Version history for 3Z8BYQsh9EoNBsadmuUP - LS14FOTI
Version: 1.0.6
- lastVersion: 1.0.5
- curator: nicholas
- timestamp: 2025-05-20 16:18:58.705157 UTC
- changes:
- Paleo Interpretation metadata:
- year (MAT24a1c7baff): interpretation5_scope: NULL has been replaced
by ‘climate’
- depth (MATa2cbe1b687): interpretation5_scope: NULL has been replaced
by ‘climate’
Version: 1.0.5
- lastVersion: 1.0.4
- curator: nicholas
- timestamp: 2025-04-17 20:04:40.303059 UTC
- changes:
- Paleo Column metadata:
- d2H (LS14FOTI01A): paleoData_isPrimary: NULL has been replaced by
‘FALSE’
- d2H (LS14FOTI01A): paleoData_primaryAgeColumn: NULL has been
replaced by ‘FALSE’
- d2H (LS14FOTI01B): paleoData_isPrimary: NULL has been replaced by
‘FALSE’
- d2H (LS14FOTI01B): paleoData_primaryAgeColumn: NULL has been
replaced by ‘FALSE’
- year (MAT24a1c7baff): paleoData_isPrimary: NULL has been replaced by
‘TRUE’
- year (MAT24a1c7baff): paleoData_primaryAgeColumn: NULL has been
replaced by ‘TRUE’
- depth (MATa2cbe1b687): paleoData_isPrimary: NULL has been replaced
by ‘FALSE’
- depth (MATa2cbe1b687): paleoData_primaryAgeColumn: NULL has been
replaced by ‘FALSE’
Version: 1.0.4
- lastVersion: 1.0.3
- curator: nicholas
- timestamp: 2025-04-11 16:26:58.668466 UTC
- changes:
- Paleo Interpretation metadata:
- d2H (LS14FOTI01A): interpretation2_basis: ‘Results from both
observational and modeling studies suggest that the dominant control on
modern interannual Andean ?Dp variability is Rayleigh-type fractionation
during rainout along the trajectory of moist air masses across the
Amazon Basin up to the Andes (e.g., Rozanski et al., 1993; Hoffmann et
al., 2003; Vimeux et al., 2005; Vuille and Werner, 2005). Increased
rainout along this trajectory, as well as increased local precipitation
in the Andes, results in more depleted ?Dp, consistent with the
continentality and amount effects that dominate ?Dp variability
throughout most of tropical South America (Vuille et al., 2003).’ has
been replaced by NULL
- d2H (LS14FOTI01A): interpretation2_direction: ‘positive’ has been
replaced by NULL
- d2H (LS14FOTI01A): interpretation2_inferredMaterial: ‘soil water’
has been replaced by NULL
- d2H (LS14FOTI01A): interpretation2_rank: ‘1’ has been replaced by
NULL
- d2H (LS14FOTI01A): interpretation2_scope: ‘isotope’ has been
replaced by ‘climate’
- d2H (LS14FOTI01A): interpretation2_seasonality: ‘Dec-Feb’ has been
replaced by NULL
- d2H (LS14FOTI01A): interpretation2_seasonalityOriginal: ‘SH summer’
has been replaced by NULL
- d2H (LS14FOTI01A): interpretation2_variable: ‘precipitationIsotope’
has been replaced by NULL
- d2H (LS14FOTI01A): interpretation2_variableGroup: ‘P_isotope’ has
been replaced by NULL
- d2H (LS14FOTI01A): interpretation2_variableGroupDirection:
‘positive’ has been replaced by NULL
- d2H (LS14FOTI01A): interpretation3_basis: ‘Results from both
observational and modeling studies suggest that the dominant control on
modern interannual Andean ?Dp variability is Rayleigh-type fractionation
during rainout along the trajectory of moist air masses across the
Amazon Basin up to the Andes (e.g., Rozanski et al., 1993; Hoffmann et
al., 2003; Vimeux et al., 2005; Vuille and Werner, 2005). Increased
rainout along this trajectory, as well as increased local precipitation
in the Andes, results in more depleted ?Dp, consistent with the
continentality and amount effects that dominate ?Dp variability
throughout most of tropical South America (Vuille et al., 2003).’ has
been replaced by NULL
