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Steven J. Phipps, Helen V. McGregor, Joëlle Gergis, Ailie J. E. Gallant, Raphael Neukom, Samantha Stevenson, Duncan Ackerley, Josephine R. Brown, Matt J. Fischer, and Tas D. van Ommen

model, Brown et al. (2006) therefore use the following relationship: Most climate models, including the one employed in this study, cannot use this approach as they do not include any representation of 18 O. The pseudocoral approach therefore approximates the δ 18 O signal that would be generated by a climate model if isotopes were included. This has been accomplished previously by relating coral δ 18 O to local sea surface temperature and salinity ( Thompson et al. 2011 ) or by relating the

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