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enriched the δ13C and the δ18O of the calcite, the wetter the climate...δ18O and δ13C variations, as observed on the present day calcite, are mainly controlled by the isotopic equilibrium state during precipitation of the calcite, which depends on the drip rate, and consequently, through recharge, on the rainfall amount to\" (Verheyden et al., 2008)", "proxy": "d13C", "QCCertification": "CH", "meanValue12k": -7.292, "medianRes12k": 65.7647, "proxyDetail": "calcite", "proxyGeneral": "isotope", "proxyLumps": "isotope", "proxyLumpsOriginal": "d13C", "meetsHoloceneHydroclimateCriteria": "TRUE", "primaryTimeseries": "TRUE", "values": [-3.199, -2.561, -3.974, -4.593, -5.598, -5.56, -5.288, -8.7675, -8.565, -8.698, -8.546, -8.646, -3.2895, -5.935, -8.53, -7.644, -3.4255, -4.952, -8.065, -4.47, -7.432, -7.168, -8.105, -8.35, -7.361, -8.304, -8.499, -8.991, -7.289, -5.852, -5.584, -6.726, -8.793, -8.588, -7.429, -6.5805, -8.265, -8.113, -7.901, -8.363, -9.459, -9.338, -5.1355, -7.798, -6.71, 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["uncertaintyLow (S2LRfpQK1AtSwB): interpretation3_scope: '' has been replaced by 'climate'"], ["uncertaintyLow (S2LRfpQK1AtSwB): interpretation4_scope: '' has been replaced by 'isotope'"], ["uncertaintyLow (S2LRfpQK1AtSwB): interpretation5_scope: '' has been replaced by 'isotope'"], ["uncertaintyLow (S2LRfpQK1AtSwB): interpretation6_scope: '' has been replaced by 'isotope'"], ["sampleID (S2LRgSlbbJADra): interpretation2_scope: '' has been replaced by 'climate'"], ["sampleID (S2LRgSlbbJADra): interpretation3_scope: '' has been replaced by 'climate'"], ["sampleID (S2LRgSlbbJADra): interpretation4_scope: '' has been replaced by 'isotope'"], ["sampleID (S2LRgSlbbJADra): interpretation5_scope: '' has been replaced by 'isotope'"], ["sampleID (S2LRgSlbbJADra): interpretation6_scope: '' has been replaced by 'isotope'"], ["uncertainty (S2LRip5obuHZID): interpretation2_scope: '' has been replaced by 'climate'"], ["uncertainty (S2LRip5obuHZID): interpretation3_scope: '' has been replaced by 'climate'"], ["uncertainty (S2LRip5obuHZID): interpretation4_scope: '' has been replaced by 'isotope'"], ["uncertainty (S2LRip5obuHZID): interpretation5_scope: '' has been replaced by 'isotope'"], ["uncertainty (S2LRip5obuHZID): interpretation6_scope: '' has been replaced by 'isotope'"], ["uncertaintyHigh (S2LRpq55DUa0Qf): interpretation2_scope: '' has been replaced by 'climate'"], ["uncertaintyHigh (S2LRpq55DUa0Qf): interpretation3_scope: '' has been replaced by 'climate'"], ["uncertaintyHigh (S2LRpq55DUa0Qf): interpretation4_scope: '' has been replaced by 'isotope'"], ["uncertaintyHigh (S2LRpq55DUa0Qf): interpretation5_scope: '' has been replaced by 'isotope'"], ["uncertaintyHigh (S2LRpq55DUa0Qf): interpretation6_scope: '' has been replaced by 'isotope'"], ["uncertaintyLow (S2LRtRoiaRzyp8): interpretation2_scope: '' has been replaced by 'climate'"], ["uncertaintyLow (S2LRtRoiaRzyp8): interpretation3_scope: '' has been replaced by 'climate'"], ["uncertaintyLow (S2LRtRoiaRzyp8): interpretation4_scope: '' has been replaced by 'isotope'"], ["uncertaintyLow (S2LRtRoiaRzyp8): interpretation5_scope: '' has been replaced by 'isotope'"], ["uncertaintyLow (S2LRtRoiaRzyp8): interpretation6_scope: '' has been replaced by 'isotope'"] ] } }, { "version": "1.0.12", "lastVersion": "1.0.11", "curator": "nicholas", "timestamp": "2023-08-10 23:11:17 UTC", "changes": { "Base metadata": [ ["originalDataUrl: 'http://dx.doi.org/10.17864/1947.256' has been replaced by 'https://doi.org/10.17864/1947.256'"] ], "Publication metadata": [ ["pub1_doi: 'https://popups.uliege.be/1374-8505/index.php?id=4421&file=1&pid=4412' has been replaced by 'Verheyden, S., Keppens, E., Quinif, Y., Cheng, H. & Edwards, L. (2014). Late-glacial and Holocene climate reconstruction as inferred from a stalagmite - Grotte du Pere Noel, Han-sur-Lesse, Belgium. Geologica Belgica. 