Samples of fossil tooth enamels taken from different depths of Karain
Cave (Antalya, Turkey) were studied by the ESR method. The accumulated
doses (D(E)s) of the samples were determined using the paramagnetic c
enter at g = 2.0020 +/- 0.0003 by means of three different microwave p
ower conditions. It is found that the dating signal at g = 2.0020 (Del
ta Hpp approximate to 0.34 mT) is disturbed significantly by the isotr
opic signal at g = 2.0007 +/- 0.0003 at high microwave power. The life
time of this signal is significantly smaller than the lifetime of the
dating signal. However, the statistical uncertainty caused by differen
t microwave powers is still within the total uncertainty in the age de
termination of the tooth enamels under investigation. The ESR ages of
the samples were calculated using early uranium (EU) and linear uraniu
m (LU) uptake models. The ages due to EU and LU models are in agreemen
t within an error of 10% due to the low uranium content of the samples
.