Version history for qY1riXUUSDxAuiHdlrl9 - ElSoplaocave.Rossi.2018

Version: 1.0.14

lastVersion: 1.0.13
curator: nicholas
timestamp: 2025-06-25 22:46:07.447853 UTC
changes:
- Paleo Interpretation metadata:
  - d13C (S2LRAXA3YOxDUQ): interpretation1_variable: ‘((( null ))) T /// temperature’ has been replaced by ‘temperature’
  - d18O (S2LRIixYo5wDj1): interpretation1_variable: ‘((( null ))) P /// precipitation’ has been replaced by ‘precipitation’

Version: 1.0.13

lastVersion: 1.0.12
curator: nicholas
timestamp: 2025-06-25 21:21:47.801708 UTC
changes:
- Paleo Column metadata:
  - d13C (S2LRAXA3YOxDUQ): paleoData_notes: ‘“Also, SIR-1 growth rate is much reduced in periods of high d13C. Given the strong temperature control on Speleothem growth rates (Borsato et al., 2016), such relationship is consistent with reduced soil productivity during colder periods….colder intervals limited soil pro- ductivity and dripwater availability, leading to higher d13C and [Mg], reduced growth rate, and poor or null development of fluo- rescent lamination. Conversely, relatively warm and humid cli- mates favored forest development and resulted in higher growth rates, lower d13C and [Mg], and well developed annual fluorescent lamination…As recorded by SIR-1 and other stalagmites of the region, the YD is marked by a prominent positive d13C excursion whose chronol- ogy (12.95 ± 0.14 to 11.62 ± 0.16 ka) closely matches the YD as defined in Greenland ice, supporting a high YD synchronicity and the sensitivity of stalagmitic d13C in this region to changes in regional temperature.” (Rossi et al., 2018)’ has been replaced by ‘((( null ))) “Also, SIR-1 growth rate is much reduced in periods of high d13C. Given the strong temperature control on speleothem growth rates (Borsato et al., 2016), such relationship is consistent with reduced soil productivity during colder periods….colder intervals limited soil pro- ductivity and dripwater availability, leading to higher d13C and [Mg], reduced growth rate, and poor or null development of fluo- rescent lamination. Conversely, relatively warm and humid cli- mates favored forest development and resulted in higher growth rates, lower d13C and [Mg], and well developed annual fluorescent lamination…As recorded by SIR-1 and other stalagmites of the region, the YD is marked by a prominent positive d13C excursion whose chronol- ogy (12.95 ± 0.14 to 11.62 ± 0.16 ka) closely matches the YD as defined in Greenland ice, supporting a high YD synchronicity and the sensitivity of stalagmitic d13C in this region to changes in regional temperature.” (Rossi et al., 2018) /// “Also, SIR-1 growth rate is much reduced in periods of high d13C. Given the strong temperature control on Speleothem growth rates (Borsato et al., 2016), such relationship is consistent with reduced soil productivity during colder periods….colder intervals limited soil pro- ductivity and dripwater availability, leading to higher d13C and [Mg], reduced growth rate, and poor or null development of fluo- rescent lamination. Conversely, relatively warm and humid cli- mates favored forest development and resulted in higher growth rates, lower d13C and [Mg], and well developed annual fluorescent lamination…As recorded by SIR-1 and other stalagmites of the region, the YD is marked by a prominent positive d13C excursion whose chronol- ogy (12.95 ± 0.14 to 11.62 ± 0.16 ka) closely matches the YD as defined in Greenland ice, supporting a high YD synchronicity and the sensitivity of stalagmitic d13C in this region to changes in regional temperature.” (Rossi et al., 2018)’
  - d13C (S2LRAXA3YOxDUQ): paleoData_meetsHoloceneHydroclimateCriteria: NULL has been replaced by ‘TRUE’
  - d13C (S2LRAXA3YOxDUQ): paleoData_primaryTimeseries: NULL has been replaced by ‘TRUE’
  - d18O (S2LRIixYo5wDj1): paleoData_meetsHoloceneHydroclimateCriteria: NULL has been replaced by ‘TRUE’
  - d18O (S2LRIixYo5wDj1): paleoData_primaryTimeseries: NULL has been replaced by ‘TRUE’
- Paleo Interpretation metadata:
  - d13C (S2LRAXA3YOxDUQ): interpretation1_variable: ‘temperature’ has been replaced by ‘((( null ))) T /// temperature’
  - d18O (S2LRIixYo5wDj1): interpretation1_variable: ‘precipitation’ has been replaced by ‘((( null ))) P /// precipitation’

