Stable oxygen isotope ratios of benthic foraminifera from sediment core RC13-110 (Table 1), supplement to: Pisias, Nicklas G; Mix, Alan C; Zahn, Rainer (1990): Nonlinear response in the global climate system: evidence from benthic oxygen isotopic record in core RC13-110. Paleoceanography, 5(2), 147-160

Nicklas G Pisias, Alan C Mix & Rainer Zahn
The Milankovitch theory of climate change predicts that variations of the climate system should match the dominant frequencies of the orbital forcing in the 41 and 23 kyr**-1 frequency bands. Such a linear theory would predict that the amplitude variations of the climate response in these bands should match amplitude variations in orbital forcing. Here we compare amplitude variations of the marine oxygen isotope record with orbital forcing in these bands over the last 700,000...
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