Refers to the unique identifier for the sample (as given in sample table)
NA; paleoData_isPrimary has been standardized
Description of the mineralogy of the sample
Indication of whether the isotope measurements have been corrected in aragonite samples
NA; paleoData_method has been standardized
" 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)
Laboratory precision on the d18O measurement
NA; paleoData_measurementMaterial has been standardized; paleoData_method has been standardized
"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)
Laboratory precision on the d13C measurement
Original published calibrated age of the sample in years BP
NA; paleoData_isPrimary has been standardized; paleoData_datum has been standardized
Calendar age in years BP, method = linInterp
NA; paleoData_method has been standardized; paleoData_isPrimary has been standardized; paleoData_datum has been standardized
Positive age uncertaintyin years BP, method = linInterp
NA; paleoData_inferredMaterial has been standardized; paleoData_method has been standardized; paleoData_datum has been standardized
Negative age uncertaintyin years BP, method = linInterp
Calendar age in years BP, method = Bchron
Positive age uncertaintyin years BP, method = Bchron
Negative age uncertaintyin years BP, method = Bchron
Calendar age in years BP, method = Bacon
Positive age uncertaintyin years BP, method = Bacon
Negative age uncertaintyin years BP, method = Bacon
Calendar age in years BP, method = copRa
Positive age uncertaintyin years BP, method = copRa
Negative age uncertaintyin years BP, method = copRa
Calendar age in years BP, method = StalAge
Positive age uncertaintyin years BP, method = StalAge
Negative age uncertaintyin years BP, method = StalAge
Minimum weight of the dated sample in mg
Maximum weight of the dated sample in mg
Indication of whether the date is used in the original age model (opposite of rejected)
230Th/232Th activity ratio of the dated sample
234U/238U activity ratio of the dated sample
Description of the half-life used for 230Th and 234U for U/Th samples
Corrected age of the dated sample in years
Positive uncertainty of corrected age of the dated sample in years
Negative uncertainty of corrected age of the dated sample in years
originalDataUrl: 'http://dx.doi.org/10.17864/1947.256' has been replaced by 'https://doi.org/10.17864/1947.256'
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.'
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)'
d18O (S2LR5E5HYoppj9): interpretation1_variable: 'P-E' has been replaced by 'effectivePrecipitation'
d13C (S2LR6dZP0RBWKz): interpretation1_variable: 'P-E' has been replaced by 'effectivePrecipitation'
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)'
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)'
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'
Updated lipdverse database entry with a changed file.
geo_elevation: '' has been replaced by '230'
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'
uncertaintyLow (S2LRf9zcOoZJhq): paleoData_variableName: 'ageStalAgeUncertaintyLow' has been replaced by 'uncertaintyLow'
uncertaintyLow (S2LRf9zcOoZJhq): paleoData_datum: '' has been replaced by '1950'