- d2H (LS14FOTI01A): interpretation3_direction: ‘negative’ has been
replaced by NULL
- d2H (LS14FOTI01A): interpretation3_inferredMaterial: ‘soil water’
has been replaced by NULL
- d2H (LS14FOTI01A): interpretation3_rank: ‘2’ has been replaced by
NULL
- d2H (LS14FOTI01A): interpretation3_scope: ‘isotope’ has been
replaced by ‘climate’
- d2H (LS14FOTI01A): interpretation3_seasonality: ‘Dec-Feb’ has been
replaced by NULL
- d2H (LS14FOTI01A): interpretation3_seasonalityOriginal: ‘SH summer’
has been replaced by NULL
- d2H (LS14FOTI01A): interpretation3_variable: ‘deleteMe’ has been
replaced by NULL
- d2H (LS14FOTI01A): interpretation3_variableGroup: ‘continental
effect’ has been replaced by NULL
- d2H (LS14FOTI01A): interpretation4_basis: ‘While the isotopic
composition of precipitation appears to be the primary control on the
structure of the LT ?Dwax record, it is clear that secondary effects
also contribute to this signal. Most notably, the much larger range at
LT (102h) than at Illimani (58h) over the past 19 kyr suggests the
influence of compounding effects on LT ?Dwax, such as decreased regional
precipitation, resulting in a more enriched ?Dp, and low local humidity,
which would tend to further enrich plant source water by soil water
evaporation and/or leaf transpiration. Since such local
evapotranspiration feedbacks would be expected to act in step with ?Dp
changes, this would serve to amplify the ?Dwax signal and increase its
sensitivity to ?Dp variability.’ has been replaced by ‘Results from both
observational and modeling studies suggest that the dominant control on
modern interannual Andean ?Dp variability is Rayleigh-type fractionation
during rainout along the trajectory of moist air masses across the
Amazon Basin up to the Andes (e.g., Rozanski et al., 1993; Hoffmann et
al., 2003; Vimeux et al., 2005; Vuille and Werner, 2005). Increased
rainout along this trajectory, as well as increased local precipitation
in the Andes, results in more depleted ?Dp, consistent with the
continentality and amount effects that dominate ?Dp variability
throughout most of tropical South America (Vuille et al., 2003).’
- d2H (LS14FOTI01A): interpretation4_rank: ‘3’ has been replaced by
‘1’
- d2H (LS14FOTI01A): interpretation4_variable: ‘evaporation’ has been
replaced by ‘precipitationIsotope’
- d2H (LS14FOTI01A): interpretation4_variableGroup:
‘EffectiveMoisture’ has been replaced by ‘P_isotope’
- d2H (LS14FOTI01A): interpretation4_variableGroupDirection:
‘negative’ has been replaced by ‘positive’
- d2H (LS14FOTI01A): interpretation4_variableGroupOriginal: ‘soil
water evapotranspiration’ has been replaced by NULL
- d2H (LS14FOTI01A): interpretation4_seasonality: NULL has been
replaced by ‘Dec-Feb’
- d2H (LS14FOTI01A): interpretation4_seasonalityOriginal: NULL has
been replaced by ‘SH summer’
- d2H (LS14FOTI01A): interpretation5_basis: NULL has been replaced by
‘Results from both observational and modeling studies suggest that the
dominant control on modern interannual Andean ?Dp variability is
Rayleigh-type fractionation during rainout along the trajectory of moist
air masses across the Amazon Basin up to the Andes (e.g., Rozanski et
al., 1993; Hoffmann et al., 2003; Vimeux et al., 2005; Vuille and
Werner, 2005). Increased rainout along this trajectory, as well as
increased local precipitation in the Andes, results in more depleted
?Dp, consistent with the continentality and amount effects that dominate
?Dp variability throughout most of tropical South America (Vuille et
al., 2003).’
