Abstract
When the fluoride content of bone is measured with an ion-selective electrode, and when the technique is correctly applied, fluoride dating is a very economical method for developing fine-scale relative chronologies. It has been successfully used to develop relative chronologies for prehistoric human burials and fossilized bones throughout the world, but its much greater potential for the dating of unfossilized faunal materials has been neglected. The fluoride contents of 889 lagomorph and 16 artiodactyl bones from 183 contexts at Los Pozos, an Early Agricultural period site in Arizona, illustrate how fluoride measurements can be used to date features. Fluoride dating offers a temporal resolution capable of distinguishing between features separated by as little as 20 to 40 years.
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