uncertaintyLow (S2LRf9zcOoZJhq): paleoData_inferredMaterial: '' has been replaced by 'age'
uncertaintyLow (S2LRf9zcOoZJhq): paleoData_method: '' has been replaced by 'StalAge'
uncertaintyLow (S2LRfpQK1AtSwB): paleoData_notes: '' has been replaced by 'NA; paleoData_inferredMaterial has been standardized; paleoData_method has been standardized; paleoData_datum has been standardized'
uncertaintyLow (S2LRfpQK1AtSwB): paleoData_units: 'BP' has been replaced by 'yr BP'
uncertaintyLow (S2LRfpQK1AtSwB): paleoData_variableName: 'agelinInterpUncertaintyLow' has been replaced by 'uncertaintyLow'
uncertaintyLow (S2LRfpQK1AtSwB): paleoData_datum: '' has been replaced by '1950'
uncertaintyLow (S2LRfpQK1AtSwB): paleoData_inferredMaterial: '' has been replaced by 'age'
uncertaintyLow (S2LRfpQK1AtSwB): paleoData_method: '' has been replaced by 'linInterp'
sampleID (S2LRgSlbbJADra): paleoData_variableName: 'sisalSampleID' has been replaced by 'sampleID'
uncertaintyHigh (S2LRGY5ayanpuZ): paleoData_notes: '' has been replaced by 'NA; paleoData_inferredMaterial has been standardized; paleoData_method has been standardized; paleoData_datum has been standardized'
uncertaintyHigh (S2LRGY5ayanpuZ): paleoData_units: 'BP' has been replaced by 'yr BP'
uncertaintyHigh (S2LRGY5ayanpuZ): paleoData_variableName: 'ageStalAgeUncertaintyHigh' has been replaced by 'uncertaintyHigh'
uncertaintyHigh (S2LRGY5ayanpuZ): paleoData_datum: '' has been replaced by '1950'
uncertaintyHigh (S2LRGY5ayanpuZ): paleoData_inferredMaterial: '' has been replaced by 'age'
uncertaintyHigh (S2LRGY5ayanpuZ): paleoData_method: '' has been replaced by 'StalAge'
uncertainty (S2LRip5obuHZID): paleoData_notes: '' has been replaced by 'NA; paleoData_measurementMaterial has been standardized; paleoData_method has been standardized'
uncertainty (S2LRip5obuHZID): paleoData_variableName: 'd13CPrecision' has been replaced by 'uncertainty'
uncertainty (S2LRip5obuHZID): paleoData_measurementMaterial: '' has been replaced by 'd13C'
uncertainty (S2LRip5obuHZID): paleoData_method: '' has been replaced by 'precision'
age (S2LRKD4t9qFVv8): paleoData_notes: '' has been replaced by 'NA; paleoData_method has been standardized; paleoData_isPrimary has been standardized; paleoData_datum has been standardized'
age (S2LRKD4t9qFVv8): paleoData_units: 'BP' has been replaced by 'yr BP'
age (S2LRKD4t9qFVv8): paleoData_variableName: 'agelinInterp' has been replaced by 'age'
age (S2LRKD4t9qFVv8): paleoData_datum: '' has been replaced by '1950'
age (S2LRKD4t9qFVv8): paleoData_isPrimary: '' has been replaced by 'FALSE'
age (S2LRKD4t9qFVv8): paleoData_method: '' has been replaced by 'linInterp'
age (S2LRnFczx5jicL): paleoData_notes: '' has been replaced by 'NA; paleoData_isPrimary has been standardized; paleoData_datum has been standardized'
age (S2LRnFczx5jicL): paleoData_units: 'BP' has been replaced by 'yr BP'
age (S2LRnFczx5jicL): paleoData_datum: '' has been replaced by '1950'
age (S2LRnFczx5jicL): paleoData_isPrimary: '' has been replaced by 'TRUE'
age (S2LRoATJAvQFxt): paleoData_notes: '' has been replaced by 'NA; paleoData_method has been standardized; paleoData_isPrimary has been standardized; paleoData_datum has been standardized'