17. 83-89.'"] ] } }, { "version": "1.0.11", "lastVersion": "1.0.10", "curator": "nicholas", "timestamp": "2023-05-12 22:07:33 UTC", "changes": { "Paleo Column metadata": [ ["d18O (S2LR5E5HYoppj9): paleoData_notes: '((( \" the isotopic composition of the calcite in the Pere Noel cave is largely controlled by the water availability (drip rate) in the cave. Changes in isotopic equilibrium conditions, driven by the changes in cave humidity and linked to changes in recharge, ie. precipitation minus evapo-transpiration, overprint the theoretical temperature and/or precipitation control of the ��18O.\" (Verheyden et al., 2014); Therefore, ��18O and ��13C of the stalagmite may give some information on dry/wet variations in the past: the more enriched the ��13C and the ��18O of the calcite, the wetter the climate...��18O and ��13C variations, as observed on the present day calcite, are mainly controlled by the isotopic equilibrium state during precipitation of the calcite, which depends on the drip rate, and consequently, through recharge, on the rainfall amount to\" (Verheyden et al., 2008) ))) \" the isotopic composition of the calcite in the Pere Noel cave is largely controlled by the water availability (drip rate) in the cave. Changes in isotopic equilibrium conditions, driven by the changes in cave humidity and linked to changes in recharge, ie. precipitation minus evapo-transpiration, overprint the theoretical temperature and/or precipitation control of the δ18O.\" (Verheyden et al., 2014); Therefore, δ18O and δ13C of the stalagmite may give some information on dry/wet variations in the past: the more enriched the δ13C and the δ18O of the calcite, the wetter the climate...δ18O and δ13C variations, as observed on the present day calcite, are mainly controlled by the isotopic equilibrium state during precipitation of the calcite, which depends on the drip rate, and consequently, through recharge, on the rainfall amount to\" (Verheyden et al., 2008) /// \" the isotopic composition of the calcite in the Pere Noel cave is largely controlled by the water availability (drip rate) in the cave. Changes in isotopic equilibrium conditions, driven by the changes in cave humidity and linked to changes in recharge, ie. precipitation minus evapo-transpiration, overprint the theoretical temperature and/or precipitation control of the δ18O.\" (Verheyden et al., 2014); Therefore, δ18O and δ13C of the stalagmite may give some information on dry/wet variations in the past: the more enriched the δ13C and the δ18O of the calcite, the wetter the climate...δ18O and δ13C variations, as observed on the present day calcite, are mainly controlled by the isotopic equilibrium state during precipitation of the calcite, which depends on the drip rate, and consequently, through recharge, on the rainfall amount to\" (Verheyden et al., 2008)' has been replaced by '\" the isotopic composition of the calcite in the Pere Noel cave is largely controlled by the water availability (drip rate) in the cave. Changes in isotopic equilibrium conditions, driven by the changes in cave humidity and linked to changes in recharge, ie. precipitation minus evapo-transpiration, overprint the theoretical temperature and/or precipitation control of the δ18O.