Figure F2. Planktonic foraminifer oxygen isotope record from Hole U1322B, as compared to low-latitude isotopic stack (Bassinot et al., 1994) and isotopic-derived paleotemperature record from Greenland ice cores (Johnsen et al., 2001) with age adjusted according to Shackleton et al. (2004). Hole U1322B record has been modified twice: Modified (1) = unusual or unreliable values (gray diamonds) are omitted, Modified (2) = slumped intervals (see Fig. F1) are omitted to show autochthonic hemipelagic δ18O readings only. MIS = marine isotope stage. YD = Younger Dryas, D/O = Dansgaard/Oeschger.
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