Title |
Persistent 400,000-year variability of Antarctic ice volume and the carbon cycle is revealed throughout the Plio-Pleistocene
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Published in |
Nature Communications, January 2014
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DOI | 10.1038/ncomms3999 |
Pubmed ID | |
Authors |
B. de Boer, Lucas J. Lourens, Roderik S.W. van de Wal |
Abstract |
Marine sediment records from the Oligocene and Miocene reveal clear 400,000-year climate cycles related to variations in orbital eccentricity. These cycles are also observed in the Plio-Pleistocene records of the global carbon cycle. However, they are absent from the Late Pleistocene ice-age record over the past 1.5 million years. Here we present a simulation of global ice volume over the past 5 million years with a coupled system of four three-dimensional ice-sheet models. Our simulation shows that the 400,000-year long eccentricity cycles of Antarctica vary coherently with δ(13)C data during the Pleistocene, suggesting that they drove the long-term carbon cycle changes throughout the past 35 million years. The 400,000-year response of Antarctica was eventually suppressed by the dominant 100,000-year glacial cycles of the large ice sheets in the Northern Hemisphere. |
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Geographical breakdown
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Unknown | 2 | 67% |
Demographic breakdown
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Members of the public | 1 | 33% |
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Geographical breakdown
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Netherlands | 1 | <1% |
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Canada | 1 | <1% |
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Researcher | 30 | 21% |
Student > Master | 19 | 14% |
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Student > Doctoral Student | 6 | 4% |
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Arts and Humanities | 2 | 1% |
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