Version history for YIwPP7ZlqUTMFrGi801m - LS09MAZO
Version: 1.0.5
- lastVersion: 1.0.4
- curator: nicholas
- timestamp: 2025-04-17 20:04:36.365787 UTC
- changes:
- Paleo Column metadata:
- d18O (LS09MAZO): paleoData_isPrimary: NULL has been replaced by
‘FALSE’
- d18O (LS09MAZO): paleoData_primaryAgeColumn: NULL has been replaced
by ‘FALSE’
- depth (MAT34e2434019): paleoData_isPrimary: NULL has been replaced
by ‘FALSE’
- depth (MAT34e2434019): paleoData_primaryAgeColumn: NULL has been
replaced by ‘FALSE’
- year (MAT7a4af74c79): paleoData_isPrimary: NULL has been replaced by
‘TRUE’
- year (MAT7a4af74c79): paleoData_primaryAgeColumn: NULL has been
replaced by ‘TRUE’
Version: 1.0.4
- lastVersion: 1.0.3
- curator: nicholas
- timestamp: 2025-04-11 16:26:54.508472 UTC
- changes:
- Paleo Interpretation metadata:
- d18O (LS09MAZO): interpretation1_basis: ‘However, the continuous
enrichment of 18O, due to evaporation, during spring and summer results
in heavier isotope values at the end of the warm seasons. Consequently,
the isotopic oscillations can be interpreted as a reflection of changes
in the intensity of the evaporation processes (Li and Ku,1997) that
cancel out the opposite effect of the temperature increase (decreasing
isotopic fractionation with increasing temperature; McCrea, 1950).’ has
been replaced by NULL
- d18O (LS09MAZO): interpretation1_direction: ‘negative’ has been
replaced by NULL
- d18O (LS09MAZO): interpretation1_equilibriumEvidence: ‘Isotopic
values ?18O of calcite precipitating in the surface waters of Zo�ar Lake
obtained from a buoy and anchor rope concretion growth show values
(between ?2 to +1? vs V-PDB) coherent with calcite formation in isotopic
equilibriumwith epilimnetic lake waters (+1 to + 6??18Owater (V-SMOW))’
has been replaced by NULL
- d18O (LS09MAZO): interpretation1_inferredMaterial: ‘lake water’ has
been replaced by NULL
- d18O (LS09MAZO): interpretation1_rank: ‘1’ has been replaced by
NULL
- d18O (LS09MAZO): interpretation1_scope: ‘isotope’ has been replaced
by ‘climate’
- d18O (LS09MAZO): interpretation1_variable: ‘hydrologicBalance’ has
been replaced by NULL
- d18O (LS09MAZO): interpretation1_variableGroup: ‘EffectiveMoisture’
has been replaced by NULL
- d18O (LS09MAZO): interpretation1_variableGroupDirection: ‘negative’
has been replaced by NULL
- d18O (LS09MAZO): interpretation1_variableGroupOriginal: ‘I_E’ has
been replaced by NULL
- d18O (LS09MAZO): interpretation2_direction: ‘negative’ has been
replaced by NULL
- d18O (LS09MAZO): interpretation2_equilibriumEvidence: ‘Isotopic
values ?18O of calcite precipitating in the surface waters of Zo�ar Lake
obtained from a buoy and anchor rope concretion growth show values
(between ?2 to +1? vs V-PDB) coherent with calcite formation in isotopic
equilibriumwith epilimnetic lake waters (+1 to + 6??18Owater (V-SMOW))’
has been replaced by NULL
- d18O (LS09MAZO): interpretation2_inferredMaterial: ‘lake water’ has
been replaced by NULL
- d18O (LS09MAZO): interpretation2_rank: ‘2’ has been replaced by
NULL
- d18O (LS09MAZO): interpretation2_scope: ‘isotope’ has been replaced
by ‘climate’
- d18O (LS09MAZO): interpretation2_variable: ‘temperature’ has been
replaced by NULL
- d18O (LS09MAZO): interpretation2_variableGroup: ‘Temperature’ has
been replaced by NULL
- d18O (LS09MAZO): interpretation2_variableGroupDirection: ‘negative’
has been replaced by NULL
- d18O (LS09MAZO): interpretation2_variableGroupOriginal: ‘T’ has been
replaced by NULL
- d18O (LS09MAZO): interpretation2_variableOriginal: ‘Temperature’ has
been replaced by NULL
- d18O (LS09MAZO): interpretation3_scope: NULL has been replaced by
‘climate’
- d18O (LS09MAZO): interpretation4_basis: NULL has been replaced by
‘However, the continuous enrichment of 18O, due to evaporation, during
spring and summer results in heavier isotope values at the end of the
warm seasons. Consequently, the isotopic oscillations can be interpreted
as a reflection of changes in the intensity of the evaporation processes
(Li and Ku,1997) that cancel out the opposite effect of the temperature
increase (decreasing isotopic fractionation with increasing temperature;
McCrea, 1950).’
