What Windover demonstrated was that wet-site conditions could produce exceptional organic preservation even in warm climates — that the key factors were waterlogging and anoxia rather than cold temperatures specifically.

This opened the possibility of applying wet-site analytical methods to a wider range of environments and searching more actively for similar preservation conditions in other warm-climate settings.

Florida itself has many peat ponds and waterlogged sites that might contain comparable material.

The question of which specific chemical and physical conditions at Windover produced the level of preservation observed — and whether those conditions are replicable or identifiable elsewhere — has been a subject of ongoing research in Florida archaeology.

The methods developed for excavating Windover — the dewatering procedures, the careful wet screening of peat matrix, the rapid stabilization of recovered organic material, the block-lifting of especially fragile items for laboratory recovery — became part of the methodological toolkit for Florida wet-site archaeology and have influenced practice at other wet sites in the region.