Articles | Volume 17, issue 1
https://doi.org/10.5194/cp-17-361-2021
© Author(s) 2021. 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-17-361-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Reconstructing the evolution of ice sheets, sea level, and atmospheric CO2 during the past 3.6 million years
Institute for Marine and Atmospheric research Utrecht, Utrecht
University, Utrecht, the Netherlands
Bas de Boer
Earth and Climate Cluster, Faculty of Science, Vrije Universiteit
Amsterdam, Amsterdam, the Netherlands
Roderik S. W. van de Wal
Institute for Marine and Atmospheric research Utrecht, Utrecht
University, Utrecht, the Netherlands
Faculty of Geosciences, Department of Physical Geography, Utrecht
University, Utrecht, the Netherlands
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- Pleistocene paleodrainages explain the phylogeographic structure of Malaysian populations of Asian arowana better than their chromatic variation N. Alshari et al. 10.3354/esr01152
- Revisiting the geodynamical history of the so-called uplifted atolls, north-west Tuamotu, French Polynesia, central South Pacific L. Montaggioni et al. 10.1016/j.earscirev.2023.104532
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- Meteoric diagenesis influenced by East Asian Summer Monsoon: A case study from the Pleistocene carbonate succession, Xisha Islands, South China Sea L. Wu et al. 10.1016/j.palaeo.2023.111882
- Response of eolian quartz flux and grain size in the Parece Vela Basin sediment to the mid-Pleistocene transition Y. Yan et al. 10.1016/j.jseaes.2022.105332
- Uniformitarian Prediction of Early‐Pleistocene Atmospheric CO2 P. Liautaud & P. Huybers 10.1029/2022GL100304
- Evolution of Global Ocean Tide Levels Since the Last Glacial Maximum R. Sulzbach et al. 10.1029/2022PA004556
- Insolation-paced sea level and sediment flux during the early Pleistocene in Southeast Asia R. Vaucher et al. 10.1038/s41598-021-96372-x
- Hydroclimate dynamics during the Plio-Pleistocene transition in the northwest Pacific realm R. Vaucher et al. 10.1016/j.gloplacha.2023.104088
- On the Cause of the Mid‐Pleistocene Transition C. Berends et al. 10.1029/2020RG000727
- Climate Evolution Through the Onset and Intensification of Northern Hemisphere Glaciation E. McClymont et al. 10.1029/2022RG000793
- Impact of paleoclimate on present and future evolution of the Greenland Ice Sheet H. Yang et al. 10.1371/journal.pone.0259816
- A 1.8 million year history of Amazon vegetation A. Kern et al. 10.1016/j.quascirev.2022.107867
- Biomarker proxy records of Arctic climate change during the Mid-Pleistocene transition from Lake El'gygytgyn (Far East Russia) K. Lindberg et al. 10.5194/cp-18-559-2022
- A 1.8 Million Year History of Amazonian Biomes A. Kern et al. 10.2139/ssrn.4131078
- Cadmium isotopes in Bahamas platform carbonates: A base for reconstruction of past surface water bioproductivity and their link with chromium isotopes J. Frederiksen et al. 10.1016/j.scitotenv.2021.150565
- Competing influence of the Taiwan orogen and East Asian Summer Monsoon on South China Sea paleoenvironmental proxy records A. Hsieh et al. 10.1016/j.palaeo.2023.111933
3 citations as recorded by crossref.
- The transient impact of the African monsoon on Plio-Pleistocene Mediterranean sediments B. de Boer et al. 10.5194/cp-17-331-2021
- Emergence of the Southeast Asian islands as a driver for Neogene cooling Y. Park et al. 10.1073/pnas.2011033117
- Preservation of the Climatic Signal in the Old Ice Layers at the Dome B Area (Antarctica) A. Ekaykin et al. 10.1134/S0001433823130066
Latest update: 19 Apr 2024
Short summary
For the past 2.6 million years, the Earth has experienced glacial cycles, where vast ice sheets periodically grew to cover large parts of North America and Eurasia. In the earlier part of this period, this happened every 40 000 years. This value changed 1.2 million years ago to 100 000 years: the Mid-Pleistocene Transition. We investigate this interesting period using an ice-sheet model, studying the interactions between ice sheets and the global climate.
For the past 2.6 million years, the Earth has experienced glacial cycles, where vast ice sheets...