Version history for v7SfC8Nj0B53aryVfSyk - LS14KOSA
Version: 1.0.6
- lastVersion: 1.0.5
- curator: nicholas
- timestamp: 2025-05-20 16:18:58.802213 UTC
- changes:
- Paleo Interpretation metadata:
- year (MAT11712e4d07): interpretation4_scope: NULL has been replaced
by ‘climate’
- depth (MATb0c73ae5e6): interpretation4_scope: NULL has been replaced
by ‘climate’
Version: 1.0.5
- lastVersion: 1.0.4
- curator: nicholas
- timestamp: 2025-04-17 20:04:40.414878 UTC
- changes:
- Paleo Column metadata:
- d2H (LS14KOSA01A): paleoData_isPrimary: NULL has been replaced by
‘FALSE’
- d2H (LS14KOSA01A): paleoData_primaryAgeColumn: NULL has been
replaced by ‘FALSE’
- year (MAT11712e4d07): paleoData_isPrimary: NULL has been replaced by
‘TRUE’
- year (MAT11712e4d07): paleoData_primaryAgeColumn: NULL has been
replaced by ‘TRUE’
- depth (MATb0c73ae5e6): paleoData_isPrimary: NULL has been replaced
by ‘FALSE’
- depth (MATb0c73ae5e6): paleoData_primaryAgeColumn: NULL has been
replaced by ‘FALSE’
Version: 1.0.4
- lastVersion: 1.0.3
- curator: nicholas
- timestamp: 2025-04-11 16:26:58.765008 UTC
- changes:
- Paleo Interpretation metadata:
- d2H (LS14KOSA01A): interpretation2_basis: ‘In East Africa, stable
isotopes in modern precipitation have been shown to reflect large-scale
atmospheric circulation processes (Vuille et al., 2005), and the ?18O of
precipitation (and by inference, the ?D of precipitation) on Mt. Kenya
has been shown to be a good indicator of moisture balance (Barker et
al., 2001). Leaf wax ?D reflects ?Dprecip, after a series of offsets due
to soil water evaporation, fractionation of leaf water relative to xylem
water, and biosynthesis (Sachse et al., 2012).’ has been replaced by
NULL
- d2H (LS14KOSA01A): interpretation2_direction: ‘positive’ has been
replaced by NULL
- d2H (LS14KOSA01A): interpretation2_inferredMaterial: ‘soil water’
has been replaced by NULL
- d2H (LS14KOSA01A): interpretation2_mathematicalRelation: ‘linear’
has been replaced by NULL
- d2H (LS14KOSA01A): interpretation2_rank: ‘1’ has been replaced by
NULL
- d2H (LS14KOSA01A): interpretation2_scope: ‘isotope’ has been
replaced by ‘climate’
- d2H (LS14KOSA01A): interpretation2_seasonality: ‘Annual’ has been
replaced by NULL
- d2H (LS14KOSA01A): interpretation2_seasonalityOriginal: ‘Annual’ has
been replaced by NULL
- d2H (LS14KOSA01A): interpretation2_variable: ‘precipitationIsotope’
has been replaced by NULL
- d2H (LS14KOSA01A): interpretation2_variableGroup: ‘P_isotope’ has
been replaced by NULL
- d2H (LS14KOSA01A): interpretation2_variableGroupDirection:
‘positive’ has been replaced by NULL
- d2H (LS14KOSA01A): interpretation3_basis: ‘Air temperature has 2
influences: “air temperature is important for the elevation of the zone
of maximum rainfall (ZMR) on Mt. Kenya” and for soil/lake evaporation.
