Preprints
https://doi.org/10.5194/essd-2020-357
https://doi.org/10.5194/essd-2020-357
27 Nov 2020
 | 27 Nov 2020
Status: this preprint has been withdrawn by the authors.

MIS 5e sea-level proxies in the eastern Mediterranean coastal region

Barbara Mauz, Dorit Sivan, and Ehud Galili

Abstract. Mediterranean raised beaches were subject to Quaternary research since the early years of the 20th century. The uniqueness of a warm-loving molluscs fauna immigrating into the Mediterranean made the coastline a prime subject for studying Quaternary sea-level changes. Today, we have a detailed picture of this historically important coastline characterised by tectonically dormant coastal zone alternating with zones that are subject to subsidence or uplift. As part of the Word Atlas of last interglacial shorelines (WALIS) database we compiled 21 MIS 5e proxies for the for the eastern Mediterranean area available at http://doi.org/10.5281/zenodo.4274178 (Israel; Sivan and Galili, 2020) and at http://doi.org/10.5281/zenodo.4283819 (Turkey, Egypt, Tunisia; Mauz, 2020). All these datapoints are sea-level indicators of variable quality situated between −1 ± 4 m and 7 ± 2 m resulting in a reconstructed MIS 5e palaeo-sea level situated between −1 ± 4 m and 13 ± 10 m.

This preprint has been withdrawn.

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Barbara Mauz, Dorit Sivan, and Ehud Galili

Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
Printer-friendly Version - Printer-friendly version Supplement - Supplement
Barbara Mauz, Dorit Sivan, and Ehud Galili

Data sets

The last interglacial sea-level record of the Israeli coastline - WALIS database of sea-level indicators D. Sivan and E. Galili https://doi.org/10.5281/zenodo.4274178

Database of last interglacial sea-level proxies in the eastern Mediterranean B. Mauz https://doi.org/10.5281/zenodo.4283819

Barbara Mauz, Dorit Sivan, and Ehud Galili

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Short summary
Raised beaches have long been used to infer past sea-level fluctuations. Here we review data associated with such sea-level indicators for the eastern Mediterranean. Our standardised compilation of geological data confirm, albeit with large uncertainties, the position of the last interglacial sea level at around 5 m above modern sea level as predicted by various geophysical models.
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