Figure F22. Comparison of the percent fragmentation of planktonic foraminifers (blue line) and weight percent carbonate (red line) at Site 1089 (Hodell et al., 2001) with the carbonate dissolution index (CDI) from the Indian Ocean (Peterson and Prell, 1985). The carbonate signal is very similar to Indo-Pacific dissolution records, but Site 1089 has greater fidelity because of its high sedimentation rates.

Figure F22. Comparison of the percent fragmentation of planktonic foraminifers (blue line) and weight percent carbonate (red line) at Site 1089 (Hodell et al., 2001) with the carbonate dissolution index (CDI) from the Indian Ocean (Peterson and Prell, 1985). The carbonate signal is very similar to Indo-Pacific dissolution records, but Site 1089 has greater fidelity because of its high sedimentation rates.