Version history for f59qj3Lt5K0fwOjppGym -
CuevaVictoria.Budsky.2019
Version: 1.0.13
- lastVersion: 1.0.12
- curator: nicholas
- timestamp: 2025-06-25 22:46:03.93893 UTC
- changes:
- Paleo Interpretation metadata:
- d13C (S2LR64Q0qhBLAC): interpretation1_seasonality: ‘((( null )))
3,4,5,6,7,8 /// Mar-Aug’ has been replaced by ‘Mar-Aug’
- d13C (S2LR64Q0qhBLAC): interpretation1_seasonalityGeneral: ‘((( null
))) Summer /// summerOnly’ has been replaced by ‘summerOnly’
- d13C (S2LR64Q0qhBLAC): interpretation1_variable: ‘((( null ))) P-E
/// effectivePrecipitation’ has been replaced by
‘effectivePrecipitation’
- d18O (S2LRwIx2rupVpo): interpretation1_variable: ‘((( null ))) T ///
temperature’ has been replaced by ‘temperature’
Version: 1.0.12
- lastVersion: 1.0.11
- curator: nicholas
- timestamp: 2025-06-25 21:21:44.071499 UTC
- changes:
- Paleo Interpretation metadata:
- d13C (S2LR64Q0qhBLAC): interpretation1_seasonality: ‘Mar-Aug’ has
been replaced by ‘((( null ))) 3,4,5,6,7,8 /// Mar-Aug’
- d13C (S2LR64Q0qhBLAC): interpretation1_seasonalityGeneral:
‘summerOnly’ has been replaced by ‘((( null ))) Summer ///
summerOnly’
- d13C (S2LR64Q0qhBLAC): interpretation1_variable:
‘effectivePrecipitation’ has been replaced by ‘((( null ))) P-E ///
effectivePrecipitation’
- d18O (S2LRwIx2rupVpo): interpretation1_variable: ‘temperature’ has
been replaced by ‘((( null ))) T /// temperature’
- Paleo Column metadata:
- d13C (S2LR64Q0qhBLAC): paleoData_meetsHoloceneHydroclimateCriteria:
NULL has been replaced by ‘TRUE’
- d13C (S2LR64Q0qhBLAC): paleoData_primaryTimeseries: NULL has been
replaced by ‘TRUE’
- d18O (S2LRwIx2rupVpo): paleoData_notes: ‘“On shorter timescale, we
cannot disentangle the different pro- cesses influencing the Speleothem
δ18O signal. However, on multi-millennial to orbital timescales, δ18O
values are mainly influenced by North Atlantic temperature changes and
seasonal- ity…In summary, although we cannot disentangle the processes
affecting the flowstone δ18O values and the interpretation of the δ18O
record of the CV flowstone remains challenging, we assume that the δ18O
values of the CV flowstone on orbital timescales and during the late
Glacial might be related to temperature changes on the North Atlantic,
which is supported by the good agreement with the SST records. However,
the influence of other parameters, such as seasonality of rainfall,
rainfall amount and changes in moisture source(s), cannot be excluded.
For the period from 10.5 ± 0.35 to 7.8 ± 0.2 ka, higher growth rates
coincide with lower δ18O values, which suggest an additional influence
of changes in the amount of autumn/winter precipita- tion on millennial
timescales.” (Budsky et al., 2019)’ has been replaced by ‘((( null )))
“On shorter timescale, we cannot disentangle the different pro- cesses
influencing the speleothem δ18O signal. However, on multi-millennial to
orbital timescales, δ18O values are mainly influenced by North Atlantic
temperature changes and seasonal- ity…In summary, although we cannot
disentangle the processes affecting the flowstone δ18O values and the
interpretation of the δ18O record of the CV flowstone remains
challenging, we assume that the δ18O values of the CV flowstone on
orbital timescales and during the late Glacial might be related to
temperature changes on the North Atlantic, which is supported by the
good agreement with the SST records. However, the influence of other
parameters, such as seasonality of rainfall, rainfall amount and changes
in moisture source(s), cannot be excluded. For the period from 10.5 ±
0.35 to 7.8 ± 0.2 ka, higher growth rates coincide with lower δ18O
values, which suggest an additional influence of changes in the amount
of autumn/winter precipita- tion on millennial timescales.” (Budsky et
al., 2019) /// “On shorter timescale, we cannot disentangle the
different pro- cesses influencing the Speleothem δ18O signal. However,
on multi-millennial to orbital timescales, δ18O values are mainly
influenced by North Atlantic temperature changes and seasonal- ity…In
summary, although we cannot disentangle the processes affecting the
flowstone δ18O values and the interpretation of the δ18O record of the
CV flowstone remains challenging, we assume that the δ18O values of the
CV flowstone on orbital timescales and during the late Glacial might be
related to temperature changes on the North Atlantic, which is supported
by the good agreement with the SST records. However, the influence of
other parameters, such as seasonality of rainfall, rainfall amount and
changes in moisture source(s), cannot be excluded. For the period from
10.5 ± 0.35 to 7.8 ± 0.2 ka, higher growth rates coincide with lower
δ18O values, which suggest an additional influence of changes in the
amount of autumn/winter precipita- tion on millennial timescales.”