Version: 1.0.12

lastVersion: 1.0.11
curator: nicholas
timestamp: 2025-04-11 16:15:32.870234 UTC
changes:
- Paleo Interpretation metadata:
  - mineralogy (S2LR7H0xbfGcPs): interpretation2_scope: NULL has been replaced by ‘climate’
  - mineralogy (S2LR7H0xbfGcPs): interpretation3_scope: NULL has been replaced by ‘climate’
  - mineralogy (S2LR7H0xbfGcPs): interpretation4_scope: NULL has been replaced by ‘isotope’
  - mineralogy (S2LR7H0xbfGcPs): interpretation5_scope: NULL has been replaced by ‘isotope’
  - mineralogy (S2LR7H0xbfGcPs): interpretation6_scope: NULL has been replaced by ‘isotope’
  - d13C (S2LRAXA3YOxDUQ): interpretation2_scope: NULL has been replaced by ‘climate’
  - d13C (S2LRAXA3YOxDUQ): interpretation3_scope: NULL has been replaced by ‘climate’
  - d13C (S2LRAXA3YOxDUQ): interpretation4_scope: NULL has been replaced by ‘isotope’
  - d13C (S2LRAXA3YOxDUQ): interpretation5_scope: NULL has been replaced by ‘isotope’
  - d13C (S2LRAXA3YOxDUQ): interpretation6_scope: NULL has been replaced by ‘isotope’
  - d18O (S2LRIixYo5wDj1): interpretation2_scope: NULL has been replaced by ‘climate’
  - d18O (S2LRIixYo5wDj1): interpretation3_scope: NULL has been replaced by ‘climate’
  - d18O (S2LRIixYo5wDj1): interpretation4_scope: NULL has been replaced by ‘isotope’
  - d18O (S2LRIixYo5wDj1): interpretation5_scope: NULL has been replaced by ‘isotope’
  - d18O (S2LRIixYo5wDj1): interpretation6_scope: NULL has been replaced by ‘isotope’
  - uncertainty (S2LRKkXEWkoD8W): interpretation2_scope: NULL has been replaced by ‘climate’
  - uncertainty (S2LRKkXEWkoD8W): interpretation3_scope: NULL has been replaced by ‘climate’
  - uncertainty (S2LRKkXEWkoD8W): interpretation4_scope: NULL has been replaced by ‘isotope’
  - uncertainty (S2LRKkXEWkoD8W): interpretation5_scope: NULL has been replaced by ‘isotope’
  - uncertainty (S2LRKkXEWkoD8W): interpretation6_scope: NULL has been replaced by ‘isotope’
  - uncertainty (S2LRMZgbVDudjp): interpretation2_scope: NULL has been replaced by ‘climate’
  - uncertainty (S2LRMZgbVDudjp): interpretation3_scope: NULL has been replaced by ‘climate’
  - uncertainty (S2LRMZgbVDudjp): interpretation4_scope: NULL has been replaced by ‘isotope’
  - uncertainty (S2LRMZgbVDudjp): interpretation5_scope: NULL has been replaced by ‘isotope’
  - uncertainty (S2LRMZgbVDudjp): interpretation6_scope: NULL has been replaced by ‘isotope’
  - correction (S2LROOW8Z25Uji): interpretation2_scope: NULL has been replaced by ‘climate’
  - correction (S2LROOW8Z25Uji): interpretation3_scope: NULL has been replaced by ‘climate’
  - correction (S2LROOW8Z25Uji): interpretation4_scope: NULL has been replaced by ‘isotope’
  - correction (S2LROOW8Z25Uji): interpretation5_scope: NULL has been replaced by ‘isotope’
  - correction (S2LROOW8Z25Uji): interpretation6_scope: NULL has been replaced by ‘isotope’
  - uncertainty (S2LRoirhWsuhDY): interpretation2_scope: NULL has been replaced by ‘climate’
  - uncertainty (S2LRoirhWsuhDY): interpretation3_scope: NULL has been replaced by ‘climate’
  - uncertainty (S2LRoirhWsuhDY): interpretation4_scope: NULL has been replaced by ‘isotope’
  - uncertainty (S2LRoirhWsuhDY): interpretation5_scope: NULL has been replaced by ‘isotope’
  - uncertainty (S2LRoirhWsuhDY): interpretation6_scope: NULL has been replaced by ‘isotope’
  - sampleID (S2LRq0DVFOhMeB): interpretation2_scope: NULL has been replaced by ‘climate’
  - sampleID (S2LRq0DVFOhMeB): interpretation3_scope: NULL has been replaced by ‘climate’
  - sampleID (S2LRq0DVFOhMeB): interpretation4_scope: NULL has been replaced by ‘isotope’
  - sampleID (S2LRq0DVFOhMeB): interpretation5_scope: NULL has been replaced by ‘isotope’
  - sampleID (S2LRq0DVFOhMeB): interpretation6_scope: NULL has been replaced by ‘isotope’
  - uncertainty (S2LRsRGWDu4Rd6): interpretation2_scope: NULL has been replaced by ‘climate’
  - uncertainty (S2LRsRGWDu4Rd6): interpretation3_scope: NULL has been replaced by ‘climate’
  - uncertainty (S2LRsRGWDu4Rd6): interpretation4_scope: NULL has been replaced by ‘isotope’
  - uncertainty (S2LRsRGWDu4Rd6): interpretation5_scope: NULL has been replaced by ‘isotope’
  - uncertainty (S2LRsRGWDu4Rd6): interpretation6_scope: NULL has been replaced by ‘isotope’

