Version history for VYzgVofnd2a4n10KLt6H - LS14ATJU
Version: 1.0.5
- lastVersion: 1.0.4
- curator: nicholas
- timestamp: 2025-04-17 20:04:40.089854 UTC
- changes:
- Paleo Column metadata:
- d2H (LS14ATJU01A): paleoData_isPrimary: NULL has been replaced by
‘FALSE’
- d2H (LS14ATJU01A): paleoData_primaryAgeColumn: NULL has been
replaced by ‘FALSE’
- d2H (LS14ATJU01B): paleoData_isPrimary: NULL has been replaced by
‘FALSE’
- d2H (LS14ATJU01B): paleoData_primaryAgeColumn: NULL has been
replaced by ‘FALSE’
- depth (MAT6c43cd5d85): paleoData_isPrimary: NULL has been replaced
by ‘FALSE’
- depth (MAT6c43cd5d85): paleoData_primaryAgeColumn: NULL has been
replaced by ‘FALSE’
- year (MAT795501f3aa): paleoData_isPrimary: NULL has been replaced by
‘TRUE’
- year (MAT795501f3aa): paleoData_primaryAgeColumn: NULL has been
replaced by ‘TRUE’
Version: 1.0.4
- lastVersion: 1.0.3
- curator: nicholas
- timestamp: 2025-04-11 16:26:58.440098 UTC
- changes:
- Paleo Interpretation metadata:
- d2H (LS14ATJU01A): interpretation1_basis: ‘In closed (endorheic)
lakes, lake water dD is driven by the ratio of precipitation to
evaporation and the isotopic value of the precipitation which, in the
tropics, is strongly negatively correlated with the amount of
precipitation on monthly and longer timescales. The combination of these
processes amplifies the response of lake water dD to changes in rainfall
with lower (higher) dD values occurring during periods of wetter (drier)
conditions. Changes in rainfall patterns can therefore be reconstructed
from dD values of sedimentary algal lipids, due to the near perfect
correlation between water dD and algal lipid dD values.’ has been
replaced by NULL
- d2H (LS14ATJU01A): interpretation1_direction: ‘negative’ has been
replaced by NULL
- d2H (LS14ATJU01A): interpretation1_rank: ‘1’ has been replaced by
NULL
- d2H (LS14ATJU01A): interpretation1_scope: ‘isotope’ has been
replaced by ‘climate’
- d2H (LS14ATJU01A): interpretation1_seasonality: ‘Annual’ has been
replaced by NULL
- d2H (LS14ATJU01A): interpretation1_seasonalityOriginal: ‘Annual’ has
been replaced by NULL
- d2H (LS14ATJU01A): interpretation1_variable:
‘effectivePrecipitation’ has been replaced by NULL
- d2H (LS14ATJU01A): interpretation1_variableGroup:
‘EffectiveMoisture’ has been replaced by NULL
- d2H (LS14ATJU01A): interpretation1_variableGroupDirection:
‘negative’ has been replaced by NULL
- d2H (LS14ATJU01A): interpretation1_variableGroupOriginal: ‘P_E’ has
been replaced by NULL
- d2H (LS14ATJU01A): interpretation2_basis: ‘“In closed (endorheic)
lakes, lake water dD is driven by the ratio of precipitation to
evaporation and the isotopic value of the precipitation which, in the
tropics, is strongly negatively correlated with the amount of
precipitation on monthly and longer timescales. The combination of these
processes amplifies the response of lake water dD to changes in rainfall
with lower (higher) dD values occurring during periods of wetter (drier)
conditions. Changes in rainfall patterns can therefore be reconstructed
from dD values of sedimentary algal lipids, due to the near perfect
correlation between water dD and algal lipid dD values.”’ has been
replaced by NULL
- d2H (LS14ATJU01A): interpretation2_direction: ‘positive’ has been
replaced by NULL
- d2H (LS14ATJU01A): interpretation2_rank: ‘2’ has been replaced by
NULL
- d2H (LS14ATJU01A): interpretation2_scope: ‘isotope’ has been
replaced by ‘climate’
- d2H (LS14ATJU01A): interpretation2_seasonality: ‘Annual’ has been
replaced by NULL
- d2H (LS14ATJU01A): interpretation2_seasonalityOriginal: ‘Annual’ has
been replaced by NULL
- d2H (LS14ATJU01A): interpretation2_variable: ‘precipitationIsotope’
has been replaced by NULL
- d2H (LS14ATJU01A): interpretation2_variableGroup: ‘P_isotope’ has
been replaced by NULL
- d2H (LS14ATJU01A): interpretation2_variableGroupDirection:
‘positive’ has been replaced by NULL
- d2H (LS14ATJU01A): interpretation3_scope: NULL has been replaced by
‘climate’
- d2H (LS14ATJU01A): interpretation4_basis: NULL has been replaced by
‘In closed (endorheic) lakes, lake water dD is driven by the ratio of
precipitation to evaporation and the isotopic value of the precipitation
which, in the tropics, is strongly negatively correlated with the amount
of precipitation on monthly and longer timescales. The combination of
these processes amplifies the response of lake water dD to changes in
rainfall with lower (higher) dD values occurring during periods of
wetter (drier) conditions. Changes in rainfall patterns can therefore be
reconstructed from dD values of sedimentary algal lipids, due to the
near perfect correlation between water dD and algal lipid dD
values.’