age (S2LRoATJAvQFxt): paleoData_units: 'BP' has been replaced by 'yr BP'
age (S2LRoATJAvQFxt): paleoData_variableName: 'ageBacon' has been replaced by 'age'
age (S2LRoATJAvQFxt): paleoData_datum: '' has been replaced by '1950'
age (S2LRoATJAvQFxt): paleoData_isPrimary: '' has been replaced by 'FALSE'
age (S2LRoATJAvQFxt): paleoData_method: '' has been replaced by 'Bacon'
uncertaintyHigh (S2LRpq55DUa0Qf): paleoData_notes: '' has been replaced by 'NA; paleoData_inferredMaterial has been standardized; paleoData_method has been standardized; paleoData_datum has been standardized'
uncertaintyHigh (S2LRpq55DUa0Qf): paleoData_units: 'BP' has been replaced by 'yr BP'
uncertaintyHigh (S2LRpq55DUa0Qf): paleoData_variableName: 'agecopRaUncertaintyHigh' has been replaced by 'uncertaintyHigh'
uncertaintyHigh (S2LRpq55DUa0Qf): paleoData_datum: '' has been replaced by '1950'
uncertaintyHigh (S2LRpq55DUa0Qf): paleoData_inferredMaterial: '' has been replaced by 'age'
uncertaintyHigh (S2LRpq55DUa0Qf): paleoData_method: '' has been replaced by 'copRa'
uncertainty (S2LRQ6jTuAh7Xw): paleoData_notes: '' has been replaced by 'NA; paleoData_measurementMaterial has been standardized; paleoData_method has been standardized'
uncertainty (S2LRQ6jTuAh7Xw): paleoData_variableName: 'd13CStandard' has been replaced by 'uncertainty'
uncertainty (S2LRQ6jTuAh7Xw): paleoData_measurementMaterial: '' has been replaced by 'd13C'
uncertainty (S2LRQ6jTuAh7Xw): paleoData_method: '' has been replaced by 'standard'
uncertaintyHigh (S2LRS4jI2IXGj8): paleoData_notes: '' has been replaced by 'NA; paleoData_inferredMaterial has been standardized; paleoData_method has been standardized; paleoData_datum has been standardized'
uncertaintyHigh (S2LRS4jI2IXGj8): paleoData_units: 'BP' has been replaced by 'yr BP'
uncertaintyHigh (S2LRS4jI2IXGj8): paleoData_variableName: 'ageBchronUncertaintyHigh' has been replaced by 'uncertaintyHigh'
uncertaintyHigh (S2LRS4jI2IXGj8): paleoData_datum: '' has been replaced by '1950'
uncertaintyHigh (S2LRS4jI2IXGj8): paleoData_inferredMaterial: '' has been replaced by 'age'
uncertaintyHigh (S2LRS4jI2IXGj8): paleoData_method: '' has been replaced by 'Bchron'
age (S2LRtjBVQkGsP3): paleoData_notes: '' has been replaced by 'NA; paleoData_method has been standardized; paleoData_isPrimary has been standardized; paleoData_datum has been standardized'
age (S2LRtjBVQkGsP3): paleoData_units: 'BP' has been replaced by 'yr BP'
age (S2LRtjBVQkGsP3): paleoData_variableName: 'ageStalAge' has been replaced by 'age'
age (S2LRtjBVQkGsP3): paleoData_datum: '' has been replaced by '1950'
age (S2LRtjBVQkGsP3): paleoData_isPrimary: '' has been replaced by 'FALSE'
age (S2LRtjBVQkGsP3): paleoData_method: '' has been replaced by 'StalAge'
uncertaintyLow (S2LRtRoiaRzyp8): paleoData_notes: '' has been replaced by 'NA; paleoData_inferredMaterial has been standardized; paleoData_method has been standardized; paleoData_datum has been standardized'
uncertaintyLow (S2LRtRoiaRzyp8): paleoData_units: 'BP' has been replaced by 'yr BP'
