Version history for KtlvbpDKcMitTxvwKXej -
Han-sur-Lessecave.Genty.1999
Version: 1.0.4
- lastVersion: 1.0.3
- curator: nicholas
- timestamp: 2025-06-25 22:46:11.65172 UTC
- changes:
- Paleo Interpretation metadata:
- d13C (S2LRBCzk3hPPAC): interpretation1_variable: ‘((( null ))) Mixed
/// deleteMe’ has been replaced by ‘deleteMe’
- d13C (S2LRJVZt4Oq0uG): interpretation1_variable: ‘((( null ))) Mixed
/// deleteMe’ has been replaced by ‘deleteMe’
- d18O (S2LRNDNiKrHu9d): interpretation1_variable: ‘((( null ))) Mixed
/// deleteMe’ has been replaced by ‘deleteMe’
- d18O (S2LRcAxAsRumAY): interpretation1_variable: ‘((( null ))) Mixed
/// deleteMe’ has been replaced by ‘deleteMe’
Version: 1.0.1
- lastVersion: 1.0.0
- curator: nick
- timestamp: 2021-01-12 02:28:58 UTC
- changes:
- Paleo Interpretation metadata:
- d13CStandardComposite (S2LR0XnDUL6zJJ): interpretation1_scope: NULL
has been replaced by ‘climate’
- hasHiatus (S2LR2j7jqXNB5W): interpretation1_scope: NULL has been
replaced by ‘climate’
- d13CPrecision (S2LR4giPds3qS2): interpretation1_scope: NULL has been
replaced by ‘climate’
- thickness (S2LR6TGBvrLCmH): interpretation1_scope: NULL has been
replaced by ‘climate’
- mineralogy (S2LR7eCZKWtASf): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OPrecision (S2LR8ce3jhNwhb): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OPrecision (S2LR9nYHOrMnCz): interpretation1_scope: NULL has been
replaced by ‘climate’
- d13C (S2LRBCzk3hPPAC): interpretation1_scope: NULL has been replaced
by ‘climate’
- d13C (S2LRBCzk3hPPAC): interpretation1_variable: NULL has been
replaced by ‘Mixed’
- d13C (S2LRBCzk3hPPAC): interpretation1_variableDetail: NULL has been
replaced by ‘Vegetation’
- d13CStandard (S2LRbMZtuy97pj): interpretation1_scope: NULL has been
replaced by ‘climate’
- d13CPrecisionComposite (S2LRBpJnqYHY8b): interpretation1_scope: NULL
has been replaced by ‘climate’
- d18O (S2LRcAxAsRumAY): interpretation1_scope: NULL has been replaced
by ‘climate’
- d18O (S2LRcAxAsRumAY): interpretation1_variable: NULL has been
replaced by ‘Mixed’
- hasAragoniteCorrection (S2LRE2r17qo3k7): interpretation1_scope: NULL
has been replaced by ‘climate’
- sisalSampleID (S2LRf7sdVcjCrX): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OPrecisionComposite (S2LRFrwQpQMu2S): interpretation1_scope: NULL
has been replaced by ‘climate’
- entityName (S2LRgAIdU9Q4hK): interpretation1_scope: NULL has been
replaced by ‘climate’
- d13CComposite (S2LRH6E7LPSxii): interpretation1_scope: NULL has been
replaced by ‘climate’
- d13CStandard (S2LRHmQn7pTexx): interpretation1_scope: NULL has been
replaced by ‘climate’
- sisalSampleID (S2LRiQ9cUMoB97): interpretation1_scope: NULL has been
replaced by ‘climate’
- d13C (S2LRIvTlMubKNo): interpretation1_scope: NULL has been replaced
by ‘climate’
- d13CPrecision (S2LRjSd4iMvS1c): interpretation1_scope: NULL has been
replaced by ‘climate’
- d13C (S2LRJVZt4Oq0uG): interpretation1_scope: NULL has been replaced
by ‘climate’
- d13C (S2LRJVZt4Oq0uG): interpretation1_variable: NULL has been
replaced by ‘Mixed’
- d13C (S2LRJVZt4Oq0uG): interpretation1_variableDetail: NULL has been
replaced by ‘Vegetation’
- d18OStandard (S2LRkpzSe7q6Dv): interpretation1_scope: NULL has been
replaced by ‘climate’
- d13CPrecision (S2LRlAVi6xrvTy): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OPrecision (S2LRmX9OApUPsJ): interpretation1_scope: NULL has been
replaced by ‘climate’
- hasAragoniteCorrection (S2LRN7HZ0pn2f3): interpretation1_scope: NULL
has been replaced by ‘climate’
- d18O (S2LRNDNiKrHu9d): interpretation1_scope: NULL has been replaced
by ‘climate’
- d18O (S2LRNDNiKrHu9d): interpretation1_variable: NULL has been
replaced by ‘Mixed’
- d18OStandard (S2LRnW1x1EMzQO): interpretation1_scope: NULL has been
replaced by ‘climate’
- sisalSampleIDComposite (S2LRp2xpDL8ljx): interpretation1_scope: NULL
has been replaced by ‘climate’
- hasAragoniteCorrection (S2LRP37crMW0ke): interpretation1_scope: NULL
has been replaced by ‘climate’
- d18OStandardComposite (S2LRp3x1cebYmn): interpretation1_scope: NULL
