Fig. 3: Scatter plot of Δ14C data from Dispilio against reference from Brehm et al.22 and IntCal2070, and best last ring-fit for the dated wood samples (χ2). | Nature Communications

Fig. 3: Scatter plot of Δ14C data from Dispilio against reference from Brehm et al.22 and IntCal2070, and best last ring-fit for the dated wood samples (χ2).

From: Absolute dating of the European Neolithic using the 5259 BC rapid 14C excursion

Fig. 3: Scatter plot of Δ14C data from Dispilio against reference from Brehm et al.22 and IntCal2070, and best last ring-fit for the dated wood samples (χ2).

a Measured 14C concentrations represented as Δ14C, vertical bars represent 1σ errors (Supplementary Data 1); legend labels marked with “DISP-“ and larger symbols refer to wood samples from Dispilio and corresponding 14C measurements obtained in this study; other labels represent data from Brehm et al.22, measurements from Siberian larch, Bristlecone pine, and Irish oak measured at two different labs, symbol shapes according to Lab; Bristlecone pine 14C data are shifted forward by 1 year from the original BR22 publication following a correction to the dating of the bristlecone master tree-ring chronology (Supplementary Note 2); shaded band represents IntCal2070. Inset in right corner same as in main panel a. but at higher resolution, spanning 14 years centred around the 14C spike. Lower two panels: χ2 tests of Dispilio measurements against the average from BR2222, b. χ2 test results for wood samples DISP-10,070 and DISP-10063 (χ2 crit. value = 9.49), and c for wood samples DISP-10206 and DISP-10611 (χ2 crit. value = 15.51), legend as in panel above. Figure panels produced in R101, code and source data available in Supplementary Data 3.

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