(Budsky et al., 2019)’
- d18O (S2LRwIx2rupVpo): paleoData_meetsHoloceneHydroclimateCriteria:
NULL has been replaced by ‘TRUE’
- d18O (S2LRwIx2rupVpo): paleoData_primaryTimeseries: NULL has been
replaced by ‘TRUE’
Version: 1.0.11
- lastVersion: 1.0.10
- curator: nicholas
- timestamp: 2025-04-11 16:15:29.809636 UTC
- changes:
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Version: 1.0.10
- lastVersion: 1.0.9
- curator: nicholas
- timestamp: 2023-08-10 22:47:02 UTC
- changes:
- Base metadata:
- Publication metadata:
- pub1_author: NULL has been replaced by ‘Alexander Budsky and Denis
Scholz and Jasper A Wassenburg and Regina Mertz-Kraus and Christoph
Spötl and Dana FC Riechelmann and Luis Gibert and Klaus Peter Jochum
and Meinrat O Andreae’
- pub1_journal: NULL has been replaced by ‘The Holocene’
- pub1_pages: NULL has been replaced by ‘1113–1133’
- pub1_title: NULL has been replaced by ‘Speleothem \(updelta\)\(less\)sup$greater\(13\)less\(/sup\)greater$C record suggests enhanced
spring/summer drought in south-eastern Spain between 9.7 and 7.8 ka
{textendash} A circum-Western Mediterranean anomaly?’
Version: 1.0.9
- lastVersion: 1.0.8
- curator: nicholas
- timestamp: 2023-03-29 19:44:46 UTC
- changes:
- Paleo Column metadata:
- d13C (S2LR64Q0qhBLAC): paleoData_notes: ‘((( “��13C values reflect
the vegetation density and microbiological activity in the soil and are
therefore a spring to summer signal…the ��13C values of the CV flowstone
should be a sensitive proxy for past spring and summer drought even if
aquifer recharge and flow- stone growth predominantly occur during the
autumn and winter season (Carrasco et al., 2006). Therefore, we
interpret the ��13C values as a proxy for soil microbial activity and
vegetation den- sity reflecting changes in the length of the vegetation
period and, thus, spring/summer drought.” (Budsky et al., 2019) )))
“δ13C values reflect the vegetation density and microbiological activity
in the soil and are therefore a spring to summer signal…the δ13C values
of the CV flowstone should be a sensitive proxy for past spring and
summer drought even if aquifer recharge and flow- stone growth
predominantly occur during the autumn and winter season (Carrasco et
al., 2006). Therefore, we interpret the δ13C values as a proxy for soil
microbial activity and vegetation den- sity reflecting changes in the
length of the vegetation period and, thus, spring/summer drought.”
(Budsky et al., 2019) /// “δ13C values reflect the vegetation density
and microbiological activity in the soil and are therefore a spring to
summer signal…the δ13C values of the CV flowstone should be a sensitive
proxy for past spring and summer drought even if aquifer recharge and
flow- stone growth predominantly occur during the autumn and winter
season (Carrasco et al., 2006). Therefore, we interpret the δ13C values
as a proxy for soil microbial activity and vegetation den- sity
reflecting changes in the length of the vegetation period and, thus,
spring/summer drought.” (Budsky et al., 2019)’ has been replaced by
‘“δ13C values reflect the vegetation density and microbiological
activity in the soil and are therefore a spring to summer signal…the
δ13C values of the CV flowstone should be a sensitive proxy for past
spring and summer drought even if aquifer recharge and flow- stone
growth predominantly occur during the autumn and winter season (Carrasco
et al., 2006). Therefore, we interpret the δ13C values as a proxy for
soil microbial activity and vegetation den- sity reflecting changes in
the length of the vegetation period and, thus, spring/summer drought.”
