Version history for bZLQf0iz5XeCyN8Fe3Ib -
PereNoelcave.Verheyden.2014
Version: 1.0.15
- lastVersion: 1.0.14
- curator: nicholas
- timestamp: 2025-06-25 22:46:32.076839 UTC
- changes:
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/// effectivePrecipitation’ has been replaced by
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Version: 1.0.14
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- curator: nicholas
- timestamp: 2025-06-25 21:22:14.6335 UTC
- changes:
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Version: 1.0.13
- lastVersion: 1.0.12
- curator: nicholas
- timestamp: 2025-04-11 16:27:13.776635 UTC
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Version: 1.0.12
- lastVersion: 1.0.11
- curator: nicholas
- timestamp: 2023-08-10 23:11:17 UTC
- changes:
- Base metadata:
- 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has been replaced by ‘Verheyden, S., Keppens, E., Quinif, Y., Cheng, H.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: NULL has
been replaced by ‘climate’
- uncertaintyLow (S2LR9DAMVk2hF0): interpretation1_scope: NULL has
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been replaced by ‘climate’
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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: NULL has been replaced by ‘230’
- Paleo Column metadata:
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Version: 1.0.7
- lastVersion: 1.0.6
- curator: nicholas
- timestamp: 2022-07-28 17:39:25 UTC
- changes:
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Version: 1.0.6
- lastVersion: 1.0.5
- curator: nicholas
- timestamp: 2022-07-15 23:08:33 UTC
- changes:
- Paleo Interpretation metadata:
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Version: 1.0.5
- lastVersion: 1.0.4
- curator: nicholas
- timestamp: 2022-05-18 00:29:05 UTC
- changes:
- Paleo Interpretation metadata:
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- d18OPrecision (S2LR2uU7iKZLIJ): interpretation1_scope: ‘climate’ has
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- d13CStandard (S2LRQ6jTuAh7Xw): interpretation1_scope: ‘climate’ has
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- agelinInterpUncertaintyHigh (S2LR6iWbJ6Ie95):
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- ageBaconUncertaintyHigh (S2LRaB26MmrAzh): paleoData_unitsOriginal:
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- agelinInterpUncertaintyLow (S2LRfpQK1AtSwB): paleoData_units: ‘yr
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- agelinInterpUncertaintyLow (S2LRfpQK1AtSwB):
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- ageStalAgeUncertaintyHigh (S2LRGY5ayanpuZ): paleoData_unitsOriginal:
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- ageBaconUncertaintyLow (S2LRtRoiaRzyp8): paleoData_units: ‘yr BP’
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- ageBaconUncertaintyLow (S2LRtRoiaRzyp8): paleoData_unitsOriginal:
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- ageBchron (S2LRU8QglDCUFs): paleoData_units: ‘yr BP’ has been
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- Chron Column metadata:
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- age_type (S2LcRZnPi4tt2K3): chronData_variableNameOriginal: NULL has
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Version: 1.0.4
- lastVersion: 1.0.3
- curator: nicholas
- timestamp: 2021-10-05 21:42:12 UTC
- changes:
- Geographic metadata:
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Version: 1.0.3
- lastVersion: 1.0.2
- curator: nick
- timestamp: 2021-04-13 02:35:48 UTC
- changes:
- Paleo Interpretation metadata:
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Version: 1.0.2
- lastVersion: 1.0.1
- curator: nick
- timestamp: 2021-03-17 01:56:47 UTC
- changes:
- Base metadata:
- archiveType: ‘speleothem’ has been replaced by ‘Speleothem’
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Version: 1.0.1
- lastVersion: 1.0.0
- curator: nick
- timestamp: 2021-01-12 02:29:30 UTC
- changes:
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- d18O (S2LR5E5HYoppj9): interpretation1_variable: NULL has been
replaced by ‘P-E’
- d18O (S2LR5E5HYoppj9): interpretation1_variableDetail: NULL has been
replaced by ‘infiltration’
- d13C (S2LR6dZP0RBWKz): interpretation1_direction: NULL has been
replaced by ‘negative’
- d13C (S2LR6dZP0RBWKz): interpretation1_scope: NULL has been replaced
by ‘climate’
- d13C (S2LR6dZP0RBWKz): interpretation1_seasonalityGeneral: NULL has
been replaced by ‘Annual’
- d13C (S2LR6dZP0RBWKz): interpretation1_variable: NULL has been
replaced by ‘P-E’
- d13C (S2LR6dZP0RBWKz): interpretation1_variableDetail: NULL has been
replaced by ‘infiltration’
- d18OStandard (S2LRDdJTOcv8eq): interpretation1_scope: NULL has been
replaced by ‘climate’
- sisalSampleID (S2LRgSlbbJADra): interpretation1_scope: NULL has been
replaced by ‘climate’
- d13CPrecision (S2LRip5obuHZID): interpretation1_scope: NULL has been
replaced by ‘climate’
- mineralogy (S2LROCBNGpbUPS): interpretation1_scope: NULL has been
replaced by ‘climate’
- d13CStandard (S2LRQ6jTuAh7Xw): interpretation1_scope: NULL has been
replaced by ‘climate’
- Paleo Column metadata:
- d18O (S2LR5E5HYoppj9): paleoData_notes: NULL 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: NULL has been replaced by
‘d18O’
- d18O (S2LR5E5HYoppj9): paleoData_proxyDetail: NULL has been replaced
by ‘calcite’
- d18O (S2LR5E5HYoppj9): paleoData_proxyGeneral: NULL has been
replaced by ‘isotope’
- d18O (S2LR5E5HYoppj9): paleoData_QCCertification: NULL has been
replaced by ‘CH’
- d13C (S2LR6dZP0RBWKz): paleoData_notes: NULL 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: NULL has been replaced by
‘d13C’
- d13C (S2LR6dZP0RBWKz): paleoData_proxyDetail: NULL has been replaced
by ‘calcite’
- d13C (S2LR6dZP0RBWKz): paleoData_proxyGeneral: NULL has been
replaced by ‘isotope’
- d13C (S2LR6dZP0RBWKz): paleoData_QCCertification: NULL has been
replaced by ‘CH’
Version: 1.0.0
- curator: nick
- timestamp: 2020-09-29 14:29:32 UTC
- notes: Created from SISALv2