The open-air Acheulian site in Holon, Israel, was dated by the luminescence
methods and by electron spin resonance (ESR), Situated in the coastal plai
n Quaternary Kurkar Group, the Holon site was first excavated in the late 1
960s, when typical lower Paleolithic lithics and middle Pleistocene fauna w
ere found. In order to date the site, new test pits were dug adjacent to th
e earlier excavations and the archaeological bed was exposed in a section c
omprising a series of paleosols and aeolianites. Alkali feldspars separated
from the sediments were dated using the infrared stimulated luminescence a
nd thermoluminescence signals, and quartz was dated using the optically sti
mulated luminescence signal. The age of the archaeological bed is constrain
ed by two samples to 198,000 +/- 22,000-201,000 +/- 17,000 yr, The age of t
he base of the section is 240,000 +/- 29,000 yr, and the age of the top is
81,000 +/- 8000 yr. Two teeth from the archaeological bed, recovered from t
he original excavation collection, yielded an average ESR age of 204,000 +/
- 16,000 yr, calculated using the linear uptake model, which is in a very g
ood agreement with the luminescence ages; These dates place Holon within th
e range of other late Acheulian and Acheulo-Yabrudian sites in this region
such as Tabun E (younger chronology), Yabrud I (archaeological level 18), a
nd Berekhat Ram, (C) 1999 University of Washington.