(Budsky et al., 2019)’
- d18O (S2LRwIx2rupVpo): paleoData_notes: ‘((( “On shorter timescale,
we cannot disentangle the different pro- cesses influencing the
Speleothem ��18O signal. However, on multi-millennial to orbital
timescales, ��18O values are mainly influenced by North Atlantic
temperature changes and seasonal- ity…In summary, although we cannot
disentangle the processes affecting the flowstone ��18O values and the
interpretation of the ��18O record of the CV flowstone remains
challenging, we assume that the ��18O values of the CV flowstone on
orbital timescales and during the late Glacial might be related to
temperature changes on the North Atlantic, which is supported by the
good agreement with the SST records. However, the influence of other
parameters, such as seasonality of rainfall, rainfall amount and changes
in moisture source(s), cannot be excluded. For the period from 10.5 ��
0.35 to 7.8 �� 0.2 ka, higher growth rates coincide with lower ��18O
values, which suggest an additional influence of changes in the amount
of autumn/winter precipita- tion on millennial timescales.” (Budsky et
al., 2019) ))) “On shorter timescale, we cannot disentangle the
different pro- cesses influencing the Speleothem δ18O signal. However,
on multi-millennial to orbital timescales, δ18O values are mainly
influenced by North Atlantic temperature changes and seasonal- ity…In
summary, although we cannot disentangle the processes affecting the
flowstone δ18O values and the interpretation of the δ18O record of the
CV flowstone remains challenging, we assume that the δ18O values of the
CV flowstone on orbital timescales and during the late Glacial might be
related to temperature changes on the North Atlantic, which is supported
by the good agreement with the SST records. However, the influence of
other parameters, such as seasonality of rainfall, rainfall amount and
changes in moisture source(s), cannot be excluded. For the period from
10.5 ± 0.35 to 7.8 ± 0.2 ka, higher growth rates coincide with lower
δ18O values, which suggest an additional influence of changes in the
amount of autumn/winter precipita- tion on millennial timescales.”
(Budsky et al., 2019) /// “On shorter timescale, we cannot disentangle
the different pro- cesses influencing the Speleothem δ18O signal.
However, on multi-millennial to orbital timescales, δ18O values are
mainly influenced by North Atlantic temperature changes and seasonal-
ity…In summary, although we cannot disentangle the processes affecting
the flowstone δ18O values and the interpretation of the δ18O record of
the CV flowstone remains challenging, we assume that the δ18O values of
the CV flowstone on orbital timescales and during the late Glacial might
be related to temperature changes on the North Atlantic, which is
supported by the good agreement with the SST records. However, the
influence of other parameters, such as seasonality of rainfall, rainfall
amount and changes in moisture source(s), cannot be excluded. For the
period from 10.5 ± 0.35 to 7.8 ± 0.2 ka, higher growth rates coincide
with lower δ18O values, which suggest an additional influence of changes
in the amount of autumn/winter precipita- tion on millennial
timescales.” (Budsky et al., 2019)’ has been replaced by ‘“On shorter
timescale, we cannot disentangle the different pro- cesses influencing
the Speleothem δ18O signal. However, on multi-millennial to orbital
timescales, δ18O values are mainly influenced by North Atlantic
temperature changes and seasonal- ity…In summary, although we cannot
disentangle the processes affecting the flowstone δ18O values and the
interpretation of the δ18O record of the CV flowstone remains
challenging, we assume that the δ18O values of the CV flowstone on
orbital timescales and during the late Glacial might be related to
temperature changes on the North Atlantic, which is supported by the
good agreement with the SST records. However, the influence of other
parameters, such as seasonality of rainfall, rainfall amount and changes
