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List of results

• 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.Calibration  + (Composite of Blue Tier, Ralphs Falls and Ben Ridge Rd)
• Aus 015.trsgi  + (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)
• 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))
• 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))
• 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))
• 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))
• 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))
• 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))
• 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))
• 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)
• PYTEM6NA7PQ.g. ruber d18o.Uncertainty1  + (Determined by running duplicates on 18 out of a total of 140 samples)
• ODP1019.Barron.2003.paleo0measurement3  + (Diatom Assemblages)
• MD982181.Khider.2014.chron1model1ensemble  + (Ensemble age for SST)
• PYTVVKA7U87.δ18osw  + (Ensemble and summary tables do not take into account horizons with NaN values)
• PYTES973TGM.sst  + (Ensemble and summary tables ignore NaN values)
• Chron1.depthUTh  + (Essential)
• PYTBBK5OX43.d13 cpdb per mil  + (Estimated d13C)
• GIK17940-2.Pelejero.1999.chron1measurement1  + (Fom Wang et al. 1999)
• ODP1098B.Shevenell.2011.chron1measurement1  + (From Domack et al. 2011)
• MD95-2015.Marchal.2002.chron1measurement1  + (From Giraudeau et al. 2000)
• DSDP502.deMenocal.1992.paleo1measurement1  + (From Lisiecki and Raymo 2005)
• ODP664.Raymo.1997.paleo1measurement2  + (From Lisiecki and Raymo 2005)
• GIK16160-3.Wang.2003.chron1measurement1  + (From Wang et al. (2013))
• PYTIQTPJ37O.mg/ca  + (G. ruber (pink))
• PYTUTE5IVBM.d18og  + (G. ruber (pink))
• PYTXGCXHYIV.ba/ca  + (G. ruber (pink))
• PYTJNLD539P.d18osl  + (G. ruber sensu lato, 250-350 size fraction)
• PYTZ77JHCM1.mgcasl sst  + (G. ruber sensu lato, 250-350 size fraction)
• PYTHETAMMNY.d18oss  + (G. ruber sensu stricto, 250-350 size fraction)