{ "paleoData": [ { "measurementTable": [ { "googleWorkSheetKey": "osznvyi", "tableName": "paleo1measurement1", "missingValue": "NaN", "d18O": { "paleoDataTableName": "pt1_1", "measurementTableName": "measurementTable1", "TSid": "LS10ANBL01a", "description": "carbonate", "hasMaxValue": -8.8861, "hasMeanValue": -10.7875, "hasMedianValue": -10.795, "hasMinValue": -12.0048, "instrument": "Finnegan MAT 252 mass spectrometer", "iso2kPrimaryTimeseries": "TRUE", "measurementMaterial": "mollusk", "measurementMaterialDetail": "and algal crusts", "measurementMaterialScreening": "no", "measurementStandard": "VPDB", "measurementTableMD5": "3d0a6da80b37e9ca735488c7a97d4524", "notes": "\"Overall, the Lake Blektjaernen isotope record shows similar δ18O and δ13C trends (Figs 3 and 7). We argue that this is because increased evaporation and enhanced vapour exchange led to preferential loss of lighter isotopes, which resulted in elevated values of δ18O and δ13C during periods with relatively drier climate (Talbot, 1990; Li and Ku, 1997). The correlation coefficient for covariance is large (r2 = 0.54) between δ18O and δ13C values in Chara, indicating that past changes in the isotopic composition of Lake Blektjaernen in the summer is controlled to a large degree by variation in the E/I ratio. If so, more negative δ18O and δ13C values would imply more humid conditions...Our results show the potential of using lacustrine stable isotope data to reconstruct past changes in humidity during summer (Chara) \"", "paleoMeasurementTableMD5": "3d0a6da80b37e9ca735488c7a97d4524", "uncertaintyAnalytical": "� 0.1", "units": "permil", "variableName": "d18O", "variableType": "measured", "equilibriumEvidence": "Comparison with lake water d18O", "hasChron": "0", "hasPaleoDepth": "0", "inferredMaterial": "lake water", "QCCertification": "MJ, CH", "inferredMaterialGroup": "surface water", "inferredMaterialGroupOriginal": "lake water", "iso2kUI": "LS10ANBL01", "iso2kCertification": "MJ", "samplingMethod": "Samples collected from core", "meanValue12k": -10.7875, "medianRes12k": 51.5918, "hasMean": -10.7875, "hasMedian": -10.9553, "hasMax": -8.8861, "hasMin": -12.0048, "proxy": "d18O", "proxyDetail": "Chara", "proxyGeneral": "isotope", "datum": "VSMOW", "proxyLumps": "isotope", "proxyLumpsOriginal": "d18O", "values": [-11.1452, -11.598, -10.3647, -11.4159, -11.8905, -12.0048, -11.0745, -11.6275, -11.2144, -11.2409, -11.5629, -11.0204, -11.0328, -11.4964, -11.6356, -11.1699, -11.6411, -11.2763, -10.3775, -10.9293, -10.4076, -11.3637, -10.3739, -11.0472, -10.8424, -10.4219, -10.6859, -10.8205, -10.5226, -10.5128, -8.8861, -11.3332, -10.9627, -10.5791, -10.277, -10.11, -9.812, -11.4393, -10.1488, -10.3855, -9.9021, -10.9319, -10.4118, -9.8559, -10.7695, -10.3653, -10.3498, -9.9958, -10.4124, -10.8866, -10.3957, -10.1064, -10.7543, -11.1053, -11.0028, -10.7639, -10.6609, -9.9382, -11.082, -11.145, -11.5025, -11.1165, -11.8975, -11.115, -11.5642, -10.9479, -10.5184, -11.026, -10.121, -10.1604, -10.4823, -10.2154, -10.4443, -10.3786, -10.5147, -10.3624], "QCnotes": null, "interpretation": [ { "basis": "Consistent with other records, d18O/d13C records", "interpDirection": "decrease", "scope": "climate", "variable": "effectivePrecipitation", "variableDetail": "lakebalance@surface", "direction": "negative", "variableGroup": "P-E", "seasonality": "Jun-Aug", "seasonalityGeneral": "summerOnly" }, { "basis": "Comparison with lake water, similar trend in both species analysed", "direction": "negative", "equilibriumEvidence": "Comparison with lake water d18O", "inferredMaterial": "lake water", "integrationTimeUncertaintyType": "chronological; resolution;", "integrationTimeUnits": "years", "rank": 1, "scope": "isotope", "variable": "hydrologicBalance", "variableGroup": "EffectiveMoisture", "variableGroupOriginal": "I_E", "variableGroupDirection": "negative" }, { "direction": "negative", "equilibriumEvidence": "Comparison with lake water d18O", "inferredMaterial": "lake water", "integrationTimeUncertaintyType": "chronological; resolution;", "integrationTimeUnits": "years", "rank": 2, "scope": "isotope", "variable": "temperature", "variableGroup": "Temperature", "variableGroupOriginal": "T_air", "variableGroupDirection": "negative" } ], "calibration": { "method": null, "seasonality": null }, "hasResolution": { "hasMean": 59.6328, "hasMedian": 