in moisture source(s), cannot be excluded. For the period from 10.5 ±
0.35 to 7.8 ± 0.2 ka, higher growth rates coincide with lower δ18O
values, which suggest an additional influence of changes in the amount
of autumn/winter precipita- tion on millennial timescales.” (Budsky et
al., 2019)’
- Paleo Interpretation metadata:
- d13C (S2LR64Q0qhBLAC): interpretation1_variable: ‘P-E’ has been
replaced by ‘effectivePrecipitation’
Version: 1.0.8
- lastVersion: 1.0.7
- curator: nicholas
- timestamp: 2023-02-13 23:40:23 UTC
- changes:
- Paleo Interpretation metadata:
- uncertaintyHigh (S2LR23SuZHg2tm): interpretation1_scope: NULL has
been replaced by ‘climate’
- uncertaintyHigh (S2LRCjzWuimmkl): interpretation1_scope: NULL has
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- Paleo Column metadata:
- d13C (S2LR64Q0qhBLAC): paleoData_notes: ‘“δ13C values reflect the
vegetation density and microbiological activity in the soil and are
therefore a spring to summer signal…the δ13C values of the CV flowstone
should be a sensitive proxy for past spring and summer drought even if
aquifer recharge and flow- stone growth predominantly occur during the
autumn and winter season (Carrasco et al., 2006). Therefore, we
interpret the δ13C values as a proxy for soil microbial activity and
vegetation den- sity reflecting changes in the length of the vegetation
period and, thus, spring/summer drought.” (Budsky et al., 2019)’ has
been replaced by ‘((( “��13C values reflect the vegetation density and
microbiological activity in the soil and are therefore a spring to
summer signal…the ��13C values of the CV flowstone should be a sensitive
proxy for past spring and summer drought even if aquifer recharge and
flow- stone growth predominantly occur during the autumn and winter
season (Carrasco et al., 2006). Therefore, we interpret the ��13C values
as a proxy for soil microbial activity and vegetation den- sity
reflecting changes in the length of the vegetation period and, thus,
spring/summer drought.” (Budsky et al., 2019) ))) “δ13C values reflect
the vegetation density and microbiological activity in the soil and are
therefore a spring to summer signal…the δ13C values of the CV flowstone
should be a sensitive proxy for past spring and summer drought even if
aquifer recharge and flow- stone growth predominantly occur during the
autumn and winter season (Carrasco et al., 2006). Therefore, we
interpret the δ13C values as a proxy for soil microbial activity and
vegetation den- sity reflecting changes in the length of the vegetation
period and, thus, spring/summer drought.” (Budsky et al., 2019) ///
“δ13C values reflect the vegetation density and microbiological activity
in the soil and are therefore a spring to summer signal…the δ13C values
of the CV flowstone should be a sensitive proxy for past spring and
summer drought even if aquifer recharge and flow- stone growth
predominantly occur during the autumn and winter season (Carrasco et
al., 2006). Therefore, we interpret the δ13C values as a proxy for soil
microbial activity and vegetation den- sity reflecting changes in the
length of the vegetation period and, thus, spring/summer drought.”
(Budsky et al., 2019)’
- d18O (S2LRwIx2rupVpo): paleoData_notes: ‘“On shorter timescale, we
cannot disentangle the different pro- cesses influencing the Speleothem
δ18O signal. However, on multi-millennial to orbital timescales, δ18O
values are mainly influenced by North Atlantic temperature changes and
seasonal- ity…In summary, although we cannot disentangle the processes
affecting the flowstone δ18O values and the interpretation of the δ18O
record of the CV flowstone remains challenging, we assume that the δ18O
values of the CV flowstone on orbital timescales and during the late
Glacial might be related to temperature changes on the North Atlantic,
which is supported by the good agreement with the SST records. However,
the influence of other parameters, such as seasonality of rainfall,
rainfall amount and changes in moisture source(s), cannot be excluded.