\" (Verheyden et al., 2014); Therefore, δ18O and δ13C of the stalagmite may give some information on dry/wet variations in the past: the more enriched the δ13C and the δ18O of the calcite, the wetter the climate...δ18O and δ13C variations, as observed on the present day calcite, are mainly controlled by the isotopic equilibrium state during precipitation of the calcite, which depends on the drip rate, and consequently, through recharge, on the rainfall amount to\" (Verheyden et al., 2008)'"] ] } }, { "version": "1.0.10", "lastVersion": "1.0.9", "curator": "nicholas", "timestamp": "2023-03-29 20:00:13 UTC", "changes": { "Paleo Interpretation metadata": [ ["d18O (S2LR5E5HYoppj9): interpretation1_variable: 'P-E' has been replaced by 'effectivePrecipitation'"], ["d13C (S2LR6dZP0RBWKz): interpretation1_variable: 'P-E' has been replaced by 'effectivePrecipitation'"] ], "Paleo Column metadata": [ ["d13C (S2LR6dZP0RBWKz): paleoData_notes: '((( \"Degassing of CO2, increasing ��13C values of the calcite, becomes increasingly important at lower drip rates and overprint the vegetation signal\" (Verheyden et al., 2014); Therefore, ��18O and ��13C of the stalagmite may give some information on dry/wet variations in the past: the more enriched the ��13C and the ��18O of the calcite, the wetter the climate...��18O and ��13C variations, as observed on the present day calcite, are mainly controlled by the isotopic equilibrium state during precipitation of the calcite, which depends on the drip rate, and consequently, through recharge, on the rainfall amount to\" (Verheyden et al., 2008) ))) \"Degassing of CO2, increasing δ13C values of the calcite, becomes increasingly important at lower drip rates and overprint the vegetation signal\" (Verheyden et al., 2014); Therefore, δ18O and δ13C of the stalagmite may give some information on dry/wet variations in the past: the more enriched the δ13C and the δ18O of the calcite, the wetter the climate...δ18O and δ13C variations, as observed on the present day calcite, are mainly controlled by the isotopic equilibrium state during precipitation of the calcite, which depends on the drip rate, and consequently, through recharge, on the rainfall amount to\" (Verheyden et al., 2008) /// \"Degassing of CO2, increasing δ13C values of the calcite, becomes increasingly important at lower drip rates and overprint the vegetation signal\" (Verheyden et al., 2014); Therefore, δ18O and δ13C of the stalagmite may give some information on dry/wet variations in the past: the more enriched the δ13C and the δ18O of the calcite, the wetter the climate...δ18O and δ13C variations, as observed on the present day calcite, are mainly controlled by the isotopic equilibrium state during precipitation of the calcite, which depends on the drip rate, and consequently, through recharge, on the rainfall amount to\" (Verheyden et al., 2008)' has been replaced by '\"Degassing of CO2, increasing δ13C values of the calcite, becomes increasingly important at lower drip rates and overprint the vegetation signal\" (Verheyden et al., 2014); Therefore, δ18O and δ13C of the stalagmite may give some information on dry/wet variations in the past: the more enriched the δ13C and the δ18O of the calcite, the wetter the climate...δ18O and δ13C variations, as observed on the present day calcite, are mainly controlled by the isotopic equilibrium state during precipitation of the calcite, which depends on the drip rate, and consequently, through recharge, on the rainfall amount to\" (Verheyden et al., 2008)'"] ] } }, { "version": "1.0.9", "lastVersion": "1.0.8", "curator": "nicholas", "timestamp": "2023-02-13 23:54:16 UTC", "changes": { "Paleo Column metadata": [ ["d18O (S2LR5E5HYoppj9): paleoData_notes: '\" the isotopic composition of the calcite in the Pere Noel cave is largely controlled by the water availability (drip rate) in the cave. Changes in isotopic equilibrium conditions, driven by the changes in cave humidity and linked to changes in recharge, ie. precipitation minus evapo-transpiration, overprint the theoretical temperature and/or precipitation control of the δ18O.