“…corals (Swart, 1983;Watanabe et al, 2011), coralline algae (Halfar et al, 2008;Williams et al, 2011), land snails (Goodfriend and Ellis, 2002;Yanes et al, 2011), freshwater snails (Abell and Hoelzmann, 2000;Stevens et al, 2012), freshwater bivalves (Kaandorp et al, 2003;Versteegh et al, 2010bVersteegh et al, , 2011 and marine bivalves (Jones and Quitmyer, 1996;Santos et al, 2012;Schöne et al, 2005). The oxygen isotope composition (δ 18 O values) of marine bivalves is often used as a proxy for temperature (Carré et al, 2005;Wanamaker et al, 2011). It can, however, also be applied to reconstruct water δ 18 O (δ 18 O w ) values (Freitas et al, 2012;Khim, 2002), which usually directly relate with salinity (Ingram et al, 1996).…”