The southern and western coastlines of South Africa have an extensive archaeological record with many sites associated with widespread eolian deposits. While much of this rich archaeological record is based on cave sites, evidence of Late Stone Age occupation is additionally preserved in the form of open-site shell middens. We present here a comparative study of the application of amino acid racemization (AAR), optically stimulated luminescence (OSL), and radiocarbon analyses to three Late Stone Age (LSA) midden sites found within dunes on the southern coastline of South Africa. Preliminary geochronological analyses suggest that middens offer opportunity to fill in gaps in what is still a fragmentary archaeological record. Results show OSL and radiocarbon ages in good agreement, illustrating the potential to date not only the middens but also the surrounding dunes that constituted the dwelling sites. AAR results show increasing ratios with age and also that the application of paired shell and "whole rock" AAR can provide insights into the degree of biogenic sediment recycling at buried midden sites. However, the work also highlights that caution is required when OSL sampling sediment associated with middens which may have undergone human disturbance and that further work is required to improve the regional marine reservoir correction for radiocarbon dating in this part of South Africa. The study also illustrates that AAR will only provide useful data provided that middens have been sufficiently deeply buried to overcome fluctuations in environmental variables that affect the racemization rate and that inter-genus comparisons should be avoided. © 2008 Wiley Periodicals, Inc.
INTRODUCTIONThe South African coastline exhibits an extensive suite of Holocene coastal dunes, the most recent manifestation of multiple generations of eolianites ranging in age back to the Neogene (Illenberger, 1996;Roberts & Brink, 2002;Bateman et al., 2004). Geoarchaeology: An International Journal, Vol. 23, No. 6, 715-741 (2008 Coastal dunefields of the southern coast are commonly found within logspiral bays on the down-drift aspect of river mouths. Some localities such as Sedgefield exhibit multiple accretionary dune complexes that in places exceed 30 m in height (e.g., Tinley, 1985;Illenberger, 1996;Roberts & Brink, 2002;Bateman et al., 2004). Renowned archaeological cave sites, including Die Kelders, Blombos, Pinnacle Point, and the Klasies River mouth are also found along this coastline and contain evidence for the emergence of early anatomically and cognitively modern humans during the Middle Stone Age (MSA; ca. 250-12 ka; e.g., Henshilwood et al., 2002Henshilwood et al., , 2004Marean et al., 2007). Deposits within the caves are frequently of eolian origin and may contain or have influenced the preservation of archaeological material (Henshilwood et al., 2004;Marean et al., 2007). These sites record the human occupation and subsistence in the coastal zone as far back as marine isotope stage 6 or ca. 160 ka (Marean et al., 2007). Evide...