Journal
QUATERNARY RESEARCH
Volume 55, Issue 3, Pages 293-302Publisher
ACADEMIC PRESS INC
DOI: 10.1006/qres.2001.2230
Keywords
luminescence dating; dunes; paleoclimate; southeastern United States
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Most inland eolian dunes associated with rivers on the Georgia Coastal Plain probably date to glacial periods. Direct dating of the dune sand by optically stimulated luminescence dating, combined with limiting ages from radiocarbon dating, shows that dunes formed during isotope stage 2, stage 3, the transition between stages 4 and 5, and isotope stage 6 or earlier. Most of the dates indicate dune activity between 30,000 and 15,000 years ago. Holocene activity included limited and local reworking of the crests of some thick dunes along streams that flow from the Piedmont. (C) 2001 University of Washington.
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