The Epigravettian occupants of San Teodoro emerged against the dramatic backdrop of a warming post-glacial world. Dated human remains and associated deposits from San Teodoro cave near Messina place people on northeastern Sicily between roughly 17,171 and 11,397 BCE. Archaeological data indicates adaptation to shifting coastlines and rich marine resources as sea levels rose after the Last Glacial Maximum. Lithic typologies attributed to the Epigravettian tradition—backed blades, microliths, and retouched tools—tie Sicilian groups into a wider southern European cultural horizon.
Limited evidence suggests these groups were part of regional networks of mobility rather than isolated island populations: similarities in tool styles and raw-material procurement hint at contacts with mainland southern Italy and the central Mediterranean. Yet the island setting also fostered local innovations in subsistence and settlement. While evocative rock shelters and hearth features survive at San Teodoro, the sparse sample count and taphonomic loss over millennia mean our picture is fragmentary. Archaeology indicates a resilient human presence that negotiated dramatic environmental change, leaving a material signature that only begins to align with early genetic snapshots.