For the period from 10.5 ± 0.35 to 7.8 ± 0.2 ka, higher growth rates
coincide with lower δ18O values, which suggest an additional influence
of changes in the amount of autumn/winter precipita- tion on millennial
timescales.” (Budsky et al., 2019)’ has been replaced by ‘((( “On
shorter timescale, we cannot disentangle the different pro- cesses
influencing the Speleothem ��18O signal. However, on multi-millennial to
orbital timescales, ��18O values are mainly influenced by North Atlantic
temperature changes and seasonal- ity…In summary, although we cannot
disentangle the processes affecting the flowstone ��18O values and the
interpretation of the ��18O record of the CV flowstone remains
challenging, we assume that the ��18O values of the CV flowstone on
orbital timescales and during the late Glacial might be related to
temperature changes on the North Atlantic, which is supported by the
good agreement with the SST records. However, the influence of other
parameters, such as seasonality of rainfall, rainfall amount and changes
in moisture source(s), cannot be excluded. For the period from 10.5 ��
0.35 to 7.8 �� 0.2 ka, higher growth rates coincide with lower ��18O
values, which suggest an additional influence of changes in the amount
of autumn/winter precipita- tion on millennial timescales.” (Budsky et
al., 2019) ))) “On shorter timescale, we cannot disentangle the
different pro- cesses influencing the Speleothem δ18O signal. However,
on multi-millennial to orbital timescales, δ18O values are mainly
influenced by North Atlantic temperature changes and seasonal- ity…In
summary, although we cannot disentangle the processes affecting the
flowstone δ18O values and the interpretation of the δ18O record of the
CV flowstone remains challenging, we assume that the δ18O values of the
CV flowstone on orbital timescales and during the late Glacial might be
related to temperature changes on the North Atlantic, which is supported
by the good agreement with the SST records. However, the influence of
other parameters, such as seasonality of rainfall, rainfall amount and
changes in moisture source(s), cannot be excluded. For the period from
10.5 ± 0.35 to 7.8 ± 0.2 ka, higher growth rates coincide with lower
δ18O values, which suggest an additional influence of changes in the
amount of autumn/winter precipita- tion on millennial timescales.”
(Budsky et al., 2019) /// “On shorter timescale, we cannot disentangle
the different pro- cesses influencing the Speleothem δ18O signal.
However, on multi-millennial to orbital timescales, δ18O values are
mainly influenced by North Atlantic temperature changes and seasonal-
ity…In summary, although we cannot disentangle the processes affecting
the flowstone δ18O values and the interpretation of the δ18O record of
the CV flowstone remains challenging, we assume that the δ18O values of
the CV flowstone on orbital timescales and during the late Glacial might
be related to temperature changes on the North Atlantic, which is
supported by the good agreement with the SST records. However, the
influence of other parameters, such as seasonality of rainfall, rainfall
amount and changes in moisture source(s), cannot be excluded. For the
period from 10.5 ± 0.35 to 7.8 ± 0.2 ka, higher growth rates coincide
with lower δ18O values, which suggest an additional influence of changes
in the amount of autumn/winter precipita- tion on millennial
timescales.” (Budsky et al., 2019)’
Version: 1.0.6
- lastVersion: 1.0.5
- curator: nicholas
- timestamp: 2022-07-28 17:29:43 UTC
- changes:
- Geographic metadata:
- geo_elevation: ‘75’ has been replaced by NULL
Version: 1.0.5
- lastVersion: 1.0.4
- curator: nicholas
- timestamp: 2022-07-15 22:59:48 UTC
- changes:
- Paleo Interpretation metadata:
