Earliest Neolithic occupation and maritime adaptation on the West Pacific coast

Maritime adaptation plays a significant role in the dispersal of modern humans and the transition of subsistence strategies. The real timing of the worldwide intensification of maritime adaptation has been debated mainly because of the presumed inundation of archaeological sites (prior to 7000 cal yr BP) by early Holocene sea-level rise. In this study, we present a coastal shell midden submerged -8 m below the present sea level at the Jingtoushan site, containing robust evidence of the earliest Neolithic occupation and maritime adaptation on the West Pacific. Bayesian modelling of 15 14C dates, cultural deposits, and microfossils (pollen, phytolith, and diatom) indicated that the Jingtoushan site was an anthropogenic deposit originally accumulated on the coastline during the stable sea-level period (8000-7600 cal yr BP) and subsequently submerged by sea-level jumps. In addition to being largely dependent on marine food resources, humans also utilised the stable sealevel window of meltwater pulses and began rice cultivation. This study not only pushed back the timing of maritime adaptation to 8000 cal yr BP but also provides promise for future investigations of coastal underwater settlements, shedding new light on the understanding of the West Pacific coastal environment and cultural succession.

Automated summary

This study presents evidence from the Jingtoushan site in West Pacific, indicating that maritime adaptation dates back to 8000 cal yr BP. The site was an anthropogenic deposit accumulated during the stable sea-level period and subsequently submerged by sea-level jumps. This study sheds new light on the understanding of the West Pacific coastal environment and cultural succession.