Fig. 5: Probability distributions of end-date ranges produced by wiggle-matching different sets of annual 14C data from Dispilio modelled in OxCal v4.4, against IntCal2070, and IntCal20plus.
From: Absolute dating of the European Neolithic using the 5259 BC rapid 14C excursion
In IntCal20plus the non-annual IntCal20 data for a 82-year period around the 5259 BC Miyake event is replaced by the annual average of Brehm et al.’s.22 annual data. Dashed blue lines represent actual felling dates determined through dendrochronology and Miyake event-matching. Acronyms in brackets next to sample name refer to the AMS lab that furnished the measurements. Data for figure obtained from OxCal 4.468,69. Figure produced in R101, R code, OxCal code and source data in Supplementary Data 3.
