Version history for 4P3DWsbxQmH3Mt3GqLHY -
Molinoscave.Moreno.2017
Version: 1.0.16
- lastVersion: 1.0.15
- curator: nicholas
- timestamp: 2025-06-25 23:23:03.159059 UTC
- notes: Updated lipdverse database entry with a changed
file.
- changes:
- Paleo Interpretation metadata:
- d13C (S2LRNALbQfTwNr): interpretation1_variable: ‘P-E’ has been
replaced by ‘effectivePrecipitation’
- d13C (S2LRoFTtnudhkp): interpretation1_variable: ‘P-E’ has been
replaced by ‘effectivePrecipitation’
Version: 1.0.15
- lastVersion: 1.0.14
- curator: nicholas
- timestamp: 2025-06-25 23:19:14.836946 UTC
- notes: Changes made as part of LiPDverse vocabulary
standardization process
- changes:
- Paleo Interpretation metadata:
- d13C (S2LRNALbQfTwNr): interpretation1_variable: ‘P-E’ has been
replaced by ‘effectivePrecipitation’
- d13C (S2LRoFTtnudhkp): interpretation1_variable: ‘P-E’ has been
replaced by ‘effectivePrecipitation’
Version: 1.0.14
- lastVersion: 1.0.13
- curator: nicholas
- timestamp: 2025-06-25 22:46:28.895307 UTC
- changes:
- Paleo Interpretation metadata:
- d13C (S2LRNALbQfTwNr): interpretation1_seasonality: ‘((( null )))
11,12,1,2,3,4 /// Winter’ has been replaced by ‘Winter’
- d13C (S2LRoFTtnudhkp): interpretation1_seasonality: ‘((( null )))
11,12,1,2,3,4 /// Winter’ has been replaced by ‘Winter’
Version: 1.0.13
- lastVersion: 1.0.12
- curator: nicholas
- timestamp: 2025-06-25 21:22:11.225275 UTC
- changes:
- Paleo Column metadata:
- d18O (S2LRELjmJhtZuf): paleoData_notes: ‘“The lack of correlation
among the δ18O and δ13C records in the three Speleothems, together with
the different factors influencing isotopic composition of rainfall in
the area (Moreno et al., 2014), including the variation in the moisture
source, makes the interpretation of Holocene δ18O records unrealistic in
terms of only one climate variable…. Thus, 18O profiles are not used
for paleoenvironmental/paleoclimate interpretations since the factors
influencing 18O record in Holocene Speleothems in this area are not yet
fully understood.” (Moreno et al., 2017)’ has been replaced by ‘((( null
))) “The lack of correlation among the δ18O and δ13C records in the
three speleothems, together with the different factors influencing
isotopic composition of rainfall in the area (Moreno et al., 2014),
including the variation in the moisture source, makes the interpretation
of Holocene δ18O records unrealistic in terms of only one climate
variable…. Thus, 18O profiles are not used for
paleoenvironmental/paleoclimate interpretations since the factors
influencing 18O record in Holocene speleothems in this area are not yet
fully understood.” (Moreno et al., 2017) /// “The lack of correlation
among the δ18O and δ13C records in the three Speleothems, together with
the different factors influencing isotopic composition of rainfall in
the area (Moreno et al., 2014), including the variation in the moisture
source, makes the interpretation of Holocene δ18O records unrealistic in
terms of only one climate variable…. Thus, 18O profiles are not used
for paleoenvironmental/paleoclimate interpretations since the factors
influencing 18O record in Holocene Speleothems in this area are not yet
fully understood.” (Moreno et al., 2017)’
- d18O (S2LRELjmJhtZuf): paleoData_meetsHoloceneHydroclimateCriteria:
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- d18O (S2LRELjmJhtZuf): paleoData_primaryTimeseries: NULL has been
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- d13C (S2LRNALbQfTwNr): paleoData_meetsHoloceneHydroclimateCriteria:
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- d13C (S2LRNALbQfTwNr): paleoData_primaryTimeseries: NULL has been
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- d18O (S2LRYz0ilzEvFP): paleoData_notes: ‘“The lack of correlation
among the δ18O and δ13C records in the three Speleothems, together with
the different factors influencing isotopic composition of rainfall in
the area (Moreno et al., 2014), including the variation in the moisture
source, makes the interpretation of Holocene δ18O records unrealistic in
terms of only one climate variable…. Thus, 18O profiles are not used
for paleoenvironmental/paleoclimate interpretations since the factors
influencing 18O record in Holocene Speleothems in this area are not yet
fully understood.” (Moreno et al., 2017)’ has been replaced by ‘((( null
))) “The lack of correlation among the δ18O and δ13C records in the
three speleothems, together with the different factors influencing
isotopic composition of rainfall in the area (Moreno et al., 2014),