- d2H (LS14ATJU01A): interpretation4_direction: NULL has been replaced
by ‘negative’
- d2H (LS14ATJU01A): interpretation4_rank: NULL has been replaced by
‘1’
- d2H (LS14ATJU01A): interpretation4_scope: NULL has been replaced by
‘isotope’
- d2H (LS14ATJU01A): interpretation4_seasonality: NULL has been
replaced by ‘Annual’
- d2H (LS14ATJU01A): interpretation4_seasonalityOriginal: NULL has
been replaced by ‘Annual’
- d2H (LS14ATJU01A): interpretation4_variable: NULL has been replaced
by ‘effectivePrecipitation’
- d2H (LS14ATJU01A): interpretation4_variableGroup: NULL has been
replaced by ‘EffectiveMoisture’
- d2H (LS14ATJU01A): interpretation4_variableGroupDirection: NULL has
been replaced by ‘negative’
- d2H (LS14ATJU01A): interpretation4_variableGroupOriginal: NULL has
been replaced by ‘P_E’
- d2H (LS14ATJU01A): interpretation5_basis: NULL has been replaced by
‘“In closed (endorheic) lakes, lake water dD is driven by the ratio of
precipitation to evaporation and the isotopic value of the precipitation
which, in the tropics, is strongly negatively correlated with the amount
of precipitation on monthly and longer timescales. The combination of
these processes amplifies the response of lake water dD to changes in
rainfall with lower (higher) dD values occurring during periods of
wetter (drier) conditions. Changes in rainfall patterns can therefore be
reconstructed from dD values of sedimentary algal lipids, due to the
near perfect correlation between water dD and algal lipid dD
values.”’
- d2H (LS14ATJU01A): interpretation5_direction: NULL has been replaced
by ‘positive’
- d2H (LS14ATJU01A): interpretation5_rank: NULL has been replaced by
‘2’
- d2H (LS14ATJU01A): interpretation5_scope: NULL has been replaced by
‘isotope’
- d2H (LS14ATJU01A): interpretation5_seasonality: NULL has been
replaced by ‘Annual’
- d2H (LS14ATJU01A): interpretation5_seasonalityOriginal: NULL has
been replaced by ‘Annual’
- d2H (LS14ATJU01A): interpretation5_variable: NULL has been replaced
by ‘precipitationIsotope’
- d2H (LS14ATJU01A): interpretation5_variableGroup: NULL has been
replaced by ‘P_isotope’
- d2H (LS14ATJU01A): interpretation5_variableGroupDirection: NULL has
been replaced by ‘positive’
- d2H (LS14ATJU01A): interpretation6_scope: NULL has been replaced by
‘isotope’
- d2H (LS14ATJU01B): interpretation2_basis: ‘All botryococcene dD
values were highly correlated with water dD values (R2>0.99). And,
Zhang and Sachs 2007, Organic Geochemistry, 38: 582-608.’ has been
replaced by NULL
- d2H (LS14ATJU01B): interpretation2_direction: ‘positive’ has been
replaced by NULL
- d2H (LS14ATJU01B): interpretation2_inferredMaterial: ‘lake water’
has been replaced by NULL
- d2H (LS14ATJU01B): interpretation2_integrationTime: ‘1 to 10’ has
been replaced by NULL
- d2H (LS14ATJU01B): interpretation2_integrationTimeBasis: ‘These
lines of evidence strongly suggest that conditions favor- able for B.
