Journal article

Coeval dry events in the central and eastern Mediterranean basin at 5.2 and 5.6ka recorded in Corchia (Italy) and Soreq caves (Israel) speleothems

G Zanchetta, M Bar-Matthews, RN Drysdale, P Lionello, A Ayalon, JC Hellstrom, I Isola, E Regattieri

Global and Planetary Change | Published : 2014

Abstract

Soreq (Israel) and Corchia (central Italy) Caves are located 2500km far apart along the Mediterranean winter-storm track and are ideally suited for investigating past variations of winter rainfall in the Mediterranean region. Analyses of speleothem δ18O records from both caves for the period between ca. 7 to 4 ka BP show some striking similarities for the ca. 6 and 4ka interval, but lack agreement between ca. 7 to 6kaBP. Two prominent isotopic excursions, argued to reflect relatively drier conditions, are centred at ca. 5.6 and ca. 5.2 ka. The 5.2 ka event lasts less than a century, whereas the 5.6ka event extends from ca. 5.7 to 5.4 ka. A period of progressive drying is also apparent from c..

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University of Melbourne Researchers

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Funding Acknowledgements

We thank C. Spotl, D. Fleitmann and M. Magny for the data for Spannagel Cave, Solufar Cave and Lake Accesa. We thank two referees for the constructive comments and suggestion, which greatly improved the quality of the manuscript. For Corchia Cave, the authors are indebted to the Federezione Speleologica Toscana for the logistical and economical support during the first years of the research.