Articles | Volume 18, issue 2
https://doi.org/10.5194/cp-18-209-2022
© Author(s) 2022. 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-18-209-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| Highlight paper
| 
04 Feb 2022
Research article | Highlight paper |
| 04 Feb 2022
| 04 Feb 2022
Vegetation change across the Drake Passage region linked to late Eocene cooling and glacial disturbance after the Eocene–Oligocene transition
Nick Thompson
CORRESPONDING AUTHOR
Department of Geography and Environmental Sciences, Northumbria
University, Newcastle upon Tyne, UK
Ulrich Salzmann
Department of Geography and Environmental Sciences, Northumbria
University, Newcastle upon Tyne, UK
Adrián López-Quirós
Department of Geoscience, Aarhus University, Høegh-Guldbergs Gade
2, 8000, Aarhus C, Denmark
Instituto Andaluz de Ciencias de la Tierra, CSIC-Universidad de
Granada, Granada, Spain
Peter K. Bijl
Department of Earth Sciences, Utrecht University, Utrecht, the
Netherlands
Frida S. Hoem
Department of Earth Sciences, Utrecht University, Utrecht, the
Netherlands
Johan Etourneau
Instituto Andaluz de Ciencias de la Tierra, CSIC-Universidad de
Granada, Granada, Spain
Marie-Alexandrine Sicre
Sorbonne Université (UPMC, Univ. Paris 06)-CNRS-IRD-MNHN, LOCEAN
Laboratory, Paris, France
Sabine Roignant
Institut Universitaire Européen de la Mer, Plouzane, France
Emma Hocking
Department of Geography and Environmental Sciences, Northumbria
University, Newcastle upon Tyne, UK
Michael Amoo
Department of Geography and Environmental Sciences, Northumbria
University, Newcastle upon Tyne, UK
Carlota Escutia
Instituto Andaluz de Ciencias de la Tierra, CSIC-Universidad de
Granada, Granada, Spain
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Cited
14 citations as recorded by crossref.
- Impact of Eocene‐Oligocene Antarctic Glaciation on the Paleoceanography of the Weddell Sea V. Hojnacki et al. 10.1029/2022PA004440
- Eocene to Oligocene vegetation and climate in the Tasmanian Gateway region were controlled by changes in ocean currents and <i>p</i>CO<sub>2</sub> M. Amoo et al. 10.5194/cp-18-525-2022
- Poleward amplification, seasonal rainfall and forest heterogeneity in the Miocene of the eastern USA T. Reichgelt et al. 10.1016/j.gloplacha.2023.104073
- Resilient Antarctic monsoonal climate prevented ice growth during the Eocene M. Baatsen et al. 10.5194/cp-20-77-2024
- The Drake Passage asthenospheric and oceanic gateway Y. Martos & M. Catalán 10.1016/j.earscirev.2024.104731
- Late Cenozoic sea-surface-temperature evolution of the South Atlantic Ocean F. Hoem et al. 10.5194/cp-19-1931-2023
- Late Eocene to late Oligocene terrestrial climate and vegetation change in the western Tasmanian region M. Amoo et al. 10.1016/j.palaeo.2023.111632
- Eocene–Oligocene vegetation and climate changes in southeastern Brazil T. Akabane et al. 10.1016/j.revpalbo.2024.105142
- Cenozoic Antarctic Peninsula Temperatures and Glacial Erosion Signals From a Multi‐Proxy Biomarker Study E. Tibbett et al. 10.1029/2022PA004430
- Ice sheet–free West Antarctica during peak early Oligocene glaciation J. Klages et al. 10.1126/science.adj3931
- Terrestrial Climate and Vegetation Change in the Western Tasmanian Region from the Late Eocene to Late Oligocene M. Amoo et al. 10.2139/ssrn.4176394
- Proxy‐Model Comparison for the Eocene‐Oligocene Transition in Southern High Latitudes E. Tibbett et al. 10.1029/2022PA004496
- 3D Geophysical and Geological Modeling of the South Orkney Microcontinent (Antarctica): Tectonic Implications for the Scotia Arc Development C. Morales‐Ocaña et al. 10.1029/2022TC007602
- Climate variability, heat distribution, and polar amplification in the warm unipolar “icehouse” of the Oligocene D. Jenny et al. 10.5194/cp-20-1627-2024
14 citations as recorded by crossref.
- Impact of Eocene‐Oligocene Antarctic Glaciation on the Paleoceanography of the Weddell Sea V. Hojnacki et al. 10.1029/2022PA004440
- Eocene to Oligocene vegetation and climate in the Tasmanian Gateway region were controlled by changes in ocean currents and <i>p</i>CO<sub>2</sub> M. Amoo et al. 10.5194/cp-18-525-2022
- Poleward amplification, seasonal rainfall and forest heterogeneity in the Miocene of the eastern USA T. Reichgelt et al. 10.1016/j.gloplacha.2023.104073
- Resilient Antarctic monsoonal climate prevented ice growth during the Eocene M. Baatsen et al. 10.5194/cp-20-77-2024
- The Drake Passage asthenospheric and oceanic gateway Y. Martos & M. Catalán 10.1016/j.earscirev.2024.104731
- Late Cenozoic sea-surface-temperature evolution of the South Atlantic Ocean F. Hoem et al. 10.5194/cp-19-1931-2023
- Late Eocene to late Oligocene terrestrial climate and vegetation change in the western Tasmanian region M. Amoo et al. 10.1016/j.palaeo.2023.111632
- Eocene–Oligocene vegetation and climate changes in southeastern Brazil T. Akabane et al. 10.1016/j.revpalbo.2024.105142
- Cenozoic Antarctic Peninsula Temperatures and Glacial Erosion Signals From a Multi‐Proxy Biomarker Study E. Tibbett et al. 10.1029/2022PA004430
- Ice sheet–free West Antarctica during peak early Oligocene glaciation J. Klages et al. 10.1126/science.adj3931
- Terrestrial Climate and Vegetation Change in the Western Tasmanian Region from the Late Eocene to Late Oligocene M. Amoo et al. 10.2139/ssrn.4176394
- Proxy‐Model Comparison for the Eocene‐Oligocene Transition in Southern High Latitudes E. Tibbett et al. 10.1029/2022PA004496
- 3D Geophysical and Geological Modeling of the South Orkney Microcontinent (Antarctica): Tectonic Implications for the Scotia Arc Development C. Morales‐Ocaña et al. 10.1029/2022TC007602
- Climate variability, heat distribution, and polar amplification in the warm unipolar “icehouse” of the Oligocene D. Jenny et al. 10.5194/cp-20-1627-2024
Latest update: 20 Nov 2024
Short summary
New pollen and spore data from the Antarctic Peninsula region reveal temperate rainforests that changed and adapted in response to Eocene climatic cooling, roughly 35.5 Myr ago, and glacially related disturbance in the early Oligocene, approximately 33.5 Myr ago. The timing of these events indicates that the opening of ocean gateways alone did not trigger Antarctic glaciation, although ocean gateways may have played a role in climate cooling.
New pollen and spore data from the Antarctic Peninsula region reveal temperate rainforests that...
