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- W1999080586 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." @default.
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- W1999080586 date "2000-12-08" @default.
- W1999080586 modified "2023-10-14" @default.
- W1999080586 title "Synchronous Radiocarbon and Climate Shifts During the Last Deglaciation" @default.
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- W1999080586 doi "https://doi.org/10.1126/science.290.5498.1951" @default.
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