- d2H (LS14FOTI01A): interpretation5_direction: NULL has been replaced
by ‘negative’
- d2H (LS14FOTI01A): interpretation5_inferredMaterial: NULL has been
replaced by ‘soil water’
- d2H (LS14FOTI01A): interpretation5_rank: NULL has been replaced by
‘2’
- d2H (LS14FOTI01A): interpretation5_scope: NULL has been replaced by
‘isotope’
- d2H (LS14FOTI01A): interpretation5_seasonality: NULL has been
replaced by ‘Dec-Feb’
- d2H (LS14FOTI01A): interpretation5_seasonalityOriginal: NULL has
been replaced by ‘SH summer’
- d2H (LS14FOTI01A): interpretation5_variable: NULL has been replaced
by ‘deleteMe’
- d2H (LS14FOTI01A): interpretation5_variableGroup: NULL has been
replaced by ‘continental effect’
- d2H (LS14FOTI01A): interpretation6_basis: NULL has been replaced by
‘While the isotopic composition of precipitation appears to be the
primary control on the structure of the LT ?Dwax record, it is clear
that secondary effects also contribute to this signal. Most notably, the
much larger range at LT (102h) than at Illimani (58h) over the past 19
kyr suggests the influence of compounding effects on LT ?Dwax, such as
decreased regional precipitation, resulting in a more enriched ?Dp, and
low local humidity, which would tend to further enrich plant source
water by soil water evaporation and/or leaf transpiration. Since such
local evapotranspiration feedbacks would be expected to act in step with
?Dp changes, this would serve to amplify the ?Dwax signal and increase
its sensitivity to ?Dp variability.’
- d2H (LS14FOTI01A): interpretation6_direction: NULL has been replaced
by ‘positive’
- d2H (LS14FOTI01A): interpretation6_inferredMaterial: NULL has been
replaced by ‘soil water’
- d2H (LS14FOTI01A): interpretation6_rank: NULL has been replaced by
‘3’
- d2H (LS14FOTI01A): interpretation6_scope: NULL has been replaced by
‘isotope’
- d2H (LS14FOTI01A): interpretation6_variable: NULL has been replaced
by ‘evaporation’
- d2H (LS14FOTI01A): interpretation6_variableGroup: NULL has been
replaced by ‘EffectiveMoisture’
- d2H (LS14FOTI01A): interpretation6_variableGroupDirection: NULL has
been replaced by ‘negative’
- d2H (LS14FOTI01A): interpretation6_variableGroupOriginal: NULL has
been replaced by ‘soil water evapotranspiration’
- d2H (LS14FOTI01B): interpretation2_basis: ‘Results from both
observational and modeling studies suggest that the dominant control on
modern interannual Andean ?Dp variability is Rayleigh-type fractionation
during rainout along the trajectory of moist air masses across the
Amazon Basin up to the Andes (e.g., Rozanski et al., 1993; Hoffmann et
al., 2003; Vimeux et al., 2005; Vuille and Werner, 2005). Increased
rainout along this trajectory, as well as increased local precipitation
in the Andes, results in more depleted ?Dp, consistent with the
continentality and amount effects that dominate ?Dp variability
throughout most of tropical South America (Vuille et al., 2003).’ has
been replaced by NULL
- d2H (LS14FOTI01B): interpretation2_direction: ‘positive’ has been
replaced by NULL
- d2H (LS14FOTI01B): interpretation2_inferredMaterial: ‘soil water’
has been replaced by NULL
- d2H (LS14FOTI01B): interpretation2_rank: ‘1’ has been replaced by
NULL
- d2H (LS14FOTI01B): interpretation2_scope: ‘isotope’ has been
replaced by ‘climate’
- d2H (LS14FOTI01B): interpretation2_seasonality: ‘Dec-Feb’ has been
replaced by NULL
- d2H (LS14FOTI01B): interpretation2_seasonalityOriginal: ‘SH summer’
has been replaced by NULL
- d2H (LS14FOTI01B): interpretation2_variable: ‘precipitationIsotope’
has been replaced by NULL
- d2H (LS14FOTI01B): interpretation2_variableGroup: ‘P_isotope’ has
been replaced by NULL
- d2H (LS14FOTI01B): interpretation2_variableGroupDirection:
‘positive’ has been replaced by NULL
- d2H (LS14FOTI01B): interpretation3_basis: ‘Results from both
observational and modeling studies suggest that the dominant control on
modern interannual Andean ?Dp variability is Rayleigh-type fractionation
during rainout along the trajectory of moist air masses across the
