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Science 19 January 1968:
Vol. 159. no. 3812, pp. 297 - 300
DOI: 10.1126/science.159.3812.297

Articles

Milankovitch Hypothesis Supported by Precise Dating of Coral Reefs and Deep-Sea Sediments

Wallace S. Broecker 1, David L. Thurber 1, John Goddard 1, Teh-lung Ku 2, R. K. Matthews 3, and Kenneth J. Mesolella 3

1 Lamont Geological Observatory, Columbia University, Palisades, and Queens College, Flushing, New York
2 Department of Chemistry, Woods Hole Oceanographic Institution, Woods Hole, Massachusetts
3 Department of Geological Sciences, Brown University, Providence, Rhode Island

Barbados provides a possibly unique opportunity for reconstruction of the times and elevations of late-Pleistocene high stands of the sea. The island appears to be rising from the sea at a uniform rate that is fast enough to separate in elevation coral-reef tracts formed at successive high stands of the sea. Unaltered coral found in the lower terraces enables high-precision Th230: U234 and Pa231: U235 dating. Three distinct high stands of the sea are found about 122,000, 103,000, and 82,000 years ago. New Pa231 and Th230 dates from a deep-sea core also indicate that Ericson's W-X cold-to-warm climatic change occurred close to 126,000 years ago. These data show a parallelism over the last 150,000 years between changes in Earth's climate and changes in the summer insolation predicted from cycles in the tilt and precession of Earth's axis.


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E. Rona, E. Rona, and C. Emiliani (1969)
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Subaerial Diagenesis of Carbonate Sediments: Efficiency of the Solution-Reprecipitation Process.
W. H. Harris and R. K. Matthews (1968)
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