Version history for o0r2hzqf7MhaDmTCjsbh - CovadaArcoia.Railsback.2011

Version: 1.0.15

lastVersion: 1.0.14
curator: nicholas
timestamp: 2025-06-25 22:46:02.266815 UTC
changes:
- Paleo Interpretation metadata:
  - d13C (S2LRP1bVgbttoT): interpretation1_variable: ‘((( null ))) P-E /// effectivePrecipitation’ has been replaced by ‘effectivePrecipitation’

Version: 1.0.14

lastVersion: 1.0.13
curator: nicholas
timestamp: 2025-06-25 21:21:42.328097 UTC
changes:
- Paleo Interpretation metadata:
  - d13C (S2LRP1bVgbttoT): interpretation1_variable: ‘effectivePrecipitation’ has been replaced by ‘((( null ))) P-E /// effectivePrecipitation’
- Paleo Column metadata:
  - d13C (S2LRP1bVgbttoT): paleoData_meetsHoloceneHydroclimateCriteria: NULL has been replaced by ‘TRUE’
  - d13C (S2LRP1bVgbttoT): paleoData_primaryTimeseries: NULL has been replaced by ‘TRUE’
  - d18O (S2LRywXyK822Qq): paleoData_meetsHoloceneHydroclimateCriteria: NULL has been replaced by ‘TRUE’
  - d18O (S2LRywXyK822Qq): paleoData_primaryTimeseries: NULL has been replaced by ‘TRUE’