Amazon Basin up to the Andes (e.g., Rozanski et al., 1993; Hoffmann et
al., 2003; Vimeux et al., 2005; Vuille and Werner, 2005). Increased
rainout along this trajectory, as well as increased local precipitation
in the Andes, results in more depleted ?Dp, consistent with the
continentality and amount effects that dominate ?Dp variability
throughout most of tropical South America (Vuille et al., 2003).’ has
been replaced by NULL
- d2H (LS14FOTI01B): interpretation3_direction: ‘negative’ has been
replaced by NULL
- d2H (LS14FOTI01B): interpretation3_rank: ‘2’ has been replaced by
NULL
- d2H (LS14FOTI01B): interpretation3_scope: ‘isotope’ has been
replaced by ‘climate’
- d2H (LS14FOTI01B): interpretation3_seasonality: ‘Dec-Feb’ has been
replaced by NULL
- d2H (LS14FOTI01B): interpretation3_seasonalityOriginal: ‘SH summer’
has been replaced by NULL
- d2H (LS14FOTI01B): interpretation3_variable: ‘deleteMe’ has been
replaced by NULL
- d2H (LS14FOTI01B): interpretation3_variableGroup: ‘continental
effect’ has been replaced by NULL
- d2H (LS14FOTI01B): interpretation4_basis: ‘While the isotopic
composition of precipitation appears to be the primary control on the
structure of the LT ?Dwax record, it is clear that secondary effects
also contribute to this signal. Most notably, the much larger range at
LT (102h) than at Illimani (58h) over the past 19 kyr suggests the
influence of compounding effects on LT ?Dwax, such as decreased regional
precipitation, resulting in a more enriched ?Dp, and low local humidity,
which would tend to further enrich plant source water by soil water
evaporation and/or leaf transpiration. Since such local
evapotranspiration feedbacks would be expected to act in step with ?Dp
changes, this would serve to amplify the ?Dwax signal and increase its
sensitivity to ?Dp variability.’ has been replaced by ‘Results from both
observational and modeling studies suggest that the dominant control on
modern interannual Andean ?Dp variability is Rayleigh-type fractionation
during rainout along the trajectory of moist air masses across the
Amazon Basin up to the Andes (e.g., Rozanski et al., 1993; Hoffmann et
al., 2003; Vimeux et al., 2005; Vuille and Werner, 2005). Increased
rainout along this trajectory, as well as increased local precipitation
in the Andes, results in more depleted ?Dp, consistent with the
continentality and amount effects that dominate ?Dp variability
throughout most of tropical South America (Vuille et al., 2003).’
- d2H (LS14FOTI01B): interpretation4_inferredMaterial: NULL has been
replaced by ‘soil water’
- d2H (LS14FOTI01B): interpretation4_rank: ‘3’ has been replaced by
‘1’
- d2H (LS14FOTI01B): interpretation4_variable: ‘evaporation’ has been
replaced by ‘precipitationIsotope’
- d2H (LS14FOTI01B): interpretation4_variableGroup:
‘EffectiveMoisture’ has been replaced by ‘P_isotope’
- d2H (LS14FOTI01B): interpretation4_variableGroupDirection:
‘negative’ has been replaced by ‘positive’
- d2H (LS14FOTI01B): interpretation4_variableGroupOriginal: ‘soil
water evapotranspiration’ has been replaced by NULL
- d2H (LS14FOTI01B): interpretation4_seasonality: NULL has been
replaced by ‘Dec-Feb’
- d2H (LS14FOTI01B): interpretation4_seasonalityOriginal: NULL has
been replaced by ‘SH summer’
- d2H (LS14FOTI01B): interpretation5_basis: NULL has been replaced by
‘Results from both observational and modeling studies suggest that the
dominant control on modern interannual Andean ?Dp variability is
Rayleigh-type fractionation during rainout along the trajectory of moist
air masses across the Amazon Basin up to the Andes (e.g., Rozanski et
al., 1993; Hoffmann et al., 2003; Vimeux et al., 2005; Vuille and
Werner, 2005). Increased rainout along this trajectory, as well as
increased local precipitation in the Andes, results in more depleted
?Dp, consistent with the continentality and amount effects that dominate
?Dp variability throughout most of tropical South America (Vuille et
al., 2003).’