- d18O (LS09MAZO): interpretation4_direction: NULL has been replaced
by ‘negative’
- d18O (LS09MAZO): interpretation4_equilibriumEvidence: NULL has been
replaced by ‘Isotopic values ?18O of calcite precipitating in the
surface waters of Zo�ar Lake obtained from a buoy and anchor rope
concretion growth show values (between ?2 to +1? vs V-PDB) coherent with
calcite formation in isotopic equilibriumwith epilimnetic lake waters
(+1 to + 6??18Owater (V-SMOW))’
- d18O (LS09MAZO): interpretation4_inferredMaterial: NULL has been
replaced by ‘lake water’
- d18O (LS09MAZO): interpretation4_rank: NULL has been replaced by
‘1’
- d18O (LS09MAZO): interpretation4_scope: NULL has been replaced by
‘isotope’
- d18O (LS09MAZO): interpretation4_variable: NULL has been replaced by
‘hydrologicBalance’
- d18O (LS09MAZO): interpretation4_variableGroup: NULL has been
replaced by ‘EffectiveMoisture’
- d18O (LS09MAZO): interpretation4_variableGroupDirection: NULL has
been replaced by ‘negative’
- d18O (LS09MAZO): interpretation4_variableGroupOriginal: NULL has
been replaced by ‘I_E’
- d18O (LS09MAZO): interpretation5_direction: NULL has been replaced
by ‘negative’
- d18O (LS09MAZO): interpretation5_equilibriumEvidence: NULL has been
replaced by ‘Isotopic values ?18O of calcite precipitating in the
surface waters of Zo�ar Lake obtained from a buoy and anchor rope
concretion growth show values (between ?2 to +1? vs V-PDB) coherent with
calcite formation in isotopic equilibriumwith epilimnetic lake waters
(+1 to + 6??18Owater (V-SMOW))’
- d18O (LS09MAZO): interpretation5_inferredMaterial: NULL has been
replaced by ‘lake water’
- d18O (LS09MAZO): interpretation5_rank: NULL has been replaced by
‘2’
- d18O (LS09MAZO): interpretation5_scope: NULL has been replaced by
‘isotope’
- d18O (LS09MAZO): interpretation5_variable: NULL has been replaced by
‘temperature’
- d18O (LS09MAZO): interpretation5_variableGroup: NULL has been
replaced by ‘Temperature’
- d18O (LS09MAZO): interpretation5_variableGroupDirection: NULL has
been replaced by ‘negative’
- d18O (LS09MAZO): interpretation5_variableGroupOriginal: NULL has
been replaced by ‘T’
- d18O (LS09MAZO): interpretation5_variableOriginal: NULL has been
replaced by ‘Temperature’
- d18O (LS09MAZO): interpretation6_scope: NULL has been replaced by
‘isotope’
- depth (MAT34e2434019): interpretation1_scope: NULL has been replaced
by ‘climate’
- depth (MAT34e2434019): interpretation2_scope: NULL has been replaced
by ‘climate’
- year (MAT7a4af74c79): interpretation1_scope: NULL has been replaced
by ‘climate’
- year (MAT7a4af74c79): interpretation2_scope: NULL has been replaced
by ‘climate’
Version: 1.0.3
- lastVersion: 1.0.2
- curator: nicholas
- timestamp: 2025-04-09 20:47:36.875478 UTC
- notes: Updated lipdverse database entry with a changed
file.
- changes:
- Paleo Interpretation metadata:
- d18O (LS09MAZO): interpretation1_variable: ‘I_E’ has been replaced
by ‘hydrologicBalance’
- d18O (LS09MAZO): interpretation2_variable: ‘T’ has been replaced by
‘temperature’
Version: 1.0.2
- lastVersion: 1.0.1
- curator: nicholas
- timestamp: 2025-04-09 18:13:49.489485 UTC
- notes: Changes made as part of LiPDverse vocabulary
standardization process
- changes:
- Paleo Interpretation metadata:
- d18O (LS09MAZO): interpretation1_variable: ‘I_E’ has been replaced
by ‘hydrologicBalance’
- d18O (LS09MAZO): interpretation2_variable: ‘T’ has been replaced by
‘temperature’
Version: 1.0.1
- lastVersion: 1.0.0
- curator: nicholas
- timestamp: 2025-04-08 17:32:55.083023 UTC
- notes: Changes made as part of LiPDverse vocabulary
standardization process
- changes:
- Paleo Column metadata:
- d18O (LS09MAZO): paleoData_longName: NULL has been replaced by
‘AD’
- depth (MAT34e2434019): paleoData_longName: NULL has been replaced by
‘AD’
- year (MAT7a4af74c79): paleoData_units: ‘AD’ has been replaced by ‘yr
AD’
- year (MAT7a4af74c79): paleoData_longName: NULL has been replaced by
‘AD’