TEMPERATURE ESTIMATES AND HYDROCLIMATE VARIABILITY IN CORRESPONDENCE TO DANSGAARD-OESCHGER EVENTS AND GLACIAL TERMINATIONS FROM THE EASTERN MEDITERRANEAN
Reconstructed magnitudes of temperature and precipitation changes in the Eastern Mediterranean are unknown over the last 150 kyrs although it covers a critical time and area in human and mammal evolution. We quantified temperature and hydroclimate changes within a multi-proxy biomarker study. Lipid biomarkers during several D-O events from MIS 3 and over the last two terminations were extracted at centennial resolution. Mean air temperatures (MAT) based on down-core distributional changes in branched glycerol dialkyl glycerol tetraethers (brGDGTs), indicate a 1.5-3° warming at stadial/interstadial transitions and 2-4° warming for glacials/interglacial transitions. Simultaneous analysis of the leaf wax hydrogen isotopic composition (δ2Hwax) result in a reconstruction of changes in the source water due to variable precipitation/evaporation ratio. Isotopically 10 ‰ (20 ‰) lighter dD-values of leaf-wax n-alkane C29 argue for a significantly increased humidity during the interstadials (interglacials) compared to the stadials (glacials). Recently, it has been proposed that highly variable climates, substantially influenced megafaunal transition events instead of the more often proposed effect of long-lasting glacial coldness. How far, the changes in magnitude of the reconstructed temperatures and precipitation in the Eastern Mediterranean fit into the proposed climate-driven mechanism of megafaunal evolution needs to be tested.