In-solution DNA enrichment and sequencing of ancient individuals.All dates are calibrated using OxCal v4.2.458 with a mixture of the Marine13 and Intcal13 curves59 as determined by linear interpolation between dietary terrestrial/marine δ13C isotopic endpoints (−21‰/−12‰) with an uncertainty of ±10% on the per-cent marine carbon result following previous recommendations60. Two of the dates have been previously reported (for I1368/B30A and I1370/B17)61, and in this study we add two new dates: for I1369/B10B from Tonga (on the same petrous bone used for ancient DNA analysis) and on CP30/SK10 from Tonga (on a fibula). Measured 13C and 15N values for I1369/B10B are −14.5 and 13.7‰ respectively, and for SK10 −16.44‰ and 10.48‰. As justified in ref. 61, we also applied a location-specific reservoir correction (ΔR) of 40±44 14C years to the marine curve to adjust for regional oceanic variation in 14C around Vanuatu, and 11±83 14C years for Tongatapu62.