@article{de_boer_persistent_2014,
	title = {Persistent 400,000-year variability of antarctic ice volume and the carbon cycle is revealed throughout the plio-pleistocene},
	volume = {5},
	issn = {20411723},
	doi = {10.1038/ncomms3999},
	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.},
	journal = {Nature Communications},
	author = {De Boer, B and Lourens, Lucas J and Van De Wal, Roderik S.W.},
	year = {2014},
	pmid = {24385005},
	note = {ISBN: 2041-1723
Publisher: Nature Publishing Group},
}

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