The theoretical and experimental basis for the development of a new dating
technique using beta-gradient isochrons and ESR is presented. For uranium-f
ree portions of enamel adjacent to sediment, we can determine a beta-dose g
radient due to sources in the nearest 2 mm layer of the sediment. If the eq
uivalent dose to successive layers of enamel is plotted against the beta do
se rate to each layer, an estimate of the age (equal to the slope of the li
ne) that depends only on the environmental beta dose rate can be determined
. Experimental methods and results for four teeth are discussed. The signif
icance of this approach lies in its ability to isolate an age estimate that
is independent of the uranium uptake model, since only portions of the ena
mel which are far away enough from internal sources of uranium, such, as de
ntine, are used. In addition, this technique provides a time-averaged estim
ate of the actual gamma plus cosmic dose rate provided that a reasonable es
timate of the average moisture content is used to calculate the environment
al beta dose rate. (C) 2000 Published by Elsevier Science Ltd.