Palaeodose determination is central to luminescence dating of Quaternary sa
mples, both archaeological and geological. All existing methods assume some
knowledge of the palaeodose prior to analysis. This may be gained from est
imates of the age of the sample, or from laboratory tests. However, the for
mer is sometimes incorrect, and the latter is time consuming. Here we descr
ibe a fully automated variant of the 'single aliquot regeneration and added
dose' (SARA) method that makes no such assumptions. The software algorithm
is designed so that the system intelligently selects the radiation doses i
t gives to the sample in the laboratory on the basis of the optically stimu
lated luminescence (OSL) measurements that it makes. This reduces the numbe
r of replicate analyses that are required.
The OSL method is tested on a sample of heated quartz given known radiation
doses in the laboratory, and then on quartz extracted from a suite of arch
aeological samples (burnt stones and bricks) whose palaeodoses have been me
asured using other methods. The results are encouraging, though show the ne
ed for some further investigations. (C) 1999 Elsevier Science Ltd. All righ
ts reserved.