- d2H (LS14FOTI01B): interpretation5_direction: NULL has been replaced
by ‘negative’
- d2H (LS14FOTI01B): interpretation5_rank: NULL has been replaced by
‘2’
- d2H (LS14FOTI01B): interpretation5_scope: NULL has been replaced by
‘isotope’
- d2H (LS14FOTI01B): interpretation5_seasonality: NULL has been
replaced by ‘Dec-Feb’
- d2H (LS14FOTI01B): interpretation5_seasonalityOriginal: NULL has
been replaced by ‘SH summer’
- d2H (LS14FOTI01B): interpretation5_variable: NULL has been replaced
by ‘deleteMe’
- d2H (LS14FOTI01B): interpretation5_variableGroup: NULL has been
replaced by ‘continental effect’
- d2H (LS14FOTI01B): interpretation6_basis: NULL has been replaced by
‘While the isotopic composition of precipitation appears to be the
primary control on the structure of the LT ?Dwax record, it is clear
that secondary effects also contribute to this signal. Most notably, the
much larger range at LT (102h) than at Illimani (58h) over the past 19
kyr suggests the influence of compounding effects on LT ?Dwax, such as
decreased regional precipitation, resulting in a more enriched ?Dp, and
low local humidity, which would tend to further enrich plant source
water by soil water evaporation and/or leaf transpiration. Since such
local evapotranspiration feedbacks would be expected to act in step with
?Dp changes, this would serve to amplify the ?Dwax signal and increase
its sensitivity to ?Dp variability.’
- d2H (LS14FOTI01B): interpretation6_direction: NULL has been replaced
by ‘positive’
- d2H (LS14FOTI01B): interpretation6_rank: NULL has been replaced by
‘3’
- d2H (LS14FOTI01B): interpretation6_scope: NULL has been replaced by
‘isotope’
- d2H (LS14FOTI01B): interpretation6_variable: NULL has been replaced
by ‘evaporation’
- d2H (LS14FOTI01B): interpretation6_variableGroup: NULL has been
replaced by ‘EffectiveMoisture’
- d2H (LS14FOTI01B): interpretation6_variableGroupDirection: NULL has
been replaced by ‘negative’
- d2H (LS14FOTI01B): interpretation6_variableGroupOriginal: NULL has
been replaced by ‘soil water evapotranspiration’
- year (MAT24a1c7baff): interpretation1_scope: NULL has been replaced
by ‘climate’
- year (MAT24a1c7baff): interpretation2_scope: NULL has been replaced
by ‘climate’
- year (MAT24a1c7baff): interpretation3_scope: NULL has been replaced
by ‘climate’
- year (MAT24a1c7baff): interpretation4_scope: NULL has been replaced
by ‘climate’
- depth (MATa2cbe1b687): interpretation1_scope: NULL has been replaced
by ‘climate’
- depth (MATa2cbe1b687): interpretation2_scope: NULL has been replaced
by ‘climate’
- depth (MATa2cbe1b687): interpretation3_scope: NULL has been replaced
by ‘climate’
- depth (MATa2cbe1b687): interpretation4_scope: NULL has been replaced
by ‘climate’
Version: 1.0.3
- lastVersion: 1.0.2
- curator: nicholas
- timestamp: 2025-04-09 20:48:18.679689 UTC
- notes: Updated lipdverse database entry with a changed
file.
