Climate Variability in the Levant basin during the last deglaciation
Climate variability of the eastern part of the Mediterranean Sea during the last deglaciation has been reconstructed from a marine sediment core MD04-2722 (33°09 N; 33°49 E, 1780 m w.d.) retrieved in the Levant basin. A multi-proxy approach provided records of surface waters conditions and of detrital inputs to the core location through chemical
Vidal, L. et al.
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2012