HistoryLate PleistoceneFlorida, United Stateshigh confidence

The Page-Ladson site lies in a 30-foot-deep sinkhole in Florida's Aucilla River, which during the late Pleistocene—when sea levels were approximately 300 feet lower—was a spring-fed pond rather than part of a river.

Notes on verification

Well-documented archaeological/paleontological site with peer-reviewed publications (Science Advances) and multiple independent corroborating sources including academic and museum references.

Sources