2000/12/08 by Konrad A Hughen, John Southon, Scott J. Lehman +1 · 8 citations
Earth and Planetary Sciences · Environmental Science · #Geology and Paleoclimatology Research #Isotope Analysis in Ecology #Archaeology and ancient environmental studies
paper · doi:10.1126/science.290.5498.1951
openalex publication_date 2000/12/08 · openalex created_date 2025/10/10 · openalex updated_date 2026/07/23
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.