Version: 1.0.11

lastVersion: 1.0.10
curator: nicholas
timestamp: 2023-08-10 22:49:03 UTC
changes:
- Base metadata:
  - originalDataUrl: ‘http://dx.doi.org/10.17864/1947.256’ has been replaced by ‘https://doi.org/10.17864/1947.256’
- Publication metadata:
  - pub1_author: NULL has been replaced by ‘Carlos Rossi and Petra Bajo and Rafael P. Lozano and John Hellstrom’
  - pub1_journal: NULL has been replaced by ‘Quaternary Science Reviews’
  - pub1_pages: NULL has been replaced by ‘71–85’
  - pub1_title: NULL has been replaced by ‘Younger Dryas to Early Holocene paleoclimate in Cantabria (N Spain): Constraints from speleothem Mg, annual fluorescence banding and stable isotope records’

Version: 1.0.10

lastVersion: 1.0.9
curator: nicholas
timestamp: 2023-05-12 21:53:52 UTC
changes:
- Paleo Column metadata:
  - d13C (S2LRAXA3YOxDUQ): paleoData_notes: ‘((( “Also, SIR-1 growth rate is much reduced in periods of high d13C. Given the strong temperature control on Speleothem growth rates (Borsato et al., 2016), such relationship is consistent with reduced soil productivity during colder periods….colder intervals limited soil pro- ductivity and dripwater availability, leading to higher d13C and [Mg], reduced growth rate, and poor or null development of fluo- rescent lamination. Conversely, relatively warm and humid cli- mates favored forest development and resulted in higher growth rates, lower d13C and [Mg], and well developed annual fluorescent lamination…As recorded by SIR-1 and other stalagmites of the region, the YD is marked by a prominent positive d13C excursion whose chronol- ogy (12.95 �� 0.14 to 11.62 �� 0.16 ka) closely matches the YD as defined in Greenland ice, supporting a high YD synchronicity and the sensitivity of stalagmitic d13C in this region to changes in regional temperature.” (Rossi et al., 2018) ))) “Also, SIR-1 growth rate is much reduced in periods of high d13C. Given the strong temperature control on Speleothem growth rates (Borsato et al., 2016), such relationship is consistent with reduced soil productivity during colder periods….colder intervals limited soil pro- ductivity and dripwater availability, leading to higher d13C and [Mg], reduced growth rate, and poor or null development of fluo- rescent lamination. Conversely, relatively warm and humid cli- mates favored forest development and resulted in higher growth rates, lower d13C and [Mg], and well developed annual fluorescent lamination…As recorded by SIR-1 and other stalagmites of the region, the YD is marked by a prominent positive d13C excursion whose chronol- ogy (12.95 ± 0.14 to 11.62 ± 0.16 ka) closely matches the YD as defined in Greenland ice, supporting a high YD synchronicity and the sensitivity of stalagmitic d13C in this region to changes in regional temperature.” (Rossi et al., 2018) /// “Also, SIR-1 growth rate is much reduced in periods of high d13C. Given the strong temperature control on Speleothem growth rates (Borsato et al., 2016), such relationship is consistent with reduced soil productivity during colder periods….colder intervals limited soil pro- ductivity and dripwater availability, leading to higher d13C and [Mg], reduced growth rate, and poor or null development of fluo- rescent lamination. Conversely, relatively warm and humid cli- mates favored forest development and resulted in higher growth rates, lower d13C and [Mg], and well developed annual fluorescent lamination…As recorded by SIR-1 and other stalagmites of the region, the YD is marked by a prominent positive d13C excursion whose chronol- ogy (12.95 ± 0.14 to 11.62 ± 0.16 ka) closely matches the YD as defined in Greenland ice, supporting a high YD synchronicity and the sensitivity of stalagmitic d13C in this region to changes in regional temperature.” (Rossi et al., 2018)’ has been replaced by ‘“Also, SIR-1 growth rate is much reduced in periods of high d13C. Given the strong temperature control on Speleothem growth rates (Borsato et al., 2016), such relationship is consistent with reduced soil productivity during colder periods….colder intervals limited soil pro- ductivity and dripwater availability, leading to higher d13C and [Mg], reduced growth rate, and poor or null development of fluo- rescent lamination. Conversely, relatively warm and humid cli- mates favored forest development and resulted in higher growth rates, lower d13C and [Mg], and well developed annual fluorescent lamination…As recorded by SIR-1 and other stalagmites of the region, the YD is marked by a prominent positive d13C excursion whose chronol- ogy (12.95 ± 0.14 to 11.62 ± 0.16 ka) closely matches the YD as defined in Greenland ice, supporting a high YD synchronicity and the sensitivity of stalagmitic d13C in this region to changes in regional temperature.” (Rossi et al., 2018)’

