2005
DOI: 10.1016/j.palaeo.2005.03.045
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Stable isotopes and sclerochronology of the bivalve Mesodesma donacium: Potential application to Peruvian paleoceanographic reconstructions

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Cited by 119 publications
(89 citation statements)
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“…Many calcitic bivalve species precipitate their shells in oxygen isotopic equilibrium with the ambient water (Chauvaud et al, 2005;Freitas et al, 2012;Hickson et al, 1999) In both equations T is the temperature in K and α is the isotope fractionation factor: (Freitas et al, 2006;Goewert et al, 2007;Versteegh et al, 2010a).…”
Section: Calculation Of Predicted δ 18 O C Valuesmentioning
confidence: 99%
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“…Many calcitic bivalve species precipitate their shells in oxygen isotopic equilibrium with the ambient water (Chauvaud et al, 2005;Freitas et al, 2012;Hickson et al, 1999) In both equations T is the temperature in K and α is the isotope fractionation factor: (Freitas et al, 2006;Goewert et al, 2007;Versteegh et al, 2010a).…”
Section: Calculation Of Predicted δ 18 O C Valuesmentioning
confidence: 99%
“…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).…”
Section: Introductionmentioning
confidence: 99%
“…This is particularly advantageous for studying short-term climate variability (e.g. interdecadal phenomena such as El Niň o Southern Oscillation (ENSO); Carré et al 2005aCarré et al , 2005b and for filling in the gaps often left by other commonly used proxies such as diatoms, ostracods and foraminifera that can be biased towards an average of a particular season over decades. Furthermore, this level of detail is essential when trying to assess cultural-climatic links in the past, as changing seasonal conditions can be extremely detrimental to societies, often leading to long-term climate stress and in extreme cases abandonment of settlements, migration or societal collapse (e.g.…”
Section: Notation and Standardisationmentioning
confidence: 99%
“…Intra-shell variations are thought to record past seawater salinity and/or temperature (e.g. Kennett and Voorhies 1996;Klein et al 1997;Aguire et al 1998;Carré et al 2005aCarré et al , 2005bMannino et al 2008;Stephens et al 2008;Patterson et al 2010;Azzoug et al 2012), with some studies using modern environmentshell δ…”
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