Abstract

AbstractThe mineral assemblages in prehistoric sites can provide essential information on several important topics in archaeology. One of the key analytical tools used is Fourier‐transform infrared spectrometry, which is operated both on‐site during the excavation and in the laboratory. Three topics are reviewed here based on studies of Hayonim and Kebara caves in Israel. (1) Reaction rims form on calcitic and dolomitic rocks buried in the sediments. They are normally the result of interaction of the rock minerals with phosphate‐rich groundwater. The mineralogical nature of these reaction rims can be indicative of prevailing chemical conditions in the sediments, which in turn provide information on whether or not bones are preserved at the site, or are preserved at specific locales within the site. Thus, a survey of reaction rims can be helpful in determining the potential of a future excavation site, or areas within a site, and for optimizing excavation strategies during an ongoing project. (2) The preservational states of the bones themselves, together with information on the mineralogical nature of some of the more labile sediment components, can be used for ascertaining whether or not the bone distribution patterns as excavated represent the original burial locations, or have been affected by secondary dissolution of bones in some areas and not others. (3) The ashes from wood fires are a major component of the sediments in both caves studied. Understanding and monitoring the complex series of diagenetic changes that ashes undergo in these environments can provide invaluable information, not only on the manner in which fire was used by the cave occupants, but also on a series of important processes that affect the depositional history of the site itself. The study of mineral assemblages in prehistoric cave sites, as illustrated here with 3 examples, and possibly in open‐air sites as well, has the potential for contributing significantly to a better understanding of many archaeological problems.

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