37.5249, "hasMax": 210.5884, "hasMin": 4.8986 }, "inCompilationBeta": [ { "compilationName": "iso2k", "compilationVersion": ["0_14_8", "0_15_0", "1_0_0"] }, { "compilationName": "HoloceneHydroclimate", "compilationVersion": ["0_1_0", "0_2_0", "0_3_0", "0_4_0", "0_5_0", "0_6_0", "0_7_0", "0_8_0", "0_9_0", "0_9_1"] }, { "compilationName": "RapidArcticWarming", "compilationVersion": ["0_1_1", "0_2_0", "0_3_0", "0_4_0", "0_5_0", "0_5_1", "0_5_2", "0_5_3"] }, { "compilationName": "HoloceneAbruptChange", "compilationVersion": ["0_11_0", "0_11_0", "0_11_0", "0_11_0", "0_11_0", "0_11_0"] } ] }, "year": { "paleoDataTableName": "pt1_1", "measurementTableName": "measurementTable1", "TSid": "MAT423a41a367", "dataType": "float", "description": "Year AD", "hasMaxValue": 2010, "hasMeanValue": -176.8622, "hasMedianValue": -280.5234, "hasMinValue": -2435.5066, "inferredVariableType": "year", "iso2kPrimaryTimeseries": "FALSE", "measurementTableMD5": "3d0a6da80b37e9ca735488c7a97d4524", "paleoMeasurementTableMD5": "3d0a6da80b37e9ca735488c7a97d4524", "units": "yr AD", "variableName": "year", "variableType": "inferred", "samplingMethod": "Samples collected from core", "unitsOriginal": "CE", "hasMean": -176.8622, "hasMedian": -489.3281, "hasMax": 2010, "hasMin": -2435.5066, "isPrimary": true, "notes": "NA; paleoData_isPrimary has been standardized", "values": [2010, 1988.2063, 1967.3173, 1942.4487, 1916.0689, 1891.2745, 1879.1735, 1830.1818, 1775.3193, 1720.5466, 1664.4738, 1616.2538, 1567.6163, 1450.1917, 1330.1461, 1222.8836, 1115.5469, 1007.8405, 884.2652, 808.9624, 742.4321, 683.569, 625.1714, 523.0186, 451.0453, 392.1667, 326.2279, 270.9796, 211.5619, 150.876, 26.4553, -53.1388, -124.3829, -163.1808, -149.7055, -179.3351, -238.7527, -276.2776, -284.7693, -312.1266, -326.1936, -344.8953, -374.9951, -396.8406, -437.2981, -453.7378, -479.9854, -498.6709, -532.8927, -743.4812, -763.5882, -786.6069, -979.7411, -1029.8689, -1069.9034, -1095.1681, -1145.3222, -1192.7495, -1244.3413, -1291.1768, -1359.5517, -1457.0434, -1565.7435, -1665.5391, -1782.9003, -1873.3055, -1974.6548, -2076.0783, -2173.3109, -2266.6015, -2324.6982, -2329.5968, -2373.1138, -2393.0677, -2413.9094, -2435.5066], "hasResolution": { "hasMean": 59.6328, "hasMedian": 37.5249, "hasMax": 210.5884, "hasMin": 4.8986 } }, "age": { "archiveType": "LakeSediment", "variableName": "age", "proxyObservationType": "na", "units": "yr BP", "TSid": "WEB028eebbb", "hasMean": 2126.8622, "hasMedian": 2703.5347, "hasMax": 4385.5066, "hasMin": -60, "unitsOriginal": "yr BP", "datum": 1950, "isPrimary": true, "notes": "NA; paleoData_isPrimary has been standardized; paleoData_datum has been standardized", "values": [-60, -38.2063, -17.3173, 7.5513, 33.9311, 58.7255, 70.8265, 119.8182, 174.6807, 229.4534, 285.5262, 333.7462, 382.3837, 499.8083, 619.8539, 727.1164, 834.4531, 942.1595, 1065.7348, 1141.0376, 1207.5679, 1266.431, 1324.8286, 1426.9814, 1498.9547, 1557.8333, 1623.7721, 1679.0204, 1738.4381, 1799.124, 1923.5447, 2003.1388, 2074.3829, 2113.1808, 2099.7055, 2129.3351, 2188.7527, 2226.2776, 2234.7693, 2262.1266, 2276.1936, 2294.8953, 2324.9951, 2346.8406, 2387.2981, 2403.7378, 2429.9854, 2448.6709, 2482.8927, 2693.4812, 2713.5882, 2736.6069, 2929.7411, 2979.8689, 3019.9034, 3045.1681, 3095.3222, 3142.7495, 3194.3413, 3241.1768, 3309.5517, 3407.0434, 3515.7435, 3615.5391, 3732.9003, 3823.3055, 3924.6548, 4026.0783, 4123.3109, 4216.6015, 4274.6982, 4279.5968, 4323.1138, 4343.0677, 4363.9094, 4385.5066] } } ] } ], "chronData": [ { "measurementTable": [ { "googleWorkSheetKey": "o72xn8l", "tableName": "chron1measurement1", "missingValue": "NaN", "googWorkSheetKey": "obkjfp6", "depth": { "chronMeasMD5": "fc82720bd513525adf678411f4452547", "measurementTableName": "measurementTable1", "TSid": "chron1", "variableName": "depth", "description": "mid-point depth", "units": "cm", "chronName": "chron1", "chronMeasurementTableMD5": "fc82720bd513525adf678411f4452547", "chronMeasurementTableNumber": 1, "chronNumber": 1, "hasMaxValue": "_NaN_", "hasMeanValue": "_NaN_", "hasMedianValue": "_NaN_", "hasMinValue": "_NaN_", "paleoName": "chron1", "number": 1, "values": ["NA", "NA", "NA", "NA", "NA", "NA", "NA", "NA"] }, "age14C": { "chronMeasMD5": "fc82720bd513525adf678411f4452547", "measurementTableName": "measurementTable1", "TSid": "chron2", "variableName": "age14C", "description": "14C