“Recent drying may have also been locally enhanced by a recent rise in
temperature (via an upward shift in the ZMR and/or increased evaporation
of soil water).”’ has been replaced by NULL
- d2H (LS14KOSA01A): interpretation3_direction: ‘positive’ has been
replaced by NULL
- d2H (LS14KOSA01A): interpretation3_inferredMaterial: ‘soil water’
has been replaced by NULL
- d2H (LS14KOSA01A): interpretation3_rank: ‘2’ has been replaced by
NULL
- d2H (LS14KOSA01A): interpretation3_scope: ‘isotope’ has been
replaced by ‘climate’
- d2H (LS14KOSA01A): interpretation3_seasonality: ‘Annual’ has been
replaced by NULL
- d2H (LS14KOSA01A): interpretation3_seasonalityOriginal: ‘Annual’ has
been replaced by NULL
- d2H (LS14KOSA01A): interpretation3_variable: ‘temperature’ has been
replaced by NULL
- d2H (LS14KOSA01A): interpretation3_variableGroup: ‘Temperature’ has
been replaced by NULL
- d2H (LS14KOSA01A): interpretation3_variableGroupDirection:
‘negative’ has been replaced by NULL
- d2H (LS14KOSA01A): interpretation3_variableGroupOriginal: ‘T_air’
has been replaced by NULL
- d2H (LS14KOSA01A): interpretation4_basis: NULL has been replaced by
‘In East Africa, stable isotopes in modern precipitation have been shown
to reflect large-scale atmospheric circulation processes (Vuille et al.,
2005), and the ?18O of precipitation (and by inference, the ?D of
precipitation) on Mt. Kenya has been shown to be a good indicator of
moisture balance (Barker et al., 2001). Leaf wax ?D reflects ?Dprecip,
after a series of offsets due to soil water evaporation, fractionation
of leaf water relative to xylem water, and biosynthesis (Sachse et al.,
2012).’
- d2H (LS14KOSA01A): interpretation4_direction: NULL has been replaced
by ‘positive’
- d2H (LS14KOSA01A): interpretation4_inferredMaterial: NULL has been
replaced by ‘soil water’
- d2H (LS14KOSA01A): interpretation4_mathematicalRelation: NULL has
been replaced by ‘linear’
- d2H (LS14KOSA01A): interpretation4_rank: NULL has been replaced by
‘1’
- d2H (LS14KOSA01A): interpretation4_scope: NULL has been replaced by
‘isotope’
- d2H (LS14KOSA01A): interpretation4_seasonality: NULL has been
replaced by ‘Annual’
- d2H (LS14KOSA01A): interpretation4_seasonalityOriginal: NULL has
been replaced by ‘Annual’
- d2H (LS14KOSA01A): interpretation4_variable: NULL has been replaced
by ‘precipitationIsotope’
- d2H (LS14KOSA01A): interpretation4_variableGroup: NULL has been
replaced by ‘P_isotope’
- d2H (LS14KOSA01A): interpretation4_variableGroupDirection: NULL has
been replaced by ‘positive’
- d2H (LS14KOSA01A): interpretation5_basis: NULL has been replaced by
‘Air temperature has 2 influences: “air temperature is important for the
elevation of the zone of maximum rainfall (ZMR) on Mt. Kenya” and for
soil/lake evaporation. “Recent drying may have also been locally
enhanced by a recent rise in temperature (via an upward shift in the ZMR
and/or increased evaporation of soil water).”’
