Figure F3. Correlation of oxygen isotope and color reflectance records at Sites 1089 (41°S), 1093 (50°S), and 1094 (53°S). Marine isotope stages represent the major terminations of the late Pleistocene. The great depth of these stage boundaries illustrates the high sedimentation rates, especially at Site 1093. The oxygen isotope record at the lowest-latitude Site 1089 is nearly complete, but the signals at higher-latitude Sites 1093 and 1094 are discontinuous because of the scarcity of foraminifers (Hodell et al., Chap. 9, this volume).

Figure F3. Correlation of oxygen isotope and color reflectance records at Sites 1089 (41°S), 1093 (50°S), and 1094 (53°S). Marine isotope stages represent the major terminations of the late Pleistocene. The great depth of these stage boundaries illustrates the high sedimentation rates, especially at Site 1093. The oxygen isotope record at the lowest-latitude Site 1089 is nearly complete, but the signals at higher-latitude Sites 1093 and 1094 are discontinuous because of the scarcity of foraminifers (Hodell et al., Chap. 9, this volume).