THE TIMING OF HIGH SEA LEVELS OVER THE PAST 200,000 YEARS

The Th-230 ages and U-234/U-238 ratios were determined for Barbados co rals that grew during periods of high sea level within the last 200,00 0 years. The similarity of the initial U-234/U-238 ratios of some of t he corals to the modern marine value suggests that these samples are p ristine and that the marine U-234/U-238 ratio 83,000 and 200,000 years ago was within 2 per mil of the modern value. The accuracies of the T h-230 ages are evaluated on the basis of the U-234/U-238 values and a model of the behavior of uranium and thorium isotopes during diagenesi s. For the last three interglacial and two intervening interstadial pe riod, sea level peaked at or after peaks in summer insolation in the N orthern Hemisphere. This overall pattern supports the idea that glacia l-interglacial cycles are caused by changes in Earth's orbital geometr y. The sea-level drop at the end of the penultimate interglacial, the last interglacial, and a subsequent interstadial period lagged behind the decease in insolation by 5,000 to 10,000 years.