Articles | Volume 12, issue 1
Clim. Past, 12, 75–90, 2016
https://doi.org/10.5194/cp-12-75-2016
Clim. Past, 12, 75–90, 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 et al.

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Cited articles

Almogi-Labin, A., Bar-Matthews, M., Shriki, D., Kolosovsky, E., Paterne, M., Schilman, B., Ayalon, A., Aizenshtat, Z., and Matthews, A.: Climatic variability during the last  ∼  90 ka of the southern and northern Levantine Basin as evident from marine records and speleothems, Quaternary Sci. Rev., 28, 2882–2896, https://doi.org/10.1016/j.quascirev.2009.07.017, 2009.
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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.