\" (Verheyden et al., 2014); Therefore, δ18O and δ13C of the stalagmite may give some information on dry/wet variations in the past: the more enriched the δ13C and the δ18O of the calcite, the wetter the climate...δ18O and δ13C variations, as observed on the present day calcite, are mainly controlled by the isotopic equilibrium state during precipitation of the calcite, which depends on the drip rate, and consequently, through recharge, on the rainfall amount to\" (Verheyden et al., 2008)' has been replaced by '((( \" the isotopic composition of the calcite in the Pere Noel cave is largely controlled by the water availability (drip rate) in the cave. Changes in isotopic equilibrium conditions, driven by the changes in cave humidity and linked to changes in recharge, ie. precipitation minus evapo-transpiration, overprint the theoretical temperature and/or precipitation control of the ��18O.\" (Verheyden et al., 2014); Therefore, ��18O and ��13C of the stalagmite may give some information on dry/wet variations in the past: the more enriched the ��13C and the ��18O of the calcite, the wetter the climate...��18O and ��13C variations, as observed on the present day calcite, are mainly controlled by the isotopic equilibrium state during precipitation of the calcite, which depends on the drip rate, and consequently, through recharge, on the rainfall amount to\" (Verheyden et al., 2008) ))) \" the isotopic composition of the calcite in the Pere Noel cave is largely controlled by the water availability (drip rate) in the cave. Changes in isotopic equilibrium conditions, driven by the changes in cave humidity and linked to changes in recharge, ie. precipitation minus evapo-transpiration, overprint the theoretical temperature and/or precipitation control of the δ18O.\" (Verheyden et al., 2014); Therefore, δ18O and δ13C of the stalagmite may give some information on dry/wet variations in the past: the more enriched the δ13C and the δ18O of the calcite, the wetter the climate...δ18O and δ13C variations, as observed on the present day calcite, are mainly controlled by the isotopic equilibrium state during precipitation of the calcite, which depends on the drip rate, and consequently, through recharge, on the rainfall amount to\" (Verheyden et al., 2008) /// \" the isotopic composition of the calcite in the Pere Noel cave is largely controlled by the water availability (drip rate) in the cave. Changes in isotopic equilibrium conditions, driven by the changes in cave humidity and linked to changes in recharge, ie. precipitation minus evapo-transpiration, overprint the theoretical temperature and/or precipitation control of the δ18O.\" (Verheyden et al., 2014); Therefore, δ18O and δ13C of the stalagmite may give some information on dry/wet variations in the past: the more enriched the δ13C and the δ18O of the calcite, the wetter the climate...δ18O and δ13C variations, as observed on the present day calcite, are mainly controlled by the isotopic equilibrium state during precipitation of the calcite, which depends on the drip rate, and consequently, through recharge, on the rainfall amount to\" (Verheyden et al., 2008)'"], ["d13C (S2LR6dZP0RBWKz): paleoData_notes: '\"Degassing of CO2, increasing δ13C values of the calcite, becomes increasingly important at lower drip rates and overprint the vegetation signal\" (Verheyden et al., 2014); Therefore, δ18O and δ13C of the stalagmite may give some information on dry/wet variations in the past: the more enriched the δ13C and the δ18O of the calcite, the wetter the climate...