years before 1950", "units": "yr14C BP", "chronName": "chron1", "chronMeasurementTableMD5": "fc82720bd513525adf678411f4452547", "chronMeasurementTableNumber": 1, "chronNumber": 1, "hasMaxValue": "_NaN_", "hasMeanValue": "_NaN_", "hasMedianValue": "_NaN_", "hasMinValue": "_NaN_", "paleoName": "chron1", "number": 2, "values": ["NA", "NA", "NA", "NA", "NA", "NA", "NA", "NA"] }, "SD": { "chronMeasMD5": "fc82720bd513525adf678411f4452547", "measurementTableName": "measurementTable1", "TSid": "chron3", "variableName": "SD", "description": "14C years uncertainty", "units": "yr14C BP", "chronName": "chron1", "chronMeasurementTableMD5": "fc82720bd513525adf678411f4452547", "chronMeasurementTableNumber": 1, "chronNumber": 1, "hasMaxValue": "_NaN_", "hasMeanValue": "_NaN_", "hasMedianValue": "_NaN_", "hasMinValue": "_NaN_", "paleoName": "chron1", "variableNameOriginal": "age14Cuncertainty", "number": 3, "values": ["NA", "NA", "NA", "NA", "NA", "NA", "NA", "NA"] }, "fractionModern": { "chronMeasMD5": "fc82720bd513525adf678411f4452547", "measurementTableName": "measurementTable1", "TSid": "chron4", "variableName": "fractionModern", "description": "fraction of modern 14C activity", "chronName": "chron1", "chronMeasurementTableMD5": "fc82720bd513525adf678411f4452547", "chronMeasurementTableNumber": 1, "chronNumber": 1, "hasMaxValue": "_NaN_", "hasMeanValue": "_NaN_", "hasMedianValue": "_NaN_", "hasMinValue": "_NaN_", "paleoName": "chron1", "units": "unitless", "number": 4, "values": ["NA", "NA", "NA", "NA", "NA", "NA", "NA", "NA"] }, "fractionModernUncertainty": { "chronMeasMD5": "fc82720bd513525adf678411f4452547", "measurementTableName": "measurementTable1", "TSid": "chron5", "variableName": "fractionModernUncertainty", "description": "fraction of modern 14C activity uncertainty", "chronName": "chron1", "chronMeasurementTableMD5": "fc82720bd513525adf678411f4452547", "chronMeasurementTableNumber": 1, "chronNumber": 1, "hasMaxValue": "_NaN_", "hasMeanValue": "_NaN_", "hasMedianValue": "_NaN_", "hasMinValue": "_NaN_", "paleoName": "chron1", "units": "unitless", "number": 5, "values": ["NA", "NA", "NA", "NA", "NA", "NA", "NA", "NA"] }, "delta13C": { "chronMeasMD5": "fc82720bd513525adf678411f4452547", "measurementTableName": "measurementTable1", "TSid": "chron6", "variableName": "delta13C", "description": "delta13C of material analyzed for 14C", "units": "permil", "chronName": "chron1", "chronMeasurementTableMD5": "fc82720bd513525adf678411f4452547", "chronMeasurementTableNumber": 1, "chronNumber": 1, "hasMaxValue": "_NaN_", "hasMeanValue": "_NaN_", "hasMedianValue": "_NaN_", "hasMinValue": "_NaN_", "paleoName": "chron1", "number": 6, "values": ["NA", "NA", "NA", "NA", "NA", "NA", "NA", "NA"] }, "delta13Cuncertainty": { "chronMeasMD5": "fc82720bd513525adf678411f4452547", "measurementTableName": "measurementTable1", "TSid": "chron7", "variableName": "delta13Cuncertainty", "description": "delta13C uncertainty", "units": "permil", "chronName": "chron1", "chronMeasurementTableMD5": "fc82720bd513525adf678411f4452547", "chronMeasurementTableNumber": 1, "chronNumber": 1, "hasMaxValue": "_NaN_", "hasMeanValue": "_NaN_", "hasMedianValue": "_NaN_", "hasMinValue": "_NaN_", "paleoName": "chron1", "number": 7, "values": ["NA", "NA", "NA", "NA", "NA", "NA", "NA", "NA"] }, "thickness": { "chronMeasMD5": "fc82720bd513525adf678411f4452547", "measurementTableName": "measurementTable1", "TSid": "chron8", "variableName": "thickness", "description": "thickness of sample (along depth axis)", "units": "cm", "chronName": "chron1", "chronMeasurementTableMD5": "fc82720bd513525adf678411f4452547", "chronMeasurementTableNumber": 1, "chronNumber": 1, "hasMaxValue": "_NaN_", "hasMeanValue": "_NaN_", "hasMedianValue": "_NaN_", "hasMinValue": "_NaN_", "paleoName": "chron1", "number": 8, "values": ["NA", "NA", "NA", "NA", "NA", "NA", "NA", "NA"] }, "labID": { "chronMeasMD5": "fc82720bd513525adf678411f4452547", "measurementTableName": "measurementTable1", "TSid": "chron9", "variableName": "labID", "description": "laboratory ID from radiocarbon facility", "chronName": "chron1", "chronMeasurementTableMD5": "fc82720bd513525adf678411f4452547", "chronMeasurementTableNumber": 1, "chronNumber": 1, "hasMaxValue": "_NaN_", "hasMeanValue": "_NaN_", "hasMedianValue": "_NaN_", "hasMinValue": "_NaN_", "paleoName": "chron1", "units": "unitless", "number": 