Version: 1.0.13

lastVersion: 1.0.12
curator: nicholas
timestamp: 2025-04-11 16:15:28.36876 UTC
changes:
- Paleo Interpretation metadata:
  - uncertainty (S2LR2IM9Eo2EJZ): interpretation2_scope: NULL has been replaced by ‘climate’
  - uncertainty (S2LR2IM9Eo2EJZ): interpretation3_scope: NULL has been replaced by ‘climate’
  - uncertainty (S2LR2IM9Eo2EJZ): interpretation4_scope: NULL has been replaced by ‘isotope’
  - uncertainty (S2LR2IM9Eo2EJZ): interpretation5_scope: NULL has been replaced by ‘isotope’
  - uncertainty (S2LR2IM9Eo2EJZ): interpretation6_scope: NULL has been replaced by ‘isotope’
  - uncertainty (S2LR2rXzUnvy7N): interpretation2_scope: NULL has been replaced by ‘climate’
  - uncertainty (S2LR2rXzUnvy7N): interpretation3_scope: NULL has been replaced by ‘climate’
  - uncertainty (S2LR2rXzUnvy7N): interpretation4_scope: NULL has been replaced by ‘isotope’
  - uncertainty (S2LR2rXzUnvy7N): interpretation5_scope: NULL has been replaced by ‘isotope’
  - uncertainty (S2LR2rXzUnvy7N): interpretation6_scope: NULL has been replaced by ‘isotope’
  - uncertainty (S2LR50R8pzOObC): interpretation2_scope: NULL has been replaced by ‘climate’
  - uncertainty (S2LR50R8pzOObC): interpretation3_scope: NULL has been replaced by ‘climate’
  - uncertainty (S2LR50R8pzOObC): interpretation4_scope: NULL has been replaced by ‘isotope’
  - uncertainty (S2LR50R8pzOObC): interpretation5_scope: NULL has been replaced by ‘isotope’
  - uncertainty (S2LR50R8pzOObC): interpretation6_scope: NULL has been replaced by ‘isotope’
  - d13C (S2LRP1bVgbttoT): interpretation2_scope: NULL has been replaced by ‘climate’
  - d13C (S2LRP1bVgbttoT): interpretation3_scope: NULL has been replaced by ‘climate’
  - d13C (S2LRP1bVgbttoT): interpretation4_scope: NULL has been replaced by ‘isotope’
  - d13C (S2LRP1bVgbttoT): interpretation5_scope: NULL has been replaced by ‘isotope’
  - d13C (S2LRP1bVgbttoT): interpretation6_scope: NULL has been replaced by ‘isotope’
  - correction (S2LRPK65HatXRt): interpretation2_scope: NULL has been replaced by ‘climate’
  - correction (S2LRPK65HatXRt): interpretation3_scope: NULL has been replaced by ‘climate’
  - correction (S2LRPK65HatXRt): interpretation4_scope: NULL has been replaced by ‘isotope’
  - correction (S2LRPK65HatXRt): interpretation5_scope: NULL has been replaced by ‘isotope’
  - correction (S2LRPK65HatXRt): interpretation6_scope: NULL has been replaced by ‘isotope’
  - hasHiatus (S2LRSO5zb7KJ3p): interpretation2_scope: NULL has been replaced by ‘climate’
  - hasHiatus (S2LRSO5zb7KJ3p): interpretation3_scope: NULL has been replaced by ‘climate’
  - hasHiatus (S2LRSO5zb7KJ3p): interpretation4_scope: NULL has been replaced by ‘isotope’
  - hasHiatus (S2LRSO5zb7KJ3p): interpretation5_scope: NULL has been replaced by ‘isotope’
  - hasHiatus (S2LRSO5zb7KJ3p): interpretation6_scope: NULL has been replaced by ‘isotope’
  - mineralogy (S2LRZsh8y6x7dF): interpretation2_scope: NULL has been replaced by ‘climate’
  - mineralogy (S2LRZsh8y6x7dF): interpretation3_scope: NULL has been replaced by ‘climate’
  - mineralogy (S2LRZsh8y6x7dF): interpretation4_scope: NULL has been replaced by ‘isotope’
  - mineralogy (S2LRZsh8y6x7dF): interpretation5_scope: NULL has been replaced by ‘isotope’
  - mineralogy (S2LRZsh8y6x7dF): interpretation6_scope: NULL has been replaced by ‘isotope’
  - uncertainty (S2LRrvGcKGKUa5): interpretation2_scope: NULL has been replaced by ‘climate’
  - uncertainty (S2LRrvGcKGKUa5): interpretation3_scope: NULL has been replaced by ‘climate’
  - uncertainty (S2LRrvGcKGKUa5): interpretation4_scope: NULL has been replaced by ‘isotope’
  - uncertainty (S2LRrvGcKGKUa5): interpretation5_scope: NULL has been replaced by ‘isotope’
  - uncertainty (S2LRrvGcKGKUa5): interpretation6_scope: NULL has been replaced by ‘isotope’
  - sampleID (S2LRttgTD3ecLi): interpretation2_scope: NULL has been replaced by ‘climate’
  - sampleID (S2LRttgTD3ecLi): interpretation3_scope: NULL has been replaced by ‘climate’
  - sampleID (S2LRttgTD3ecLi): interpretation4_scope: NULL has been replaced by ‘isotope’
  - sampleID (S2LRttgTD3ecLi): interpretation5_scope: NULL has been replaced by ‘isotope’
  - sampleID (S2LRttgTD3ecLi): interpretation6_scope: NULL has been replaced by ‘isotope’
  - d18O (S2LRywXyK822Qq): interpretation2_scope: NULL has been replaced by ‘climate’
  - d18O (S2LRywXyK822Qq): interpretation3_scope: NULL has been replaced by ‘climate’
  - d18O (S2LRywXyK822Qq): interpretation4_scope: NULL has been replaced by ‘isotope’
  - d18O (S2LRywXyK822Qq): interpretation5_scope: NULL has been replaced by ‘isotope’
  - d18O (S2LRywXyK822Qq): interpretation6_scope: NULL has been replaced by ‘isotope’

