Figure F2. A. Comparison of the benthic stable isotope records for Sites 1170 and 1190 (Billups et al., 2002) across the late Oligocene-early Miocene providing the basis for matching up the Mi-1a and Mi-1 events. B. A detailed comparison of the Mi-1 events including the magnetic reversal points at Site 1170 show that the pattern of the characteristic double-peak of this event is different between sites. Ages are after Cande and Kent (1995). MR = magnetic reversal.

Figure F2. A. Comparison of the benthic stable isotope records for Sites 1170 and 1190 (Billups et al., 2002) across the late Oligocene-early Miocene providing the basis for matching up the Mi-1a and Mi-1 events. B. A detailed comparison of the Mi-1 events including the magnetic reversal points at Site 1170 show that the pattern of the characteristic double-peak of this event is different between sites. Ages are after Cande and Kent (1995). MR = magnetic reversal.