Version: 1.0.9

lastVersion: 1.0.8
curator: nicholas
timestamp: 2023-02-13 23:41:41 UTC
changes:
- Paleo Column metadata:
  - d13C (S2LRAXA3YOxDUQ): paleoData_notes: ‘“Also, SIR-1 growth rate is much reduced in periods of high d13C. Given the strong temperature control on Speleothem growth rates (Borsato et al., 2016), such relationship is consistent with reduced soil productivity during colder periods….colder intervals limited soil pro- ductivity and dripwater availability, leading to higher d13C and [Mg], reduced growth rate, and poor or null development of fluo- rescent lamination. Conversely, relatively warm and humid cli- mates favored forest development and resulted in higher growth rates, lower d13C and [Mg], and well developed annual fluorescent lamination…As recorded by SIR-1 and other stalagmites of the region, the YD is marked by a prominent positive d13C excursion whose chronol- ogy (12.95 ± 0.14 to 11.62 ± 0.16 ka) closely matches the YD as defined in Greenland ice, supporting a high YD synchronicity and the sensitivity of stalagmitic d13C in this region to changes in regional temperature.” (Rossi et al., 2018)’ has been replaced by ‘((( “Also, SIR-1 growth rate is much reduced in periods of high d13C. Given the strong temperature control on Speleothem growth rates (Borsato et al., 2016), such relationship is consistent with reduced soil productivity during colder periods….colder intervals limited soil pro- ductivity and dripwater availability, leading to higher d13C and [Mg], reduced growth rate, and poor or null development of fluo- rescent lamination. Conversely, relatively warm and humid cli- mates favored forest development and resulted in higher growth rates, lower d13C and [Mg], and well developed annual fluorescent lamination…As recorded by SIR-1 and other stalagmites of the region, the YD is marked by a prominent positive d13C excursion whose chronol- ogy (12.95 �� 0.14 to 11.62 �� 0.16 ka) closely matches the YD as defined in Greenland ice, supporting a high YD synchronicity and the sensitivity of stalagmitic d13C in this region to changes in regional temperature.” (Rossi et al., 2018) ))) “Also, SIR-1 growth rate is much reduced in periods of high d13C. Given the strong temperature control on Speleothem growth rates (Borsato et al., 2016), such relationship is consistent with reduced soil productivity during colder periods….colder intervals limited soil pro- ductivity and dripwater availability, leading to higher d13C and [Mg], reduced growth rate, and poor or null development of fluo- rescent lamination. Conversely, relatively warm and humid cli- mates favored forest development and resulted in higher growth rates, lower d13C and [Mg], and well developed annual fluorescent lamination…As recorded by SIR-1 and other stalagmites of the region, the YD is marked by a prominent positive d13C excursion whose chronol- ogy (12.95 ± 0.14 to 11.62 ± 0.16 ka) closely matches the YD as defined in Greenland ice, supporting a high YD synchronicity and the sensitivity of stalagmitic d13C in this region to changes in regional temperature.” (Rossi et al., 2018) /// “Also, SIR-1 growth rate is much reduced in periods of high d13C. Given the strong temperature control on Speleothem growth rates (Borsato et al., 2016), such relationship is consistent with reduced soil productivity during colder periods….colder intervals limited soil pro- ductivity and dripwater availability, leading to higher d13C and [Mg], reduced growth rate, and poor or null development of fluo- rescent lamination. Conversely, relatively warm and humid cli- mates favored forest development and resulted in higher growth rates, lower d13C and [Mg], and well developed annual fluorescent lamination…As recorded by SIR-1 and other stalagmites of the region, the YD is marked by a prominent positive d13C excursion whose chronol- ogy (12.95 ± 0.14 to 11.62 ± 0.16 ka) closely matches the YD as defined in Greenland ice, supporting a high YD synchronicity and the sensitivity of stalagmitic d13C in this region to changes in regional temperature.” (Rossi et al., 2018)’

