2000
DOI: 10.1006/jhev.1999.0352
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ESR dating of the Die Kelders Cave 1 Site, South Africa

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Cited by 41 publications
(16 citation statements)
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“…For luminescence, 5.5 m of rock above the cave was assumed, while for ESR, 24 m of overburden was assumed. Examination of the photographs of Marean et al (2000) shows that 5.5 m is likely to be the correct value, so the values given by Feathers and Bush (2000) were used for this study instead of the values of Schwarcz and Rink (2000). Two of the ESR samples were conjoining pieces of a tooth found in layers 4/5 and 6, so these layers have to be regarded as one stratigraphic unit for dating purposes.…”
Section: Comment [Msu34]: Referencesmentioning
confidence: 99%
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“…For luminescence, 5.5 m of rock above the cave was assumed, while for ESR, 24 m of overburden was assumed. Examination of the photographs of Marean et al (2000) shows that 5.5 m is likely to be the correct value, so the values given by Feathers and Bush (2000) were used for this study instead of the values of Schwarcz and Rink (2000). Two of the ESR samples were conjoining pieces of a tooth found in layers 4/5 and 6, so these layers have to be regarded as one stratigraphic unit for dating purposes.…”
Section: Comment [Msu34]: Referencesmentioning
confidence: 99%
“…Feathers and Bush (2000) calculated alternative dates using 10%, 15%, and 20% water content with an uncertainty of ±5%. Schwarcz and Rink (2000) calculated alternative dates assuming 10%, 20%, and 30% water content. It seems prudent to allow for this uncertainty by assuming a water content of 20 ± 10%.…”
Section: Comment [Msu34]: Referencesmentioning
confidence: 99%
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“…In the early 1990s, research resumed at the site under G. Avery, C. Marean, and F. Grine in order to expand the MSA artifact collection, explore the paleoenvironmental context of the cave sequence, and understand the geologic contexts. While the absolute dating of the full DK1 sequence is still not fully known, it is arguably close to 70 ± 10 ka (Feathers and Bush, 2000;Schwarcz and Rink, 2000). Grine et al (1991) report the MSA lithic assemblage from the Schweitzer excavations and note a dramatic increase in the frequency of fine-grained raw materials (silcrete) in Layer 9-12, while also indicating that the assemblage is not typologically linked to the HP or SB.…”
Section: Pinnacle Pointmentioning
confidence: 99%