9, "values": ["NA", "NA", "NA", "NA", "NA", "NA", "NA", "NA"] }, "materialDated": { "chronMeasMD5": "fc82720bd513525adf678411f4452547", "measurementTableName": "measurementTable1", "TSid": "chron10", "variableName": "materialDated", "description": "material analyzed", "chronName": "chron1", "chronMeasurementTableMD5": "fc82720bd513525adf678411f4452547", "chronMeasurementTableNumber": 1, "chronNumber": 1, "hasMaxValue": "_NaN_", "hasMeanValue": "_NaN_", "hasMedianValue": "_NaN_", "hasMinValue": "_NaN_", "paleoName": "chron1", "units": "unitless", "number": 10, "values": ["NA", "NA", "NA", "NA", "NA", "NA", "NA", "NA"] }, "activity": { "chronMeasMD5": "fc82720bd513525adf678411f4452547", "measurementTableName": "measurementTable1", "TSid": "chron11", "variableName": "activity", "description": "210Pb, 239+240Pu or 137Cs activity", "units": "Bq g-1", "chronName": "chron1", "chronMeasurementTableMD5": "fc82720bd513525adf678411f4452547", "chronMeasurementTableNumber": 1, "chronNumber": 1, "hasMaxValue": "_NaN_", "hasMeanValue": "_NaN_", "hasMedianValue": "_NaN_", "hasMinValue": "_NaN_", "paleoName": "chron1", "number": 11, "values": ["NA", "NA", "NA", "NA", "NA", "NA", "NA", "NA"] }, "activityUncertainty": { "chronMeasMD5": "fc82720bd513525adf678411f4452547", "measurementTableName": "measurementTable1", "TSid": "chron12", "variableName": "activityUncertainty", "description": "210Pb, 239+240Pu or 137Cs activity uncertainty", "units": "Bq g-1", "chronName": "chron1", "chronMeasurementTableMD5": "fc82720bd513525adf678411f4452547", "chronMeasurementTableNumber": 1, "chronNumber": 1, "hasMaxValue": "_NaN_", "hasMeanValue": "_NaN_", "hasMedianValue": "_NaN_", "hasMinValue": "_NaN_", "paleoName": "chron1", "number": 12, "values": ["NA", "NA", "NA", "NA", "NA", "NA", "NA", "NA"] }, "supportedActivity": { "chronMeasMD5": "fc82720bd513525adf678411f4452547", "measurementTableName": "measurementTable1", "TSid": "chron13", "variableName": "supportedActivity", "description": "Y if supported 210Pb activity, N if unsupported 210Pb activity", "chronName": "chron1", "chronMeasurementTableMD5": "fc82720bd513525adf678411f4452547", "chronMeasurementTableNumber": 1, "chronNumber": 1, "hasMaxValue": "_NaN_", "hasMeanValue": "_NaN_", "hasMedianValue": "_NaN_", "hasMinValue": "_NaN_", "paleoName": "chron1", "units": "unitless", "number": 13, "values": ["NA", "NA", "NA", "NA", "NA", "NA", "NA", "NA"] }, "x210PbModel": { "chronMeasMD5": "fc82720bd513525adf678411f4452547", "measurementTableName": "measurementTable1", "TSid": "chron14", "variableName": "x210PbModel", "description": "model used to convert 210Pb activity to age (e.g., constant rate of supply)", "chronName": "chron1", "chronMeasurementTableMD5": "fc82720bd513525adf678411f4452547", "chronMeasurementTableNumber": 1, "chronNumber": 1, "hasMaxValue": "_NaN_", "hasMeanValue": "_NaN_", "hasMedianValue": "_NaN_", "hasMinValue": "_NaN_", "paleoName": "chron1", "units": "unitless", "number": 14, "values": ["NA", "NA", "NA", "NA", "NA", "NA", "NA", "NA"] }, "age": { "chronMeasMD5": "fc82720bd513525adf678411f4452547", "measurementTableName": "measurementTable1", "TSid": "chron15", "variableName": "age", "description": "years before 1950 (calibrated age, or ages that dont need calibration)", "units": "yr BP", "chronName": "chron1", "chronMeasurementTableMD5": "fc82720bd513525adf678411f4452547", "chronMeasurementTableNumber": 1, "chronNumber": 1, "hasMaxValue": "_NaN_", "hasMeanValue": "_NaN_", "hasMedianValue": "_NaN_", "hasMinValue": "_NaN_", "paleoName": "chron1", "number": 15, "values": ["NA", "NA", "NA", "NA", "NA", "NA", "NA", "NA"] }, "SD-1": { "chronMeasMD5": "fc82720bd513525adf678411f4452547", "measurementTableName": "measurementTable1", "TSid": "chron16", "variableName": "SD", "description": "uncertainty in age", "units": "yr BP", "chronName": "chron1", "chronMeasurementTableMD5": "fc82720bd513525adf678411f4452547", "chronMeasurementTableNumber": 1, "chronNumber": 1, "hasMaxValue": "_NaN_", "hasMeanValue": "_NaN_", "hasMedianValue": "_NaN_", "hasMinValue": "_NaN_", "paleoName": "chron1", "variableNameOriginal": "ageUncertainty", "number": 16, "values": ["NA", "NA", "NA", "NA", "NA", "NA", "NA", "NA"] }, "reservoirAge14C": { "chronMeasMD5": "fc82720bd513525adf678411f4452547", "measurementTableName": "measurementTable1", "TSid": "chron17", "variableName": "reservoirAge14C", "description": "14C