uncertaintyLow (S2LRtRoiaRzyp8): paleoData_variableName: 'ageBaconUncertaintyLow' has been replaced by 'uncertaintyLow'
uncertaintyLow (S2LRtRoiaRzyp8): paleoData_datum: '' has been replaced by '1950'
uncertaintyLow (S2LRtRoiaRzyp8): paleoData_inferredMaterial: '' has been replaced by 'age'
uncertaintyLow (S2LRtRoiaRzyp8): paleoData_method: '' has been replaced by 'Bacon'
age (S2LRU8QglDCUFs): paleoData_notes: '' has been replaced by 'NA; paleoData_method has been standardized; paleoData_isPrimary has been standardized; paleoData_datum has been standardized'
age (S2LRU8QglDCUFs): paleoData_units: 'BP' has been replaced by 'yr BP'
age (S2LRU8QglDCUFs): paleoData_variableName: 'ageBchron' has been replaced by 'age'
age (S2LRU8QglDCUFs): paleoData_datum: '' has been replaced by '1950'
age (S2LRU8QglDCUFs): paleoData_isPrimary: '' has been replaced by 'FALSE'
age (S2LRU8QglDCUFs): paleoData_method: '' has been replaced by 'Bchron'
d18O (S2LR5E5HYoppj9): interpretation1_seasonality: '1,2,3,4,5,6,7,8,9,10,11,12' has been replaced by 'Annual'
d13C (S2LR6dZP0RBWKz): interpretation1_seasonality: '1,2,3,4,5,6,7,8,9,10,11,12' has been replaced by 'Annual'
geo_elevation: '230' has been replaced by ''
hasAragoniteCorrection (S2LR0zZx2O4ux7): interpretation1_scope: '' has been replaced by 'climate'
d18OPrecision (S2LR2uU7iKZLIJ): interpretation1_scope: '' has been replaced by 'climate'
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'
hasAragoniteCorrection (S2LR0zZx2O4ux7): interpretation1_scope: 'climate' has been replaced by ''
d18OPrecision (S2LR2uU7iKZLIJ): interpretation1_scope: 'climate' has been replaced by ''
d18O (S2LR5E5HYoppj9): interpretation1_variableGroup: '' has been replaced by 'P-E'
d13C (S2LR6dZP0RBWKz): interpretation1_variableGroup: '' has been replaced by 'P-E'
d18OStandard (S2LRDdJTOcv8eq): interpretation1_scope: 'climate' has been replaced by ''
sisalSampleID (S2LRgSlbbJADra): interpretation1_scope: 'climate' has been replaced by ''
d13CPrecision (S2LRip5obuHZID): interpretation1_scope: 'climate' has been replaced by ''
mineralogy (S2LROCBNGpbUPS): interpretation1_scope: 'climate' has been replaced by ''
d13CStandard (S2LRQ6jTuAh7Xw): interpretation1_scope: 'climate' has been replaced by ''
d18O (S2LR5E5HYoppj9): paleoData_proxyLumps: '' has been replaced by 'isotope'
d18O (S2LR5E5HYoppj9): paleoData_proxyLumpsOriginal: '' has been replaced by 'd18O'
d13C (S2LR6dZP0RBWKz): paleoData_proxyLumps: '' has been replaced by 'isotope'
d13C (S2LR6dZP0RBWKz): paleoData_proxyLumpsOriginal: '' has been replaced by 'd13C'
agelinInterpUncertaintyHigh (S2LR6iWbJ6Ie95): paleoData_units: 'yr BP' has been replaced by 'BP'
agelinInterpUncertaintyHigh (S2LR6iWbJ6Ie95): paleoData_unitsOriginal: '' has been replaced by 'yr BP'
agecopRa (S2LR76xsjzFxpW): paleoData_units: 'yr BP' has been replaced by 'BP'
agecopRa (S2LR76xsjzFxpW): paleoData_unitsOriginal: '' has been replaced by 'yr BP'
agecopRaUncertaintyLow (S2LR9DAMVk2hF0): paleoData_units: 'yr BP' has been replaced by 'BP'
agecopRaUncertaintyLow (S2LR9DAMVk2hF0): paleoData_unitsOriginal: '' has been replaced by 'yr BP'
ageBaconUncertaintyHigh (S2LRaB26MmrAzh): paleoData_units: 'yr BP' has been replaced by 'BP'