- mineralogy (S2LR2VpUt8ryEN): interpretation1_scope: NULL has been
replaced by ‘climate’
- d13CStandard (S2LR5k5cHtgPV7): interpretation1_scope: NULL has been
replaced by ‘climate’
- hasAragoniteCorrection (S2LRDR6YC9Wzjk): interpretation1_scope: NULL
has been replaced by ‘climate’
- d18OStandard (S2LRKAhyygYbB5): interpretation1_scope: NULL has been
replaced by ‘climate’
- sisalSampleID (S2LROlJkEjS9Fh): interpretation1_scope: NULL has been
replaced by ‘climate’
- d13CPrecision (S2LRuPbC0k2YQw): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OPrecision (S2LRyz0yLvk0am): interpretation1_scope: NULL has been
replaced by ‘climate’
Version: 1.0.4
- lastVersion: 1.0.3
- curator: nicholas
- timestamp: 2022-05-18 00:25:15 UTC
- changes:
- Paleo Column metadata:
- ageBaconUncertaintyHigh (S2LR23SuZHg2tm): paleoData_units: ‘yr BP’
has been replaced by ‘BP’
- ageBaconUncertaintyHigh (S2LR23SuZHg2tm): paleoData_unitsOriginal:
NULL has been replaced by ‘yr BP’
- d13C (S2LR64Q0qhBLAC): paleoData_proxyLumps: NULL has been replaced
by ‘isotope’
- d13C (S2LR64Q0qhBLAC): paleoData_proxyLumpsOriginal: NULL has been
replaced by ‘d13C’
- ageUncertaintyHigh (S2LRCjzWuimmkl): paleoData_units: ‘yr BP’ has
been replaced by ‘BP’
- ageUncertaintyHigh (S2LRCjzWuimmkl): paleoData_unitsOriginal: NULL
has been replaced by ‘yr BP’
- ageBchronUncertaintyHigh (S2LRcV1AcpxqJY): paleoData_units: ‘yr BP’
has been replaced by ‘BP’
- ageBchronUncertaintyHigh (S2LRcV1AcpxqJY): paleoData_unitsOriginal:
NULL has been replaced by ‘yr BP’
- ageBacon (S2LRFYPM2WuDGW): paleoData_units: ‘yr BP’ has been
replaced by ‘BP’
- ageBacon (S2LRFYPM2WuDGW): paleoData_unitsOriginal: NULL has been
replaced by ‘yr BP’
- ageStalAgeUncertaintyLow (S2LRksYsm3oIWC): paleoData_units: ‘yr BP’
has been replaced by ‘BP’
- ageStalAgeUncertaintyLow (S2LRksYsm3oIWC): paleoData_unitsOriginal:
NULL has been replaced by ‘yr BP’
- ageStalAge (S2LRmJHRHpp24z): paleoData_units: ‘yr BP’ has been
replaced by ‘BP’
- ageStalAge (S2LRmJHRHpp24z): paleoData_unitsOriginal: NULL has been
replaced by ‘yr BP’
- ageBaconUncertaintyLow (S2LRtPVFvN10Pd): paleoData_units: ‘yr BP’
has been replaced by ‘BP’
- ageBaconUncertaintyLow (S2LRtPVFvN10Pd): paleoData_unitsOriginal:
NULL has been replaced by ‘yr BP’
- ageBchron (S2LRtwRfO7sqi5): paleoData_units: ‘yr BP’ has been
replaced by ‘BP’
- ageBchron (S2LRtwRfO7sqi5): paleoData_unitsOriginal: NULL has been
replaced by ‘yr BP’
- ageBchronUncertaintyLow (S2LRuGVy3afygQ): paleoData_units: ‘yr BP’
has been replaced by ‘BP’
- ageBchronUncertaintyLow (S2LRuGVy3afygQ): paleoData_unitsOriginal:
NULL has been replaced by ‘yr BP’
- age (S2LRVNoGLHhMnq): paleoData_units: ‘yr BP’ has been replaced by
‘BP’
- age (S2LRVNoGLHhMnq): paleoData_unitsOriginal: NULL has been
replaced by ‘yr BP’
- ageUncertaintyLow (S2LRwAeFTzzH2W): paleoData_units: ‘yr BP’ has
been replaced by ‘BP’
- ageUncertaintyLow (S2LRwAeFTzzH2W): paleoData_unitsOriginal: NULL
has been replaced by ‘yr BP’
- d18O (S2LRwIx2rupVpo): paleoData_proxyLumps: NULL has been replaced
by ‘isotope’
- d18O (S2LRwIx2rupVpo): paleoData_proxyLumpsOriginal: NULL has been
replaced by ‘d18O’
- ageStalAgeUncertaintyHigh (S2LRYgesMl2OtQ): paleoData_units: ‘yr BP’
has been replaced by ‘BP’
- ageStalAgeUncertaintyHigh (S2LRYgesMl2OtQ): paleoData_unitsOriginal:
NULL has been replaced by ‘yr BP’
- Paleo Interpretation metadata:
- mineralogy (S2LR2VpUt8ryEN): interpretation1_scope: ‘climate’ has
been replaced by NULL
- d13CStandard (S2LR5k5cHtgPV7): interpretation1_scope: ‘climate’ has
been replaced by NULL
- d13C (S2LR64Q0qhBLAC): interpretation1_variableGroup: NULL has been
replaced by ‘P-E’
- hasAragoniteCorrection (S2LRDR6YC9Wzjk): interpretation1_scope:
‘climate’ has been replaced by NULL
- d18OStandard (S2LRKAhyygYbB5): interpretation1_scope: ‘climate’ has
