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List of results

• Arc 101.uncertainty temperature  + (Regional tree-ring network; paleoData_variableName changed - was originally uncertainty_temperature; paleoData_variableName changed - was originally uncertainty_temperature; paleoData_variableName changed - was originally uncertainty_temperature)
• PYTN8GRCHGY.sst.Uncertainty1  + (Reproducibility_checked_on_duplicates_of_18_out_of_140_samples)
• GeoB10042-1.Setiawan.2016.chron1measurement1  + (Reservoir Age correction of 100 years)
• KNR195-5-CDH26.Bova.2015.chron1measurement1  + (Reservoir Age: 500 yrs)
• A7.Sun.2005.chron1measurement1  + (Reservoir Age: 700 years)
• MD01-2412.Harada.2006.chron1measurement1  + (Reservoir Age: 784yr)
• PYTFH8INQ03.calendar age  + (Reservoir age correction 200 ±50 years)
• GeoB1023-5.Kim.2002.chron1measurement1  + (Reservoir age correction of 125+/-20 years)
• GeoB12610-2.Rippert.2015.chron1measurement1  + (Reservoir age of 150 years (+/- 60 years))
• PYTLE0KGBBD.yrbp.Calibration  + (Reservoir age of 600 years)
• KNR195-5-CDH23.Bova.2015.chron1measurement1  + (Reservoir age: 500 years)
• GIK17748-2.Kim.2002.chron1measurement1  + (Reservoir effect: 400 years)
• PYTDK4DZ147.ghostMeasured.Calibration  + (SON1997: T(sediments) = (Uk37-0.316)/(0.023))
• O2kLR 116.temperature.Calibration  + (SON1997: T(sediments) = (Uk37-0.316)/(0.023))
• O2kLR 114.temperature.Calibration  + (SON1997: T(sediments) = (Uk37-0.316)/(0.023))
• O2kLR 114.temperature  + (SON1997: T(sediments) = (Uk37-0.316)/(0.023); paleoData_units changed - was originally deg C; climateInterpretation_seasonality changed - was originally Annual)
• O2kLR 189.temperature  + (SST data from author not placed on age-dep …
  SST data from author not placed on age-depth scale, so I had to generate a control point-to-point linear interpolation using authors reported age control. All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement; climateInterpretation_seasonality changed - was originally Annual
  easonality changed - was originally Annual)
• MD982181.Khider.2014.paleo1model1ensemble  + (SST ensemble from the Bayesian calibration described in Khider et al. 2014)
• LV29-114-3.Max.2012.paleo1measurement1  + (Sea surface temperature calculated from alkenones)
• GIK16160-3.Wang.2003.paleo1measurement2  + (Sea surface temperatures reconstructed from Mg/Ca ratios in sediment core GIK16160-3)
• ODP1019.Barron.2003.paleo0measurement2  + (Sediment composition)
• KT05-7 PC02.Kawahata.2009.paleo1measurement3  + (Stable carbon isotope ratios of benthic foraminifera from sediment core KT05-7_PC-02)
• ODP1098B.Shevenell.2011.paleo1measurement1  + (Stable oxygen isotope ratios of Neogloboquadrina pachyderma and sea surface temperature reconstruction for ODP Hole 178-1098B.)
• MD982181.Khider.2014.paleo1model1summary  + (Summary of the SST ensembleTable)
• MD982181.Khider.2014.chron1model1summary  + (Summary of the age model ensemble for SST)

• MD982181.Khider.2014.chron1model2summary  + (Summary of the age model ensemble for d18Osw)

