{ "paleoData": [ { "measurementTable": [ { "googleWorkSheetKey": "oezjde7", "tableName": "paleo1measurement1", "missingValue": "NaN", "d18O": { "chronologyIntegrationTime": "1", "chronologyIntegrationTimeBasis": "In South Florida, the dense band forms in the late summer, but it is generally thought that there is as much as a i¿½ two month variation in timing. By counting the number of bands in a coral, the age can be assessed. Errors in age interpretation arise when dense bands are indistinct or when so-called \"stress bands\", resulting from events such as temperature extremes, occur. Generally speaking, a year in which a stress band forms may actually contain two dense bands or a thicker dense band which is a combination of the stress and normal dense band. Although it is possible to misinterpret a stress band as an annual band, the annual bands can be recognized by their regular spacing. Therefore, density changes can still provide a clear annual chronology.", "chronologyIntegrationTimeUncertainty": "subannual samples averaged to annual for archived data", "chronologyIntegrationTimeUncertaintyType": "chronological", "chronologyIntegrationTimeUnits": "year", "description": "carbonate", "hasChron": "0", "hasMaxValue": "-1.64", "hasMeanValue": "-2.5917", "hasMedianValue": "-2.54", "hasMinValue": "-3.86", "hasPaleoDepth": "0", "inferredMaterial": "surface seawater", "inferredMaterialGroup": "surface water", "inferredMaterialGroupOriginal": "surface seawater", "instrument": "MAT 251 mass spectometer, reactions at 90 degrees C. All data have been corrected for the usual isobaric interferences.", "iso2kCertification": "DMT (1/14/19)", "iso2kPrimaryTimeseries": "TRUE", "iso2kUI": "CO96SWFB01A", "longName": "AD", "measurementMaterial": "coral", "measurementMaterialDetail": "aragonite", "measurementStandard": "PDB", "measurementTableMD5": "b66c531c8f4194891d8d0f6723e3f957", "measurementTableName": "measurementTable1", "medianRes12k": "NA", "notes": "; archiveType changed - was originally Coral (CO)", "paleoDataTableName": "pt1_1", "paleoMeasurementTableMD5": "48c2ba2fd581573d02422c0763662a4c", "QCCertification": "DMT (1/14/19)", "QCnotes": "This coral species is Solenastrea bournoni, one not used in coral climate reconstructions, and it is located in a complex system of Florida Bay where waters from the Everglades enter the ocean and ther eare high rates of evaporation. The d18O system is not additive but subtractive for SSS and SST. Swart 1999 revisited this coral colony and they collect a new core from the same colony. Hudson 1989 gives a map with the coral location, which is 24degrees 55 minutes, and ~80 degrees and between 40 and 50 minutes, about 44 minutes nu my eye. Swart 1999 NOAA has different corrdinates for this coral 25 0N, 80 36W, Looking at Google earth and Hudsons map, the Swart 1999 corrdinates incorrect, they should be 24 degrees 55 minutes N, and ~80 degrees, 43.5 minutes W", "TSid": "CO96SWFB01A", "units": "permil", "variableName": "d18O", "variableType": "measured", "isPrimary": false, "primaryAgeColumn": false, "hasTimeTsid": "MAT7d0bc1f777", "values": [-2.54, -2.49, -2.8, -3.2, -2.81, -2.6, -2.91, -2.58, -2.49, -2.4, -2.15, -2.02, -2.42, -2.2, -2.51, -2.33, -1.94, -2.91, -2.38, -2.54, -2.23, -2.3, -2.14, -1.98, -1.94, -2.48, -2.6, -2.47, -2.62, -2.6, -2.31, -2.34, -2.35, -2.69, -2.41, -2.47, -2.33, -2.36, -3.02, -2.58, -2.49, -2.21, -2.71, -2.5, -2.63, -2.3, -2.02, -2.39, -2.4, -2.55, -2.38, -2.1, -2.82, -2.47, -2.33, -2.13, -2.6, -2.46, -2.2, -2.3, -2.24, -2.23, -2.49, -2.12, -2.63, -2.68, -2.48, -2.37, -2.31, -2.3, -2.04, -2.22, -1.92, -2.11, -2.28, -2.19, -2.58, -3.1, -2.76, -2.45, -2.98, -2.5, -2.78, -2.77, -2.87, -3.86, -3.04, -3.73, -3, -2.71, -2.99, -3.21, -2.82, -3.22, -2.84, -2.53, -2.75, -1.84, -1.96, -2.29, -2.31, -2.49, -1.89, -1.64, -2.49, -2.47, -2.54, -2.24, -2.45, -2.38, -2.02, -2.67, -2.66, -2.95, -3.52, -3.39, -3.09, -3.02, -3.11, -2.73, -2.8, -2.66, -2.38, -2.69, -2.03, -2.44, -2.35, -2.31, -2.84, -3.46, -3.01, -3.24, -2.66, -2.54, -2.34, -2.71, -3.1, -3.33, -2.97, -3.21, -2.3, -2.81, -2.64, -2.69, -2.71, -2.73, -2.19, -1.96, -2.06, -2.92, -2.88, -2.81, -3.48, -3.25, -3.08, -3.07, -3.23, -2.74, -3.02, -3.13, -3.5, -2.91], "mostRecentCompilations": null, "primaryTimeseries": null, "proxy": null, "interpretation": [ { "basis": "Florida bay experiences more evaporation in the summer thus d18O is not additive, warm dry summers, cold wet winters.", "direction": "increase", "interpDirection": "increase", "scope": "climate", "variable": "salinity", "variableDetail": "sea surface", "variableGroup": "EffectiveMoisture", "variableGroupDirection": "negative", "variableGroupOriginal": "S", "variableOriginal": "Salinity", "dynamical": null, "seasonality": null }, { "scope": "climate", "basis": null, "direction": null, "seasonality": null, "variable": null, "variableDetail": null }, { "scope": "climate", "basis": null, "direction": null, "seasonality": null, "variable": null, "variableDetail": null }, { "basis": "The higher skeletal d18O value reflects the high d180 value of the Bay water itself (Lloyd, 1964; Swart et al., 1989), which is enriched in d18O as a result of evaporation and the input of 1so enriched freshwater from the Everglades (Meyers et al., 1993). Salinity values are the highest during the summer, as a result of evaporation, and lower during the winter when the Bay becomes dominated by water from the Gulf of Mexico and the Florida Reef Tract. These changes in salinity should be manifested in the 6180 of the coral, but as the maximum enrichment in the water occurs during the warmest portion of the year (the summer), the temperature and salinity effects tend to counteract each other, thereby reducing the observed range of oxygen isotopic variation seen in the coral.", "direction": "positive", "inferredMaterial": "seawater", "integrationTime": "1", "integrationTimeBasis": "In South Florida, the dense band forms in the late summer, but it is generally thought that there is as much as a � two month variation in timing. By counting the number of bands in a coral, the age can be assessed. Errors in age interpretation arise when dense bands are indistinct or when so-called \"stress bands\", resulting from events such as temperature extremes, occur. Generally speaking, a year in which a stress band forms may actually contain two dense bands or a thicker dense band which is a combination of the stress and normal dense band. Although it is possible to misinterpret a stress band as an annual band, the annual bands can be recognized by their regular spacing. Therefore, density changes can still provide a clear annual chronology.", "integrationTimeUncertainty": "subannual samples averaged to annual for archived data", "integrationTimeUncertaintyType": "chronological", "integrationTimeUnits": "year", "mathematicalRelation": "linear", "rank": 1, "scope": "isotope", "seasonality": "Annual", "seasonalityOriginal": "Annual", "variable": "seawaterIsotope", "variableGroup": "EffectiveMoisture", "variableGroupDirection": "negative", "variableGroupOriginal": "d18O_seawater", "coefficient": "NA", "fraction": "NA" }, { "basis": "Temperature is not significant (r= 0.08)", "fraction": 0, "inferredMaterial": "seawater", "integrationTime": "1", "integrationTimeBasis": "In South Florida, the dense band forms in the late summer, but it is generally thought that there is as much as a � two month variation in timing. By counting the number of bands in a coral, the age can be assessed. Errors in age interpretation arise when dense bands are indistinct or when so-called \"stress bands\", resulting from events such as temperature extremes, occur. Generally speaking, a year in which a stress band forms may actually contain two dense bands or a thicker dense band which is a combination of the stress and normal dense band. Although it is possible to misinterpret a stress band as an annual band, the annual bands can be recognized by their regular spacing. Therefore, density changes can still provide a clear annual chronology.", "integrationTimeUncertainty": "subannual samples averaged to annual for archived data", "integrationTimeUncertaintyType": "chronological", "integrationTimeUnits": "year", "rank": 2, "scope": "isotope", "variable": "temperature", "variableGroup": "Temperature", "variableGroupDirection": "negative", "variableGroupOriginal": "T_water", "coefficient": "NA", "direction": null, "seasonality": null }, { "scope": "isotope", "coefficient": "NA", "fraction": "NA", "rank": "NA", "direction": null, "seasonality": null, "variable": null } ], "hasResolution": { "hasMaxValue": 1, "hasMeanValue": 1, "hasMedianValue": 1, "hasMinValue": 1, "units": "AD" }, "inCompilationBeta": [ { "compilationName": "iso2k", "compilationVersion": ["0_14_8", "0_15_0", "1_0_0", "1_1_0", "1_1_1", "1_1_2"] } ] }, "year": { "dataType": "float", "description": "Year AD", "hasMaxValue": "1985", "hasMeanValue": "1904.5", "hasMedianValue": "1904.5", "hasMinValue": "1824", "inferredVariableType": "year", "iso2kPrimaryTimeseries": "FALSE", "longName": "AD", "measurementTableMD5": "b66c531c8f4194891d8d0f6723e3f957", "measurementTableName": "measurementTable1", "medianRes12k": "NA", "paleoDataTableName": "pt1_1", "paleoMeasurementTableMD5": "b66c531c8f4194891d8d0f6723e3f957", "TSid": "MAT7d0bc1f777", "units": "yr AD", "unitsOriginal": "CE", "variableName": "year", "variableType": "inferred", "isPrimary": true, "primaryAgeColumn": true, "hasTimeTsid": "MAT7d0bc1f777", "values": [1985, 1984, 1983, 1982, 1981, 1980, 1979, 1978, 1977, 1976, 1975, 1974, 1973, 1972, 1971, 1970, 1969, 1968, 1967, 1966, 1965, 1964, 1963, 1962, 1961, 1960, 