Version: 1.0.8

lastVersion: 1.0.7
curator: nicholas
timestamp: 2023-02-09 15:39:52 UTC
notes: Updated lipdverse database entry with a changed file.
changes:
- Geographic metadata:
  - geo_elevation: NULL has been replaced by ‘550’
- Paleo Interpretation metadata:
  - d13C (S2LRAXA3YOxDUQ): interpretation1_variable: ‘T’ has been replaced by ‘temperature’
  - d18O (S2LRIixYo5wDj1): interpretation1_seasonality: ‘1,2,3,4,5,6,7,8,9,10,11,12’ has been replaced by ‘Annual’
  - d18O (S2LRIixYo5wDj1): interpretation1_variable: ‘P’ has been replaced by ‘precipitation’
- Paleo Column metadata:
  - uncertainty (S2LRKkXEWkoD8W): paleoData_notes: NULL has been replaced by ‘NA; paleoData_measurementMaterial has been standardized; paleoData_method has been standardized’
  - uncertainty (S2LRKkXEWkoD8W): paleoData_variableName: ‘d18OPrecision’ has been replaced by ‘uncertainty’
  - uncertainty (S2LRKkXEWkoD8W): paleoData_measurementMaterial: NULL has been replaced by ‘d18O carbonate’
  - uncertainty (S2LRKkXEWkoD8W): paleoData_method: NULL has been replaced by ‘precision’
  - age (S2LRmVXKEwajmg): paleoData_notes: NULL has been replaced by ‘NA; paleoData_isPrimary has been standardized; paleoData_datum has been standardized’
  - age (S2LRmVXKEwajmg): paleoData_units: ‘BP’ has been replaced by ‘yr BP’
  - age (S2LRmVXKEwajmg): paleoData_datum: NULL has been replaced by ‘1950’
  - age (S2LRmVXKEwajmg): paleoData_isPrimary: NULL has been replaced by ‘TRUE’
  - uncertainty (S2LRMZgbVDudjp): paleoData_notes: NULL has been replaced by ‘NA; paleoData_measurementMaterial has been standardized; paleoData_method has been standardized’
  - uncertainty (S2LRMZgbVDudjp): paleoData_variableName: ‘d13CPrecision’ has been replaced by ‘uncertainty’
  - uncertainty (S2LRMZgbVDudjp): paleoData_measurementMaterial: NULL has been replaced by ‘d13C’
  - uncertainty (S2LRMZgbVDudjp): paleoData_method: NULL has been replaced by ‘precision’
  - uncertainty (S2LRoirhWsuhDY): paleoData_notes: NULL has been replaced by ‘NA; paleoData_measurementMaterial has been standardized; paleoData_method has been standardized’
  - uncertainty (S2LRoirhWsuhDY): paleoData_variableName: ‘d18OStandard’ has been replaced by ‘uncertainty’
  - uncertainty (S2LRoirhWsuhDY): paleoData_measurementMaterial: NULL has been replaced by ‘d18O carbonate’
  - uncertainty (S2LRoirhWsuhDY): paleoData_method: NULL has been replaced by ‘standard’
  - correction (S2LROOW8Z25Uji): paleoData_notes: NULL has been replaced by ‘NA; paleoData_method has been standardized’
  - correction (S2LROOW8Z25Uji): paleoData_variableName: ‘hasAragoniteCorrection’ has been replaced by ‘correction’
  - correction (S2LROOW8Z25Uji): paleoData_method: NULL has been replaced by ‘aragonite correction’
  - sampleID (S2LRq0DVFOhMeB): paleoData_variableName: ‘sisalSampleID’ has been replaced by ‘sampleID’
  - uncertainty (S2LRsRGWDu4Rd6): paleoData_notes: NULL has been replaced by ‘NA; paleoData_measurementMaterial has been standardized; paleoData_method has been standardized’
  - uncertainty (S2LRsRGWDu4Rd6): paleoData_variableName: ‘d13CStandard’ has been replaced by ‘uncertainty’
  - uncertainty (S2LRsRGWDu4Rd6): paleoData_measurementMaterial: NULL has been replaced by ‘d13C’
  - uncertainty (S2LRsRGWDu4Rd6): paleoData_method: NULL has been replaced by ‘standard’
  - depth (S2LRzeZ6CjoyaD): paleoData_notes: NULL has been replaced by ‘NA; paleoData_isPrimary has been standardized’
  - depth (S2LRzeZ6CjoyaD): paleoData_units: ‘depth_sample’ has been replaced by ‘mm’
  - depth (S2LRzeZ6CjoyaD): paleoData_isPrimary: NULL has been replaced by ‘TRUE’

