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List of results

• 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).)
• 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))
• 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))
• 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)
• ODP664.Raymo.1997.paleo1measurement2  + (From Lisiecki and Raymo 2005)
• DSDP502.deMenocal.1992.paleo1measurement1  + (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)
• PYTXBEWD6RF.mgcass sst  + (G. ruber sensu stricto, 250-350 size fraction)
• Ocn-MD98-2177.Newton.2010  + (In original online data source, Newton et …
  In original online data source, Newton et al only provide Mg/Ca ratios, so these had to be converted to Mg/Ca SST using equations in paper. Also, no age-depth model was provided, though 14C date information was, so a direct point-to-point linear interpolation age model was generated. All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement.
  published in Nature Geoscience supplement.)
• GeoB7702-3  + (Incl. core catcher sample)
• MD95-2043.Cacho.1999.chron1measurement2  + (Isotopic tie points)
• Juxtlahuaca.Lachniet.2013.Chron1.measurementTable2  + (JX-10)
• Juxtlahuaca.Lachniet.2013.Paleo1.measurementTable1  + (JX-10)
• Juxtlahuaca.Lachniet.2013.Chron1.measurementTable1  + (JX-2)
• Juxtlahuaca.Lachniet.2013.Paleo1.measurementTable2  + (JX-2)
• Juxtlahuaca.Lachniet.2012.Chron1.measurementTable1  + (JX-6)
• Juxtlahuaca.Lachniet.2012.Paleo1.measurementTable1  + (JX-6)
• Juxtlahuaca.Lachniet.2017.Chron1.measurementTable1  + (JX-7)
• Juxtlahuaca.Lachniet.2017.Paleo1.measurementTable1  + (JX-7)
• LPD2a3997a7.temperature.Calibration  + (KIM2008: SST (¡C)= (0.0125*TEX86)+0.3038, (Kim et al., (2008), error ±2.2¡C))
• O2kLR 165.temperature.Calibration  + (KIM2010: SST=(68.4*TEX86H)+38.6)
• O2kLR 166.temperature.Calibration  + (KIM2010: SST=(68.4*TEX86H)+38.6)
• PYTDEIE3KHK.ghostMeasured.Calibration  + (KIM2010: SST=(68.4*TEX86H)+38.6)
• O2kLR 165.temperature  + (KIM2010: SST=(68.4*TEX86H)+38.6; paleoData_units changed - was originally deg C; climateInterpretation_seasonality changed - was originally Annual)
• PYTOQEOF9ML.core sample  + (LMG98-2 = Laurence M Gould cruise 1998-02, PD92 = Polar Duke cruise 1992-02, ODP = Ocean Drilling Program leg 178 Site 1098 (A,B,C) (Joides Resolution))
• PYTPBECVZ1M.sample code  + (LSCE (Gif-sur-Yvette))