Gagan, MichaelDunbar, GavinSuzuki, Atsushi2015-12-100883-8305http://hdl.handle.net/1885/52664Paleotemperature estimates based on coral Sr/Ca have not been widely accepted because the reconstructed glacial-Holocene shift in tropical sea-surface temperature (∼4-6C) is larger than that indicated by foraminiferal Mg/Ca (∼2-4C). We show that coralKeywords: aragonite; biogenic deposit; calcium; calibration; coral; experimental study; foraminifera; glaciation; growth rate; Holocene; magnesium; oxygen isotope; paleoceanography; paleotemperature; reconstruction; sea surface temperature; skeleton; strontium; tra201210.1029/2011PA0022152016-02-24