Articles | Volume 12, issue 1
https://doi.org/10.5194/cp-12-75-2016
https://doi.org/10.5194/cp-12-75-2016
Research article
 | 
18 Jan 2016
Research article |  | 18 Jan 2016

Hydroclimatic variability in the Levant during the early last glacial (∼  117–75 ka) derived from micro-facies analyses of deep Dead Sea sediments

I. Neugebauer, M. J. Schwab, N. D. Waldmann, R. Tjallingii, U. Frank, E. Hadzhiivanova, R. Naumann, N. Taha, A. Agnon, Y. Enzel, and A. Brauer

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Short summary
Micro-facies changes and elemental variations in deep Dead Sea sediments are used to reconstruct relative lake level changes for the early last glacial period. The results indicate a close link of hydroclimatic variability in the Levant to North Atlantic-Mediterranean climates during the time of the build-up of Northern Hemisphere ice shields. First petrographic analyses of gravels in the deep core question the recent hypothesis of a Dead Sea dry-down at the end of the last interglacial.