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Radiocarbon calibration beyond 20,000 <sup>14</sup>C yr B.P. by means of planktonic foraminifera of the Iberian Margin
We present a new set of 14 C ages obtained by accelerator mass spectrometry (AMS) on planktonic foraminifera from a deep-sea core collected off the Iberian Margin (MD952042). Th...
Comparison of <sup>14</sup>C and U-Th Ages in Corals from IODP #310 Cores Offshore Tahiti
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Atmospheric Radiocarbon Calibration to 45,000 yr B.P.: Late Glacial Fluctuations and Cosmogenic Isotope Production
More than 250 carbon-14 accelerator mass spectrometry dates of terrestrial macrofossils from annually laminated sediments from Lake Suigetsu (Japan) provide a first atmospheric ...
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We built a floating, 1382-ring pine chronology covering the radiocarbon age interval of 12,000 to 10,650 BP. Based on the strong rise of Δ 14 C at the onset of the Younger Dryas...
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Publication Info
- Year
- 1990
- Type
- article
- Volume
- 346
- Issue
- 6283
- Pages
- 456-458
- Citations
- 825
- Access
- Closed
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Identifiers
- DOI
- 10.1038/346456a0