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