They left behind artifacts and archeological evidence.
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The findings are controversial, and funding has not been available for follow-up studies.
As the glaciers began retreating about 8000 BC, the climate of Florida became warmer and wetter.
As the glaciers melted, the sea level rose, reducing the land mass.
Many prehistoric habitation sites along the old coastline were slowly submerged, making artifacts from early coastal cultures difficult to find.
As a result, most paleo-Indian activity was around the watering holes.
Sinkholes and basins in the beds of modern rivers (such as the Page-Ladson prehistory site in the Aucilla River) have yielded a rich trove of paleo-Indian artifacts, including Clovis points.
As a result, the Florida peninsula not only emerged, but had a land area about twice what it is today.
Florida also had a drier and cooler climate than in more recent times. Across large areas of Florida, fresh water was available only in sinkholes and limestone catchment basins.
Two decades later, in 1845, Florida was admitted to the union as the 27th US state.