1959, 1958, 1957, 1956, 1955, 1954, 1953, 1952, 1951, 1950, 1949, 1948, 1947, 1946, 1945, 1944, 1943, 1942, 1941, 1940, 1939, 1938, 1937, 1936, 1935, 1934, 1933, 1932, 1931, 1930, 1929, 1928, 1927, 1926, 1925, 1924, 1923, 1922, 1921, 1920, 1919, 1918, 1917, 1916, 1915, 1914, 1913, 1912, 1911, 1910, 1909, 1908, 1907, 1906, 1905, 1904, 1903, 1902, 1901, 1900, 1899, 1898, 1897, 1896, 1895, 1894, 1893, 1892, 1891, 1890, 1889, 1888, 1887, 1886, 1885, 1884, 1883, 1882, 1881, 1880, 1879, 1878, 1877, 1876, 1875, 1874, 1873, 1872, 1871, 1870, 1869, 1868, 1867, 1866, 1865, 1864, 1863, 1862, 1861, 1860, 1859, 1858, 1857, 1856, 1855, 1854, 1853, 1852, 1851, 1850, 1849, 1848, 1847, 1846, 1845, 1844, 1843, 1842, 1841, 1840, 1839, 1838, 1837, 1836, 1835, 1834, 1833, 1832, 1831, 1830, 1829, 1828, 1827, 1826, 1825, 1824], "interpretation": [ { "rank": "NA", "scope": "climate" }, { "fraction": "NA", "rank": "NA", "scope": "climate" }, { "fraction": "NA", "rank": "NA", "scope": "climate" }, { "fraction": "NA", "rank": "NA", "scope": "climate" } ], "hasResolution": { "hasMaxValue": 1, "hasMeanValue": 1, "hasMedianValue": 1, "hasMinValue": 1, "units": "AD" } }, "depth": { "dataType": "float", "description": "depth", "hasMaxValue": "_NaN_", "hasMeanValue": "_NaN_", "hasMedianValue": "_NaN_", "hasMinValue": "_NaN_", "iso2kPrimaryTimeseries": "FALSE", "longName": "AD", "measurementTableMD5": "b66c531c8f4194891d8d0f6723e3f957", "measurementTableName": "measurementTable1", "medianRes12k": "NA", "paleoDataTableName": "pt1_1", "paleoMeasurementTableMD5": "b66c531c8f4194891d8d0f6723e3f957", "TSid": "MAT4b082cc2d4", "units": "cm", "variableName": "depth", "variableType": "measured", "isPrimary": false, "primaryAgeColumn": false, "hasTimeTsid": "MAT7d0bc1f777", "values": ["NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN", "NaN"], "interpretation": [ { "rank": "NA", "scope": "climate" }, { "fraction": "NA", "rank": "NA", "scope": "climate" }, { "fraction": "NA", "rank": "NA", "scope": "climate" }, { "fraction": "NA", "rank": "NA", "scope": "climate" } ], "hasResolution": { "hasMaxValue": 1, "hasMeanValue": 1, "hasMedianValue": 1, "hasMinValue": 1, "units": "AD" } } } ] } ], "chronData": [ { "measurementTable": [ { "googleWorkSheetKey": "o2ko1cj", "tableName": "chron1measurement1", "missingValue": "NaN", "depthUTh": { "chronMeasMD5": "163544aec6e3567a9368f247423ad78b", "measurementTableName": "measurementTable1", "TSid": "chron1", "variableName": "depthUTh", "units": "mm", "chronName": "c1", "description": "mid-point depth of the sub-sample drilled for U-Th age", "notes": "Essential", "hasMaxValue": "_NaN_", "hasMinValue": "_NaN_", "hasMeanValue": "_NaN_", "hasMedianValue": "_NaN_", "number": 1, "values": ["NA", "NA", "NA", "NA", "NA", "NA", "NA", "NA"] }, "SampleID": { "chronMeasMD5": "163544aec6e3567a9368f247423ad78b", "measurementTableName": "measurementTable1", "TSid": "chron2", "variableName": "SampleID", "chronName": "c1", "description": "Sample ID for the U-Th age measured", "hasMaxValue": "_NaN_", "hasMinValue": "_NaN_", "hasMeanValue": "_NaN_", "hasMedianValue": "_NaN_", "number": 2, "values": ["NA", "NA", "NA", "NA", "NA", "NA", "NA", "NA"] }, "weight": { "chronMeasMD5": "163544aec6e3567a9368f247423ad78b", "measurementTableName": "measurementTable1", "TSid": "chron3", "variableName": "weight", "units": "mg", "chronName": "c1", "description": "Weight of powder analyzed for U-Th age", "hasMaxValue": "_NaN_", "hasMinValue": "_NaN_", "hasMeanValue": "_NaN_", "hasMedianValue": "_NaN_", "number": 3, "values": ["NA", "NA", "NA", "NA", "NA", "NA", "NA", "NA"] }, "U238": { "chronMeasMD5": "163544aec6e3567a9368f247423ad78b", "measurementTableName": "measurementTable1", "TSid": "chron4", "variableName": "U238", "units": "ppb", "chronName": "c1", "description": "238U content of the sub-sample", "notes": "Essential", "hasMaxValue": "_NaN_", "hasMinValue": "_NaN_", "hasMeanValue": "_NaN_", "hasMedianValue": "_NaN_", "number": 4, "values": ["NA", "NA", "NA", "NA", "NA", "NA", "NA", "NA"] }, "U238_error": { "chronMeasMD5": "163544aec6e3567a9368f247423ad78b", "measurementTableName": "measurementTable1", "TSid": "chron5", "variableName": "U238_error", "units": "ppb", "chronName": "c1", "description": "Analytical uncertainty of 238U", "uncertaintyLevel": "2 sigma", "hasMaxValue": "_NaN_", "hasMinValue": "_NaN_", "hasMeanValue": "_NaN_", "hasMedianValue": "_NaN_", "number": 5, "values": ["NA", "NA", "NA", "NA", "NA", "NA", "NA", "NA"] }, "Th232": { "chronMeasMD5": "163544aec6e3567a9368f247423ad78b", "measurementTableName": "measurementTable1", "TSid": "chron6", "variableName": "Th232", "units": "ppt", "chronName": "c1", "description": "232Th content of the sub-sample", "notes": "Essential", "hasMaxValue": "_NaN_", "hasMinValue": "_NaN_", "hasMeanValue": "_NaN_", "hasMedianValue": "_NaN_", "number": 