δ18O and δ13C variations, as observed on the present day calcite, are mainly controlled by the isotopic equilibrium state during precipitation of the calcite, which depends on the drip rate, and consequently, through recharge, on the rainfall amount to\" (Verheyden et al., 2008)' has been replaced by '((( \"Degassing of CO2, increasing ��13C values of the calcite, becomes increasingly important at lower drip rates and overprint the vegetation signal\" (Verheyden et al., 2014); Therefore, ��18O and ��13C of the stalagmite may give some information on dry/wet variations in the past: the more enriched the ��13C and the ��18O of the calcite, the wetter the climate...��18O and ��13C variations, as observed on the present day calcite, are mainly controlled by the isotopic equilibrium state during precipitation of the calcite, which depends on the drip rate, and consequently, through recharge, on the rainfall amount to\" (Verheyden et al., 2008) ))) \"Degassing of CO2, increasing δ13C values of the calcite, becomes increasingly important at lower drip rates and overprint the vegetation signal\" (Verheyden et al., 2014); Therefore, δ18O and δ13C of the stalagmite may give some information on dry/wet variations in the past: the more enriched the δ13C and the δ18O of the calcite, the wetter the climate...δ18O and δ13C variations, as observed on the present day calcite, are mainly controlled by the isotopic equilibrium state during precipitation of the calcite, which depends on the drip rate, and consequently, through recharge, on the rainfall amount to\" (Verheyden et al., 2008) /// \"Degassing of CO2, increasing δ13C values of the calcite, becomes increasingly important at lower drip rates and overprint the vegetation signal\" (Verheyden et al., 2014); Therefore, δ18O and δ13C of the stalagmite may give some information on dry/wet variations in the past: the more enriched the δ13C and the δ18O of the calcite, the wetter the climate...δ18O and δ13C variations, as observed on the present day calcite, are mainly controlled by the isotopic equilibrium state during precipitation of the calcite, which depends on the drip rate, and consequently, through recharge, on the rainfall amount to\" (Verheyden et al., 2008)'"] ], "Paleo Interpretation metadata": [ ["uncertaintyHigh (S2LR6iWbJ6Ie95): interpretation1_scope: '' has been replaced by 'climate'"], ["uncertaintyLow (S2LR9DAMVk2hF0): interpretation1_scope: '' has been replaced by 'climate'"], ["uncertaintyHigh (S2LRaB26MmrAzh): interpretation1_scope: '' has been replaced by 'climate'"], ["uncertaintyLow (S2LRebefD2sqOH): interpretation1_scope: '' has been replaced by 'climate'"], ["uncertaintyLow (S2LRf9zcOoZJhq): interpretation1_scope: '' has been replaced by 'climate'"], ["uncertaintyLow (S2LRfpQK1AtSwB): interpretation1_scope: '' has been replaced by 'climate'"], ["uncertaintyHigh (S2LRGY5ayanpuZ): interpretation1_scope: '' has been replaced by 'climate'"], ["uncertaintyHigh (S2LRpq55DUa0Qf): interpretation1_scope: '' has been replaced by 'climate'"], ["uncertaintyHigh (S2LRS4jI2IXGj8): interpretation1_scope: '' has been replaced by 'climate'"], ["uncertaintyLow (S2LRtRoiaRzyp8): interpretation1_scope: '' has been replaced by 'climate'"] ] } }, { "version": "1.0.8", "lastVersion": "1.0.7", "curator": "nicholas", "timestamp": "2023-02-09 