- d2H (LS14KOSA01A): interpretation5_direction: NULL has been replaced
by ‘positive’
- d2H (LS14KOSA01A): interpretation5_inferredMaterial: NULL has been
replaced by ‘soil water’
- d2H (LS14KOSA01A): interpretation5_rank: NULL has been replaced by
‘2’
- d2H (LS14KOSA01A): interpretation5_scope: NULL has been replaced by
‘isotope’
- d2H (LS14KOSA01A): interpretation5_seasonality: NULL has been
replaced by ‘Annual’
- d2H (LS14KOSA01A): interpretation5_seasonalityOriginal: NULL has
been replaced by ‘Annual’
- d2H (LS14KOSA01A): interpretation5_variable: NULL has been replaced
by ‘temperature’
- d2H (LS14KOSA01A): interpretation5_variableGroup: NULL has been
replaced by ‘Temperature’
- d2H (LS14KOSA01A): interpretation5_variableGroupDirection: NULL has
been replaced by ‘negative’
- d2H (LS14KOSA01A): interpretation5_variableGroupOriginal: NULL has
been replaced by ‘T_air’
- d2H (LS14KOSA01A): interpretation6_scope: NULL has been replaced by
‘isotope’
- year (MAT11712e4d07): interpretation1_scope: NULL has been replaced
by ‘climate’
- year (MAT11712e4d07): interpretation2_scope: NULL has been replaced
by ‘climate’
- year (MAT11712e4d07): interpretation3_scope: NULL has been replaced
by ‘climate’
- depth (MATb0c73ae5e6): interpretation1_scope: NULL has been replaced
by ‘climate’
- depth (MATb0c73ae5e6): interpretation2_scope: NULL has been replaced
by ‘climate’
- depth (MATb0c73ae5e6): interpretation3_scope: NULL has been replaced
by ‘climate’
Version: 1.0.3
- lastVersion: 1.0.2
- curator: nicholas
- timestamp: 2025-04-09 20:48:19.100465 UTC
- notes: Updated lipdverse database entry with a changed
file.
- changes:
- Paleo Interpretation metadata:
- d2H (LS14KOSA01A): interpretation1_seasonality: ‘OND’ has been
replaced by ‘Oct-Dec’
- d2H (LS14KOSA01A): interpretation1_variable: ‘strength of Indian
ocean moisture transport’ has been replaced by
‘circulationVariable’
- d2H (LS14KOSA01A): interpretation2_seasonality: ‘annual’ has been
replaced by ‘Annual’
- d2H (LS14KOSA01A): interpretation2_variable: ‘P_isotope’ has been
replaced by ‘precipitationIsotope’
- d2H (LS14KOSA01A): interpretation3_seasonality: ‘annual’ has been
replaced by ‘Annual’
- d2H (LS14KOSA01A): interpretation3_variable: ‘T_air’ has been
replaced by ‘temperature’
Version: 1.0.2
- lastVersion: 1.0.1
- curator: nicholas
- timestamp: 2025-04-09 18:36:02.48522 UTC
- notes: Changes made as part of LiPDverse vocabulary
standardization process
- changes:
- Paleo Interpretation metadata:
- d2H (LS14KOSA01A): interpretation1_seasonality: ‘OND’ has been
replaced by ‘Oct-Dec’
- d2H (LS14KOSA01A): interpretation1_variable: ‘strength of Indian
ocean moisture transport’ has been replaced by
‘circulationVariable’
- d2H (LS14KOSA01A): interpretation2_seasonality: ‘annual’ has been
replaced by ‘Annual’
- d2H (LS14KOSA01A): interpretation2_variable: ‘P_isotope’ has been
replaced by ‘precipitationIsotope’
- d2H (LS14KOSA01A): interpretation3_seasonality: ‘annual’ has been
replaced by ‘Annual’
- d2H (LS14KOSA01A): interpretation3_variable: ‘T_air’ has been
replaced by ‘temperature’
Version: 1.0.1
- lastVersion: 1.0.0
- curator: nicholas
- timestamp: 2025-04-08 17:32:59.452481 UTC
- notes: Changes made as part of LiPDverse vocabulary
standardization process
- changes:
- Paleo Column metadata:
- d2H (LS14KOSA01A): paleoData_longName: NULL has been replaced by
‘AD’
- year (MAT11712e4d07): paleoData_units: ‘AD’ has been replaced by ‘yr
AD’
- year (MAT11712e4d07): paleoData_longName: NULL has been replaced by
‘AD’
- depth (MATb0c73ae5e6): paleoData_longName: NULL has been replaced by
‘AD’