We thank Neil Roberts for editing this article and an anonymous reviewer for helpful comments to improve the discussion. Furthermore, we would like to thank H. Brückner and M. Engel (University of Cologne), who organised and performed the Tayma coring campaign in 2013, M. Stöttele (GFZ) for tephra sample preparation and M. Dinies (FU Berlin) for valuable discussions. This work was supported by the German Science Foundation DFG [BR2208/10-1
; PL535/2-1] and is a contribution to the projects “Interglacial climate variability recorded in the Dead Sea sediments” and “CLEAR: Holocene Climatic Events of Northern Arabia” (https://clear2018.wordpress.com).
GFZ German Research Centre for Geosciences, Section 5.2 – Climate Dynamics and Landscape Evolution, Telegrafenberg, Potsdam, Germany; University of Geneva, Department of Earth Sciences, Rue des Maraichers 13, Geneva, Switzerland; GFZ German Research Centre for Geosciences, Section 5.1 – Geomorphology, Telegrafenberg, Potsdam, Germany; Heidelberg University, Institute of Earth Sciences, Im Neuenheimer Feld 234, Heidelberg, Germany; GFZ German Research Centre for Geosciences, Section 4.3 – Chemistry and Physics of Earth Materials, Telegrafenberg, Potsdam, Germany
Recommended Citation:
Neugebauer I.,Wulf S.,Schwab M.J.,et al. Implications of S1 tephra findings in Dead Sea and Tayma palaeolake sediments for marine reservoir age estimation and palaeoclimate synchronisation[J]. Quaternary Science Reviews,2017-01-01,170