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U-Th ages obtained by mass spectrometry in corals from Barbados: sea level during the past 130,000 years

Abstract

THE study of the sea level record during the last glacial cycle has primarily proceeded indirectly by means of oxygen isotope measurements on foraminifera from deep-sea sediments1,2. The direct approach of dating sea level indicators stagnated during the past decade, mainly because the samples required to complete our knowledge of the past glaciations are below the present-day sea level3–7. Using the 14C ages of Acropora palmata samples collected by drilling offshore the island of Barbados, Fairbanks8 presented the first detailed chronology for the last deglaciation. This radiocarbon chronology is limited to the past 30 kyr because of the short half-life of 14C (5,730 yr); we must therefore rely on other dating methods to obtain information for the whole last glacial cycle. During the past four years 230Th–234U dating of corals by thermal-ionization mass spectrometry has been shown to be significantly more precise and accurate than the classical α counting method9–14. We have used this technique to measure U–Th ages in coral samples from the Barbados collection and from subaerially exposed outcrops (see also ref. 15). Here we present results bearing on the sea level record for the past 130,000 years; we conclude that the last deglaciation started 3,000 years earlier than previously thought and confirm that there were two surges in melt water8 at about 11 kyr and 14 kyr BP (before present).

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Bard, E., Hamelin, B. & Fairbanks, R. U-Th ages obtained by mass spectrometry in corals from Barbados: sea level during the past 130,000 years. Nature 346, 456–458 (1990). https://doi.org/10.1038/346456a0

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