TABLE 1. — Phases time range from 14C modeling in the cultural sequence of Doi Pha Kan site. See stratigraphic sketch for the location of dating. Data was calibrated and modeled in ChronoModel 3.1.8 (Lanos & Dufresne 2019), using IntCal20 calibration curve (Reimer et al. 2020). The starting and ending points of the posterior distribution are defined as the maximum a posteriori (MAP) of the phase distribution, in each case (fourth and fifth columns), at 95% confidence level. The phase time range (sixth column) is also given for a 95% confidence level. Posterior distributionPhase14 CCodeMaterial supportBegin MAP (cal BP) (95%)End MAP (cal BP) (95%)Phase Time Range (cal BP) (95%)dpk DE-5 (1)11895 ± 45SacA32917Human femoral shaft137091370914093-11604dpk D-4 (2)12340 ± 50SacA32916Human femoral shaft140521405214484-12567dpk E-5 (3)11170 ± 40SacA27054Human third molar155451415317004-1288912540 ± 50SacA27053Human femoral shaft12210 ± 50SacA27055Muntjac metapod shaft12920 ± 80SacA27057Fresh water oyster shell12930 ± 50SacA27056Charcoal

Published as part of Forestier, Hubert, Guibert, Justin, Pérez-Balarezo, Antonio, Auetrakulvit, Prasit, Tiamtinkrit, Chaturaporn, Sukkasen, Yoddanai & Zeitoun, Valéry, 2025, Technological variability in the Hoabinhian: the example of slab lithic production from the Doi Pha Kan site (Northern Thailand), pp. 22 in Comptes Rendus Palevol 24 (2) on page 22, DOI: 10.5852/cr-palevol2025v24a2, http://zenodo.org/record/14902333