|Northeastern Section (45th Annual) and Southeastern Section (59th Annual) Joint Meeting (13-16 March 2010)|
|Paper No. 10-23|
|Presentation Time: 8:00 AM-12:05 PM|
GEOARCHAEOLOGICAL INVESTIGATIONS OF CAROLINA BAYS IN SOUTH CAROLINA: METHODOLOGICAL APPROACHES FOR INTERPRETING SITE FORMATION PROCESSES, ARCHAEOSTRATIGRAPHY AND GEOCHRONOLOGY
MOORE, Christopher R.1, BROOKS, Mark J.1, IVESTER, Andrew H.2, and FERGUSON, Terry A.3, (1) Savannah River Archaeological Research Program, South Carolina Institute of Archaeology and Anthropology, USC, PO Box 400, New Ellenton, SC 29809, email@example.com, (2) Department of Geosciences, University of West Georgia, 1601 Maple Street, Carrollton, GA 30118, (3) Wofford College, 429 N Church St, Spartanburg, SC 29303-3663|
This long-term Carolina bay study addresses four basic research objectives. These are: 1) determining the age, origin, and evolution of Carolina bays; 2) delineating prehistoric cultural activities and site formation processes on Carolina bay sand rims; 3) determining the role of Carolina bays in prehistoric settlement systems; and 4) exploring linkages at Carolina bays between climate change, depositional processes, and prehistoric adaptations.
Recent geoarchaeological investigations of Carolina bay sand rims indicate they have accreted ~1 meter of sand since the beginning of the Holocene (ca. 11,450 Cal BP). Bay rim deposits at Flamingo Bay (Aiken County, SC), Johns Bay (Allendale County, SC) and Frierson Bay (Barnwell County, SC) were tested to determine archaeostratigraphy and intensively sampled for grainsize, soil chemistry, bulk phytolith, sediment bulk density, LOI, field water content, micromorphology and magnetic susceptibility. Ground Penetrating Radar (GPR) surveys were conducted to broadly delineate bay rim stratigraphy and geomorphology. Sediment samples were taken from continuous columns at 2.5 cm intervals from the ground surface to ~1 to 1.8 meters below surface. In addition, 5 single-grain luminescence (OSL) age estimates were acquired for the upper meter at Flamingo Bay using 2 cm diameter sampling tubes. Eight single-grain OSL ages were acquired for Johns Bay and Frierson Bay, including a basal rim age for Johns Bay at 2.8 meters below surface. Sediments associated with Early and Middle Archaic occupations at all three bay sites were also dated.
Tangentially, our research has implications for the recently proposed comet impact origin for Carolina bays by Firestone et al. (2007), who suggest that such impacts precipitated the Younger Dryas stadial (ca. 12,800-11,450 Cal BP), megafauna extinctions, and the demise of Clovis culture at the end of the last ice-age. Our data, however, demonstrate that Carolina bays were formed by high-energy lacustrine processes over lengths of time far greater than the onset of the YD and that bay evolution is a long-term process rather than a synchronous event.
Northeastern Section (45th Annual) and Southeastern Section (59th Annual) Joint Meeting (13-16 March 2010)
General Information for this Meeting
|Session No. 10--Booth# 40|
Quaternary Geology, Geomorphology, and Archaeological Geology (Posters)
Sheraton Baltimore City Center: International ABCDF
8:00 AM-12:05 PM, Sunday, 14 March 2010
Geological Society of America Abstracts with Programs, Vol. 42, No. 1, p. 70
© Copyright 2010 The Geological Society of America (GSA), all rights reserved. Permission is hereby granted to the author(s) of this abstract to reproduce and distribute it freely, for noncommercial purposes. Permission is hereby granted to any individual scientist to download a single copy of this electronic file and reproduce up to 20 paper copies for noncommercial purposes advancing science and education, including classroom use, providing all reproductions include the complete content shown here, including the author information. All other forms of reproduction and/or transmittal are prohibited without written permission from GSA Copyright Permissions.