{
  "paleoData": [
    {
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        {
          "googleWorkSheetKey": "owvplz0",
          "tableName": "paleo1measurement1",
          "missingValue": "NaN",
          "d18O": {
            "archiveGenus": "Porites",
            "archiveSpecies": "NaN",
            "chronologyIntegrationTime": "43467",
            "chronologyIntegrationTimeBasis": "We use the pronounced seasonal cycle in d18O and Sr/Ca to develop the final chronology of the coral core and assigned the highest d18O and Sr/Ca values to august 15 of each year, which is on average the coldest month. [...] The d18O and Sr/Ca time series were interpolated linearly into 6 and 12 equi- distant points for any given year between these anchor points using the Analyseries software,.083 to 0.167 yrs,chronological,months,on a seasonal scale coral d18O  and Sr/Ca at this location primarily reflects SST variability (Fig. 5; Table 1). \"",
            "chronologyIntegrationTimeUncertaintyType": "decrease",
            "description": "carbonate",
            "hasChron": "0",
            "hasMaxValue": -3.41,
            "hasMeanValue": -4.4255,
            "hasMedianValue": -4.42,
            "hasMinValue": -5.43,
            "hasPaleoDepth": "0",
            "hasTimeTsid": "MAT4c306207d3",
            "inCompilation": "Ocean2k_v1.0.0 | PAGES2k_v1.12.0",
            "inferredMaterial": "surface seawater",
            "inferredMaterialGroup": "surface water",
            "inferredMaterialGroupOriginal": "surface seawater",
            "instrument": "Finnigan MAT 252 with a Kiel carbonate device",
            "iso2kCertification": "DMT (1/14/19)",
            "iso2kPrimaryTimeseries": "TRUE",
            "iso2kUI": "CO04ZIMG01A",
            "isPrimary": false,
            "longName": "AD",
            "measurementMaterial": "coral",
            "measurementMaterialDetail": "aragonite",
            "measurementStandard": "PDB",
            "measurementTableMD5": "ead69f0fa0dd0ca668a51893cbb936e2",
            "measurementTableName": "measurementTable1",
            "medianRes12k": "NA",
            "notes": "; climateInterpretation_seasonality changed - was originally monthly; archiveType changed - was originally Coral (CO)",
            "ocean2kID": "IndianIfatyTulearZinke2014if4",
            "pages2kId": "Ocn_075",
            "pages2kID": "Ocn_075",
            "paleoDataMD5": "636d325be5cf6febd96b8f551072eaae",
            "paleoDataTableName": "pt1_1",
            "paleoMeasurementTableMD5": "ead69f0fa0dd0ca668a51893cbb936e2",
            "primaryAgeColumn": false,
            "proxy": "d18O",
            "proxyLumps": "isotope",
            "proxyLumpsOriginal": "d18O",
            "QCCertification": "DMT (1/14/19)",
            "TSid": "Ocean2kHR_020_iso2k",
            "uncertaintyAnalytical": "0.07permil (1sigma)",
            "units": "permil",
            "useInGlobalTemperatureAnalysis": "TRUE",
            "variableName": "d18O",
            "variableType": "measured",
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                "direction": "decrease/increase",
                "interpDirection": "decrease/increase",
                "scope": "climate",
                "seasonality": "subannual",
                "variable": "temperature",
                "variableDetail": "sea surface",
                "variableGroup": "temperature and salinity",
                "basis": null,
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                "basis": null,
                "direction": null,
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                "basis": "A correlation of seasonal mean rainfall anomalies derived from the NCEP/NCAR reanalysis data set (1948-1995; averaged over 3545E, 20-30S; http://www. cdc.noaa.gov/cdc/data.ncep.reanalysis.derived.html) with coral d18O shows a clear relationship during austral summer (NDJF) significant above the 90% level (Fig. 6). This also holds for a correlation with South African summer rainfall averaged over 25-30E and 15-25S (significant N95%) (Fig. 6). Thus, summer coral d18O is also related to changes in the regional hydrologic (P/E) balance",
                "coefficient": "NA",
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                "integrationTime": "2-Jan",
                "integrationTimeBasis": "We use the pronounced seasonal cycle in d18O and Sr/Ca to develop the final chronology of the coral core and assigned the highest d18O and Sr/Ca values to august 15 of each year, which is on average the coldest month. [...] The d18O and Sr/Ca time series were interpolated linearly into 6 and 12 equi- distant points for any given year between these anchor points using the Analyseries software,.083 to 0.167 yrs,chronological,months,on a seasonal scale coral d18O  and Sr/Ca at this location primarily reflects SST variability (Fig. 5; Table 1). \"",
                "integrationTimeUncertaintyType": "decrease",
                "mathematicalRelation": "linear",
                "rank": 1,
                "scope": "isotope",
                "seasonality": "subannual",
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                "inferredMaterial": "seawater",
                "integrationTime": "2-Jan",
                "integrationTimeBasis": "We use the pronounced seasonal cycle in d18O and Sr/Ca to develop the final chronology of the coral core and assigned the highest d18O and Sr/Ca values to august 15 of each year, which is on average the coldest month. [...] The d18O and Sr/Ca time series were interpolated linearly into 6 and 12 equi- distant points for any given year between these anchor points using the Analyseries software|.083 to 0.167 yrs|chronological|months|on a seasonal scale coral d18O  and Sr/Ca at this location primarily reflects SST variability (Fig. 5; Table 1). \"",
                "integrationTimeUncertaintyType": "decrease",
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                "scope": "isotope",
                "seasonality": null,
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              },
              {
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                "fraction": "NA",
                "inferredMaterial": "seawater",
                "integrationTime": "2-Jan",
                "integrationTimeBasis": "We use the pronounced seasonal cycle in d18O and Sr/Ca to develop the final chronology of the coral core and assigned the highest d18O and Sr/Ca values to august 15 of each year, which is on average the coldest month. [...] The d18O and Sr/Ca time series were interpolated linearly into 6 and 12 equi- distant points for any given year between these anchor points using the Analyseries software|.083 to 0.167 yrs|chronological|months|on a seasonal scale coral d18O  and Sr/Ca at this location primarily reflects SST variability (Fig. 5; Table 1). \"",
                "integrationTimeUncertaintyType": "decrease",
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                "rank": "NA",
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      "citation": "Zinke, J., Dullo, W.-C., Heiss, G. A. and Eisenhauer, A.: ENSO and Indian Ocean subtropical dipole variability is recorded in a coral record off southwest Madagascar for the period 1659 to 1995, Earth and Planetary Science Letters, 228(1-2), 177–194, doi:10.1016/j.epsl.2004.09.028, 2004.",
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      "pages": -17,
      "publisher": "Elsevier BV",
      "title": "ENSO and Indian Ocean subtropical dipole variability is recorded in a coral record off southwest Madagascar for the period 1659 to 1995",
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    {
      "author": {
        "name": "Tierney, Jessica E. , Abram, Nerilie J. , Anchukaitis, Kevin J. , Evans, Michael N. , Giry, Cyril , Kilbourne, K. Halimeda , Saenger, Casey P. , Wu, Henry C. , Zinke, Jens"
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      "citeKey": "tierney2015tropical",
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      "institution": "World Data Center for Paleoclimatology",
      "title": "Ocean2kHR-IndianIfatyTulearZinke2014if4",
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      "url": "https://www.ncdc.noaa.gov/paleo/study/16438",
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