LATE GLACIAL-HOLOCENE PALEOCLIMATIC AND PALEOCEANOGRAPHIC EVOLUTION OF THE AEGEAN SEA - MICROPALEONTOLOGICAL AND STABLE ISOTOPIC EVIDENCE

Late glacial to Holocene paleoclimatic and paleoceanographic changes a re examined using records of calcareous and organic-walled marine micr ofossils, pollen and terrestrial spores and oxygen isotope data in cor es from the Aegean Sea basins. Planktic foraminiferal, coccolith and d inoflagellate data show that the late glacial-Holocene transition in t he region was associated with a large warming of surface water. Medite rranean-based paleotransfer functions for planktic foraminifera show a 5 degrees-10 degrees C increase in surface water temperature from sim ilar to 14,000 to similar to 9600 yr B.P. Estimates of surface water o xygen isotopic composition (delta(18)O(w)) derived from planktic foram iniferal oxygen isotopic and transfer function data indicate that this warming was associated with a 2.0 to 2.5 parts per thousand reduction in delta(18)O(w). Transfer function results indicate corresponding 1. 0 to 1.5 parts per thousand salinity reductions for this time (ca. 960 0-6400 yr B.P.) throughout the Aegean Sea. Pollen, dinoflagellate and isotopic data show that the early Holocene excess fresh water originat ed from rapid melting of the northern European and Siberian ice sheets ,supplied primarily from the Black Sea by the opening of Bosphorus and Dardanelles Channels, during the post glacial sea-level rise, and sup plemented by major rivers entering the Aegean Sea, Continuous outflow of fresh water into the Aegean Sea provided a low salinity surface lid , preventing the ventilation of the deep water. Benthic foraminifera s hows a major turn-over that indicates low dissolved oxygen; however, b ottom waters were not anoxic. Sapropel level S1 resulted from a combin ation of stagnant deep water in isolated depressions, increased terrig enous organic matter and periods of high primary productivity, as indi cated by pollen and dinocysts, respectively. The surface water tempera ture and salinity reached present-day values at similar to 6400 yr B.P ., with little subsequent change despite the major deforestation onsho re.