reservoir age", "units": "yr14C BP", "chronName": "chron1", "chronMeasurementTableMD5": "fc82720bd513525adf678411f4452547", "chronMeasurementTableNumber": 1, "chronNumber": 1, "hasMaxValue": "_NaN_", "hasMeanValue": "_NaN_", "hasMedianValue": "_NaN_", "hasMinValue": "_NaN_", "paleoName": "chron1", "number": 17, "values": ["NA", "NA", "NA", "NA", "NA", "NA", "NA", "NA"] }, "reservoirAge14CUncertainty": { "chronMeasMD5": "fc82720bd513525adf678411f4452547", "measurementTableName": "measurementTable1", "TSid": "chron18", "variableName": "reservoirAge14CUncertainty", "description": "14C reservoir age uncertainty", "units": "yr14C BP", "chronName": "chron1", "chronMeasurementTableMD5": "fc82720bd513525adf678411f4452547", "chronMeasurementTableNumber": 1, "chronNumber": 1, "hasMaxValue": "_NaN_", "hasMeanValue": "_NaN_", "hasMedianValue": "_NaN_", "hasMinValue": "_NaN_", "paleoName": "chron1", "number": 18, "values": ["NA", "NA", "NA", "NA", "NA", "NA", "NA", "NA"] }, "useInAgeModel": { "chronMeasMD5": "fc82720bd513525adf678411f4452547", "measurementTableName": "measurementTable1", "TSid": "chron19", "variableName": "useInAgeModel", "description": "was this date used in the age model?", "chronName": "chron1", "chronMeasurementTableMD5": "fc82720bd513525adf678411f4452547", "chronMeasurementTableNumber": 1, "chronNumber": 1, "hasMaxValue": "_NaN_", "hasMeanValue": "_NaN_", "hasMedianValue": "_NaN_", "hasMinValue": "_NaN_", "paleoName": "chron1", "units": "unitless", "number": 19, "values": ["NA", "NA", "NA", "NA", "NA", "NA", "NA", "NA"] } } ] } ], "Notes": "Constrained by 11 14C dates + correlated tephra deposits", "archiveType": "LakeSediment", "createdBy": "matlab", "dataSetName": "LS10ANBL", "googleMetadataWorksheet": "ouzm6nr", "googleSpreadSheetKey": "1OXwEpk43s2hW8jL5zCUGecbgArJM5TZwEdF8d3gCOAQ", "hasPaleoDepth": 0, "samplingMethod": "Samples collected from core", "tagMD5": "f8206d04ff6336d52609302f1d325212", "lipdverseLink": "https://lipdverse.org/data/4vITsrnIhvLaeqiYcqko/1_0_12", "nUniqueAges": 0, "archiveTypeOriginal": "lake sediment", "maxYear": 4385.5066, "minYear": -60, "nUniqueOtherAges": 0, "nUniqueGoodAges": 0, "hasDepth": 0, "hasChron": "0", "originalDataUrl": "https://doi.org/10.5194/essd-12-2261-2020", "datasetId": "4vITsrnIhvLaeqiYcqko", "agesPerKyr": 0, "otherAgesPerKyr": "0", "lipdComplete": "100%", "lipdVersion": 1.3, "datasetVersion": "1.0.12", "changelog": [ { "version": "1.0.12", "lastVersion": "1.0.11", "curator": "nicholas", "timestamp": "2023-05-25 17:49:23 UTC", "notes": "Updated lipdverse database entry with a changed file.", "changes": { "Geographic metadata": [ ["geo_elevation: '' has been replaced by '330'"] ] } }, { "version": "1.0.11", "lastVersion": "1.0.10", "curator": "nicholas", "timestamp": "2023-05-12 22:03:25 UTC", "changes": { "Paleo Column metadata": [ ["d18O (LS10ANBL01a): paleoData_notes: '((( \"Overall, the Lake Blektjaernen isotope record shows similar ��18O and ��13C trends (Figs 3 and 7). We argue that this is because increased evaporation and enhanced vapour exchange led to preferential loss of lighter isotopes, which resulted in elevated values of ��18O and ��13C during periods with relatively drier climate (Talbot, 1990; Li and Ku, 1997). The correlation coefficient for covariance is large (r2���=���0.54) between ��18O and ��13C values in Chara, indicating that past changes in the isotopic composition of Lake Blektjaernen in the summer is controlled to a large degree by variation in the E/I ratio. If so, more negative ��18O and ��13C values would imply more humid conditions...Our results show the potential of using lacustrine stable isotope data to reconstruct past changes in humidity during summer (Chara) \" ))) \"Overall, the Lake Blektjaernen isotope record shows similar δ18O and δ13C trends (Figs 3 and 7). We argue that this is because increased evaporation and enhanced vapour exchange led to preferential loss of lighter isotopes, which resulted in elevated values of δ18O and δ13C during periods with relatively drier climate (Talbot, 1990; Li and Ku, 1997). The correlation coefficient for covariance is large (r2 = 0.54) between δ18O and δ13C values in Chara, indicating that past changes in the isotopic composition of Lake Blektjaernen