6, "values": ["NA", "NA", "NA", "NA", "NA", "NA", "NA", "NA"] }, "Th232_error": { "chronMeasMD5": "163544aec6e3567a9368f247423ad78b", "measurementTableName": "measurementTable1", "TSid": "chron7", "variableName": "Th232_error", "units": "ppt", "chronName": "c1", "description": "Analytical uncertainty of 232Th", "uncertaintyLevel": "2 sigma", "hasMaxValue": "_NaN_", "hasMinValue": "_NaN_", "hasMeanValue": "_NaN_", "hasMedianValue": "_NaN_", "number": 7, "values": ["NA", "NA", "NA", "NA", "NA", "NA", "NA", "NA"] }, "d234U": { "chronMeasMD5": "163544aec6e3567a9368f247423ad78b", "measurementTableName": "measurementTable1", "TSid": "chron8", "variableName": "d234U", "units": "(ratio)", "chronName": "c1", "description": "d234U measured in the sub-sample", "notes": "Essential", "hasMaxValue": "_NaN_", "hasMinValue": "_NaN_", "hasMeanValue": "_NaN_", "hasMedianValue": "_NaN_", "number": 8, "values": ["NA", "NA", "NA", "NA", "NA", "NA", "NA", "NA"] }, "d234U_error": { "chronMeasMD5": "163544aec6e3567a9368f247423ad78b", "measurementTableName": "measurementTable1", "TSid": "chron9", "variableName": "d234U_error", "chronName": "c1", "description": "Analytical uncertainty of d234U", "uncertaintyLevel": "2 sigma", "hasMaxValue": "_NaN_", "hasMinValue": "_NaN_", "hasMeanValue": "_NaN_", "hasMedianValue": "_NaN_", "number": 9, "values": ["NA", "NA", "NA", "NA", "NA", "NA", "NA", "NA"] }, "Th230_U238activity": { "chronMeasMD5": "163544aec6e3567a9368f247423ad78b", "measurementTableName": "measurementTable1", "TSid": "chron10", "variableName": "Th230_U238activity", "units": "activity", "chronName": "c1", "description": "[230Th/238U] activity measured in the sub-sample", "hasMaxValue": "_NaN_", "hasMinValue": "_NaN_", "hasMeanValue": "_NaN_", "hasMedianValue": "_NaN_", "number": 10, "values": ["NA", "NA", "NA", "NA", "NA", "NA", "NA", "NA"] }, "U_Thactivity_error": { "chronMeasMD5": "163544aec6e3567a9368f247423ad78b", "measurementTableName": "measurementTable1", "TSid": "chron11", "variableName": "U_Thactivity_error", "chronName": "c1", "description": "Analytical uncertainty of 230Th-238U activity", "uncertaintyLevel": "2 sigma", "hasMaxValue": "_NaN_", "hasMinValue": "_NaN_", "hasMeanValue": "_NaN_", "hasMedianValue": "_NaN_", "number": 11, "values": ["NA", "NA", "NA", "NA", "NA", "NA", "NA", "NA"] }, "Th230_Th232ratio": { "chronMeasMD5": "163544aec6e3567a9368f247423ad78b", "measurementTableName": "measurementTable1", "TSid": "chron12", "variableName": "Th230_Th232ratio", "units": "ppm", "chronName": "c1", "description": "[230Th/232Th] ratio in the sub-sample", "hasMaxValue": "_NaN_", "hasMinValue": "_NaN_", "hasMeanValue": "_NaN_", "hasMedianValue": "_NaN_", "number": 12, "values": ["NA", "NA", "NA", "NA", "NA", "NA", "NA", "NA"] }, "Thratio_error": { "chronMeasMD5": "163544aec6e3567a9368f247423ad78b", "measurementTableName": "measurementTable1", "TSid": "chron13", "variableName": "Thratio_error", "units": "ppm", "chronName": "c1", "description": "Analytical uncertainty of 230Th-232Th ratio", "uncertaintyLevel": "2 sigma", "hasMaxValue": "_NaN_", "hasMinValue": "_NaN_", "hasMeanValue": "_NaN_", "hasMedianValue": "_NaN_", "number": 13, "values": ["NA", "NA", "NA", "NA", "NA", "NA", "NA", "NA"] }, "AgeUncorrected": { "chronMeasMD5": "163544aec6e3567a9368f247423ad78b", "measurementTableName": "measurementTable1", "TSid": "chron14", "variableName": "AgeUncorrected", "units": "years ago", "chronName": "c1", "description": "Uncorrected U-Th age of the sub-sample", "notes": "Essential", "hasMaxValue": "_NaN_", "hasMinValue": "_NaN_", "hasMeanValue": "_NaN_", "hasMedianValue": "_NaN_", "number": 14, "values": ["NA", "NA", "NA", "NA", "NA", "NA", "NA", "NA"] }, "AgeUncorr_error": { "chronMeasMD5": "163544aec6e3567a9368f247423ad78b", "measurementTableName": "measurementTable1", "TSid": "chron15", "variableName": "AgeUncorr_error", "units": "yrs", "chronName": "c1", "description": "Analytical uncertainty of Uncorrected Age", "uncertaintyLevel": "2 sigma", "notes": "Essential", "hasMaxValue": "_NaN_", "hasMinValue": "_NaN_", "hasMeanValue": "_NaN_", "hasMedianValue": "_NaN_", "number": 15, "values": ["NA", "NA", "NA", "NA", "NA", "NA", "NA", "NA"] }, "age": { "chronMeasMD5": "163544aec6e3567a9368f247423ad78b", "measurementTableName": "measurementTable1", "TSid": "chron16", "variableName": "age", "units": "years ago", "chronName": "c1", "description": "Corrected U-Th age of the sub-sample", "notes": "Essential", "hasMaxValue": "_NaN_", "hasMinValue": "_NaN_", "hasMeanValue": "_NaN_", "hasMedianValue": "_NaN_", "number": 16, "values": ["NA", "NA", "NA", "NA", "NA", "NA", "NA", "NA"] }, "AgeCorr_error": { "chronMeasMD5": "163544aec6e3567a9368f247423ad78b", "measurementTableName": "measurementTable1", "TSid": "chron17", "variableName": "AgeCorr_error", "units": "yrs", "chronName": "c1", "description": "Uncertainty