Version: 1.0.7

lastVersion: 1.0.6
curator: nicholas
timestamp: 2022-07-28 17:30:40 UTC
changes:
- Geographic metadata:
  - geo_elevation: ‘550’ has been replaced by NULL

Version: 1.0.6

lastVersion: 1.0.5
curator: nicholas
timestamp: 2022-07-15 23:00:39 UTC
changes:
- Paleo Interpretation metadata:
  - mineralogy (S2LR7H0xbfGcPs): interpretation1_scope: NULL has been replaced by ‘climate’
  - d18OPrecision (S2LRKkXEWkoD8W): interpretation1_scope: NULL has been replaced by ‘climate’
  - d13CPrecision (S2LRMZgbVDudjp): interpretation1_scope: NULL has been replaced by ‘climate’
  - d18OStandard (S2LRoirhWsuhDY): interpretation1_scope: NULL has been replaced by ‘climate’
  - hasAragoniteCorrection (S2LROOW8Z25Uji): interpretation1_scope: NULL has been replaced by ‘climate’
  - sisalSampleID (S2LRq0DVFOhMeB): interpretation1_scope: NULL has been replaced by ‘climate’
  - d13CStandard (S2LRsRGWDu4Rd6): interpretation1_scope: NULL has been replaced by ‘climate’

Version: 1.0.5

lastVersion: 1.0.4
curator: nicholas
timestamp: 2022-05-18 00:25:36 UTC
changes:
- Paleo Interpretation metadata:
  - mineralogy (S2LR7H0xbfGcPs): interpretation1_scope: ‘climate’ has been replaced by NULL
  - d13C (S2LRAXA3YOxDUQ): interpretation1_variableGroup: NULL has been replaced by ‘Temperature’
  - d13C (S2LRAXA3YOxDUQ): interpretation1_variableGroupDirection: NULL has been replaced by ‘negative’
  - d13C (S2LRAXA3YOxDUQ): interpretation1_variableGroupOriginal: NULL has been replaced by ‘T’
  - d18O (S2LRIixYo5wDj1): interpretation1_variableGroup: NULL has been replaced by ‘P’
  - d18OPrecision (S2LRKkXEWkoD8W): interpretation1_scope: ‘climate’ has been replaced by NULL
  - d13CPrecision (S2LRMZgbVDudjp): interpretation1_scope: ‘climate’ has been replaced by NULL
  - d18OStandard (S2LRoirhWsuhDY): interpretation1_scope: ‘climate’ has been replaced by NULL
  - hasAragoniteCorrection (S2LROOW8Z25Uji): interpretation1_scope: ‘climate’ has been replaced by NULL
  - sisalSampleID (S2LRq0DVFOhMeB): interpretation1_scope: ‘climate’ has been replaced by NULL
  - d13CStandard (S2LRsRGWDu4Rd6): interpretation1_scope: ‘climate’ has been replaced by NULL
- Paleo Column metadata:
  - d18O (S2LRIixYo5wDj1): paleoData_proxyLumps: NULL has been replaced by ‘isotope’
  - d18O (S2LRIixYo5wDj1): paleoData_proxyLumpsOriginal: NULL has been replaced by ‘d18O’
  - age (S2LRmVXKEwajmg): paleoData_units: ‘yr BP’ has been replaced by ‘BP’
  - age (S2LRmVXKEwajmg): paleoData_unitsOriginal: NULL has been replaced by ‘yr BP’
- Chron Column metadata:
  - age_type (S2LcRIsVGuQfCWr): chronData_variableName: ‘ageType’ has been replaced by ‘age_type’
  - age_type (S2LcRIsVGuQfCWr): chronData_variableNameOriginal: NULL has been replaced by ‘ageType’