Version: 1.0.12

lastVersion: 1.0.11
curator: nicholas
timestamp: 2023-08-10 22:46:33 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 ‘L. Bruce Railsback and Fuyuan Liang and Juan Ram{’{o}}n Vidal Roman{‘{i}} and Aurora Grandal-d{textquotesingle}Anglade and Marcos Vaqueiro Rodr{’{i}}guez and Luisa Santos Fidalgo and Daniel Fern{‘{a}}ndez Mosquera and Hai Cheng and R. Lawrence Edwards’
  - pub1_journal: NULL has been replaced by ‘Palaeogeography, Palaeoclimatology, Palaeoecology’
  - pub1_pages: NULL has been replaced by ‘172–184’
  - pub1_title: NULL has been replaced by ‘Petrographic and isotopic evidence for Holocene long-term climate change and shorter-term environmental shifts from a stalagmite from the Serra do Courel of northwestern Spain, and implications for climatic history across Europe and the Mediterranean’

Version: 1.0.11

lastVersion: 1.0.10
curator: nicholas
timestamp: 2023-05-12 21:52:01 UTC
changes:
- Paleo Column metadata:
  - d13C (S2LRP1bVgbttoT): paleoData_notes: ‘((( “Greater abundance of aragonite, greater values of ��13C, and lesser frequency of Type E surfaces early in the stalagmite suggest a drier and perhaps warmer early to middle Holocene, whereas greater abundance of calcite and frequent Type E surfaces higher in the stalagmite suggest wetter conditions later in the Holocene….The large range of ��13C values in Stalagmite ESP03 and the presence of the greatest values of ��13C beneath Type L surfaces suggests episodes in which climate became sufficiently dry that vegetative input of 12C- enriched CO2 was minimized (giving comparatively large values of ��13C) and little water dripped onto the stalagmite (resulting in layers of diminished lateral extent) (Fig. 8C). Several other lines of evidence support this interpretation…the inverse relationship between fluorescence and ��13C further supports the inference that the greatest values of ��13C in Stalagmite ESP03 represent dry periods in which vegetative input of soil CO2 diminished…precipitation of aragonite with large values of ��13C suggests that the change from exceptionally wet conditions to exceptionally dry conditions was ecologically abrupt” (Railsback et al., 2011) ))) “Greater abundance of aragonite, greater values of δ13C, and lesser frequency of Type E surfaces early in the stalagmite suggest a drier and perhaps warmer early to middle Holocene, whereas greater abundance of calcite and frequent Type E surfaces higher in the stalagmite suggest wetter conditions later in the Holocene….The large range of δ13C values in Stalagmite ESP03 and the presence of the greatest values of δ13C beneath Type L surfaces suggests episodes in which climate became sufficiently dry that vegetative input of 12C- enriched CO2 was minimized (giving comparatively large values of δ13C) and little water dripped onto the stalagmite (resulting in layers of diminished lateral extent) (Fig. 8C). Several other lines of evidence support this interpretation…the inverse relationship between fluorescence and δ13C further supports the inference that the greatest values of δ13C in Stalagmite ESP03 represent dry periods in which vegetative input of soil CO2 diminished…precipitation of aragonite with large values of δ13C suggests that the change from exceptionally wet conditions to exceptionally dry conditions was ecologically abrupt” (Railsback et al., 2011) /// “Greater abundance of aragonite, greater values of δ13C, and lesser frequency of Type E surfaces early in the stalagmite suggest a drier and perhaps warmer early to middle Holocene, whereas greater abundance of calcite and frequent Type E surfaces higher in the stalagmite suggest wetter conditions later in the Holocene….The large range of δ13C values in Stalagmite ESP03 and the presence of the greatest values of δ13C beneath Type L surfaces suggests episodes in which climate became sufficiently dry that vegetative input of 12C- enriched CO2 was minimized (giving comparatively large values of δ13C) and little water dripped onto the stalagmite (resulting in layers of diminished lateral extent) (Fig. 8C). Several other lines of evidence support this interpretation…the inverse relationship between fluorescence and δ13C further supports the inference that the greatest values of δ13C in Stalagmite ESP03 represent dry periods in which vegetative input of soil CO2 diminished…precipitation of aragonite with large values of δ13C suggests that the change from exceptionally wet conditions to exceptionally dry conditions was ecologically abrupt” (Railsback et al., 2011)’ has been replaced by ‘“Greater abundance of aragonite, greater values of δ13C, and lesser frequency of Type E surfaces early in the stalagmite suggest a drier and perhaps warmer early to middle Holocene, whereas greater abundance of calcite and frequent Type E surfaces higher in the stalagmite suggest wetter conditions later in the Holocene….The large range of δ13C values in Stalagmite ESP03 and the presence of the greatest values of δ13C beneath Type L surfaces suggests episodes in which climate became sufficiently dry that vegetative input of 12C- enriched CO2 was minimized (giving comparatively large values of δ13C) and little water dripped onto the stalagmite (resulting in layers of diminished lateral extent) (Fig. 8C). Several other lines of evidence support this interpretation…the inverse relationship between fluorescence and δ13C further supports the inference that the greatest values of δ13C in Stalagmite ESP03 represent dry periods in which vegetative input of soil CO2 diminished…precipitation of aragonite with large values of δ13C suggests that the change from exceptionally wet conditions to exceptionally dry conditions was ecologically abrupt” (Railsback et al., 2011)’