of Corrected Age (includes Th correction)", "uncertaintyLevel": "2 sigma", "notes": "Essential", "hasMaxValue": "_NaN_", "hasMinValue": "_NaN_", "hasMeanValue": "_NaN_", "hasMedianValue": "_NaN_", "number": 17, "values": ["NA", "NA", "NA", "NA", "NA", "NA", "NA", "NA"] }, "dU234initial": { "chronMeasMD5": "163544aec6e3567a9368f247423ad78b", "measurementTableName": "measurementTable1", "TSid": "chron18", "variableName": "dU234initial", "units": "(ratio)", "chronName": "c1", "description": "Calculated initial d234U in the sub-sample", "hasMaxValue": "_NaN_", "hasMinValue": "_NaN_", "hasMeanValue": "_NaN_", "hasMedianValue": "_NaN_", "number": 18, "values": ["NA", "NA", "NA", "NA", "NA", "NA", "NA", "NA"] }, "dU234i_error": { "chronMeasMD5": "163544aec6e3567a9368f247423ad78b", "measurementTableName": "measurementTable1", "TSid": "chron19", "variableName": "dU234i_error", "chronName": "c1", "description": "Analytical uncertainty of calculated d234U initial", "uncertaintyLevel": "2 sigma", "hasMaxValue": "_NaN_", "hasMinValue": "_NaN_", "hasMeanValue": "_NaN_", "hasMedianValue": "_NaN_", "number": 19, "values": ["NA", "NA", "NA", "NA", "NA", "NA", "NA", "NA"] }, "depthtopPb": { "chronMeasMD5": "163544aec6e3567a9368f247423ad78b", "measurementTableName": "measurementTable1", "TSid": "chron20", "variableName": "depthtopPb", "units": "mm", "chronName": "c1", "description": "Depth at the top of the sub-sample for 210Pb analysis", "hasMaxValue": "_NaN_", "hasMinValue": "_NaN_", "hasMeanValue": "_NaN_", "hasMedianValue": "_NaN_", "number": 20, "values": ["NA", "NA", "NA", "NA", "NA", "NA", "NA", "NA"] }, "depthbottomPb": { "chronMeasMD5": "163544aec6e3567a9368f247423ad78b", "measurementTableName": "measurementTable1", "TSid": "chron21", "variableName": "depthbottomPb", "units": "mm", "chronName": "c1", "description": "Depth at the bottom of the sub-sample for 210Pb analysis", "hasMaxValue": "_NaN_", "hasMinValue": "_NaN_", "hasMeanValue": "_NaN_", "hasMedianValue": "_NaN_", "number": 21, "values": ["NA", "NA", "NA", "NA", "NA", "NA", "NA", "NA"] }, "Pb210excess": { "chronMeasMD5": "163544aec6e3567a9368f247423ad78b", "measurementTableName": "measurementTable1", "TSid": "chron22", "variableName": "Pb210excess", "units": "dpm/g", "chronName": "c1", "description": "Lead-210 excess measured in the sub-sample", "hasMaxValue": "_NaN_", "hasMinValue": "_NaN_", "hasMeanValue": "_NaN_", "hasMedianValue": "_NaN_", "number": 22, "values": ["NA", "NA", "NA", "NA", "NA", "NA", "NA", "NA"] }, "Pb210_error": { "chronMeasMD5": "163544aec6e3567a9368f247423ad78b", "measurementTableName": "measurementTable1", "TSid": "chron23", "variableName": "Pb210_error", "units": "dpm/g", "chronName": "c1", "description": "Analytical uncertainty of 210Pb excess", "uncertaintyLevel": "1 sigma", "hasMaxValue": "_NaN_", "hasMinValue": "_NaN_", "hasMeanValue": "_NaN_", "hasMedianValue": "_NaN_", "number": 23, "values": ["NA", "NA", "NA", "NA", "NA", "NA", "NA", "NA"] }, "depthtopCs": { "chronMeasMD5": "163544aec6e3567a9368f247423ad78b", "measurementTableName": "measurementTable1", "TSid": "chron24", "variableName": "depthtopCs", "units": "mm", "chronName": "c1", "description": "Depth at the top of the sub-sample for 137Cs analysis", "hasMaxValue": "_NaN_", "hasMinValue": "_NaN_", "hasMeanValue": "_NaN_", "hasMedianValue": "_NaN_", "number": 24, "values": ["NA", "NA", "NA", "NA", "NA", "NA", "NA", "NA"] }, "depthbottomCs": { "chronMeasMD5": "163544aec6e3567a9368f247423ad78b", "measurementTableName": "measurementTable1", "TSid": "chron25", "variableName": "depthbottomCs", "units": "mm", "chronName": "c1", "description": "Depth at the bottom of the sub-sample for 137Cs analysis", "hasMaxValue": "_NaN_", "hasMinValue": "_NaN_", "hasMeanValue": "_NaN_", "hasMedianValue": "_NaN_", "number": 25, "values": ["NA", "NA", "NA", "NA", "NA", "NA", "NA", "NA"] }, "Cs137gamactivity": { "chronMeasMD5": "163544aec6e3567a9368f247423ad78b", "measurementTableName": "measurementTable1", "TSid": "chron26", "variableName": "Cs137gamactivity", "units": "Bq/g", "chronName": "c1", "description": "Cesium-137 g-activity measured in the sub-sample", "hasMaxValue": "_NaN_", "hasMinValue": "_NaN_", "hasMeanValue": "_NaN_", "hasMedianValue": "_NaN_", "number": 26, "values": ["NA", "NA", "NA", "NA", "NA", "NA", "NA", "NA"] }, "Cs137_error": { "chronMeasMD5": "163544aec6e3567a9368f247423ad78b", "measurementTableName": "measurementTable1", "TSid": "chron27", "variableName": "Cs137_error", "units": "Bq/g", "chronName": "c1", "description": "Analytical uncertainty of 137Cs g-activity", "uncertaintyLevel": "1 sigma", "hasMaxValue": "_NaN_", "hasMinValue": "_NaN_", "hasMeanValue": "_NaN_", "hasMedianValue": "_NaN_", "number": 