braunii growth occur during moderate-to-strong El Nin?o events and thus
that C34 botryococcene ?D records the hydrologic conditions of the lake
during these events. In contrast, the avail- able evidence suggests that
the dinoflagellate population persists throughout the varying hydrologic
conditions experienced by El Junco Lake and thus that sedimentary
dinosterol ?D records the long-term (decadal-to-centennial) mean lake
conditions.’ has been replaced by NULL
- d2H (LS14ATJU01B): interpretation2_integrationTimeUnits: ‘years’ has
been replaced by NULL
- d2H (LS14ATJU01B): interpretation2_mathematicalRelation: ‘linear’
has been replaced by NULL
- d2H (LS14ATJU01B): interpretation2_scope: ‘isotope’ has been
replaced by ‘climate’
- d2H (LS14ATJU01B): interpretation2_seasonality: ‘Annual’ has been
replaced by NULL
- d2H (LS14ATJU01B): interpretation2_seasonalityOriginal: ‘Annual’ has
been replaced by NULL
- d2H (LS14ATJU01B): interpretation2_variable: ‘precipitationIsotope’
has been replaced by NULL
- d2H (LS14ATJU01B): interpretation2_variableGroup: ‘P_isotope’ has
been replaced by NULL
- d2H (LS14ATJU01B): interpretation2_variableGroupDirection:
‘positive’ has been replaced by NULL
- d2H (LS14ATJU01B): interpretation3_basis: ‘changes in rainfall
amount are imprinted in the isotopic composition of botryococcenes, with
negative (posi- tive) ?D values co-occurring with wetter (drier)
periods.’ has been replaced by NULL
- d2H (LS14ATJU01B): interpretation3_direction: ‘negative’ has been
replaced by NULL
- d2H (LS14ATJU01B): interpretation3_inferredMaterial: ‘lake water’
has been replaced by NULL
- d2H (LS14ATJU01B): interpretation3_integrationTime: ‘1 to 10’ has
been replaced by NULL
- d2H (LS14ATJU01B): interpretation3_integrationTimeBasis: ‘These
lines of evidence strongly suggest that conditions favor- able for B.
braunii growth occur during moderate-to-strong El Nin?o events and thus
that C34 botryococcene ?D records the hydrologic conditions of the lake
during these events. In contrast, the avail- able evidence suggests that
the dinoflagellate population persists throughout the varying hydrologic
conditions experienced by El Junco Lake and thus that sedimentary
dinosterol ?D records the long-term (decadal-to-centennial) mean lake
conditions.’ has been replaced by NULL
- d2H (LS14ATJU01B): interpretation3_integrationTimeUnits: ‘years’ has
been replaced by NULL
- d2H (LS14ATJU01B): interpretation3_mathematicalRelation: ‘linear’
has been replaced by NULL
- d2H (LS14ATJU01B): interpretation3_scope: ‘isotope’ has been
replaced by ‘climate’
- d2H (LS14ATJU01B): interpretation3_seasonality: ‘Annual’ has been
replaced by NULL
- d2H (LS14ATJU01B): interpretation3_seasonalityOriginal: ‘Annual’ has
been replaced by NULL
- d2H (LS14ATJU01B): interpretation3_variable:
‘effectivePrecipitation’ has been replaced by NULL
- d2H (LS14ATJU01B): interpretation3_variableGroup:
‘EffectiveMoisture’ has been replaced by NULL
- d2H (LS14ATJU01B): interpretation3_variableGroupDirection:
‘negative’ has been replaced by NULL
- d2H (LS14ATJU01B): interpretation3_variableGroupOriginal: ‘P_E’ has
been replaced by NULL
- d2H (LS14ATJU01B): interpretation4_basis: NULL has been replaced by
‘All botryococcene dD values were highly correlated with water dD values
(R2>0.99). And, Zhang and Sachs 2007, Organic Geochemistry, 38:
582-608.’
