{ "paleoData": [ { "measurementTable": [ { "googleWorkSheetKey": "ohpo27p", "tableName": "paleo1measurement1", "missingValue": "NaN", "d18O": { "chronologyIntegrationTime": "43607", "chronologyIntegrationTimeUnits": "years", "description": "carbonate", "equilibriumEvidence": "Three Hendy tests were carried out, i.e. at 10mm (AD 70), 20mm (837 BC) and 33mm (1453 BC), based on 7, 7 and 5 samples, respectively. The variations of d18O along individual growth layers, expressed in I”d18O, are 0.31, 0.74 and 0.18%, respectively. The correlation between oxygen and carbon in one of the three layers, at 200 mm, is high, R=0.9 (P<0.01) indicating that kinetic effects may have occurred. The other two test did not show fractionation.", "hasChron": "1", "hasMaxValue": "-8.2256", "hasMeanValue": "-9.286", "hasMedianValue": "-9.2719", "hasMinValue": "-10.3901", "hasPaleoDepth": "0", "inferredMaterial": "groundwater", "inferredMaterialGroup": "soil water", "inferredMaterialGroupOriginal": "groundwater", "instrument": "on-line, automated carbonate preparation system linked to a triple collector gas source mass spectrometer at the University of Innsbruck.", "iso2kCertification": "ZK", "iso2kHackathonNotes": "BD missing", "iso2kPrimaryTimeseries": "TRUE", "iso2kUI": "SP10SUSE01A", "longName": "AD", "measurementMaterial": "carbonate", "measurementMaterialDetail": "calcite", "measurementStandard": "not said", "measurementTableMD5": "5e2f58fe93972e9f61e66ec089f08f53", "measurementTableName": "measurementTable1", "medianRes12k": "NA", "notes": "; archiveType changed - was originally Speleothem (SP)", "paleoDataTableName": "pt1_1", "paleoMeasurementTableMD5": 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less winter contribution to the cave drip water will result in relatively higher d18O values and vice versa. Depleted/enriched oxygen isotopesisotopes are interpreted mainly to indicate relatively more/less winter precipitation and higher/lower summer evaporation reflecting warmer/colder conditions.", "coefficient": "NA", "direction": "negative", "equilibriumEvidence": "Three Hendy tests were carried out, i.e. at 10mm (AD 70), 20mm (837 BC) and 33mm (1453 BC), based on 7, 7 and 5 samples, respectively. The variations of d18O along individual growth layers, expressed in Δd18O, are 0.31, 0.74 and 0.18%, respectively. The correlation between oxygen and carbon in one of the three layers, at 200 mm, is high, R=0.9 (P<0.01) indicating that kinetic effects may have occurred. 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'climate'"], ["depth (MAT71379e2f3f): interpretation3_scope: '' has been replaced by 'climate'"], ["d18O (SP10SUSE01A): interpretation2_basis: 'During cold climate periods, relatively less winter contribution to the cave drip water will result in relatively higher d18O values and vice versa. Depleted/enriched oxygen isotopesisotopes are interpreted mainly to indicate relatively more/less winter precipitation and higher/lower summer evaporation reflecting warmer/colder conditions.' has been replaced by ''"], ["d18O (SP10SUSE01A): interpretation2_direction: 'negative' has been replaced by ''"], ["d18O (SP10SUSE01A): interpretation2_equilibriumEvidence: 'Three Hendy tests were carried out, i.e. at 10mm (AD 70), 20mm (837 BC) and 33mm (1453 BC), based on 7, 7 and 5 samples, respectively. The variations of d18O along individual growth layers, expressed in Δd18O, are 0.31, 0.74 and 0.18%, respectively. The correlation between oxygen and carbon in one of the three layers, at 200 mm, is high, R=0.9 (P<0.01) indicating that kinetic effects may have occurred. The other two test did not show fractionation.' has been replaced by ''"], ["d18O (SP10SUSE01A): interpretation2_inferredMaterial: 'groundwater d18O' has been replaced by ''"], ["d18O (SP10SUSE01A): interpretation2_integrationTimeUncertainty: 'average time resolution from 22 years at the top to 5 years at the base.' has been replaced by ''"], ["d18O (SP10SUSE01A): interpretation2_integrationTimeUnits: 'year' has been replaced by ''"], ["d18O (SP10SUSE01A): interpretation2_rank: '1' has been replaced by ''"], ["d18O (SP10SUSE01A): interpretation2_scope: 'isotope' has been replaced by 'climate'"], ["d18O (SP10SUSE01A): interpretation2_variable: 'temperature' has been replaced by ''"], ["d18O (SP10SUSE01A): interpretation2_variableGroup: 'Temperature' has been replaced by ''"], ["d18O (SP10SUSE01A): interpretation2_variableGroupDirection: 'negative' has been replaced by ''"], ["d18O (SP10SUSE01A): interpretation2_variableGroupOriginal: 'T_air' has been replaced by ''"], ["d18O (SP10SUSE01A): interpretation3_rank: '2' has been replaced by ''"], ["d18O (SP10SUSE01A): interpretation3_scope: 'isotope' has been replaced