been replaced by NULL
- sisalSampleID (S2LROlJkEjS9Fh): interpretation1_scope: ‘climate’ has
been replaced by NULL
- d13CPrecision (S2LRuPbC0k2YQw): interpretation1_scope: ‘climate’ has
been replaced by NULL
- d18O (S2LRwIx2rupVpo): interpretation1_variableGroup: NULL has been
replaced by ‘Temperature’
- d18O (S2LRwIx2rupVpo): interpretation1_variableGroupDirection: NULL
has been replaced by ‘negative’
- d18O (S2LRwIx2rupVpo): interpretation1_variableGroupOriginal: NULL
has been replaced by ‘T’
- d18OPrecision (S2LRyz0yLvk0am): interpretation1_scope: ‘climate’ has
been replaced by NULL
- Chron Column metadata:
- age_type (S2LcRaRsY3dz7ZL): chronData_variableName: ‘ageType’ has
been replaced by ‘age_type’
- age_type (S2LcRaRsY3dz7ZL): chronData_variableNameOriginal: NULL has
been replaced by ‘ageType’
Version: 1.0.3
- lastVersion: 1.0.2
- curator: nicholas
- timestamp: 2021-10-05 21:38:53 UTC
- changes:
- Geographic metadata:
- geo_gcmdLocation: NULL has been replaced by ‘Europe>Southern
Europe>Spain’
Version: 1.0.2
- lastVersion: 1.0.1
- curator: nick
- timestamp: 2021-03-17 01:52:29 UTC
- changes:
- Base metadata:
- archiveType: ‘speleothem’ has been replaced by ‘Speleothem’
- Paleo Interpretation metadata:
- d13C (S2LR64Q0qhBLAC): interpretation1_seasonalityGeneral: ‘Summer’
has been replaced by ‘summerOnly’
- Paleo Column metadata:
- d18O (S2LRwIx2rupVpo): paleoData_notes: ‘“On shorter timescale, we
cannot disentangle the different pro- cesses influencing the speleothem
δ18O signal. However, on multi-millennial to orbital timescales, δ18O
values are mainly influenced by North Atlantic temperature changes and
seasonal- ity…In summary, although we cannot disentangle the processes
affecting the flowstone δ18O values and the interpretation of the δ18O
record of the CV flowstone remains challenging, we assume that the δ18O
values of the CV flowstone on orbital timescales and during the late
Glacial might be related to temperature changes on the North Atlantic,
which is supported by the good agreement with the SST records. However,
the influence of other parameters, such as seasonality of rainfall,
rainfall amount and changes in moisture source(s), cannot be excluded.
For the period from 10.5 ± 0.35 to 7.8 ± 0.2 ka, higher growth rates
coincide with lower δ18O values, which suggest an additional influence
of changes in the amount of autumn/winter precipita- tion on millennial
timescales.” (Budsky et al., 2019)’ has been replaced by ‘“On shorter
timescale, we cannot disentangle the different pro- cesses influencing
the Speleothem δ18O signal. However, on multi-millennial to orbital
timescales, δ18O values are mainly influenced by North Atlantic
temperature changes and seasonal- ity…In summary, although we cannot
disentangle the processes affecting the flowstone δ18O values and the
interpretation of the δ18O record of the CV flowstone remains
challenging, we assume that the δ18O values of the CV flowstone on
orbital timescales and during the late Glacial might be related to
temperature changes on the North Atlantic, which is supported by the
good agreement with the SST records. However, the influence of other
parameters, such as seasonality of rainfall, rainfall amount and changes
in moisture source(s), cannot be excluded. For the period from 10.5 ±
0.35 to 7.8 ± 0.2 ka, higher growth rates coincide with lower δ18O
values, which suggest an additional influence of changes in the amount
of autumn/winter precipita- tion on millennial timescales.” (Budsky et
al., 2019)’
Version: 1.0.1
- lastVersion: 1.0.0
- curator: nick
- timestamp: 2021-01-12 02:28:45 UTC
- changes:
- Paleo Interpretation metadata:
- mineralogy (S2LR2VpUt8ryEN): interpretation1_scope: NULL has been
replaced by ‘climate’