in the summer is controlled to a large degree by variation in the E/I ratio. If so, more negative δ18O and δ13C values would imply more humid conditions...Our results show the potential of using lacustrine stable isotope data to reconstruct past changes in humidity during summer (Chara) \" /// \"Overall, the Lake Blektjaernen isotope record shows similar δ18O and δ13C trends (Figs 3 and 7). We argue that this is because increased evaporation and enhanced vapour exchange led to preferential loss of lighter isotopes, which resulted in elevated values of δ18O and δ13C during periods with relatively drier climate (Talbot, 1990; Li and Ku, 1997). The correlation coefficient for covariance is large (r2 = 0.54) between δ18O and δ13C values in Chara, indicating that past changes in the isotopic composition of Lake Blektjaernen in the summer is controlled to a large degree by variation in the E/I ratio. If so, more negative δ18O and δ13C values would imply more humid conditions...Our results show the potential of using lacustrine stable isotope data to reconstruct past changes in humidity during summer (Chara) \"' has been replaced by '\"Overall, the Lake Blektjaernen isotope record shows similar δ18O and δ13C trends (Figs 3 and 7). We argue that this is because increased evaporation and enhanced vapour exchange led to preferential loss of lighter isotopes, which resulted in elevated values of δ18O and δ13C during periods with relatively drier climate (Talbot, 1990; Li and Ku, 1997). The correlation coefficient for covariance is large (r2 = 0.54) between δ18O and δ13C values in Chara, indicating that past changes in the isotopic composition of Lake Blektjaernen in the summer is controlled to a large degree by variation in the E/I ratio. If so, more negative δ18O and δ13C values would imply more humid conditions...Our results show the potential of using lacustrine stable isotope data to reconstruct past changes in humidity during summer (Chara) \"'"] ] } }, { "version": "1.0.10", "lastVersion": "1.0.9", "curator": "nicholas", "timestamp": "2023-03-29 19:56:03 UTC", "changes": { "Paleo Interpretation metadata": [ ["d18O (LS10ANBL01a): interpretation1_variable: 'P-E' has been replaced by 'effectivePrecipitation'"] ] } }, { "version": "1.0.9", "lastVersion": "1.0.8", "curator": "nicholas", "timestamp": "2023-02-13 23:50:37 UTC", "changes": { "Paleo Column metadata": [ ["d18O (LS10ANBL01a): paleoData_notes: '\"Overall, the Lake Blektjaernen isotope record shows similar δ18O and δ13C trends (Figs 3 and 7). We argue that this is because increased evaporation and enhanced vapour exchange led to preferential loss of lighter isotopes, which resulted in elevated values of δ18O and δ13C during periods with relatively drier climate (Talbot, 1990; Li and Ku, 1997). The correlation coefficient for covariance is large (r2 = 0.54) between δ18O and δ13C values in Chara, indicating that past changes in the isotopic composition of Lake Blektjaernen in the summer is controlled to a large degree by variation in the E/I ratio. If so, more negative δ18O and δ13C values would imply more humid conditions...Our results show the potential of using lacustrine stable isotope data to reconstruct past changes in humidity during summer (Chara) \"' has been replaced by '((( \"Overall, the Lake Blektjaernen isotope record shows similar ��18O and ��13C trends (Figs 3 and 7). We argue that this is because increased evaporation and enhanced vapour exchange led to preferential loss of lighter isotopes, which resulted in elevated values of ��18O and ��13C during periods with relatively drier climate (Talbot, 1990; Li and Ku, 1997). The correlation coefficient for covariance is large (r2���=���0.54) between ��18O and ��13C values in Chara, indicating that past changes in the isotopic composition of Lake Blektjaernen in the summer is controlled to a large degree by variation in the E/I ratio. If so, more negative ��18O and ��13C values would imply more humid conditions...Our results show the potential of using lacustrine stable isotope data to reconstruct past changes in humidity during summer (Chara) \" ))) \"Overall, the Lake Blektjaernen isotope record shows similar δ18O and δ13C trends (Figs 3 and 7). We argue that this is because increased evaporation and enhanced vapour exchange led to preferential loss of lighter