16:09:15 UTC", "notes": "Updated lipdverse database entry with a changed file.", "changes": { "Geographic metadata": [ ["geo_elevation: '' has been replaced by '230'"] ], "Paleo Column metadata": [ ["correction (S2LR0zZx2O4ux7): paleoData_notes: '' has been replaced by 'NA; paleoData_method has been standardized'"], ["correction (S2LR0zZx2O4ux7): paleoData_variableName: 'hasAragoniteCorrection' has been replaced by 'correction'"], ["correction (S2LR0zZx2O4ux7): paleoData_method: '' has been replaced by 'aragonite correction'"], ["uncertainty (S2LR2uU7iKZLIJ): paleoData_notes: '' has been replaced by 'NA; paleoData_measurementMaterial has been standardized; paleoData_method has been standardized'"], ["uncertainty (S2LR2uU7iKZLIJ): paleoData_variableName: 'd18OPrecision' has been replaced by 'uncertainty'"], ["uncertainty (S2LR2uU7iKZLIJ): paleoData_measurementMaterial: '' has been replaced by 'd18O carbonate'"], ["uncertainty (S2LR2uU7iKZLIJ): paleoData_method: '' has been replaced by 'precision'"], ["uncertaintyHigh (S2LR6iWbJ6Ie95): paleoData_notes: '' has been replaced by 'NA; paleoData_inferredMaterial has been standardized; paleoData_method has been standardized; paleoData_datum has been standardized'"], ["uncertaintyHigh (S2LR6iWbJ6Ie95): paleoData_units: 'BP' has been replaced by 'yr BP'"], ["uncertaintyHigh (S2LR6iWbJ6Ie95): paleoData_variableName: 'agelinInterpUncertaintyHigh' has been replaced by 'uncertaintyHigh'"], ["uncertaintyHigh (S2LR6iWbJ6Ie95): paleoData_datum: '' has been replaced by '1950'"], ["uncertaintyHigh (S2LR6iWbJ6Ie95): paleoData_inferredMaterial: '' has been replaced by 'age'"], ["uncertaintyHigh (S2LR6iWbJ6Ie95): paleoData_method: '' has been replaced by 'linInterp'"], ["age (S2LR76xsjzFxpW): paleoData_notes: '' has been replaced by 'NA; paleoData_method has been standardized; paleoData_isPrimary has been standardized; paleoData_datum has been standardized'"], ["age (S2LR76xsjzFxpW): paleoData_units: 'BP' has been replaced by 'yr BP'"], ["age (S2LR76xsjzFxpW): paleoData_variableName: 'agecopRa' has been replaced by 'age'"], ["age (S2LR76xsjzFxpW): paleoData_datum: '' has been replaced by '1950'"], ["age (S2LR76xsjzFxpW): paleoData_isPrimary: '' has been replaced by 'FALSE'"], ["age (S2LR76xsjzFxpW): paleoData_method: '' has been replaced by 'copRa'"], ["uncertaintyLow (S2LR9DAMVk2hF0): paleoData_notes: '' has been replaced by 'NA; paleoData_inferredMaterial has been standardized; paleoData_method has been standardized; paleoData_datum has been standardized'"], ["uncertaintyLow (S2LR9DAMVk2hF0): paleoData_units: 'BP' has been replaced by 'yr BP'"], ["uncertaintyLow (S2LR9DAMVk2hF0): paleoData_variableName: 'agecopRaUncertaintyLow' has been replaced by 'uncertaintyLow'"], ["uncertaintyLow (S2LR9DAMVk2hF0): paleoData_datum: '' has been replaced by '1950'"], ["uncertaintyLow (S2LR9DAMVk2hF0): paleoData_inferredMaterial: '' has been replaced by 'age'"], ["uncertaintyLow (S2LR9DAMVk2hF0): paleoData_method: '' has been replaced by 'copRa'"], ["uncertaintyHigh (S2LRaB26MmrAzh): paleoData_notes: '' has been replaced by 'NA; paleoData_inferredMaterial has been standardized; paleoData_method has been standardized; paleoData_datum has been standardized'"], ["uncertaintyHigh (S2LRaB26MmrAzh): paleoData_units: 'BP' has been replaced by 'yr BP'"], ["uncertaintyHigh (S2LRaB26MmrAzh): paleoData_variableName: 'ageBaconUncertaintyHigh' has been replaced by 'uncertaintyHigh'"], ["uncertaintyHigh (S2LRaB26MmrAzh): paleoData_datum: '' has been replaced by '1950'"], ["uncertaintyHigh (S2LRaB26MmrAzh): paleoData_inferredMaterial: '' has been replaced by 