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J. Black Sea/Mediterranean Environment
              Special Issue: 78-83 (2015)

              Late Pleistocene-Holocene climate transition in the
              western Mediterranean: a view from the stable isotopes of
              land snail shells

                                   1*
              André Carlo Colonese , Giovanni Zanchetta 2,3,4 ,
                                                 6
                                5
              Anthony E. Fallick , Russell Drysdale

              1  BioArCh, Department of Archaeology, University of York, Biology S. Block,
              York YO10 5DD, UK
              2  Dipartimento di Scienze della Terra, University of Pisa, Via S. Maria, 53,
              56126 Pisa, ITALY
              3  IGG-CNR Via Moruzzi, 1 56100 Pisa, ITALY
              4  INGV sez. Pisa, Via della Faggiola 32, 56126 Pisa, ITALY
              5  Scottish Universities Environmental Research Centre, East Kilbride G75 0QF,
              Glasgow, SCOTLAND
              6  Department of Resource Management and Geography, University of Melbourne,
              Victoria 3010, AUSTRALIA

              * Corresponding author: andre.colonese@york.ac.uk

              Abstract

              Late Pleistocene and Holocene archaeological deposits from the central Mediterranean
              regions contain abundant terrestrial gastropod shell remains. Stable isotope studies of
              their shell carbonate are valuable proxies for various aspects of climate and
              environmental change such as temperature, hydrological sources and balance, as well as
              vegetation. Here we present stable carbon and oxygen isotope data of snail shells from
              several archaeological deposits in the western Mediterranean (Iberian, Italian Peninsula
              and Sicily). Isotope ratios differ remarkably between the Late Pleistocene, Holocene and
              modern shells. The results can  be interpreted in terms of hydrological variations and
              changes in vegetation over time. Fossil shells offer the opportunity to examine the effects
              of past climate change on local and regional environments.

              Keywords:  Western Mediterranean, archaeological record,  land snail shells, stable
              isotopes, palaeoclimate, palaeoenvironment

              Introduction

              Late Pleistocene - Holocene archaeological deposits around the Mediterranean
              have  preserved  numerous  shells of  land  snails  and  offer  the  exceptional
              opportunity to explore shell isotopic response to late Quaternary climate change.
              Land snails are sensitive to environmental conditions and the stable isotopes
              (oxygen and carbon) composition of their shells are  valuable sources for






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