- d2H (LS14ATJU01B): interpretation4_direction: NULL has been replaced
by ‘positive’
- d2H (LS14ATJU01B): interpretation4_inferredMaterial: NULL has been
replaced by ‘lake water’
- d2H (LS14ATJU01B): interpretation4_integrationTime: NULL has been
replaced by ‘1 to 10’
- d2H (LS14ATJU01B): interpretation4_integrationTimeBasis: NULL has
been replaced by ‘These lines of evidence strongly suggest that
conditions favor- able for B. braunii growth occur during
moderate-to-strong El Nin?o events and thus that C34 botryococcene ?D
records the hydrologic conditions of the lake during these events. In
contrast, the avail- able evidence suggests that the dinoflagellate
population persists throughout the varying hydrologic conditions
experienced by El Junco Lake and thus that sedimentary dinosterol ?D
records the long-term (decadal-to-centennial) mean lake
conditions.’
- d2H (LS14ATJU01B): interpretation4_integrationTimeUnits: NULL has
been replaced by ‘years’
- d2H (LS14ATJU01B): interpretation4_mathematicalRelation: NULL has
been replaced by ‘linear’
- d2H (LS14ATJU01B): interpretation4_scope: NULL has been replaced by
‘isotope’
- d2H (LS14ATJU01B): interpretation4_seasonality: NULL has been
replaced by ‘Annual’
- d2H (LS14ATJU01B): interpretation4_seasonalityOriginal: NULL has
been replaced by ‘Annual’
- d2H (LS14ATJU01B): interpretation4_variable: NULL has been replaced
by ‘precipitationIsotope’
- d2H (LS14ATJU01B): interpretation4_variableGroup: NULL has been
replaced by ‘P_isotope’
- d2H (LS14ATJU01B): interpretation4_variableGroupDirection: NULL has
been replaced by ‘positive’
- d2H (LS14ATJU01B): interpretation5_basis: NULL has been replaced by
‘changes in rainfall amount are imprinted in the isotopic composition of
botryococcenes, with negative (posi- tive) ?D values co-occurring with
wetter (drier) periods.’
- d2H (LS14ATJU01B): interpretation5_direction: NULL has been replaced
by ‘negative’
- d2H (LS14ATJU01B): interpretation5_inferredMaterial: NULL has been
replaced by ‘lake water’
- d2H (LS14ATJU01B): interpretation5_integrationTime: NULL has been
replaced by ‘1 to 10’
- d2H (LS14ATJU01B): interpretation5_integrationTimeBasis: NULL has
been replaced by ‘These lines of evidence strongly suggest that
conditions favor- able for B. braunii growth occur during
moderate-to-strong El Nin?o events and thus that C34 botryococcene ?D
records the hydrologic conditions of the lake during these events. In
contrast, the avail- able evidence suggests that the dinoflagellate
population persists throughout the varying hydrologic conditions
experienced by El Junco Lake and thus that sedimentary dinosterol ?D
records the long-term (decadal-to-centennial) mean lake
conditions.’
- d2H (LS14ATJU01B): interpretation5_integrationTimeUnits: NULL has
been replaced by ‘years’
- d2H (LS14ATJU01B): interpretation5_mathematicalRelation: NULL has
been replaced by ‘linear’
- d2H (LS14ATJU01B): interpretation5_scope: NULL has been replaced by
‘isotope’
- d2H (LS14ATJU01B): interpretation5_seasonality: NULL has been
replaced by ‘Annual’
- d2H (LS14ATJU01B): interpretation5_seasonalityOriginal: NULL has
been replaced by ‘Annual’
- d2H (LS14ATJU01B): interpretation5_variable: NULL has been replaced
by ‘effectivePrecipitation’
- d2H (LS14ATJU01B): interpretation5_variableGroup: NULL has been
replaced by ‘EffectiveMoisture’
- d2H (LS14ATJU01B): interpretation5_variableGroupDirection: NULL has
been replaced by ‘negative’
- d2H (LS14ATJU01B): interpretation5_variableGroupOriginal: NULL has
been replaced by ‘P_E’
- d2H (LS14ATJU01B): interpretation6_scope: NULL has been replaced by
‘isotope’
- depth (MAT6c43cd5d85): interpretation1_scope: NULL has been replaced
by ‘climate’
- depth (MAT6c43cd5d85): interpretation2_scope: NULL has been replaced
by ‘climate’
- year (MAT795501f3aa): interpretation1_scope: NULL has been replaced
by ‘climate’
- year (MAT795501f3aa): interpretation2_scope: NULL has been replaced
by ‘climate’
Version: 1.0.3
- lastVersion: 1.0.2
- curator: nicholas
- timestamp: 2025-04-09 20:48:15.233721 UTC
- notes: Updated lipdverse database entry with a changed
file.
