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Synchronous Radiocarbon and Climate Shifts During the Last Deglaciation

Science  08 Dec 2000:
Vol. 290, Issue 5498, pp. 1951-1954
DOI: 10.1126/science.290.5498.1951

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Abstract

Radiocarbon data from the Cariaco Basin provide calibration of the carbon-14 time scale across the period of deglaciation (15,000 to 10,000 years ago) with resolution available previously only from Holocene tree rings. Reconstructed changes in atmospheric carbon-14 are larger than previously thought, with the largest change occurring simultaneously with the sudden climatic cooling of the Younger Dryas event. Carbon-14 and published beryllium-10 data together suggest that concurrent climate and carbon-14 changes were predominantly the result of abrupt shifts in deep ocean ventilation.

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