The Natufian horizon emerged in the Levant at the close of the Pleistocene, between roughly 12,000 and 9,500 BCE. Archaeological sites such as Raqefet Cave (Haifa Hills) preserve stone-built features, burials, and dense deposits of cultural debris that signal a shift from highly mobile foraging to prolonged seasonal occupation and incipient sedentism.
This transformation unfolded against post-glacial environmental change: rising temperatures and expanding wild-grass resources created ecological niches favorable to year-round or repeated seasonal use of key sites. At Raqefet, layers of hearths, stone-built platforms, and ritual burials attest to community focal points where food processing, social interaction, and mortuary practice converged.
Genetic data from six individuals at Raqefet fit this archaeological picture by revealing local continuity in male lineages (Y-haplogroup E predominant in five samples) alongside mitochondrial diversity (J, N1b, H). While these genetic signals hint at a stable regional population with complex connections across the Near East, the small sample size makes broader population-level inferences provisional. Limited evidence suggests the Natufians were a mosaic of local hunter-gatherer ancestry with genetic links that would later contribute to Neolithic Levantine groups.