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Science 12 January 2001:
Vol. 291. no. 5502, pp. 290 - 293
DOI: 10.1126/science.291.5502.290

Reports

Orbital Forcing of the Marine Isotope Stage 9 Interglacial

C. H. Stirling,12* T. M. Esat,3 K. Lambeck,3 M. T. McCulloch,3 S. G. Blake,3 D.-C. Lee,12 A. N. Halliday12

Milankovitch orbital forcing theory has been used to assign time scales to many paleoclimate records. However, the validity of this theory remains uncertain, and independent sea-level chronologies used to test its applicability have been restricted largely to the past ~135,000 years. Here, we report U-series ages for coral reefs formed on Henderson Island during sea-level high-stands occurring at ~630,000 and ~330,000 years ago. These data are consistent with the hypothesis that interglacial climates are forced by Northern Hemisphere summer solar insolation centered at 65°N latitude, as predicted by Milankovitch theory.

1 Department of Geological Sciences, University of Michigan, Ann Arbor, Michigan 48109-1063, USA.
2 Institute for Isotope Geology and Mineral Resources, Department of Earth Sciences, ETH Zentrum, 8092 Zürich, Switzerland.
3 Research School of Earth Sciences, Australian National University, Canberra, ACT 0200, Australia.
*   To whom correspondence should be addressed. E-mail: stirling{at}erdw.ethz.ch


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