Constraints on hydrological and paleotemperature variations in the Eastern Mediterranean region in the last 140 ka given by the δD values of speleothem fluid inclusions

This article appears in the special issue "Isotopes in Quaternary Paleoenvironmental Reconstruction", which emerged from a 2002 meeting on “Isotopes in Quaternary Palaeoenvironmental reconstruction” (ISOPAL) that was one of a series of PAGES sponsored workshops contributing to the Pole–Equator–Pole (PEP III) transect.