Plio-Pleistocene Ice Volume, Antarctic Climate, and the Global δ18O Record

By M. Raymo, L. Lisiecki, K. Nisancioglu. Science, 2006

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Tephrochronology of the Mont-Dore volcanic Massif (Massif Central, France): new 40Ar/39Ar constraints on the Late Pliocene and Early Pleistocene activity (2014, background): “The global temperature in the northern hemisphere gradually dropped during the Late Pliocene, along with an increase in glacial activity (Haug et al. 2005; Raymo et al. 2006; Lisiecki and Raymo 2007).”
Cyclostratigraphy and its revolutionizing applications in the earth and planetary sciences (2013, background): “Raymo et al. (2006) observed that precession-forced glaciations in the northern and southern polar regions are antiphased, and thus would cancel the precession signal in ocean volume and reinforce the obliquity.”
Cosmoclimatology: a new theory emerges (2007, background): “To account for high rates of deglaciation associated with particular insolation frequencies, amplifying mechanisms on offer include surges in atmospheric carbon dioxide (Shackleton 2000) and changes in ice-sheet geography (Raymo et al. 2006).”
Where to find 1.5 million yr old ice for the IPICS "Oldest-Ice" ice core (2013, background): “This would cause canceling effects on marine isotopes between Northern Hemisphere and smaller-than-present Southern Hemisphere ice sheets, both driven by 23 kyr precession cycles, but out of phase (Raymo et al., 2006).”