Abstract
We synthesize results of extensive archaeological surveys and geoarchaeological investigations of Carolina bays and other depressional wetlands on the U.S. Department of Energy’s Savannah River Site (SRS). The SRS is located along the Savannah River in the upper Coastal Plain of South Carolina. These data are augmented with data from Carolina bays elsewhere within their middle to south Atlantic Coastal Plain range. Carolina bays are shallow, oriented upland ponds that formed during the late Pleistocene under climatic conditions very different from present. Their use by prehistoric populations was most intensive during the Paleoindian and Archaic periods. Subsequent use by Woodland and Mississippian populations tended to be ephemeral. Change through time in the prehistoric use of Carolina bays and other depressional wetlands is linked to regional-scale changes in climate, particularly to the hydrologic regime.
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