A Raman micro-spectroscopy study of 77,000 to 71,000 year old ochre processing tools from Sibudu, KwaZulu-Natal, South Africa

Abstract Many Middle Stone Age sites in South Africa yielded hundreds, even thousands, of ochre pieces sometimes showing use traces. Less attention has been paid to the tools used for their processing. Here, seven tools excavated from the oldest layers (71,000 to 77,000 years ago) of Sibudu rock she...

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Main Authors: Marine Wojcieszak, Lyn Wadley
Format: Article
Language:English
Published: SpringerOpen 2019-05-01
Series:Heritage Science
Subjects:
Online Access:http://link.springer.com/article/10.1186/s40494-019-0267-9
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spelling doaj-70ffb1e1e3b94e67b24b1263597b8f4f2020-11-25T02:57:40ZengSpringerOpenHeritage Science2050-74452019-05-017111410.1186/s40494-019-0267-9A Raman micro-spectroscopy study of 77,000 to 71,000 year old ochre processing tools from Sibudu, KwaZulu-Natal, South AfricaMarine Wojcieszak0Lyn Wadley1Evolutionary Studies Institute (ESI), University of the WitwatersrandEvolutionary Studies Institute (ESI), University of the WitwatersrandAbstract Many Middle Stone Age sites in South Africa yielded hundreds, even thousands, of ochre pieces sometimes showing use traces. Less attention has been paid to the tools used for their processing. Here, seven tools excavated from the oldest layers (71,000 to 77,000 years ago) of Sibudu rock shelter were studied non-invasively to identify the micro-residues on them. The tools were first examined with optical microscopy to detect areas of interest. Then, Raman micro-spectroscopy was performed on the residues present, as well as on random areas of tool surfaces. These Raman signatures were compared to those obtained from the sediments and ochre samples recovered from the same layers. All tools exhibited red, orange and brown stains on their surfaces and these comprised iron oxides (haematite and maghemite) and oxyhydroxide (goethite). The other compounds detected include amorphous carbon, quartz, anatase and manganese oxides. All of these can occur within ochre, but they may alternatively be natural components of other rocks and sediments, formed secondarily by decay processes. However, the large and thick residues present on the surfaces of the artefacts imply their use for ochre processing (microscopic observations and chemical analyses of the sediments and the local rocks showed that they contain only traces of haematite). Ochre seems to have been the only material processed with these old Sibudu artefacts whereas in younger occupations, items such as bone were also processed with grindstones. The grinding tools are morphologically varied and the ochre pieces are both morphologically and chemically diverse.http://link.springer.com/article/10.1186/s40494-019-0267-9ResiduesGrindstonesOchreMiddle Stone AgeRaman micro-spectroscopy
collection DOAJ
language English
format Article
sources DOAJ
author Marine Wojcieszak
Lyn Wadley
spellingShingle Marine Wojcieszak
Lyn Wadley
A Raman micro-spectroscopy study of 77,000 to 71,000 year old ochre processing tools from Sibudu, KwaZulu-Natal, South Africa
Heritage Science
Residues
Grindstones
Ochre
Middle Stone Age
Raman micro-spectroscopy
author_facet Marine Wojcieszak
Lyn Wadley
author_sort Marine Wojcieszak
title A Raman micro-spectroscopy study of 77,000 to 71,000 year old ochre processing tools from Sibudu, KwaZulu-Natal, South Africa
title_short A Raman micro-spectroscopy study of 77,000 to 71,000 year old ochre processing tools from Sibudu, KwaZulu-Natal, South Africa
title_full A Raman micro-spectroscopy study of 77,000 to 71,000 year old ochre processing tools from Sibudu, KwaZulu-Natal, South Africa
title_fullStr A Raman micro-spectroscopy study of 77,000 to 71,000 year old ochre processing tools from Sibudu, KwaZulu-Natal, South Africa
title_full_unstemmed A Raman micro-spectroscopy study of 77,000 to 71,000 year old ochre processing tools from Sibudu, KwaZulu-Natal, South Africa
title_sort raman micro-spectroscopy study of 77,000 to 71,000 year old ochre processing tools from sibudu, kwazulu-natal, south africa
publisher SpringerOpen
series Heritage Science
issn 2050-7445
publishDate 2019-05-01
description Abstract Many Middle Stone Age sites in South Africa yielded hundreds, even thousands, of ochre pieces sometimes showing use traces. Less attention has been paid to the tools used for their processing. Here, seven tools excavated from the oldest layers (71,000 to 77,000 years ago) of Sibudu rock shelter were studied non-invasively to identify the micro-residues on them. The tools were first examined with optical microscopy to detect areas of interest. Then, Raman micro-spectroscopy was performed on the residues present, as well as on random areas of tool surfaces. These Raman signatures were compared to those obtained from the sediments and ochre samples recovered from the same layers. All tools exhibited red, orange and brown stains on their surfaces and these comprised iron oxides (haematite and maghemite) and oxyhydroxide (goethite). The other compounds detected include amorphous carbon, quartz, anatase and manganese oxides. All of these can occur within ochre, but they may alternatively be natural components of other rocks and sediments, formed secondarily by decay processes. However, the large and thick residues present on the surfaces of the artefacts imply their use for ochre processing (microscopic observations and chemical analyses of the sediments and the local rocks showed that they contain only traces of haematite). Ochre seems to have been the only material processed with these old Sibudu artefacts whereas in younger occupations, items such as bone were also processed with grindstones. The grinding tools are morphologically varied and the ochre pieces are both morphologically and chemically diverse.
topic Residues
Grindstones
Ochre
Middle Stone Age
Raman micro-spectroscopy
url http://link.springer.com/article/10.1186/s40494-019-0267-9
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