Dynamic Greenland ice sheet driven by pCO2 variations across the Pliocene Pleistocene transition
Previous work has argued for a CO2 control on the development of the Plio-Pleistocene Transition (PPT, 3.0–2.5 Ma) Greenland Ice Sheet (GrIS). Here based on transient ice sheet experiments, the authors demonstrate the pivotal role of modern-like CO2 on the onset and dynamism of the PPT GrIS.
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Autores principales: | , , , , , |
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Formato: | article |
Lenguaje: | EN |
Publicado: |
Nature Portfolio
2018
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Materias: | |
Acceso en línea: | https://doaj.org/article/d2d78952d60d4b52a590f1b1684b98db |
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Sumario: | Previous work has argued for a CO2 control on the development of the Plio-Pleistocene Transition (PPT, 3.0–2.5 Ma) Greenland Ice Sheet (GrIS). Here based on transient ice sheet experiments, the authors demonstrate the pivotal role of modern-like CO2 on the onset and dynamism of the PPT GrIS. |
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