27, "values": ["NA", "NA", "NA", "NA", "NA", "NA", "NA", "NA"] }, "bandAge": { "chronMeasMD5": "163544aec6e3567a9368f247423ad78b", "measurementTableName": "measurementTable1", "TSid": "chron28", "variableName": "bandAge", "units": "yr CE", "chronName": "c1", "description": "Band counted age for the U-Th sample", "notes": "Essential", "hasMaxValue": "_NaN_", "hasMinValue": "_NaN_", "hasMeanValue": "_NaN_", "hasMedianValue": "_NaN_", "number": 28, "values": ["NA", "NA", "NA", "NA", "NA", "NA", "NA", "NA"] }, "sampleType": { "chronMeasMD5": "163544aec6e3567a9368f247423ad78b", "measurementTableName": "measurementTable1", "TSid": "chron29", "variableName": "sampleType", "chronName": "c1", "description": "Sample description. E.g., round plug, annual density band", "notes": "Essential", "hasMaxValue": "_NaN_", "hasMinValue": "_NaN_", "hasMeanValue": "_NaN_", "hasMedianValue": "_NaN_", "number": 29, "values": ["NA", "NA", "NA", "NA", "NA", "NA", "NA", "NA"] } } ], "model": [ { "methods": { "algorithm": "BAM", "parameters": { "nEns": 1000, "resize": 0 }, "uncertainty": "low" } }, { "methods": { "algorithm": "BAM", "parameters": { "nEns": 1000, "resize": 0 }, "uncertainty": "high" } } ] } ], "archiveType": "Coral", "archiveTypeOriginal": "coral", "createdBy": "matlab", "dataAcquisitionNotes": "http://www1.ncdc.noaa.gov/pub/data/paleo/coral/atlantic/florida-bay-1996.txt", "datasetId": "GtaQfVzeDU1H8ksSWa1m", "dataSetName": "CO96SWFB", "datasetVersion": "1.0.6", "googleMetadataWorksheet": "o35hism", "googleSpreadSheetKey": "19lz0WvnAcxWtke0yqlSwhPcfoVamUZghEKg7Ead9nIQ", "hasChron": "0", "hasDepth": "0", "hasPaleoDepth": 0, "lipdverseLink": "https://lipdverse.org/data/GtaQfVzeDU1H8ksSWa1m/1_0_6", "maxYear": 1985, "minYear": 1824, "modernSystem_instrumentalDatasetCoordinates": "24.91667, -80.75", "modernSystem_instrumentalDatasetURL": "http://www1.ncdc.noaa.gov/pub/data/paleo/coral/atlantic/florida-bay-1996.txt", "Notes": "Swart 1999 NOAA has different corrdinates for this coral 25 0N, 80 36W, Looking at Google earth and Hudsons map, the Swart 1999 corrdinates incorrect, they should be 24 degrees 55 minutes N, and ~80 degrees, 43.5 minutes W", "nUniqueAges": 0, "nUniqueGoodAges": 0, "nUniqueOtherAges": 0, "originalDataUrl": "https://www.ncdc.noaa.gov/paleo/study/1886", "tagMD5": "cdd24e5f1bd0ccfc82d5a33005835e07", "lipdVersion": 1.3, "changelog": [ { "version": "1.0.6", "lastVersion": "1.0.5", "curator": "nicholas", "timestamp": "2025-05-20 16:18:38.996904 UTC", "changes": { "Paleo Interpretation metadata": [ ["depth (MAT4b082cc2d4): interpretation4_scope: '' has been replaced by 'climate'"], ["year (MAT7d0bc1f777): interpretation4_scope: '' has been replaced by 'climate'"] ] } }, { "version": "1.0.5", "lastVersion": "1.0.4", "curator": "nicholas", "timestamp": "2025-04-17 20:04:03.520453 UTC", "changes": { "Paleo Column metadata": [ ["d18O (CO96SWFB01A): paleoData_isPrimary: '' has been replaced by 'FALSE'"], ["d18O (CO96SWFB01A): paleoData_primaryAgeColumn: '' has been replaced by 'FALSE'"], ["depth (MAT4b082cc2d4): paleoData_isPrimary: '' has been replaced by 'FALSE'"], ["depth (MAT4b082cc2d4): paleoData_primaryAgeColumn: '' has been replaced by 'FALSE'"], ["year (MAT7d0bc1f777): paleoData_isPrimary: '' has been replaced by 'TRUE'"], ["year (MAT7d0bc1f777): paleoData_primaryAgeColumn: '' has been replaced by 'TRUE'"] ] } }, { "version": "1.0.4", "lastVersion": "1.0.3", "curator": "nicholas", "timestamp": "2025-04-11 16:14:47.068085 UTC", "changes": { "Paleo Interpretation metadata": [ ["d18O (CO96SWFB01A): interpretation2_basis: 'The higher skeletal d18O value reflects the high d180 value of the Bay water itself (Lloyd, 1964; Swart et al., 1989), which is enriched in d18O as a result of evaporation and the input of 1so enriched freshwater from the Everglades (Meyers et al., 1993). Salinity values are the highest during the summer, as a result of evaporation, and lower during the winter when the Bay becomes dominated by water from the Gulf of Mexico and the Florida Reef Tract. These changes in salinity should be manifested in the 6180 of the coral, but as the maximum enrichment in the water occurs during the warmest portion of the year (the summer), the temperature and salinity effects tend to counteract each other, thereby reducing the observed range of oxygen isotopic variation seen in the coral.' has been replaced by ''"], ["d18O (CO96SWFB01A): interpretation2_direction: 'positive' has been replaced by ''"], ["d18O (CO96SWFB01A): interpretation2_inferredMaterial: 'seawater' has been replaced by ''"], ["d18O (CO96SWFB01A): interpretation2_integrationTime: '1' has been replaced by ''"], ["d18O (CO96SWFB01A): interpretation2_integrationTimeBasis: 'In South Florida, the dense band forms in the late summer, but it is generally thought that there is as much as a � two month variation in timing. By counting the number of bands in a coral, the age can be assessed. Errors in age interpretation arise when dense bands are indistinct or when so-called \"stress bands\", resulting from events such as temperature extremes, occur. Generally speaking, a year in which a stress band forms may actually contain two dense bands or a thicker dense band which is a combination of the stress and normal dense band. Although it is possible to misinterpret a stress band as an annual band, the annual bands can be recognized by their regular spacing. 