oligocene transition (EOT). A large secondary proxy dataset for high-latitude Southern Hemisphere temperature before, after and across the EOT is compiled and compared to simulations from two coupled climate models. Although there are inconsistencies between the models and data, the comparison shows amongst other things that changes in the Drake Passage were unlikely the cause of the EOT.
Global cooling and a major expansion of ice over Antarctica occurred ~ 34 million years ago at...
