Downloaded from http://sp.lyellcollection.org/ by guest on December 1, 2015 Late Quaternary beach deposits and archaeological relicts on the coasts of Cyprus, and the possible implications of sea-level changes and tectonics on the early populations E. GALILI1*, M. S¸EVKETOG˘ LU2, A. SALAMON3, D. ZVIELY4, H. K. MIENIS5, B. ROSEN6 & S. MOSHKOVITZ3 1Zinman Institute of Archaeology, University of Haifa, 199 Aba-Khoushy Avenue, Mount Carmel, Haifa 3498838, Israel 2Centre for Archaeology, Cultural Heritage and Conservation, Cyprus International University, Nicosia, 99040, Cyprus 3Geological Survey of Israel, 30 Malkhei Israel Street, Jerusalem 95501, Israel 4The Leon Recanati Institute for Maritime Studies, University of Haifa, 199 Aba-Khoushy Avenue, Mount Carmel, Haifa 3498838, Israel & School for Marine Sciences, Ruppin Academic Center, Michmoret, Israel 5The Steinhardt National Collections of Natural History, Department Zoology, Tel Aviv University, Tel Aviv 69978, Israel 6Israel Antiquities Authority, PO Box 180, Atlit 30300, Israel *Corresponding author (e-mail:
[email protected]) Abstract: Late Pleistocene beach deposits in 22 selected sites around Cyprus demonstrate the ver- tical changes in the Earth’s crust in that island over the last 125 ka. The beach/shallow-marine deposits were observed on the abraded coastal cliffs at 3–22 m above the present sea-level. They overlie Pliocene marls, and some of them contain the Senegalese marine gastropods Persististrom- bus latus, Bursa granularis and Conus ermineus that no longer live in the Mediterranean. These are index fossils for the Marine Isotope Stage (MIS) 5e in the Mediterranean and, as such, suggest an uplift of up to 15.5 m over about the last 125 ka: that is a maximal rate of 0.12 mm a21.