Version: 1.0.4

lastVersion: 1.0.3
curator: nicholas
timestamp: 2021-10-05 21:39:11 UTC
changes:
- Geographic metadata:
  - geo_gcmdLocation: NULL has been replaced by ‘Europe>Southern Europe>Spain’

Version: 1.0.3

lastVersion: 1.0.2
curator: nick
timestamp: 2021-04-13 02:31:54 UTC
changes:
- Paleo Interpretation metadata:
  - d18O (S2LRIixYo5wDj1): interpretation1_seasonality: ‘1,2,3,4,5,6,7,8,9,10,11,643’ has been replaced by ‘1,2,3,4,5,6,7,8,9,10,11,12’

Version: 1.0.2

lastVersion: 1.0.1
curator: nick
timestamp: 2021-03-17 01:52:59 UTC
changes:
- Base metadata:
  - archiveType: ‘speleothem’ has been replaced by ‘Speleothem’
- Paleo Column metadata:
  - d13C (S2LRAXA3YOxDUQ): paleoData_notes: ‘“Also, SIR-1 growth rate is much reduced in periods of high d13C. Given the strong temperature control on speleothem growth rates (Borsato et al., 2016), such relationship is consistent with reduced soil productivity during colder periods….colder intervals limited soil pro- ductivity and dripwater availability, leading to higher d13C and [Mg], reduced growth rate, and poor or null development of fluo- rescent lamination. Conversely, relatively warm and humid cli- mates favored forest development and resulted in higher growth rates, lower d13C and [Mg], and well developed annual fluorescent lamination…As recorded by SIR-1 and other stalagmites of the region, the YD is marked by a prominent positive d13C excursion whose chronol- ogy (12.95 ± 0.14 to 11.62 ± 0.16 ka) closely matches the YD as defined in Greenland ice, supporting a high YD synchronicity and the sensitivity of stalagmitic d13C in this region to changes in regional temperature.” (Rossi et al., 2018)’ has been replaced by ‘“Also, SIR-1 growth rate is much reduced in periods of high d13C. Given the strong temperature control on Speleothem growth rates (Borsato et al., 2016), such relationship is consistent with reduced soil productivity during colder periods….colder intervals limited soil pro- ductivity and dripwater availability, leading to higher d13C and [Mg], reduced growth rate, and poor or null development of fluo- rescent lamination. Conversely, relatively warm and humid cli- mates favored forest development and resulted in higher growth rates, lower d13C and [Mg], and well developed annual fluorescent lamination…As recorded by SIR-1 and other stalagmites of the region, the YD is marked by a prominent positive d13C excursion whose chronol- ogy (12.95 ± 0.14 to 11.62 ± 0.16 ka) closely matches the YD as defined in Greenland ice, supporting a high YD synchronicity and the sensitivity of stalagmitic d13C in this region to changes in regional temperature.” (Rossi et al., 2018)’
  - d13C (S2LRAXA3YOxDUQ): paleoData_proxyGeneral: NULL has been replaced by ‘isotope’
- Paleo Interpretation metadata:
  - d18O (S2LRIixYo5wDj1): interpretation1_seasonality: NULL has been replaced by ‘1,2,3,4,5,6,7,8,9,10,11,643’