ageBaconUncertaintyHigh (S2LRaB26MmrAzh): paleoData_unitsOriginal: '' has been replaced by 'yr BP'
ageBchronUncertaintyLow (S2LRebefD2sqOH): paleoData_units: 'yr BP' has been replaced by 'BP'
ageBchronUncertaintyLow (S2LRebefD2sqOH): paleoData_unitsOriginal: '' has been replaced by 'yr BP'
ageStalAgeUncertaintyLow (S2LRf9zcOoZJhq): paleoData_units: 'yr BP' has been replaced by 'BP'
ageStalAgeUncertaintyLow (S2LRf9zcOoZJhq): paleoData_unitsOriginal: '' has been replaced by 'yr BP'
agelinInterpUncertaintyLow (S2LRfpQK1AtSwB): paleoData_units: 'yr BP' has been replaced by 'BP'
agelinInterpUncertaintyLow (S2LRfpQK1AtSwB): paleoData_unitsOriginal: '' has been replaced by 'yr BP'
ageStalAgeUncertaintyHigh (S2LRGY5ayanpuZ): paleoData_units: 'yr BP' has been replaced by 'BP'
ageStalAgeUncertaintyHigh (S2LRGY5ayanpuZ): paleoData_unitsOriginal: '' has been replaced by 'yr BP'
agelinInterp (S2LRKD4t9qFVv8): paleoData_units: 'yr BP' has been replaced by 'BP'
agelinInterp (S2LRKD4t9qFVv8): paleoData_unitsOriginal: '' has been replaced by 'yr BP'
age (S2LRnFczx5jicL): paleoData_units: 'yr BP' has been replaced by 'BP'
age (S2LRnFczx5jicL): paleoData_unitsOriginal: '' has been replaced by 'yr BP'
ageBacon (S2LRoATJAvQFxt): paleoData_units: 'yr BP' has been replaced by 'BP'
ageBacon (S2LRoATJAvQFxt): paleoData_unitsOriginal: '' has been replaced by 'yr BP'
agecopRaUncertaintyHigh (S2LRpq55DUa0Qf): paleoData_units: 'yr BP' has been replaced by 'BP'
agecopRaUncertaintyHigh (S2LRpq55DUa0Qf): paleoData_unitsOriginal: '' has been replaced by 'yr BP'
ageBchronUncertaintyHigh (S2LRS4jI2IXGj8): paleoData_units: 'yr BP' has been replaced by 'BP'
ageBchronUncertaintyHigh (S2LRS4jI2IXGj8): paleoData_unitsOriginal: '' has been replaced by 'yr BP'
ageStalAge (S2LRtjBVQkGsP3): paleoData_units: 'yr BP' has been replaced by 'BP'
ageStalAge (S2LRtjBVQkGsP3): paleoData_unitsOriginal: '' has been replaced by 'yr BP'
ageBaconUncertaintyLow (S2LRtRoiaRzyp8): paleoData_units: 'yr BP' has been replaced by 'BP'
ageBaconUncertaintyLow (S2LRtRoiaRzyp8): paleoData_unitsOriginal: '' has been replaced by 'yr BP'
ageBchron (S2LRU8QglDCUFs): paleoData_units: 'yr BP' has been replaced by 'BP'
ageBchron (S2LRU8QglDCUFs): paleoData_unitsOriginal: '' has been replaced by 'yr BP'
age_type (S2LcRZnPi4tt2K3): chronData_variableName: 'ageType' has been replaced by 'age_type'
age_type (S2LcRZnPi4tt2K3): chronData_variableNameOriginal: '' has been replaced by 'ageType'
geo_gcmdLocation: '' has been replaced by 'Europe>Western Europe>Belgium'
archiveType: 'speleothem' has been replaced by 'Speleothem'
d18O (S2LR5E5HYoppj9): interpretation1_seasonality: '' has been replaced by '1,2,3,4,5,6,7,8,9,10,11,711'
d13C (S2LR6dZP0RBWKz): interpretation1_seasonality: '' has been replaced by '1,2,3,4,5,6,7,8,9,10,11,712'
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'
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'
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 P<e8>re No<eb>l, Han-sur-Lesse, Belgium, Geol. Belgica, 17(1), 83<96>89, 2014.
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.
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.