'age'"], ["uncertaintyHigh (S2LRaB26MmrAzh): paleoData_method: '' has been replaced by 'Bacon'"], ["depth (S2LRC2NwhynrJz): paleoData_notes: '' has been replaced by 'NA; paleoData_isPrimary has been standardized'"], ["depth (S2LRC2NwhynrJz): paleoData_units: 'depth_sample' has been replaced by 'mm'"], ["depth (S2LRC2NwhynrJz): paleoData_isPrimary: '' has been replaced by 'TRUE'"], ["uncertainty (S2LRDdJTOcv8eq): paleoData_notes: '' has been replaced by 'NA; paleoData_measurementMaterial has been standardized; paleoData_method has been standardized'"], ["uncertainty (S2LRDdJTOcv8eq): paleoData_variableName: 'd18OStandard' has been replaced by 'uncertainty'"], ["uncertainty (S2LRDdJTOcv8eq): paleoData_measurementMaterial: '' has been replaced by 'd18O carbonate'"], ["uncertainty (S2LRDdJTOcv8eq): paleoData_method: '' has been replaced by 'standard'"], ["uncertaintyLow (S2LRebefD2sqOH): paleoData_notes: '' has been replaced by 'NA; paleoData_inferredMaterial has been standardized; paleoData_method has been standardized; paleoData_datum has been standardized'"], ["uncertaintyLow (S2LRebefD2sqOH): paleoData_units: 'BP' has been replaced by 'yr BP'"], ["uncertaintyLow (S2LRebefD2sqOH): paleoData_variableName: 'ageBchronUncertaintyLow' has been replaced by 'uncertaintyLow'"], ["uncertaintyLow (S2LRebefD2sqOH): paleoData_datum: '' has been replaced by '1950'"], ["uncertaintyLow (S2LRebefD2sqOH): paleoData_inferredMaterial: '' has been replaced by 'age'"], ["uncertaintyLow (S2LRebefD2sqOH): paleoData_method: '' has been replaced by 'Bchron'"], ["uncertaintyLow (S2LRf9zcOoZJhq): paleoData_notes: '' has been replaced by 'NA; paleoData_inferredMaterial has been standardized; paleoData_method has been standardized; paleoData_datum has been standardized'"], ["uncertaintyLow (S2LRf9zcOoZJhq): paleoData_units: 'BP' has been replaced by 'yr BP'"], 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"nick", "timestamp": "2021-01-12 02:29:30 UTC", "changes": { "Paleo Interpretation metadata": [ ["hasAragoniteCorrection (S2LR0zZx2O4ux7): interpretation1_scope: '' has been replaced by 'climate'"], ["d18OPrecision (S2LR2uU7iKZLIJ): interpretation1_scope: '' has been replaced by 'climate'"], ["d18O (S2LR5E5HYoppj9): interpretation1_direction: '' has been replaced by 'negative'"], ["d18O (S2LR5E5HYoppj9): interpretation1_scope: '' has been replaced by 'climate'"], ["d18O (S2LR5E5HYoppj9): interpretation1_seasonalityGeneral: '' has been replaced by 'Annual'"], ["d18O (S2LR5E5HYoppj9): interpretation1_variable: '' has been replaced by 'P-E'"], ["d18O (S2LR5E5HYoppj9): interpretation1_variableDetail: '' has been replaced by 'infiltration'"], ["d13C (S2LR6dZP0RBWKz): interpretation1_direction: '' has been replaced by 'negative'"], ["d13C (S2LR6dZP0RBWKz): interpretation1_scope: '' has been replaced by 'climate'"], ["d13C (S2LR6dZP0RBWKz): interpretation1_seasonalityGeneral: '' has been replaced by 'Annual'"], ["d13C (S2LR6dZP0RBWKz): interpretation1_variable: '' has been replaced by 'P-E'"], ["d13C (S2LR6dZP0RBWKz): interpretation1_variableDetail: '' has been replaced by 'infiltration'"], ["d18OStandard (S2LRDdJTOcv8eq): interpretation1_scope: '' has been replaced by 'climate'"], ["sisalSampleID (S2LRgSlbbJADra): interpretation1_scope: '' has been replaced by 'climate'"], ["d13CPrecision (S2LRip5obuHZID): interpretation1_scope: '' has been replaced by 'climate'"], ["mineralogy (S2LROCBNGpbUPS): interpretation1_scope: '' has been replaced by 'climate'"], ["d13CStandard (S2LRQ6jTuAh7Xw): interpretation1_scope: '' has been replaced by 'climate'"] ], "Paleo Column metadata": [ ["d18O (S2LR5E5HYoppj9): paleoData_notes: '' has been replaced by '\" the isotopic composition of the calcite in the Pere Noel cave is largely controlled by the water availability (drip rate) in the cave. Changes in isotopic equilibrium conditions, driven by the changes in cave humidity and linked to changes in recharge, ie. precipitation minus evapo-transpiration, overprint the theoretical temperature and/or precipitation control of the δ18O.