has been replaced by ‘climate’
- d13CStandard (S2LRQBWVTkvUtl): interpretation1_scope: NULL has been
replaced by ‘climate’
- mineralogy (S2LRQHH7ybsJbN): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OStandard (S2LRqIpk9O1m22): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OComposite (S2LRRTKpglN3T5): interpretation1_scope: NULL has been
replaced by ‘climate’
- hasAragoniteCorrectionComposite (S2LRrzdQxKXB0F):
interpretation1_scope: NULL has been replaced by ‘climate’
- mineralogy (S2LRvqXOzX6P3Q): interpretation1_scope: NULL has been
replaced by ‘climate’
- depthComposite (S2LRWCcYfwgDyV): interpretation1_scope: NULL has
been replaced by ‘climate’
- d18O (S2LRWXzjV7rqs9): interpretation1_scope: NULL has been replaced
by ‘climate’
- mineralogyComposite (S2LRX4pi03GUML): interpretation1_scope: NULL
has been replaced by ‘climate’
- sisalSampleID (S2LRyCVyJbLCxE): interpretation1_scope: NULL has been
replaced by ‘climate’
- Paleo Column metadata:
- d13C (S2LRBCzk3hPPAC): paleoData_notes: NULL has been replaced by
‘“d13C increase, which could be due to variation in limestone disolution
proceses posibly linked with a vegetation change” (Gentry et al.,
1999)); “The δ13C in Han-9 is controlled by changes in vegetation
assembly above the cave…To summarize, the control on Han-9 δ13C
variations is the amount of biogenic CO2 in the soil, caused by changes
in the vegetation type above the cave (forest/grasses), which is
directly linked to climate. Lower, depleted δ13C values oc- cur during
warmer and wetter periods, when vegetation is dominated by temperate
trees. Higher, enriched δ13C values of speleothem calcite correspond
with a higher abundance of grasses above the cave during colder/dryer
climate intervals.” (Vansteenberge et al., 2016)’
- d13C (S2LRBCzk3hPPAC): paleoData_QCCertification: NULL has been
replaced by ‘CH’
- d18O (S2LRcAxAsRumAY): paleoData_notes: NULL has been replaced by
‘“Tem- perature and precipitation (through the amount effect) con- trols
are thus expected to contribute most to the speleothem δ18O variability,
but as this record covers an interglacial– glacial transition, other
processes acting on longer timescales (i.e., fluctuations in global ice
volume) should also be con- sidered. A significant contribution is to be
expected from the variations in δ18O of the source,” (Vansteenberge et
al., 2016)’
- d18O (S2LRcAxAsRumAY): paleoData_QCCertification: NULL has been
replaced by ‘CH’
- d13C (S2LRJVZt4Oq0uG): paleoData_notes: NULL has been replaced by
‘“d13C increase, which could be due to variation in limestone disolution
proceses posibly linked with a vegetation change” (Gentry et al.,
1999)); “The δ13C in Han-9 is controlled by changes in vegetation
assembly above the cave…To summarize, the control on Han-9 δ13C
variations is the amount of biogenic CO2 in the soil, caused by changes
in the vegetation type above the cave (forest/grasses), which is
directly linked to climate. Lower, depleted δ13C values oc- cur during
warmer and wetter periods, when vegetation is dominated by temperate
trees. Higher, enriched δ13C values of speleothem calcite correspond
with a higher abundance of grasses above the cave during colder/dryer
climate intervals.” (Vansteenberge et al., 2016)’
- d13C (S2LRJVZt4Oq0uG): paleoData_QCCertification: NULL has been
replaced by ‘CH’
- d18O (S2LRNDNiKrHu9d): paleoData_notes: NULL has been replaced by
‘“Tem- perature and precipitation (through the amount effect) con- trols
are thus expected to contribute most to the speleothem δ18O variability,
but as this record covers an interglacial– glacial transition, other
processes acting on longer timescales (i.e., fluctuations in global ice
volume) should also be con- sidered. A significant contribution is to be
expected from the variations in δ18O of the source,” (Vansteenberge et
al., 2016)’
- d18O (S2LRNDNiKrHu9d): paleoData_QCCertification: NULL has been
replaced by ‘CH’
Version: 1.0.0
- curator: nick
- timestamp: 2020-09-29 14:24:07 UTC
- notes: Created from SISALv2