Version: 1.0.10

lastVersion: 1.0.9
curator: nicholas
timestamp: 2023-03-29 19:44:26 UTC
changes:
- Paleo Interpretation metadata:
  - d13C (S2LRP1bVgbttoT): interpretation1_variable: ‘P-E’ has been replaced by ‘effectivePrecipitation’

Version: 1.0.9

lastVersion: 1.0.8
curator: nicholas
timestamp: 2023-02-13 23:40:05 UTC
changes:
- Paleo Column metadata:
  - d13C (S2LRP1bVgbttoT): paleoData_notes: ‘“Greater abundance of aragonite, greater values of δ13C, and lesser frequency of Type E surfaces early in the stalagmite suggest a drier and perhaps warmer early to middle Holocene, whereas greater abundance of calcite and frequent Type E surfaces higher in the stalagmite suggest wetter conditions later in the Holocene….The large range of δ13C values in Stalagmite ESP03 and the presence of the greatest values of δ13C beneath Type L surfaces suggests episodes in which climate became sufficiently dry that vegetative input of 12C- enriched CO2 was minimized (giving comparatively large values of δ13C) and little water dripped onto the stalagmite (resulting in layers of diminished lateral extent) (Fig. 8C). Several other lines of evidence support this interpretation…the inverse relationship between fluorescence and δ13C further supports the inference that the greatest values of δ13C in Stalagmite ESP03 represent dry periods in which vegetative input of soil CO2 diminished…precipitation of aragonite with large values of δ13C suggests that the change from exceptionally wet conditions to exceptionally dry conditions was ecologically abrupt” (Railsback et al., 2011)’ has been replaced by ‘((( “Greater abundance of aragonite, greater values of ��13C, and lesser frequency of Type E surfaces early in the stalagmite suggest a drier and perhaps warmer early to middle Holocene, whereas greater abundance of calcite and frequent Type E surfaces higher in the stalagmite suggest wetter conditions later in the Holocene….The large range of ��13C values in Stalagmite ESP03 and the presence of the greatest values of ��13C beneath Type L surfaces suggests episodes in which climate became sufficiently dry that vegetative input of 12C- enriched CO2 was minimized (giving comparatively large values of ��13C) and little water dripped onto the stalagmite (resulting in layers of diminished lateral extent) (Fig. 8C). Several other lines of evidence support this interpretation…the inverse relationship between fluorescence and ��13C further supports the inference that the greatest values of ��13C in Stalagmite ESP03 represent dry periods in which vegetative input of soil CO2 diminished…precipitation of aragonite with large values of ��13C suggests that the change from exceptionally wet conditions to exceptionally dry conditions was ecologically abrupt” (Railsback et al., 2011) ))) “Greater abundance of aragonite, greater values of δ13C, and lesser frequency of Type E surfaces early in the stalagmite suggest a drier and perhaps warmer early to middle Holocene, whereas greater abundance of calcite and frequent Type E surfaces higher in the stalagmite suggest wetter conditions later in the Holocene….The large range of δ13C values in Stalagmite ESP03 and the presence of the greatest values of δ13C beneath Type L surfaces suggests episodes in which climate became sufficiently dry that vegetative input of 12C- enriched CO2 was minimized (giving comparatively large values of δ13C) and little water dripped onto the stalagmite (resulting in layers of diminished lateral extent) (Fig. 8C). Several other lines of evidence support this interpretation…the inverse relationship between fluorescence and δ13C further supports the inference that the greatest values of δ13C in Stalagmite ESP03 represent dry periods in which vegetative input of soil CO2 diminished…precipitation of aragonite with large values of δ13C suggests that the change from exceptionally wet conditions to exceptionally dry conditions was ecologically abrupt” (Railsback et al., 2011) /// “Greater abundance of aragonite, greater values of δ13C, and lesser frequency of Type E surfaces early in the stalagmite suggest a drier and perhaps warmer early to middle Holocene, whereas greater abundance of calcite and frequent Type E surfaces higher in the stalagmite suggest wetter conditions later in the Holocene….The large range of δ13C values in Stalagmite ESP03 and the presence of the greatest values of δ13C beneath Type L surfaces suggests episodes in which climate became sufficiently dry that vegetative input of 12C- enriched CO2 was minimized (giving comparatively large values of δ13C) and little water dripped onto the stalagmite (resulting in layers of diminished lateral extent) (Fig. 8C). Several other lines of evidence support this interpretation…the inverse relationship between fluorescence and δ13C further supports the inference that the greatest values of δ13C in Stalagmite ESP03 represent dry periods in which vegetative input of soil CO2 diminished…precipitation of aragonite with large values of δ13C suggests that the change from exceptionally wet conditions to exceptionally dry conditions was ecologically abrupt” (Railsback et al., 2011)’