- changes:
- Paleo Interpretation metadata:
- d2H (LS14ATJU01A): interpretation1_seasonality: ‘annual’ has been
replaced by ‘Annual’
- d2H (LS14ATJU01A): interpretation1_variable: ‘P_E’ has been replaced
by ‘effectivePrecipitation’
- d2H (LS14ATJU01A): interpretation2_seasonality: ‘annual’ has been
replaced by ‘Annual’
- d2H (LS14ATJU01A): interpretation2_variable: ‘P_isotope’ has been
replaced by ‘precipitationIsotope’
- d2H (LS14ATJU01B): interpretation1_seasonality: ‘annual’ has been
replaced by ‘Annual’
- d2H (LS14ATJU01B): interpretation1_variable: ‘El Nino related
rainfall’ has been replaced by ‘precipitation’
- d2H (LS14ATJU01B): interpretation2_seasonality: ‘annual’ has been
replaced by ‘Annual’
- d2H (LS14ATJU01B): interpretation2_variable: ‘P_isotope’ has been
replaced by ‘precipitationIsotope’
- d2H (LS14ATJU01B): interpretation3_seasonality: ‘annual’ has been
replaced by ‘Annual’
- d2H (LS14ATJU01B): interpretation3_variable: ‘P_E’ has been replaced
by ‘effectivePrecipitation’
Version: 1.0.2
- lastVersion: 1.0.1
- curator: nicholas
- timestamp: 2025-04-09 18:34:50.223873 UTC
- notes: Changes made as part of LiPDverse vocabulary
standardization process
- changes:
- Paleo Interpretation metadata:
- d2H (LS14ATJU01A): interpretation1_seasonality: ‘annual’ has been
replaced by ‘Annual’
- d2H (LS14ATJU01A): interpretation1_variable: ‘P_E’ has been replaced
by ‘effectivePrecipitation’
- d2H (LS14ATJU01A): interpretation2_seasonality: ‘annual’ has been
replaced by ‘Annual’
- d2H (LS14ATJU01A): interpretation2_variable: ‘P_isotope’ has been
replaced by ‘precipitationIsotope’
- d2H (LS14ATJU01B): interpretation1_seasonality: ‘annual’ has been
replaced by ‘Annual’
- d2H (LS14ATJU01B): interpretation1_variable: ‘El Nino related
rainfall’ has been replaced by ‘precipitation’
- d2H (LS14ATJU01B): interpretation2_seasonality: ‘annual’ has been
replaced by ‘Annual’
- d2H (LS14ATJU01B): interpretation2_variable: ‘P_isotope’ has been
replaced by ‘precipitationIsotope’
- d2H (LS14ATJU01B): interpretation3_seasonality: ‘annual’ has been
replaced by ‘Annual’
- d2H (LS14ATJU01B): interpretation3_variable: ‘P_E’ has been replaced
by ‘effectivePrecipitation’
Version: 1.0.1
- lastVersion: 1.0.0
- curator: nicholas
- timestamp: 2025-04-08 17:32:59.034119 UTC
- notes: Changes made as part of LiPDverse vocabulary
standardization process
- changes:
- Paleo Column metadata:
- d2H (LS14ATJU01A): paleoData_longName: NULL has been replaced by
‘AD’
- d2H (LS14ATJU01B): paleoData_longName: NULL has been replaced by
‘AD’
- depth (MAT6c43cd5d85): paleoData_longName: NULL has been replaced by
‘AD’
- year (MAT795501f3aa): paleoData_units: ‘AD’ has been replaced by ‘yr
AD’
- year (MAT795501f3aa): paleoData_longName: NULL has been replaced by
‘AD’