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Lake Van Drilling Project "PALEOVAN", a long continental record in eastern Turkey: Geochronology, palynostratigraphy and environmental response on volcanic events

Subject Area Palaeontology
Term from 2013 to 2019
Project identifier Deutsche Forschungsgemeinschaft (DFG) - Project number 235992761
 
Final Report Year 2019

Final Report Abstract

The new high-resolution Lake Van pollen record provides a unique sequence of the penultimate interglacial–glacial cycle in eastern Anatolia (broadly equivalent to MIS 7 and MIS 6) that fills the gap in data coverage between the northern Levant and southern Europe. During the penultimate interglacial complex (MIS 7e, 7c, and 7a), high local and regional effective soil moisture availability is evidenced by a well-developed temperate oak steppeforest with pistachio and juniper, high charcoal accumulation, and reduced physical erosion during the climate optima. The direct comparison with southwestern European records shows that all three terrestrial warm intervals are characterized by clear interglacial conditions, with the largest extent of tree vegetation during MIS 7c instead of MIS 7e. This underlines once again the sensitive environmental response to global climate change in the continental setting of the Near East compared to global ice volume and/or greenhouse gas. During the penultimate glacial, strong aridification and cold climate conditions are inferred from open desert-steppe vegetation that favours soil erosion and high terrigenous input. In addition, the sensitive Lake Van pollen record reveals high temperate oscillations between 193 and 157 ka, followed by a period of lower tree variations and the predominance of desert-steppe from 157 to 131 ka that highlighted Dansgaard–Oeschger-like events during MIS 6.

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