Version: 1.0.8

lastVersion: 1.0.7
curator: nicholas
timestamp: 2023-02-09 15:36:09 UTC
notes: Updated lipdverse database entry with a changed file.
changes:
- Geographic metadata:
  - geo_elevation: NULL has been replaced by ‘1240’
- Paleo Column metadata:
  - uncertainty (S2LR2IM9Eo2EJZ): paleoData_notes: NULL has been replaced by ‘NA; paleoData_measurementMaterial has been standardized; paleoData_method has been standardized’
  - uncertainty (S2LR2IM9Eo2EJZ): paleoData_variableName: ‘d13CPrecision’ has been replaced by ‘uncertainty’
  - uncertainty (S2LR2IM9Eo2EJZ): paleoData_measurementMaterial: NULL has been replaced by ‘d13C’
  - uncertainty (S2LR2IM9Eo2EJZ): paleoData_method: NULL has been replaced by ‘precision’
  - uncertainty (S2LR2rXzUnvy7N): paleoData_notes: NULL has been replaced by ‘NA; paleoData_measurementMaterial has been standardized; paleoData_method has been standardized’
  - uncertainty (S2LR2rXzUnvy7N): paleoData_variableName: ‘d13CStandard’ has been replaced by ‘uncertainty’
  - uncertainty (S2LR2rXzUnvy7N): paleoData_measurementMaterial: NULL has been replaced by ‘d13C’
  - uncertainty (S2LR2rXzUnvy7N): paleoData_method: NULL has been replaced by ‘standard’
  - uncertainty (S2LR50R8pzOObC): paleoData_notes: NULL has been replaced by ‘NA; paleoData_measurementMaterial has been standardized; paleoData_method has been standardized’
  - uncertainty (S2LR50R8pzOObC): paleoData_variableName: ‘d18OPrecision’ has been replaced by ‘uncertainty’
  - uncertainty (S2LR50R8pzOObC): paleoData_measurementMaterial: NULL has been replaced by ‘d18O carbonate’
  - uncertainty (S2LR50R8pzOObC): paleoData_method: NULL has been replaced by ‘precision’
  - depth (S2LRnteR6K2JR6): paleoData_notes: NULL has been replaced by ‘NA; paleoData_isPrimary has been standardized’
  - depth (S2LRnteR6K2JR6): paleoData_units: ‘depth_sample’ has been replaced by ‘mm’
  - depth (S2LRnteR6K2JR6): paleoData_isPrimary: NULL has been replaced by ‘TRUE’
  - correction (S2LRPK65HatXRt): paleoData_notes: NULL has been replaced by ‘NA; paleoData_method has been standardized’
  - correction (S2LRPK65HatXRt): paleoData_variableName: ‘hasAragoniteCorrection’ has been replaced by ‘correction’
  - correction (S2LRPK65HatXRt): paleoData_method: NULL has been replaced by ‘aragonite correction’
  - age (S2LRr6PNPd4HGF): paleoData_notes: NULL has been replaced by ‘NA; paleoData_isPrimary has been standardized; paleoData_datum has been standardized’
  - age (S2LRr6PNPd4HGF): paleoData_units: ‘BP’ has been replaced by ‘yr BP’
  - age (S2LRr6PNPd4HGF): paleoData_datum: NULL has been replaced by ‘1950’
  - age (S2LRr6PNPd4HGF): paleoData_isPrimary: NULL has been replaced by ‘TRUE’
  - uncertainty (S2LRrvGcKGKUa5): paleoData_notes: NULL has been replaced by ‘NA; paleoData_measurementMaterial has been standardized; paleoData_method has been standardized’
  - uncertainty (S2LRrvGcKGKUa5): paleoData_variableName: ‘d18OStandard’ has been replaced by ‘uncertainty’
  - uncertainty (S2LRrvGcKGKUa5): paleoData_measurementMaterial: NULL has been replaced by ‘d18O carbonate’
  - uncertainty (S2LRrvGcKGKUa5): paleoData_method: NULL has been replaced by ‘standard’
  - sampleID (S2LRttgTD3ecLi): paleoData_variableName: ‘sisalSampleID’ has been replaced by ‘sampleID’
- Paleo Interpretation metadata:
  - d13C (S2LRP1bVgbttoT): interpretation1_seasonality: ‘1,2,3,4,5,6,7,8,9,10,11,12’ has been replaced by ‘Annual’