including the variation in the moisture source, makes the interpretation
of Holocene δ18O records unrealistic in terms of only one climate
variable…. Thus, 18O profiles are not used for
paleoenvironmental/paleoclimate interpretations since the factors
influencing 18O record in Holocene speleothems in this area are not yet
fully understood.” (Moreno et al., 2017) /// “The lack of correlation
among the δ18O and δ13C records in the three Speleothems, together with
the different factors influencing isotopic composition of rainfall in
the area (Moreno et al., 2014), including the variation in the moisture
source, makes the interpretation of Holocene δ18O records unrealistic in
terms of only one climate variable…. Thus, 18O profiles are not used
for paleoenvironmental/paleoclimate interpretations since the factors
influencing 18O record in Holocene Speleothems in this area are not yet
fully understood.” (Moreno et al., 2017)’
- d18O (S2LRYz0ilzEvFP): paleoData_meetsHoloceneHydroclimateCriteria:
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- Paleo Interpretation metadata:
- d13C (S2LRNALbQfTwNr): interpretation1_seasonality: ‘Winter’ has
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Version: 1.0.11
- lastVersion: 1.0.10
- curator: nicholas
- timestamp: 2023-08-10 23:07:20 UTC
- changes:
- Base metadata:
- Publication metadata:
- pub1_author: NULL has been replaced by ‘Ana Moreno and Carlos
P{’{e}}rez-Mej{‘{i}}as and Miguel Bartolom{’{e}} and Carlos Sancho and
Isabel Cacho and Heather Stoll and Antonio Delgado-Huertas and John
Hellstrom and R. Lawrence Edwards and Hai Cheng’
- pub1_journal: NULL has been replaced by ‘Quaternary Research’
- pub1_pages: NULL has been replaced by ‘223–233’
- pub1_title: NULL has been replaced by ‘New speleothem data from
Molinos and Ejulve caves reveal Holocene hydrological variability in
northeast Iberia’
Version: 1.0.10
- lastVersion: 1.0.9
- curator: nicholas
- timestamp: 2023-03-29 19:58:04 UTC
- changes:
- Paleo Interpretation metadata:
- d13C (S2LRZ8aI3nEQ7d): interpretation1_variable: ‘P-E’ has been
replaced by ‘effectivePrecipitation’
Version: 1.0.9
- lastVersion: 1.0.8
- curator: nicholas
- timestamp: 2023-02-13 23:52:29 UTC
- changes:
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Version: 1.0.7
- lastVersion: 1.0.6
- curator: nicholas
- timestamp: 2022-07-28 17:37:57 UTC
- changes:
- Geographic metadata:
- geo_elevation: ‘1050’ has been replaced by NULL
Version: 1.0.6
- lastVersion: 1.0.5
- curator: nicholas
- timestamp: 2022-07-15 23:07:13 UTC
- changes:
- Paleo Interpretation metadata:
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Version: 1.0.4
- lastVersion: 1.0.3
- curator: nicholas
- timestamp: 2021-11-19 21:09:26 UTC
- changes:
- Paleo Interpretation metadata:
- d13C (S2LRNALbQfTwNr): interpretation1_seasonality: ‘11,12,1,2,3,4’
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- d13C (S2LRNALbQfTwNr): interpretation1_seasonalityGeneral: ‘Winter’
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Version: 1.0.3
- lastVersion: 1.0.2
- curator: nicholas
- timestamp: 2021-10-05 21:41:40 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 01:56:06 UTC
- changes:
- Base metadata:
- archiveType: ‘speleothem’ has been replaced by ‘Speleothem’
- Paleo Column metadata:
- d18O (S2LRELjmJhtZuf): paleoData_notes: ‘“The lack of correlation
among the δ18O and δ13C records in the three speleothems, together with
the different factors influencing isotopic composition of rainfall in
the area (Moreno et al., 2014), including the variation in the moisture
source, makes the interpretation of Holocene δ18O records unrealistic in
terms of only one climate variable…. Thus, 18O profiles are not used
for paleoenvironmental/paleoclimate interpretations since the factors
influencing 18O record in Holocene speleothems in this area are not yet
fully understood.” (Moreno et al., 2017)’ has been replaced by ‘“The
lack of correlation among the δ18O and δ13C records in the three
Speleothems, together with the different factors influencing isotopic
composition of rainfall in the area (Moreno et al., 2014), including the
variation in the moisture source, makes the interpretation of Holocene
δ18O records unrealistic in terms of only one climate variable…. Thus,
18O profiles are not used for paleoenvironmental/paleoclimate
interpretations since the factors influencing 18O record in Holocene
Speleothems in this area are not yet fully understood.” (Moreno et al.,
2017)’
- d18O (S2LRYz0ilzEvFP): paleoData_notes: ‘“The lack of correlation
among the δ18O and δ13C records in the three speleothems, together with
