A long radiometrically dated oxygen isotopic record of continental climatic
variations since the penultimate glaciation was obtained from a stalagmite
deposited in a sealed cave in Jerusalem, This record shows that speleothem
s have the potential of assigning dates to long- and short-term climatic ev
ents, with possible refining of Milankovitch tuning of ice and marine recor
ds which themselves are not datable, Short-term (similar to 1000-yr) events
are very significant in the region, reaching similar to 50% of glacial/int
erglacial fluctuations. The Mediterranean Sea was the most probable source
of local precipitation throughout the last glacial cycle. (C) 1999 Universi
ty of Washington.