Version: 1.0.7

lastVersion: 1.0.6
curator: nicholas
timestamp: 2022-07-28 17:29:30 UTC
changes:
- Geographic metadata:
  - geo_elevation: ‘1240’ has been replaced by NULL

Version: 1.0.6

lastVersion: 1.0.5
curator: nicholas
timestamp: 2022-07-15 22:59:37 UTC
changes:
- Paleo Interpretation metadata:
  - d13CPrecision (S2LR2IM9Eo2EJZ): interpretation1_scope: NULL has been replaced by ‘climate’
  - d13CStandard (S2LR2rXzUnvy7N): interpretation1_scope: NULL has been replaced by ‘climate’
  - d18OPrecision (S2LR50R8pzOObC): interpretation1_scope: NULL has been replaced by ‘climate’
  - hasAragoniteCorrection (S2LRPK65HatXRt): interpretation1_scope: NULL has been replaced by ‘climate’
  - d18OStandard (S2LRrvGcKGKUa5): interpretation1_scope: NULL has been replaced by ‘climate’
  - hasHiatus (S2LRSO5zb7KJ3p): interpretation1_scope: NULL has been replaced by ‘climate’
  - sisalSampleID (S2LRttgTD3ecLi): interpretation1_scope: NULL has been replaced by ‘climate’
  - d18O (S2LRywXyK822Qq): interpretation1_scope: NULL has been replaced by ‘climate’
  - mineralogy (S2LRZsh8y6x7dF): interpretation1_scope: NULL has been replaced by ‘climate’

