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List of results

• O2kLR 166.temperature  + (All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement; climateInterpretation_seasonality changed - was originally Annual)
• O2kLR 185.core  + (All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement; composite core depths [raw depth in core = 254 cm]; see table 1 at http://dx.doi.org/10.1016/j.quaint.2012.09.006)
• O2kLR 184.temperature  + (All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement; composite core depths [raw depth in core = 254 cm]; see table 1 at http://dx.doi.org/10.1016/j.quaint.2012.09.006)
• Ocn-WesternAntarcticPeninsula.Shevenell.2011  + (All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement; see "Data (QC) tab" cell C6 for details)
• Ocn-JacafFjord.Sepúlveda.2009  + (All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement; see "Data (QC) tab" cell C6 for details)
• O2kLR 076.temperature  + (All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement; see "Data (QC) tab" cell C6 for details; climateInterpretation_seasonality changed - was originally Annual)
• Ocn-FiskBasin.Richey.2009  + (All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement; see "Data (QC) tab" cell C6 for details)
• O2kLR 019.temperature  + (All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement; see "Data (QC) tab" cell C6 for details; climateInterpretation_seasonality changed - was originally Annual)
• O2kLR 197.temperature  + (All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement;Êsee "Data (QC) tab" cell C6 for details; climateInterpretation_seasonality changed - was originally Annual)
• Africa 004.temperature.Calibration  + (Analytical error on the basis of duplicate measurements (and corrected for n=2) was ±0,1°C. This error is compounded with the leave-one-out calibration error 0,4°C to give a total 95% error of ±0,4°C.)
• Africa 004.temperature  + (Analytical error on the basis of duplicate measurements (and corrected for n=2) was ±0,1°C. This error is compounded with the leave-one-out calibration error 0,4°C to give a total 95% error of ±0,4°C.)
• PYTF5GXE39R.d18oc.mund  + (Average duplicates from paleo1measurementTable1)
• PYT73UN1SLP.d18og.rub-w  + (Average duplicates from paleo1measurementTable1)
• PYT6K1XJRVM.mg/ca-g.rub-w  + (Average duplicates from paleo1measurementTable1)
• LPDe51d17e8.temperature.Calibration  + (BLA2007: Cariaco-specific G. bulloides calibration, calibrated in TIME)
• O2kLR 019.temperature.Calibration  + (BLA2007: Mg/Ca=0.048*exp(0.173*SST), (Black et al., (2007); G. bulloides))
• PYTFEWXXRKD.d18oforams-b  + (Benthic Foraminifers)
• PYT8B98NYOV.d13cforams-b  + (Benthic Foraminifers)
• ODP1019.Barron.2003.chron0measurement1  + (Benthic data)
• GIK23258.Sarnthein.2003.chron0measurement0  + (C14 dates and other age control points in sediment core 23258/2 and /3.)
• PYTH3UK1UX7.ghostMeasured.Calibration  + (CLE2008: Cleroux et al., 2008 North Atlantic core top calibration for G. ruber (white))
• O2kLR 101.temperature.Calibration  + (CLE2008: Cleroux et al., 2008 North Atlantic core top calibration for G. ruber (white))
• O2kLR 101.temperature  + (CLE2008: Cleroux et al., 2008 North Atlantic core top calibration for G. ruber (white); paleoData_units changed - was originally deg C; climateInterpretation_seasonality changed - was originally JJA)
• PYTIH6SLQQG.d18oa  + (Calculated from Mg/Ca ratios and d18O and corrected for ice volume)
• PYTRD2CBJAC.calibrated age intercept.Calibration  + (Calibrated ages are calculated using the program CALIB v4.2 with a marine calibration dataset and a 30-year moving average to account for the likely age span of foraminifera from a 1-cm thick sample)
• MD97-2121.Marr.2013.chron1measurement1  + (Chronology information from Carter et al. 2008)

• Aus 015.trsgi  + (Composite of Blue Tier, Ralphs Falls and Ben Ridge Rd)
• Aus 015.trsgi.Calibration  + (Composite of Blue Tier, Ralphs Falls and Ben Ridge Rd)

