Figure F23. Correlation of the planktonic delta18O signal at Site 1089 with Vostok deltaD. This correlation permits development of a marine chronology for the Vostok ice core and comparison of the relative phasing of atmospheric and oceanic variables (after Ninnemann et al., 1999 and Mortyn et al., submitted [N5]).

Figure F23. Correlation of the planktonic

¹⁸O signal at Site 1089 with Vostok

D. This correlation permits development of a marine chronology for the Vostok ice core and comparison of the relative phasing of atmospheric and oceanic variables (after Ninnemann et al., 1999 and Mortyn et al., submitted [N5]).