the different factors influencing isotopic composition of rainfall in
the area (Moreno et al., 2014), including the variation in the moisture
source, makes the interpretation of Holocene δ18O records unrealistic in
terms of only one climate variable…. Thus, 18O profiles are not used
for paleoenvironmental/paleoclimate interpretations since the factors
influencing 18O record in Holocene speleothems in this area are not yet
fully understood.” (Moreno et al., 2017)’ has been replaced by ‘“The
lack of correlation among the δ18O and δ13C records in the three
Speleothems, together with the different factors influencing isotopic
composition of rainfall in the area (Moreno et al., 2014), including the
variation in the moisture source, makes the interpretation of Holocene
δ18O records unrealistic in terms of only one climate variable…. Thus,
18O profiles are not used for paleoenvironmental/paleoclimate
interpretations since the factors influencing 18O record in Holocene
Speleothems in this area are not yet fully understood.” (Moreno et al.,
2017)’
- d13CComposite (S2LRZ8aI3nEQ7d): paleoData_proxyGeneral: NULL has
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- d13CComposite (S2LRZ8aI3nEQ7d): paleoData_QCnotes: ‘“Additionally,
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to assemble a composite record” (Moreno et al., 2017)’ has been replaced
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three Speleothems allowed us to assemble a composite record” (Moreno et
al., 2017)’
- Paleo Interpretation metadata:
- d13CComposite (S2LRZ8aI3nEQ7d): interpretation1_seasonalityGeneral:
‘Winter’ has been replaced by ‘winterOnly’
Version: 1.0.1
- lastVersion: 1.0.0
- curator: nick
- timestamp: 2021-01-12 02:29:24 UTC
- changes:
- Paleo Interpretation metadata:
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‘“The lack of correlation among the δ18O and δ13C records in the three
speleothems, together with the different factors influencing isotopic
composition of rainfall in the area (Moreno et al., 2014), including the
variation in the moisture source, makes the interpretation of Holocene
δ18O records unrealistic in terms of only one climate variable…. Thus,
18O profiles are not used for paleoenvironmental/paleoclimate
interpretations since the factors influencing 18O record in Holocene
speleothems in this area are not yet fully understood.” (Moreno et al.,
2017)’
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- d13C (S2LRNALbQfTwNr): paleoData_notes: NULL has been replaced by
‘“Thus, interpreting the δ13C profiles in these terms, the three-part
Holocene can be described in terms of water availability during the
rainy season (Fig. 4), with a wetter period from the Holocene onset to
ca. 9.4 ka (Phase I, char- acterized by lower δ13C values); drier from
8.5 to 4.8 ka (Phase II, with higher δ13C values); and wet again
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‘“Thus, interpreting the δ13C profiles in these terms, the three-part
Holocene can be described in terms of water availability during the
rainy season (Fig. 4), with a wetter period from the Holocene onset to
ca. 9.4 ka (Phase I, char- acterized by lower δ13C values); drier from
8.5 to 4.8 ka (Phase II, with higher δ13C values); and wet again
afterwards (Phase III, with generally lower δ13C values again).”’
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by ‘calcite’
- d13C (S2LRoFTtnudhkp): paleoData_proxyGeneral: NULL has been
replaced by ‘isotope’
- d13C (S2LRoFTtnudhkp): paleoData_QCCertification: NULL has been
replaced by ‘CH’
- d13C (S2LRoFTtnudhkp): paleoData_QCnotes: NULL has been replaced by
‘MO-1’
- d18O (S2LRYz0ilzEvFP): paleoData_notes: NULL has been replaced by
‘“The lack of correlation among the δ18O and δ13C records in the three
speleothems, together with the different factors influencing isotopic
composition of rainfall in the area (Moreno et al., 2014), including the
variation in the moisture source, makes the interpretation of Holocene
δ18O records unrealistic in terms of only one climate variable…. Thus,
18O profiles are not used for paleoenvironmental/paleoclimate
interpretations since the factors influencing 18O record in Holocene
speleothems in this area are not yet fully understood.” (Moreno et al.,
2017)’
- d18O (S2LRYz0ilzEvFP): paleoData_QCCertification: NULL has been
replaced by ‘CH’
- d18O (S2LRYz0ilzEvFP): paleoData_QCnotes: NULL has been replaced by
‘MO-1’
Version: 1.0.0
- curator: nick
- timestamp: 2020-09-29 14:26:00 UTC
- notes: Created from SISALv2