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List of results
- 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).)
- 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)
- 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)
- 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)