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. [cascade flags: wikipedia_dropped_other_sources_exist | tier=silver indep_score=0.9 clusters=4 claim_tier=notable]

Sources