isotopes, which resulted in elevated values of δ18O and δ13C during periods with relatively drier climate (Talbot, 1990; Li and Ku, 1997). The correlation coefficient for covariance is large (r2 = 0.54) between δ18O and δ13C values in Chara, indicating that past changes in the isotopic composition of Lake Blektjaernen in the summer is controlled to a large degree by variation in the E/I ratio. If so, more negative δ18O and δ13C values would imply more humid conditions...Our results show the potential of using lacustrine stable isotope data to reconstruct past changes in humidity during summer (Chara) \" /// \"Overall, the Lake Blektjaernen isotope record shows similar δ18O and δ13C trends (Figs 3 and 7). We argue that this is because increased evaporation and enhanced vapour exchange led to preferential loss of lighter isotopes, which resulted in elevated values of δ18O and δ13C during periods with relatively drier climate (Talbot, 1990; Li and Ku, 1997). The correlation coefficient for covariance is large (r2 = 0.54) between δ18O and δ13C values in Chara, indicating that past changes in the isotopic composition of Lake Blektjaernen in the summer is controlled to a large degree by variation in the E/I ratio. If so, more negative δ18O and δ13C values would imply more humid conditions...Our results show the potential of using lacustrine stable isotope data to reconstruct past changes in humidity during summer (Chara) \"'"] ] } }, { "version": "1.0.8", "lastVersion": "1.0.7", "curator": "nicholas", "timestamp": "2023-02-09 15:58:13 UTC", "notes": "Updated lipdverse database entry with a changed file.", "changes": { "Paleo Interpretation metadata": [ ["d18O (LS10ANBL01a): interpretation1_seasonality: '6,7,8' has been replaced by 'Jun-Aug'"], ["d18O (LS10ANBL01a): interpretation2_variable: 'I_E' has been replaced by 'hydrologicBalance'"], ["d18O (LS10ANBL01a): interpretation3_variable: 'T_air' has been replaced by 'temperature'"] ], "Paleo Column metadata": [ ["year (MAT423a41a367): paleoData_notes: '' has been replaced by 'NA; paleoData_isPrimary has been standardized'"], ["year (MAT423a41a367): paleoData_units: 'AD' has been replaced by 'yr AD'"], ["year (MAT423a41a367): paleoData_isPrimary: '' has been replaced by 'TRUE'"], ["age (WEB028eebbb): paleoData_datum: '' has been replaced by '1950'"], ["age (WEB028eebbb): paleoData_notes: '' has been replaced by 'NA; paleoData_isPrimary has been standardized; paleoData_datum has been standardized'"], ["age (WEB028eebbb): paleoData_units: 'BP' has been replaced by 'yr BP'"], ["age (WEB028eebbb): paleoData_isPrimary: '' has been replaced by 'TRUE'"] ] } }, { "version": "1.0.7", "lastVersion": "1.0.6", "curator": "nicholas", "timestamp": "2022-09-21 01:24:54 UTC", "changes": { "Publication metadata": [ ["pub1_volume: '25' has been replaced by ''"] ] } }, { "version": "1.0.6", "lastVersion": "1.0.5", "curator": "nicholas", "timestamp": "2022-07-28 17:36:37 UTC", "changes": { "Base metadata": [ ["originalDataUrl: 'https://essd.copernicus.org/articles/12/2261/2020/' has been replaced by 'https://doi.org/10.5194/essd-12-2261-2020'"] ], "Geographic metadata": [ ["geo_elevation: '330' has been replaced by ''"] ] } }, { "version": "1.0.5", "lastVersion": "1.0.4", "curator": "nicholas", "timestamp": "2022-05-18 00:27:42 UTC", "changes": { "Paleo Interpretation metadata": [ ["d18O (LS10ANBL01a): interpretation1_variableGroup: 'Precipitation amount (as a function of temperature)' has been replaced by 'P-E'"] ], "Paleo Column metadata": [ ["d18O (LS10ANBL01a): paleoData_proxyLumps: '' has been replaced by 'isotope'"], ["d18O (LS10ANBL01a): paleoData_proxyLumpsOriginal: '' has been replaced by 'd18O'"], ["age (WEB028eebbb): paleoData_units: 'yr BP' has been replaced by 'BP'"], ["age (WEB028eebbb): paleoData_unitsOriginal: '' has been replaced by 'yr BP'"] ] } }, { "version": "1.0.4", "lastVersion": "1.0.3", "curator": "nicholas", "timestamp": "2022-05-16 23:09:08 UTC", "changes": { "Paleo Column metadata": [ ["d18O (LS10ANBL01a): paleoData_datum: '' has been replaced by 'VSMOW'"] ] } }, { "version": "1.0.3", "lastVersion": "1.0.2", "curator": "nicholas", "timestamp": "2021-11-17 02:08:10 UTC", "changes": { "Paleo Interpretation metadata": [ ["d18O (LS10ANBL01a): interpretation1_seasonalityGeneral: 'SummerOnly' has been replaced by 'summerOnly'"], ["d18O (LS10ANBL01a): interpretation1_variable: 'I-E' has been replaced by 'P-E'"] ] } }, { "version": "1.0.2", "lastVersion": "1.0.1", "curator": "nicholas", "timestamp": "2021-10-05 21:40:59 UTC", "changes": { "Base metadata": [ ["originalDataUrl: 'this compilation' has been replaced by 'https://essd.copernicus.org/articles/12/2261/2020/'"] ], "Geographic metadata": [ ["geo_gcmdLocation: '' has been replaced by 'Europe>Northern Europe>Scandinavia>Sweden'"] ], "Paleo Column metadata": [ ["d18O (LS10ANBL01a): paleoData_notes: '; archiveType changed - was originally Lake sediment (LS)' has been replaced by '\"Overall, the Lake Blektjaernen isotope record shows similar δ18O and δ13C trends (Figs 3 and 7). We argue that this is because increased evaporation and enhanced vapour exchange led to preferential loss of lighter isotopes, which resulted in elevated values of δ18O and δ13C during periods with relatively drier climate (Talbot, 1990; Li and Ku, 1997). The correlation coefficient for covariance is large (r2 = 0.54) between δ18O and δ13C values in Chara, indicating that past changes in the isotopic composition of Lake Blektjaernen in the summer is controlled to a large degree by variation in the E/I ratio. If so, more negative δ18O and δ13C values would imply more humid conditions...Our results show the potential of using lacustrine stable isotope data to reconstruct past changes in humidity during summer (Chara) \"'"], ["d18O (LS10ANBL01a): paleoData_proxy: '' has been replaced by 'd18O'"], ["d18O (LS10ANBL01a): paleoData_QCCertification: 'MJ' has been replaced by 'MJ, CH'"], ["d18O (LS10ANBL01a): paleoData_proxyDetail: '' has been replaced by 'Chara'"], ["d18O (LS10ANBL01a): paleoData_proxyGeneral: '' has been replaced by 'isotope'"] ], "Paleo Interpretation metadata": [ ["d18O (LS10ANBL01a): interpretation1_direction: 'decrease' has been replaced by 'negative'"], ["d18O (LS10ANBL01a): interpretation1_variable: 'Precipitation amount (as a function of temperature)' has been replaced by 'I-E'"], ["d18O (LS10ANBL01a): interpretation1_variableDetail: 'Continental Sweden' has been replaced by 'lakebalance@surface'"], ["d18O (LS10ANBL01a): interpretation1_seasonality: '' has been replaced by '6,7,8'"], ["d18O (LS10ANBL01a): interpretation1_seasonalityGeneral: '' has been replaced by 'SummerOnly'"] ] } }, { "version": "1.0.1", "lastVersion": "1.0.0", "curator": "nick", "timestamp": "2021-06-08 03:08:49 UTC", "notes": "Updated lipdverse database entry with a changed file.", "changes": { "PaleoData table": [ ["Column 'WEB028eebbb', with variable name 'age', was added to the dataset"] ], "Chron Column metadata": [ ["materialDated (chron10): chronData_units: '' has been replaced by 'unitless'"], ["supportedActivity (chron13): chronData_units: '' has been replaced by 'unitless'"], ["x210PbModel (chron14): chronData_units: '' has been replaced by 'unitless'"], ["useInAgeModel (chron19): chronData_units: '' has been replaced by 'unitless'"], ["fractionModern (chron4): chronData_units: '' has been replaced by 'unitless'"], ["fractionModernUncertainty (chron5): chronData_units: '' has been replaced by 'unitless'"], ["labID (chron9): chronData_units: '' has been replaced by 'unitless'"] ] } }, { "version": "1.0.0", "curator": "nick", "timestamp": "2021-04-12 22:52:00 UTC", "notes": "Added to lipdverse database." } ], "neotomaDatasetId": null, "pub": [ { "author": [ { "name": "Andersson, Sofia , Rosqvist, Gunhild , leng, Melanie j. , Wastegi¿½rd, Stefan , Blaauw, Maarten" } ], "dataUrl": "doi.org", "issue": "8", "journal": "J. Quaternary Sci.", "page": "1305-1316", "pages": "-11", "pubDataUrl": "doi.org", "publisher": "Wiley-Blackwell", "title": "Late Holocene climate change in central Sweden inferred from lacustrine stable isotope data", "type": "journal-article", "doi": "10.1002/jqs.1415", "year": 2010, "citation": "Andersson, S., Rosqvist, G., leng, M. j., Wastegard, S. and Blaauw, M.: Late Holocene climate change in central Sweden inferred from lacustrine stable isotope data, Journal of Quaternary Science, 25(8), 1305–1316, doi:10.1002/jqs.1415, 2010.", "volume": null } ], "geo": { "longitude": 14.65, "latitude": 62, "elevation": 330, "geometryType": "Point", "siteName": "Lake Blektjarnen", "gcmdLocation": "Europe>Northern Europe>Scandinavia>Sweden" }, "@context": "context.jsonld" }