Figure F21. Carbonate (red line) and benthic delta18O (black line) signals from Site 1089 showing the "Pacific-type" carbonate stratigraphy marked by high carbonate during glacials and low carbonate during interglacials. The benthic delta18O signal leads the carbonate signal by an average of ~7.6 k.y. (after Hodell et al., 2001).

Figure F21. Carbonate (red line) and benthic

¹⁸O (black line) signals from Site 1089 showing the "Pacific-type" carbonate stratigraphy marked by high carbonate during glacials and low carbonate during interglacials. The benthic

¹⁸O signal leads the carbonate signal by an average of ~7.6 k.y. (after Hodell et al., 2001).