Version: 1.0.1

lastVersion: 1.0.0
curator: nick
timestamp: 2021-01-12 02:28:50 UTC
changes:
- Paleo Interpretation metadata:
  - mineralogy (S2LR7H0xbfGcPs): interpretation1_scope: NULL has been replaced by ‘climate’
  - d13C (S2LRAXA3YOxDUQ): interpretation1_scope: NULL has been replaced by ‘climate’
  - d13C (S2LRAXA3YOxDUQ): interpretation1_variable: NULL has been replaced by ‘T’
  - d18O (S2LRIixYo5wDj1): interpretation1_direction: NULL has been replaced by ‘negative’
  - d18O (S2LRIixYo5wDj1): interpretation1_scope: NULL has been replaced by ‘climate’
  - d18O (S2LRIixYo5wDj1): interpretation1_seasonalityGeneral: NULL has been replaced by ‘Annual’
  - d18O (S2LRIixYo5wDj1): interpretation1_variable: NULL has been replaced by ‘P’
  - d18O (S2LRIixYo5wDj1): interpretation1_variableDetail: NULL has been replaced by ‘@surface’
  - d18OPrecision (S2LRKkXEWkoD8W): interpretation1_scope: NULL has been replaced by ‘climate’
  - d13CPrecision (S2LRMZgbVDudjp): interpretation1_scope: NULL has been replaced by ‘climate’
  - d18OStandard (S2LRoirhWsuhDY): interpretation1_scope: NULL has been replaced by ‘climate’
  - hasAragoniteCorrection (S2LROOW8Z25Uji): interpretation1_scope: NULL has been replaced by ‘climate’
  - sisalSampleID (S2LRq0DVFOhMeB): interpretation1_scope: NULL has been replaced by ‘climate’
  - d13CStandard (S2LRsRGWDu4Rd6): interpretation1_scope: NULL has been replaced by ‘climate’
- Paleo Column metadata:
  - d13C (S2LRAXA3YOxDUQ): paleoData_notes: NULL has been replaced by ‘“Also, SIR-1 growth rate is much reduced in periods of high d13C. Given the strong temperature control on speleothem growth rates (Borsato et al., 2016), such relationship is consistent with reduced soil productivity during colder periods….colder intervals limited soil pro- ductivity and dripwater availability, leading to higher d13C and [Mg], reduced growth rate, and poor or null development of fluo- rescent lamination. Conversely, relatively warm and humid cli- mates favored forest development and resulted in higher growth rates, lower d13C and [Mg], and well developed annual fluorescent lamination…As recorded by SIR-1 and other stalagmites of the region, the YD is marked by a prominent positive d13C excursion whose chronol- ogy (12.95 ± 0.14 to 11.62 ± 0.16 ka) closely matches the YD as defined in Greenland ice, supporting a high YD synchronicity and the sensitivity of stalagmitic d13C in this region to changes in regional temperature.” (Rossi et al., 2018)’
  - d13C (S2LRAXA3YOxDUQ): paleoData_QCCertification: NULL has been replaced by ‘CH’
  - d18O (S2LRIixYo5wDj1): paleoData_notes: NULL has been replaced by ‘“hese authors interpreted the trend as reflecting a general increase in rainfall amounts during the Early Holocene, based on the present-day relationship between rainfall amount and rainwater d18O observed in Cantabria (Comas- Bru and McDermott, 2015; Smith et al., 2016b). The SIR-1 record supports such interpretation. In SIR-1, the increasing d18O trend reversed from ~8.5 to ~8.0 ka. Coevally, both [Mg] and d13C also tend to increase (Fig. 7B), indicating drier conditions. This further sup- ports that the Early Holocene SIR-1 d18O variation mainly responds to variations in the amounts of precipitation.” (Rossi et al., 2018)’
  - d18O (S2LRIixYo5wDj1): paleoData_proxy: NULL has been replaced by ‘d18O’
  - d18O (S2LRIixYo5wDj1): paleoData_proxyDetail: NULL has been replaced by ‘calcite’
  - d18O (S2LRIixYo5wDj1): paleoData_proxyGeneral: NULL has been replaced by ‘isotope’
  - d18O (S2LRIixYo5wDj1): paleoData_QCCertification: NULL has been replaced by ‘CH’

Version: 1.0.0

curator: nick
timestamp: 2020-09-29 14:29:26 UTC
notes: Created from SISALv2