Version: 1.0.5

lastVersion: 1.0.4
curator: nicholas
timestamp: 2022-05-18 00:25:10 UTC
changes:
- Paleo Interpretation metadata:
  - d13CPrecision (S2LR2IM9Eo2EJZ): interpretation1_scope: ‘climate’ has been replaced by NULL
  - d13CStandard (S2LR2rXzUnvy7N): interpretation1_scope: ‘climate’ has been replaced by NULL
  - d18OPrecision (S2LR50R8pzOObC): interpretation1_scope: ‘climate’ has been replaced by NULL
  - d13C (S2LRP1bVgbttoT): interpretation1_variableGroup: NULL has been replaced by ‘P-E’
  - hasAragoniteCorrection (S2LRPK65HatXRt): interpretation1_scope: ‘climate’ has been replaced by NULL
  - d18OStandard (S2LRrvGcKGKUa5): interpretation1_scope: ‘climate’ has been replaced by NULL
  - hasHiatus (S2LRSO5zb7KJ3p): interpretation1_scope: ‘climate’ has been replaced by NULL
  - sisalSampleID (S2LRttgTD3ecLi): interpretation1_scope: ‘climate’ has been replaced by NULL
  - d18O (S2LRywXyK822Qq): interpretation1_scope: ‘climate’ has been replaced by NULL
  - mineralogy (S2LRZsh8y6x7dF): interpretation1_scope: ‘climate’ has been replaced by NULL
- Paleo Column metadata:
  - d13C (S2LRP1bVgbttoT): paleoData_proxyLumps: NULL has been replaced by ‘isotope’
  - d13C (S2LRP1bVgbttoT): paleoData_proxyLumpsOriginal: NULL has been replaced by ‘d13C’
  - age (S2LRr6PNPd4HGF): paleoData_units: ‘yr BP’ has been replaced by ‘BP’
  - age (S2LRr6PNPd4HGF): paleoData_unitsOriginal: NULL has been replaced by ‘yr BP’
  - d18O (S2LRywXyK822Qq): paleoData_proxyLumps: NULL has been replaced by ‘isotope’
  - d18O (S2LRywXyK822Qq): paleoData_proxyLumpsOriginal: NULL has been replaced by ‘d18O’
- Chron Column metadata:
  - age_type (S2LcRWNaiJrAmv5): chronData_variableName: ‘ageType’ has been replaced by ‘age_type’
  - age_type (S2LcRWNaiJrAmv5): chronData_variableNameOriginal: NULL has been replaced by ‘ageType’

Version: 1.0.4

lastVersion: 1.0.3
curator: nicholas
timestamp: 2021-10-05 21:38:49 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 02:31:30 UTC
changes:
- Paleo Interpretation metadata:
  - d13C (S2LRP1bVgbttoT): interpretation1_seasonality: ‘1,2,3,4,5,6,7,8,9,10,11,635’ 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 01:52:22 UTC
changes:
- Base metadata:
  - archiveType: ‘speleothem’ has been replaced by ‘Speleothem’
- Paleo Interpretation metadata:
  - d13C (S2LRP1bVgbttoT): interpretation1_seasonality: NULL has been replaced by ‘1,2,3,4,5,6,7,8,9,10,11,635’

