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• W2155706641 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 δ13C 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. The precise contributions of solar forcing, the carbon cycle and glaciation to the pacing of global climate remains unresolved. Using four 3D ice-sheet models, de Boer et al.show that Antarctic ice volume and carbon-cycle dynamics varied coherently during the Pleistocene, as has been observed in the Miocene." @default.
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• W2155706641 date "2014-01-02" @default.
• W2155706641 modified "2023-10-02" @default.
• W2155706641 title "Persistent 400,000-year variability of Antarctic ice volume and the carbon cycle is revealed throughout the Plio-Pleistocene" @default.
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• W2155706641 doi "https://doi.org/10.1038/ncomms3999" @default.
• W2155706641 hasPubMedId "https://pubmed.ncbi.nlm.nih.gov/24385005" @default.
• W2155706641 hasPublicationYear "2014" @default.
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