Hönisch, BärbelAllen, Katherine A.Lea, David WSpero, HowardEggins, StephenArbuszewski, JenniferdeMenocal, P.B.Rosenthal, YRussell, AnnElderfield, H2015-12-131872-9533http://hdl.handle.net/1885/74153The Mg/Ca ratio in foraminiferal calcite is one of the principal proxies used for paleoceanographic temperature reconstructions, but recent core-top sediment observations suggest that salinity may exert a significant secondary control on planktic foraminiKeywords: calcite; calcium; dissolution; habitat selection; magnesium; oxygen isotope; paleosalinity; planktonic foraminifera; reconstruction; sediment core; temperature effect; Foraminifera; Globigerinoides ruber; Globigerinoides sacculifer; Orbulina universaThe influence of salinity on Mg/Ca in planktic foraminifers - Evidence from cultures, core-top sediments and complementary δ 18 O201310.1016/j.gca.2013.07.0282016-02-24