- changes:
- Paleo Interpretation metadata:
- d2H (LS14FOTI01A): interpretation1_seasonality: ‘DJF’ has been
replaced by ‘Dec-Feb’
- d2H (LS14FOTI01A): interpretation1_variable: ‘South American Summer
Monsoon precipitation intensity’ has been replaced by
‘circulationVariable’
- d2H (LS14FOTI01A): interpretation2_seasonality: ‘DJF’ has been
replaced by ‘Dec-Feb’
- d2H (LS14FOTI01A): interpretation2_variable: ‘P_isotope’ has been
replaced by ‘precipitationIsotope’
- d2H (LS14FOTI01A): interpretation3_seasonality: ‘DJF’ has been
replaced by ‘Dec-Feb’
- d2H (LS14FOTI01A): interpretation3_variable: ‘continental effect’
has been replaced by ‘deleteMe’
- d2H (LS14FOTI01A): interpretation4_variable: ‘soil water
evapotranspiration’ has been replaced by ‘evaporation’
- d2H (LS14FOTI01B): interpretation1_seasonality: ‘DJF’ has been
replaced by ‘Dec-Feb’
- d2H (LS14FOTI01B): interpretation1_variable: ‘South American Summer
Monsoon precipitation intensity’ has been replaced by
‘circulationVariable’
- d2H (LS14FOTI01B): interpretation2_seasonality: ‘DJF’ has been
replaced by ‘Dec-Feb’
- d2H (LS14FOTI01B): interpretation2_variable: ‘P_isotope’ has been
replaced by ‘precipitationIsotope’
- d2H (LS14FOTI01B): interpretation3_seasonality: ‘DJF’ has been
replaced by ‘Dec-Feb’
- d2H (LS14FOTI01B): interpretation3_variable: ‘continental effect’
has been replaced by ‘deleteMe’
- d2H (LS14FOTI01B): interpretation4_variable: ‘soil water
evapotranspiration’ has been replaced by ‘evaporation’
Version: 1.0.2
- lastVersion: 1.0.1
- curator: nicholas
- timestamp: 2025-04-09 18:35:50.291955 UTC
- notes: Changes made as part of LiPDverse vocabulary
standardization process
- changes:
- Paleo Interpretation metadata:
- d2H (LS14FOTI01A): interpretation1_seasonality: ‘DJF’ has been
replaced by ‘Dec-Feb’
- d2H (LS14FOTI01A): interpretation1_variable: ‘South American Summer
Monsoon precipitation intensity’ has been replaced by
‘circulationVariable’
- d2H (LS14FOTI01A): interpretation2_seasonality: ‘DJF’ has been
replaced by ‘Dec-Feb’
- d2H (LS14FOTI01A): interpretation2_variable: ‘P_isotope’ has been
replaced by ‘precipitationIsotope’
- d2H (LS14FOTI01A): interpretation3_seasonality: ‘DJF’ has been
replaced by ‘Dec-Feb’
- d2H (LS14FOTI01A): interpretation3_variable: ‘continental effect’
has been replaced by ‘deleteMe’
- d2H (LS14FOTI01A): interpretation4_variable: ‘soil water
evapotranspiration’ has been replaced by ‘evaporation’
- d2H (LS14FOTI01B): interpretation1_seasonality: ‘DJF’ has been
replaced by ‘Dec-Feb’
- d2H (LS14FOTI01B): interpretation1_variable: ‘South American Summer
Monsoon precipitation intensity’ has been replaced by
‘circulationVariable’
- d2H (LS14FOTI01B): interpretation2_seasonality: ‘DJF’ has been
replaced by ‘Dec-Feb’
- d2H (LS14FOTI01B): interpretation2_variable: ‘P_isotope’ has been
replaced by ‘precipitationIsotope’
- d2H (LS14FOTI01B): interpretation3_seasonality: ‘DJF’ has been
replaced by ‘Dec-Feb’
- d2H (LS14FOTI01B): interpretation3_variable: ‘continental effect’
has been replaced by ‘deleteMe’
- d2H (LS14FOTI01B): interpretation4_variable: ‘soil water
evapotranspiration’ has been replaced by ‘evaporation’
Version: 1.0.1
- lastVersion: 1.0.0
- curator: nicholas
- timestamp: 2025-04-08 17:32:59.340868 UTC
- notes: Changes made as part of LiPDverse vocabulary
standardization process
- changes:
- Paleo Column metadata:
- d2H (LS14FOTI01A): paleoData_longName: NULL has been replaced by
‘AD’
- d2H (LS14FOTI01B): paleoData_longName: NULL has been replaced by
‘AD’
- year (MAT24a1c7baff): paleoData_units: ‘AD’ has been replaced by ‘yr
AD’
- year (MAT24a1c7baff): paleoData_longName: NULL has been replaced by
‘AD’
- depth (MATa2cbe1b687): paleoData_longName: NULL has been replaced by
‘AD’