Radiocarbon Calibration and Comparison to 50 Kyr BP with Paired 14 C and 230 Th Dating of Corals from Vanuatu and Papua New Guinea

• Published in: Radiocarbon
• Main Authors: Cutler, K B, Gray, S C, Burr, G S, Edwards, R L, Taylor, F W, Cabioch, G, Beck, J W, Cheng, H, Moore, J
• Format: Article in Journal/Newspaper
• Language: English
• Published: Cambridge University Press (CUP) 2004
• Subjects: General Earth and Planetary Sciences; Archeology; Greenland
• Online Access: http://dx.doi.org/10.1017/s0033822200033063; https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0033822200033063

We calibrated portions of the radiocarbon time scale with combined 230 Th, 231 Pa, 14 C measurements of corals collected from Espiritu Santo, Vanuatu and the Huon Peninsula, Papua New Guinea. The new data map 14 C variations ranging from the current limit of the tree-ring calibration [11,900 calendar years before present (cal BP), Kromer and Spurk 1998, now updated to 12,400 cal B P, see Kromer et al., this issue], to the 14 C-dating limit of 50,000 cal BP, with detailed structure between 14 to 16 cal kyr BP and 19 to 24 cal kyr BP. Samples older than 25,000 cal BP were analyzed with high-precision 231 Pa dating methods (Pickett et al. 1994; Edwards et al. 1997) as a rigorous second check on the accuracy of the 230 Th ages. These are the first coral calibration data to receive this additional check, adding confidence to the age data forming the older portion of the calibration. Our results, in general, show that the offset between calibrated and 14 C ages generally increases with age until about 28,000 cal BP, when the recorded 14 C age is nearly 6800 yr too young. The gap between ages before this time is less; at 50,000 cal BP, the recorded 14 C age is 4600 yr too young. Two major 14 C-age plateaus result from a 130 drop in Δ 14 C between 14–15 cal kyr BP and a 700 drop in Δ 14 C between 22–25 cal kyr BP. In addition, a large atmospheric Δ 14 C excursion to values over 1000 occurs at 28 cal kyr BP. Between 20 and 10 cal kyr BP, a component of atmospheric Δ 14 C anti-correlates with Greenland ice δ 18 O, indicating that some portion of the variability in atmospheric Δ 14 C is related to climate change, most likely through climate-related changes in the carbon cycle. Furthermore, the 28-kyr excursion occurs at about the time of significant climate shifts. Taken as a whole, our data indicate that in addition to a terrestrial magnetic field, factors related to climate change have affected the history of atmospheric 14 C.