Late Glacial 14C ages from a floating, 1382-ring pine chronology
Radiocarbon, 2004•cambridge.org
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 Δ14C at the onset of the Younger Dryas
(YD) and wiggle-matching of the decadal-scale Δ14C fluctuations, we can anchor the
floating chronology to the Cariaco varve chronology. We observe a marine reservoir
correction higher than hitherto assumed for the Cariaco site, of up to 650 yr instead of 400 yr,
for the full length of the comparison interval. The tree-ring Δ14C shows several strong …
12,000 to 10,650 BP. Based on the strong rise of Δ14C at the onset of the Younger Dryas
(YD) and wiggle-matching of the decadal-scale Δ14C fluctuations, we can anchor the
floating chronology to the Cariaco varve chronology. We observe a marine reservoir
correction higher than hitherto assumed for the Cariaco site, of up to 650 yr instead of 400 yr,
for the full length of the comparison interval. The tree-ring Δ14C shows several strong …
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 Δ14C at the onset of the Younger Dryas (YD) and wiggle-matching of the decadal-scale Δ14C fluctuations, we can anchor the floating chronology to the Cariaco varve chronology. We observe a marine reservoir correction higher than hitherto assumed for the Cariaco site, of up to 650 yr instead of 400 yr, for the full length of the comparison interval. The tree-ring Δ14C shows several strong fluctuations of short duration (a few decades) at 13,800; 13,600; and 13,350 cal BP. The amplitude of the strong Δ14C rise at the onset of the YD is about 40, whereas in the marine data set the signal appears stronger due to a re-adjustment of the marine mixed-layer Δ14C towards the atmospheric level.