• Aus 020.trsgi.Calibration  + (Composite of WEY, RCS and MUR and LaMarches Pieman site)
• Aus 020.trsgi  + (Composite of WEY, RCS and MUR and LaMarches Pieman site; climateInterpretation_seasonality changed - was originally 12 1 2 3 4 5)
• Palmyra.Cobb.2013.paleo0measurement0  + (Contains Monthly data)
• LPD9cc3baf6.temperature.Calibration  + (DEK2002: G. ruber core top calibration with a depth correction to account for dissolution effects)
• LPD30c5b95c.temperature.Calibration  + (DEK2002: Mg/Ca=0.38*exp(0.09*[SST-0.61 (core depth km)]), (Dekens et al., (2002); core tops; G ruber))
• LPD7e8e8eaa.temperature.Calibration  + (DEK2002: Mg/Ca=0.38*exp(0.09*[SST-0.61 (core depth km)]), (Dekens et al., (2002); core tops; G ruber))
• O2kLR 118.temperature.Calibration  + (DEK2002: Mg/Ca=0.38*exp(0.09*[SST-0.61 (core depth km)]), (Dekens et al., (2002); core tops; G ruber))
• O2kLR 120.temperature.Calibration  + (DEK2002: Mg/Ca=0.38*exp(0.09*[SST-0.61 (core depth km)]), (Dekens et al., (2002); core tops; G ruber))
• PYT80EV07EP.ghostMeasured.Calibration  + (DEK2002: Mg/Ca=0.38*exp(0.09*[SST-0.61 (core depth km)]), (Dekens et al., (2002); core tops; G ruber))
• PYTJH1XIT33.ghostMeasured.Calibration  + (DEK2002: Mg/Ca=0.38*exp(0.09*[SST-0.61 (core depth km)]), (Dekens et al., (2002); core tops; G ruber))
• PYTKD15BWU0.ghostMeasured.Calibration  + (DEK2002: Mg/Ca=0.38*exp(0.09*[SST-0.61 (core depth km)]), (Dekens et al., (2002); core tops; G ruber))
• O2kLR 118.temperature  + (DEK2002: Mg/Ca=0.38*exp(0.09*[SST-0.61 (core depth km)]), (Dekens et al., (2002); core tops; G ruber); paleoData_units changed - was originally deg C; climateInterpretation_seasonality changed - was originally annual)
• LPDcda1c277.temperature.Calibration  + (DEK2002: coretop G. ruber (white) calibration without the depth correction)
• Palmyra.Cobb.2013.paleo0measurement1  + (Data averaged as tropical year (March-April))
• ODP976.Jimenez-Amat.2015.chron1measurement1  + (Data from Combourieu-Nebout (2002))
• M77-2 056-5.Nurnberg.2015.chron1measurement1  + (Data from Molliet et al.)
• SK168-GC1.Gebregiorgis.2016.chron1measurement1  + (Dates from Sijinkumar et al. (2010))
• GeoB12605-3.Kuhnert.2014.chron1measurement1  + (DeltaR = 150 ± 60 years)
• PYTJC0FFJPQ.dbd  + (Depth is a result from correlations between holes A, B and C (see Depth, composite).)
• PYTBMGCSUBM.dust  + (Depth is a result from correlations betwee …
  Depth is a result from correlations between holes A, B and C (see Depth, composite). The noncarbonate fraction (100% minus %CaCO3) is considered to be purely eaolian, because the concentrations of biogenic opal (<2%), organic carbon (<0.5%), and volcanic glass are negligible and fluvial sediment supply and turbidites cannot reach this position (Tiedemann et al., 1989)
  not reach this position (Tiedemann et al., 1989))
• PYTTA8QZBTE.acc rate dust  + (Depth is a result from correlations betwee …
  Depth is a result from correlations between holes A, B and C (see Depth, composite). The noncarbonate fraction (100% minus %CaCO3) is considered to be purely eaolian, because the concentrations of biogenic opal (<2%), organic carbon (<0.5%), and volcanic glass are negligible and fluvial sediment supply and turbidites cannot reach this position (Tiedemann et al., 1989)
  not reach this position (Tiedemann et al., 1989))
• PYT7CASPXK6.c. wuellerstorfi d18o  + (Depth is a result from correlations between holes A, B and C (see Depth, composite). To adjust the d18O values of C. wuell. to seawater equilibrium, 0.64 per mil have to be added (Shackleton & Hall, 1984. The data set includes data from Schulz, 1988.)
• PYTW0D8MOY6.d18og.rub.Uncertainty1  + (Determined by replicate analyses of NBS-19 and laboratory standards (PTB-1))
• PYT3L6BW4OB.d18og.Uncertainty1  + (Determined by replicate analyses of NIST-19 and a Carrera marble laboratory standard)