by 'climate'"], ["d18O (SP10SUSE01A): interpretation4_rank: '' has been replaced by '1'"], ["d18O (SP10SUSE01A): interpretation4_basis: '' has been replaced by 'During cold climate periods, relatively less winter contribution to the cave drip water will result in relatively higher d18O values and vice versa. Depleted/enriched oxygen isotopesisotopes are interpreted mainly to indicate relatively more/less winter precipitation and higher/lower summer evaporation reflecting warmer/colder conditions.'"], ["d18O (SP10SUSE01A): interpretation4_direction: '' has been replaced by 'negative'"], ["d18O (SP10SUSE01A): interpretation4_equilibriumEvidence: '' has been replaced by 'Three Hendy tests were carried out, i.e. at 10mm (AD 70), 20mm (837 BC) and 33mm (1453 BC), based on 7, 7 and 5 samples, respectively. The variations of d18O along individual growth layers, expressed in Δd18O, are 0.31, 0.74 and 0.18%, respectively. The correlation between oxygen and carbon in one of the three layers, at 200 mm, is high, R=0.9 (P<0.01) indicating that kinetic effects may have occurred. The other two test did not show fractionation.'"], ["d18O (SP10SUSE01A): interpretation4_inferredMaterial: '' has been replaced by 'groundwater d18O'"], ["d18O (SP10SUSE01A): interpretation4_integrationTimeUncertainty: '' has been replaced by 'average time resolution from 22 years at the top to 5 years at the base.'"], ["d18O (SP10SUSE01A): interpretation4_integrationTimeUnits: '' has been replaced by 'year'"], ["d18O (SP10SUSE01A): interpretation4_variable: '' has been replaced by 'temperature'"], ["d18O (SP10SUSE01A): interpretation4_variableGroup: '' has been replaced by 'Temperature'"], ["d18O (SP10SUSE01A): interpretation4_variableGroupDirection: '' has been replaced by 'negative'"], ["d18O (SP10SUSE01A): interpretation4_variableGroupOriginal: '' has been replaced by 'T_air'"], ["d18O (SP10SUSE01A): interpretation5_rank: '' has been replaced by '2'"], ["d18O (SP10SUSE01A): interpretation5_scope: '' has been replaced by 'isotope'"], ["d18O (SP10SUSE01A): interpretation6_scope: '' has been replaced by 'isotope'"] ] } }, { "version": "1.0.4", "lastVersion": "1.0.3", "curator": "nicholas", "timestamp": "2025-04-09 21:54:29.997216 UTC", "notes": "Updated lipdverse database entry with a changed file.", "changes": { "Paleo Interpretation metadata": [ ["d18O (SP10SUSE01A): interpretation1_seasonality: 'annual' has been replaced by 'Annual'"], ["d18O (SP10SUSE01A): interpretation1_variable: 'Temperature_air' has been replaced by 'temperature'"], ["d18O (SP10SUSE01A): interpretation2_variable: 'T_air' has been replaced by 'temperature'"] ] } }, { "version": "1.0.3", "lastVersion": "1.0.2", "curator": "nicholas", "timestamp": "2025-04-09 20:22:14.378262 UTC", "notes": "Changes made as part of LiPDverse vocabulary standardization process", "changes": { "Paleo Interpretation metadata": [ ["d18O (SP10SUSE01A): interpretation1_seasonality: 'annual' has been replaced by 'Annual'"], ["d18O (SP10SUSE01A): interpretation1_variable: 'Temperature_air' has been replaced by 'temperature'"], ["d18O (SP10SUSE01A): interpretation2_variable: 'T_air' has been replaced by 'temperature'"] ] } }, { "version": "1.0.2", "lastVersion": "1.0.1", "curator": "nicholas", "timestamp": "2025-04-08 17:34:51.265677 UTC", "notes": "Changes made as part of LiPDverse vocabulary standardization process", "changes": { "Paleo Column metadata": [ ["year (MAT4dbbaa0d95): paleoData_units: 'AD' has been replaced by 'yr AD'"], ["year (MAT4dbbaa0d95): paleoData_longName: '' has been replaced by 'AD'"], ["depth (MAT71379e2f3f): paleoData_longName: '' has been replaced by 'AD'"], ["d18O (SP10SUSE01A): paleoData_longName: '' has been replaced by 'AD'"] ] } }, { "version": "1.0.1", "lastVersion": "1.0.0", "curator": "nicholas", "timestamp": "2022-08-16 23:29:43 UTC", "changes": { "Paleo Interpretation metadata": [ ["d18O (SP10SUSE01A): interpretation4_scope: '' has been replaced by 'isotope'"] ] } } ], "environmentInterpretation1_direction": null, "environmentInterpretation1_seasonality": null, "environmentInterpretation1_variable": null, "testField": null, "pub": [ { "author": { "name": "Sundqvist, HS" }, "citation": "SUNDQVIST, H. S., HOLMGREN, K., MOBERG, A., SPA–TL, C. and MANGINI, A.: Stable isotopes in a stalagmite from NW Sweden document environmental changes over the past 4000 years, Boreas, 39(1), 77–86, doi:10.1111/j.1502-3885.2009.00099.x, 2010.", "dataUrl": "https://www.ncdc.noaa.gov/cdo/f?p=519:1:::::P1_STUDY_ID:9745", "doi": "10.1111/j.1502-3885.2009.00099.x", "year": 2010 } ], "geo": { "longitude": 14.16, "latitude": 64.89, "elevation": 570, "geometryType": "Point", "siteName": "Korallgrottan, Sweden" }, "@context": "context.jsonld" }