Version: 1.0.1

lastVersion: 1.0.0
curator: nick
timestamp: 2021-01-12 02:28:42 UTC
changes:
- Paleo Interpretation metadata:
  - d13CPrecision (S2LR2IM9Eo2EJZ): interpretation1_scope: NULL has been replaced by ‘climate’
  - d13CStandard (S2LR2rXzUnvy7N): interpretation1_scope: NULL has been replaced by ‘climate’
  - d18OPrecision (S2LR50R8pzOObC): interpretation1_scope: NULL has been replaced by ‘climate’
  - d13C (S2LRP1bVgbttoT): interpretation1_direction: NULL has been replaced by ‘negative’
  - d13C (S2LRP1bVgbttoT): interpretation1_scope: NULL has been replaced by ‘climate’
  - d13C (S2LRP1bVgbttoT): interpretation1_seasonalityGeneral: NULL has been replaced by ‘Annual’
  - d13C (S2LRP1bVgbttoT): interpretation1_variable: NULL has been replaced by ‘P-E’
  - d13C (S2LRP1bVgbttoT): interpretation1_variableDetail: NULL has been replaced by ‘@surface’
  - hasAragoniteCorrection (S2LRPK65HatXRt): interpretation1_scope: NULL has been replaced by ‘climate’
  - d18OStandard (S2LRrvGcKGKUa5): interpretation1_scope: NULL has been replaced by ‘climate’
  - hasHiatus (S2LRSO5zb7KJ3p): interpretation1_scope: NULL has been replaced by ‘climate’
  - sisalSampleID (S2LRttgTD3ecLi): interpretation1_scope: NULL has been replaced by ‘climate’
  - d18O (S2LRywXyK822Qq): interpretation1_scope: NULL has been replaced by ‘climate’
  - mineralogy (S2LRZsh8y6x7dF): interpretation1_scope: NULL has been replaced by ‘climate’
- Paleo Column metadata:
  - d13C (S2LRP1bVgbttoT): paleoData_notes: NULL has been replaced by ‘“Greater abundance of aragonite, greater values of δ13C, and lesser frequency of Type E surfaces early in the stalagmite suggest a drier and perhaps warmer early to middle Holocene, whereas greater abundance of calcite and frequent Type E surfaces higher in the stalagmite suggest wetter conditions later in the Holocene….The large range of δ13C values in Stalagmite ESP03 and the presence of the greatest values of δ13C beneath Type L surfaces suggests episodes in which climate became sufficiently dry that vegetative input of 12C- enriched CO2 was minimized (giving comparatively large values of δ13C) and little water dripped onto the stalagmite (resulting in layers of diminished lateral extent) (Fig. 8C). Several other lines of evidence support this interpretation…the inverse relationship between fluorescence and δ13C further supports the inference that the greatest values of δ13C in Stalagmite ESP03 represent dry periods in which vegetative input of soil CO2 diminished…precipitation of aragonite with large values of δ13C suggests that the change from exceptionally wet conditions to exceptionally dry conditions was ecologically abrupt” (Railsback et al., 2011)’
  - d13C (S2LRP1bVgbttoT): paleoData_proxy: NULL has been replaced by ‘d13C’
  - d13C (S2LRP1bVgbttoT): paleoData_proxyDetail: NULL has been replaced by ‘mixed calcite/aragonite’
  - d13C (S2LRP1bVgbttoT): paleoData_proxyGeneral: NULL has been replaced by ‘isotope’
  - d13C (S2LRP1bVgbttoT): paleoData_QCCertification: NULL has been replaced by ‘CH’
  - d13C (S2LRP1bVgbttoT): paleoData_QCnotes: NULL has been replaced by ‘“Aragonite is more abundant in the earlier parts of the stalagmite and calcite is more abundant in the later part.” (Railsback et al., 2011)’
  - d18O (S2LRywXyK822Qq): paleoData_notes: NULL has been replaced by ‘“Furthermore, changes in the ESP03 δ18O data, although small, are compatible with warmer and more evaporative conditions during aragonite deposition…δ18O of rainwater increases with temperature in the northwestern Iberian Peninsula, and most relevantly at the inland stations of Leon and Braganca, each of which is about 130 km from Cova da Arcoia. Their Table 3 also shows that δ18O of rainwater decreases with increasing rainfall in the region and thus shows a typical “amount effect”.” (Railsback et al., 2011)’
  - d18O (S2LRywXyK822Qq): paleoData_proxy: NULL has been replaced by ‘d18O’
  - d18O (S2LRywXyK822Qq): paleoData_proxyDetail: NULL has been replaced by ‘mixed calcite/aragonite’
  - d18O (S2LRywXyK822Qq): paleoData_proxyGeneral: NULL has been replaced by ‘isotope’
  - d18O (S2LRywXyK822Qq): paleoData_QCCertification: NULL has been replaced by ‘CH’
  - d18O (S2LRywXyK822Qq): paleoData_QCnotes: NULL has been replaced by ‘“Aragonite is more abundant in the earlier parts of the stalagmite and calcite is more abundant in the later part.” (Railsback et al., 2011)’

Version: 1.0.0

curator: nick
timestamp: 2020-09-29 14:27:13 UTC
notes: Created from SISALv2