• MD982181.Khider.2014.paleo1model2summary  + (Summary of the d18Osw ensembleTable)
• LPDb17a5e9e.temperature.Calibration  + (TH2009: for G. bulloides, based on core tops. Thornalley et al. assume an exponential constant of 0.10 using Barker et al., 2005, Quat Sci Rev as a justification, then fit the pre-exponential constant using regional core top data.)
• MD972120-MD972121.Pahnke.2006.chron0measurement0  + (Tephra ages in radiocarbon and calendar years)
• MD972120-MD972121.Pahnke.2006.chron1measurement0  + (Tephra ages in radiocarbon and calendar years)
• PYTOMLKRPB1.age calyrbp  + (The ensemble and summary tables were adjusted to take into consideration NaNs in the SST and d18Osw data)
• PYT6K1XJRVM.mg/ca-g.rub-w.Uncertainty1  + (The precision is determined on replicate measurements of G. ruber samples)
• Aus-DuckholeLake.Saunders.2013  + (The relationship between total chlorin and …
  The relationship between total chlorin and temperature is NEGATIVE. Note that figure 4 in the study by Saunders et al (2013) is incorrectly labelled. The y axes for R_650;700 should be inverted and the correlation is negative (not positive as originally published). An erratum is in preparation.
  published). An erratum is in preparation.)
• MD02-2575.Ziegler.2008.chron1measurement1  + (Tie points to LR04 curve. From Nurnberg et al. 2008)
• SAm 033.uncertainty temperature  + (Upper 95% confidence Interval values; pale …
  Upper 95% confidence Interval values; paleoData_variableName changed - was originally temperatureRangeHigh; paleoData_units changed - was originally (degrees C); climateInterpretation_seasonality changed - was originally SONDJF; paleoData_variableName changed - was originally uncertainty_temperature; paleoData_variableName changed - was originally uncertainty_temperature
  d - was originally uncertainty_temperature)
• O2kLR 009.temperature  + (Used the SIMMAX data due to poorer sensiti …
  Used the SIMMAX data due to poorer sensitivity of the Mg/Ca data as reported in their paper; 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 JAS; climateInterpretation_seasonality changed - was originally 7/8/2009; climateInterpretation_seasonality changed - was originally 7 8 2009
  sonality changed - was originally 7 8 2009)
• O2kLR 082.temperature.Calibration  + (Warm and cold season SST estimates were ca …
  Warm and cold season SST estimates were calculated from the census count data using the F139 transfer function derived from faunal analysis of 191 Atlantic core tops (15, 16). Standard errors of estimate for the F139- derived warm and cold season SSTs are 1.6 and 1.3C, respectively.
  eason SSTs are 1.6 and 1.3C, respectively.)
• PYTZ4D87ZS2.ghostMeasured.Calibration  + (Warm and cold season SST estimates were ca …
  Warm and cold season SST estimates were calculated from the census count data using the F139 transfer function derived from faunal analysis of 191 Atlantic core tops (15, 16). Standard errors of estimate for the F139- derived warm and cold season SSTs are 1.6 and 1.3C, respectively.
  eason SSTs are 1.6 and 1.3C, respectively.)
• O2kLR 084.temperature.Calibration  + (Warm and cold season SST estimates were ca …
  Warm and cold season SST estimates were calculated from the census count data using the F139 transfer function derived from faunal analysis of 191 Atlantic core tops (15, 16). Standard errors of estimate for the F139- derived warm and cold season SSTs are 1.6° and 1.3°C, respectively.
  son SSTs are 1.6° and 1.3°C, respectively.)
• LV29-114-3.Max.2012.paleo1measurement3  + (X-Ray Fluoresence)
• MD95-2105  + (XXIII Sections, OK)
• MD95-2043  + (XXV Sections, OK; liner exploded in section VIII)
• PYTO6QLOKWD.benthic d18o  + (adjusted for equiibrium offsets)
• MD982181.Khider.2014.chron1model3ensemble  + (age ensemble for benthic d18Oc - 1000+/-300 yr offset from planktonic age model)
• MD982181.Khider.2014.chron1model3summary  + (age ensemble for benthic d18Oc - 1000+/-300 yr offset from planktonic age model)
• PYTXZLB1X8P.age  + (asdf)
• PYTOYBFQ376.d18o  + (asdfa)
• PYT7Z7JMLKT.mg  + (asdfad)
• PYTQ4SI5RNB.14c  + (asdfasa)
• PYT9RQ8O0TX.labcode  + (asdfasd)
• PYTWCPO4MJI.ukprime37.Uncertainty1  + (based on 22 replicate extractions on di¡er- ent days of two laboratory internal reference sediments (CC 2107-3 and CC 1706-2) from the South Atlantic)