DEPTH, sediment/rock = CCSF-A, from Wilkens et al., 2013.AGE = using Hodell and Venz-Curtis, 2006 and Hodell et al., 2001 age models.d13C and d18O non-equilibruim in per mil, values are reported against VPDB, but not corrected to equilibrium.The associated sample variability (1Sigma) based on repeat analyses of the same sample is 0.08 per mil for d13C and 0.07 per mil for d18O for samples run at ICL (italic 1), and is 0.02 per mil for d13C and 0.07 per mil for d18O for samples run at UCL (italic 2).d18O equilibrium in per mil, the data from d18O non-equilibrium that has been corrected to equilibrium by the addition of 0.64 per mil (Shackleton et al., 1995b).d18O - WMA equilibrium in per mil, a 5 point weighted moving average (1st and 5th point = 30%; 2nd and 4th point = 70%; 3rd point = 100%) of the data from d18O - equilibrium.Oxygen and carbon isotope ratios (d18O; d13C) were analyzed on 3-6 translucent specimen of the epifaunal benthic foraminifera Cibicidoides mundulus (C. mundulus).All results are reported against Vienna Peedee Belemnite (VPDB) using the standard d notation (per mille).Analytical precision (1Sigma; replicated NBS-19 and ICL's Carrera Marble (ICM)) is 0.04 per mil for d13C and 0.07 per mil for d18O for ICL, and 0.02 per mil for d13C and 0.09 per mil for d18O for UCL.