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By counting the number of bands in a coral, the age can be assessed. Errors in age interpretation arise when dense bands are indistinct or when so-called \"stress bands\", resulting from events such as temperature extremes, occur. Generally speaking, a year in which a stress band forms may actually contain two dense bands or a thicker dense band which is a combination of the stress and normal dense band. Although it is possible to misinterpret a stress band as an annual band, the annual bands can be recognized by their regular spacing. 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Salinity values are the highest during the summer, as a result of evaporation, and lower during the winter when the Bay becomes dominated by water from the Gulf of Mexico and the Florida Reef Tract. These changes in salinity should be manifested in the 6180 of the coral, but as the maximum enrichment in the water occurs during the warmest portion of the year (the summer), the temperature and salinity effects tend to counteract each other, thereby reducing the observed range of oxygen isotopic variation seen in the coral.'"], ["d18O (CO96SWFB01A): interpretation4_direction: '' has been replaced by 'positive'"], ["d18O (CO96SWFB01A): interpretation4_inferredMaterial: '' has been replaced by 'seawater'"], ["d18O (CO96SWFB01A): interpretation4_integrationTime: '' has been replaced by '1'"], ["d18O (CO96SWFB01A): interpretation4_integrationTimeBasis: '' has been replaced by 'In South Florida, the dense band forms in the late summer, but it is generally thought that there is as much as a � two month variation in timing. By counting the number of bands in a coral, the age can be assessed. Errors in age interpretation arise when dense bands are indistinct or when so-called \"stress bands\", resulting from events such as temperature extremes, occur. Generally speaking, a year in which a stress band forms may actually contain two dense bands or a thicker dense band which is a combination of the stress and normal dense band. Although it is possible to misinterpret a stress band as an annual band, the annual bands can be recognized by their regular spacing. Therefore, density changes can still provide a clear annual chronology.'"], ["d18O (CO96SWFB01A): interpretation4_integrationTimeUncertainty: '' has been replaced by 'subannual samples averaged to annual for archived data'"], ["d18O (CO96SWFB01A): interpretation4_integrationTimeUncertaintyType: '' has been replaced by 'chronological'"], ["d18O (CO96SWFB01A): interpretation4_integrationTimeUnits: '' has been replaced by 'year'"], ["d18O (CO96SWFB01A): interpretation4_mathematicalRelation: '' has been replaced by 'linear'"], ["d18O (CO96SWFB01A): interpretation4_rank: '' has been replaced by '1'"], ["d18O (CO96SWFB01A): interpretation4_scope: '' has been replaced by 'isotope'"], ["d18O (CO96SWFB01A): interpretation4_seasonality: '' has been replaced by 'Annual'"], ["d18O (CO96SWFB01A): interpretation4_seasonalityOriginal: '' has been replaced by 'Annual'"], ["d18O (CO96SWFB01A): interpretation4_variable: '' has been replaced by 'seawaterIsotope'"], ["d18O (CO96SWFB01A): interpretation4_variableGroup: '' has been replaced by 'EffectiveMoisture'"], ["d18O (CO96SWFB01A): interpretation4_variableGroupDirection: '' has been replaced by 'negative'"], ["d18O (CO96SWFB01A): interpretation4_variableGroupOriginal: '' has been replaced by 'd18O_seawater'"], ["d18O (CO96SWFB01A): interpretation5_basis: '' has been replaced by 'Temperature is not significant (r= 0.08)'"], ["d18O (CO96SWFB01A): interpretation5_fraction: '' has been replaced by '0'"], ["d18O (CO96SWFB01A): interpretation5_inferredMaterial: '' has been replaced by 'seawater'"], ["d18O (CO96SWFB01A): interpretation5_integrationTime: '' has been replaced by '1'"], ["d18O (CO96SWFB01A): interpretation5_integrationTimeBasis: '' has been replaced by 'In South Florida, the dense band forms in the late summer, but it is generally thought that there is as much as a � two month variation in timing. By counting the number of bands in a coral, the age can be assessed. Errors in age interpretation arise when dense bands are indistinct or when so-called \"stress bands\", resulting from events such as temperature extremes, occur. Generally speaking, a year in which a stress