\" (Verheyden et al., 2014); Therefore, δ18O and δ13C of the stalagmite may give some information on dry/wet variations in the past: the more enriched the δ13C and the δ18O of the calcite, the wetter the climate...δ18O and δ13C variations, as observed on the present day calcite, are mainly controlled by the isotopic equilibrium state during precipitation of the calcite, which depends on the drip rate, and consequently, through recharge, on the rainfall amount to\" (Verheyden et al., 2008)'"], ["d18O (S2LR5E5HYoppj9): paleoData_proxy: '' has been replaced by 'd18O'"], ["d18O (S2LR5E5HYoppj9): paleoData_proxyDetail: '' has been replaced by 'calcite'"], ["d18O (S2LR5E5HYoppj9): paleoData_proxyGeneral: '' has been replaced by 'isotope'"], ["d18O (S2LR5E5HYoppj9): paleoData_QCCertification: '' has been replaced by 'CH'"], ["d13C (S2LR6dZP0RBWKz): paleoData_notes: '' has been replaced by '\"Degassing of CO2, increasing δ13C values of the calcite, becomes increasingly important at lower drip rates and overprint the vegetation signal\" (Verheyden et al., 2014); Therefore, δ18O and δ13C of the stalagmite may give some information on dry/wet variations in the past: the more enriched the δ13C and the δ18O of the calcite, the wetter the climate...δ18O and δ13C variations, as observed on the present day calcite, are mainly controlled by the isotopic equilibrium state during precipitation of the calcite, which depends on the drip rate, and consequently, through recharge, on the rainfall amount to\" (Verheyden et al., 2008)'"], ["d13C (S2LR6dZP0RBWKz): paleoData_proxy: '' has been replaced by 'd13C'"], ["d13C (S2LR6dZP0RBWKz): paleoData_proxyDetail: '' has been replaced by 'calcite'"], ["d13C (S2LR6dZP0RBWKz): paleoData_proxyGeneral: '' has been replaced by 'isotope'"], ["d13C (S2LR6dZP0RBWKz): paleoData_QCCertification: '' has been replaced by 'CH'"] ] } }, { "version": "1.0.0", "curator": "nick", "timestamp": "2020-09-29 14:29:32 UTC", "notes": "Created from SISALv2" } ], "neotomaDatasetId": null, "pub": [ { "citation": "Verheyden, S., Keppens, E., Quinif, Y., Cheng, H. J. and Edwards, L. R.: Late-glacial and Holocene climate reconstruction as inferred from a stalagmite-Grotte du Pre Nol, Han-sur-Lesse, Belgium, Geol. Belgica, 17(1), 83<96>89, 2014.", "year": 2014, "doi": "Verheyden, S., Keppens, E., Quinif, Y., Cheng, H. & Edwards, L. (2014). Late-glacial and Holocene climate reconstruction as inferred from a stalagmite - Grotte du Pere Noel, Han-sur-Lesse, Belgium. Geologica Belgica. 17. 83-89.", "author": [ { "name": null } ], "citeKey": null, "issue": null, "journal": null, "pages": null, "title": null, "volume": null }, { "citation": "Verheyden, S., Keppens, E., Fairchild, I. J., McDermott, F. and Weis, D.: Mg, Sr and Sr isotope geochemistry of a Belgian Holocene speleothem: implications for paleoclimate reconstructions, Chem. Geol., 169(1<96>2), 131<96>144, 2000.", "year": 2000, "doi": "10.1016/S0009-2541(00)00299-0" } ], "geo": { "longitude": 5.2, "latitude": 50, "elevation": 230, "siteName": "Pere Noel cave", "sisalSiteId": 268, "geology": "limestone", "rockAge": "Devonian", "hasMonitoring": "yes", "gcmdLocation": "Europe>Western Europe>Belgium" }, "@context": "context.jsonld" }