- d13CStandard (S2LR5k5cHtgPV7): interpretation1_scope: NULL has been
replaced by ‘climate’
- d13C (S2LR64Q0qhBLAC): interpretation1_direction: NULL has been
replaced by ‘negative’
- d13C (S2LR64Q0qhBLAC): interpretation1_scope: NULL has been replaced
by ‘climate’
- d13C (S2LR64Q0qhBLAC): interpretation1_seasonality: NULL has been
replaced by ‘3,4,5,6,7,8’
- d13C (S2LR64Q0qhBLAC): interpretation1_seasonalityGeneral: NULL has
been replaced by ‘Summer’
- d13C (S2LR64Q0qhBLAC): interpretation1_variable: NULL has been
replaced by ‘P-E’
- d13C (S2LR64Q0qhBLAC): interpretation1_variableDetail: NULL has been
replaced by ‘@surface’
- hasAragoniteCorrection (S2LRDR6YC9Wzjk): interpretation1_scope: NULL
has been replaced by ‘climate’
- d18OStandard (S2LRKAhyygYbB5): interpretation1_scope: NULL has been
replaced by ‘climate’
- sisalSampleID (S2LROlJkEjS9Fh): interpretation1_scope: NULL has been
replaced by ‘climate’
- d13CPrecision (S2LRuPbC0k2YQw): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18O (S2LRwIx2rupVpo): interpretation1_scope: NULL has been replaced
by ‘climate’
- d18O (S2LRwIx2rupVpo): interpretation1_variable: NULL has been
replaced by ‘T’
- d18OPrecision (S2LRyz0yLvk0am): interpretation1_scope: NULL has been
replaced by ‘climate’
- Paleo Column metadata:
- d13C (S2LR64Q0qhBLAC): paleoData_notes: NULL has been replaced by
‘“δ13C values reflect the vegetation density and microbiological
activity in the soil and are therefore a spring to summer signal…the
δ13C values of the CV flowstone should be a sensitive proxy for past
spring and summer drought even if aquifer recharge and flow- stone
growth predominantly occur during the autumn and winter season (Carrasco
et al., 2006). Therefore, we interpret the δ13C values as a proxy for
soil microbial activity and vegetation den- sity reflecting changes in
the length of the vegetation period and, thus, spring/summer drought.”
(Budsky et al., 2019)’
- d13C (S2LR64Q0qhBLAC): paleoData_proxy: NULL has been replaced by
‘d13C’
- d13C (S2LR64Q0qhBLAC): paleoData_proxyDetail: NULL has been replaced
by ‘calcite’
- d13C (S2LR64Q0qhBLAC): paleoData_proxyGeneral: NULL has been
replaced by ‘isotope’
- d13C (S2LR64Q0qhBLAC): paleoData_QCCertification: NULL has been
replaced by ‘CH’
- d18O (S2LRwIx2rupVpo): paleoData_notes: NULL has been replaced by
‘“On shorter timescale, we cannot disentangle the different pro- cesses
influencing the speleothem δ18O signal. However, on multi-millennial to
orbital timescales, δ18O values are mainly influenced by North Atlantic
temperature changes and seasonal- ity…In summary, although we cannot
disentangle the processes affecting the flowstone δ18O values and the
interpretation of the δ18O record of the CV flowstone remains
challenging, we assume that the δ18O values of the CV flowstone on
orbital timescales and during the late Glacial might be related to
temperature changes on the North Atlantic, which is supported by the
good agreement with the SST records. However, the influence of other
parameters, such as seasonality of rainfall, rainfall amount and changes
in moisture source(s), cannot be excluded. For the period from 10.5 ±
0.35 to 7.8 ± 0.2 ka, higher growth rates coincide with lower δ18O
values, which suggest an additional influence of changes in the amount
of autumn/winter precipita- tion on millennial timescales.” (Budsky et
al., 2019)’
- d18O (S2LRwIx2rupVpo): paleoData_proxy: NULL has been replaced by
‘d18O’
- d18O (S2LRwIx2rupVpo): paleoData_proxyDetail: NULL has been replaced
by ‘calcite’
- d18O (S2LRwIx2rupVpo): paleoData_proxyGeneral: NULL has been
replaced by ‘isotope’
- d18O (S2LRwIx2rupVpo): paleoData_QCCertification: NULL has been
replaced by ‘CH’
Version: 1.0.0
- curator: nick
- timestamp: 2020-09-29 14:29:31 UTC
- notes: Created from SISALv2