band forms may actually contain two dense bands or a thicker dense band which is a combination of the stress and normal dense band. Although it is possible to misinterpret a stress band as an annual band, the annual bands can be recognized by their regular spacing. Therefore, density changes can still provide a clear annual chronology.'"], ["d18O (CO96SWFB01A): interpretation5_integrationTimeUncertainty: '' has been replaced by 'subannual samples averaged to annual for archived data'"], ["d18O (CO96SWFB01A): interpretation5_integrationTimeUncertaintyType: '' has been replaced by 'chronological'"], ["d18O (CO96SWFB01A): interpretation5_integrationTimeUnits: '' has been replaced by 'year'"], ["d18O (CO96SWFB01A): interpretation5_rank: '' has been replaced by '2'"], ["d18O (CO96SWFB01A): interpretation5_scope: '' has been replaced by 'isotope'"], ["d18O (CO96SWFB01A): interpretation5_variable: '' has been replaced by 'temperature'"], ["d18O (CO96SWFB01A): interpretation5_variableGroup: '' has been replaced by 'Temperature'"], ["d18O (CO96SWFB01A): interpretation5_variableGroupDirection: '' has been replaced by 'negative'"], ["d18O (CO96SWFB01A): interpretation5_variableGroupOriginal: '' has been replaced by 'T_water'"], ["d18O (CO96SWFB01A): interpretation6_scope: '' has been replaced by 'isotope'"], ["depth (MAT4b082cc2d4): interpretation1_scope: '' has been replaced by 'climate'"], ["depth (MAT4b082cc2d4): interpretation2_scope: '' has been replaced by 'climate'"], ["depth (MAT4b082cc2d4): interpretation3_scope: '' has been replaced by 'climate'"], ["year (MAT7d0bc1f777): interpretation1_scope: '' has been replaced by 'climate'"], ["year (MAT7d0bc1f777): interpretation2_scope: '' has been replaced by 'climate'"], ["year (MAT7d0bc1f777): interpretation3_scope: '' has been replaced by 'climate'"] ] } }, { "version": "1.0.3", "lastVersion": "1.0.2", "curator": "nicholas", "timestamp": "2025-04-09 20:50:25.503945 UTC", "notes": "Updated lipdverse database entry with a changed file.", "changes": { "Paleo Interpretation metadata": [ ["d18O (CO96SWFB01A): interpretation1_variable: 'S' has been replaced by 'salinity'"], ["d18O (CO96SWFB01A): interpretation2_seasonality: 'annual' has been replaced by 'Annual'"], ["d18O (CO96SWFB01A): interpretation2_variable: 'd18O_seawater' has been replaced by 'seawaterIsotope'"], ["d18O (CO96SWFB01A): interpretation3_variable: 'T_water' has been replaced by 'temperature'"] ] } }, { "version": "1.0.2", "lastVersion": "1.0.1", "curator": "nicholas", "timestamp": "2025-04-09 17:39:02.538838 UTC", "notes": "Changes made as part of LiPDverse vocabulary standardization process", "changes": { "Paleo Interpretation metadata": [ ["d18O (CO96SWFB01A): interpretation1_variable: 'S' has been replaced by 'salinity'"], ["d18O (CO96SWFB01A): interpretation2_seasonality: 'annual' has been replaced by 'Annual'"], ["d18O (CO96SWFB01A): interpretation2_variable: 'd18O_seawater' has been replaced by 'seawaterIsotope'"], ["d18O (CO96SWFB01A): interpretation3_variable: 'T_water' has been replaced by 'temperature'"] ] } }, { "version": "1.0.1", "lastVersion": "1.0.0", "curator": "nicholas", "timestamp": "2025-04-08 17:32:35.557636 UTC", "notes": "Changes made as part of LiPDverse vocabulary standardization process", "changes": { "Paleo Column metadata": [ ["d18O (CO96SWFB01A): paleoData_longName: '' has been replaced by 'AD'"], ["depth (MAT4b082cc2d4): paleoData_longName: '' has been replaced by 'AD'"], ["year (MAT7d0bc1f777): paleoData_units: 'AD' has been replaced by 'yr AD'"], ["year (MAT7d0bc1f777): paleoData_longName: '' has been replaced by 'AD'"] ] } } ], "environmentInterpretation1_direction": null, "environmentInterpretation1_seasonality": null, "environmentInterpretation1_variable": null, "testField": null, "pub": [ { "author": { "name": "Swart" }, "citation": "Swart, P. K., Healy, G. F., Dodge, R. E., Kramer, P., Hudson, J. H., Halley, R. B. and Robblee, M. B.: The stable oxygen and carbon isotopic record from a coral growing in Florida Bay: a 160 year record of climatic and anthropogenic influence, Palaeogeography, Palaeoclimatology, Palaeoecology, 123(1-4), 219–237, doi:10.1016/0031-0182(95)00078-x, 1996.", "doi": "10.1016/0031-0182(95)00078-X, 10.1016/0168-9622(91)90055-2, 10.1002/2014PA002717" }, { "citation": "Swart, P. K., Burns, S. J. and Leder, J. J.: Fractionation of the stable isotopes of oxygen and carbon in carbon dioxide during the reaction of calcite with phosphoric acid as a function of temperature and technique, Chemical Geology: Isotope Geoscience section, 86(2), 89–96, doi:10.1016/0168-9622(91)90055-2, 1991.", "doi": "10.1016/0168-9622(91)90055-2" } ], "geo": { "longitude": -80.75, "latitude": 24.9167, "elevation": -5, "geometryType": "Point", "siteName": "Lignumvitae Basin, Florida Bay" }, "@context": "context.jsonld" }