Version history for 0n4u7XGKeugICSOLYJzf - CO96QUVA
Version: 1.0.7
- lastVersion: 1.0.6
- curator: nicholas
- timestamp: 2025-05-20 18:27:41.198996 UTC
- changes:
- Paleo Interpretation metadata:
- year (MAT76b067a764): interpretation5_scope: NULL has been replaced
by ‘climate’
Version: 1.0.6
- lastVersion: 1.0.5
- curator: nicholas
- timestamp: 2025-05-20 16:18:38.776294 UTC
- changes:
- Paleo Interpretation metadata:
- year (MAT76b067a764): interpretation4_scope: NULL has been replaced
by ‘climate’
Version: 1.0.5
- lastVersion: 1.0.4
- curator: nicholas
- timestamp: 2025-04-17 20:04:03.282389 UTC
- changes:
- Paleo Column metadata:
- year (MAT76b067a764): paleoData_isPrimary: NULL has been replaced by
‘TRUE’
- year (MAT76b067a764): paleoData_primaryAgeColumn: NULL has been
replaced by ‘TRUE’
- d18O (Ocean2kHR_133): paleoData_isPrimary: NULL has been replaced by
‘FALSE’
- d18O (Ocean2kHR_133): paleoData_primaryAgeColumn: NULL has been
replaced by ‘FALSE’
Version: 1.0.4
- lastVersion: 1.0.3
- curator: nicholas
- timestamp: 2025-04-11 16:14:46.852442 UTC
- changes:
- Paleo Interpretation metadata:
- year (MAT76b067a764): interpretation1_scope: NULL has been replaced
by ‘climate’
- year (MAT76b067a764): interpretation2_scope: NULL has been replaced
by ‘climate’
- year (MAT76b067a764): interpretation3_scope: NULL has been replaced
by ‘climate’
- d18O (Ocean2kHR_133): interpretation2_basis: ‘Comparison of the d180
with SST and rainfall records indicates a correlation of 0.71 and 0.54,
respectively, over the 13-year interval where data overlaps (Fig. 2).
Just as in the precipitation and SST comparison, the correlation is much
higher at the annual cycle (coherence of 0.95). There is also a slight
suggestion of coherence at the El Nino time scale, but the calibration
time series is too short to draw any definitive conclusions. Since the
0.71 correlation between SST and d180 explains only half the variance in
the SST record, other factors are obviously responsible for the d180
variations.’ has been replaced by NULL
- d18O (Ocean2kHR_133): interpretation2_direction: ‘negative’ has been
replaced by NULL
- d18O (Ocean2kHR_133): interpretation2_inferredMaterial: ‘seawater’
has been replaced by NULL
- d18O (Ocean2kHR_133): interpretation2_integrationTime: ‘1-Jan’ has
been replaced by NULL
- d18O (Ocean2kHR_133): interpretation2_integrationTimeBasis:
‘Sampling resolution is four samples per year, one sample in the middle
of each density band. The 0.5 mm diameter, discrete point sampling
strategy used in this study creates samples that are a homogeneous
mixture of-26 (7 mm/year) to -20 (9 mm/year) days of skeletal growth,
assuming a linear extension rate. (Quinn et al, 1993). Isotope sampling
methods were also identical to Quinn et al. [1993], with new samples
being midway between the original samples reported in that study.’ has
been replaced by NULL
- d18O (Ocean2kHR_133): interpretation2_integrationTimeUncertainty: ‘1
year’ has been replaced by NULL
- d18O (Ocean2kHR_133):
interpretation2_integrationTimeUncertaintyType: ‘chronological and 230Th
dates’ has been replaced by NULL
- d18O (Ocean2kHR_133): interpretation2_integrationTimeUnits: ‘year’
has been replaced by NULL
- d18O (Ocean2kHR_133): interpretation2_mathematicalRelation: ‘linear’
has been replaced by NULL
- d18O (Ocean2kHR_133): interpretation2_rank: ‘1’ has been replaced by
NULL
- d18O (Ocean2kHR_133): interpretation2_scope: ‘isotope’ has been
replaced by ‘climate’
- d18O (Ocean2kHR_133): interpretation2_seasonality: ‘subannual’ has
been replaced by NULL
- d18O (Ocean2kHR_133): interpretation2_variable: ‘temperature’ has
been replaced by NULL
- d18O (Ocean2kHR_133): interpretation2_variableGroup: ‘Temperature’
has been replaced by NULL
- d18O (Ocean2kHR_133): interpretation2_variableGroupDirection:
‘negative’ has been replaced by NULL
- d18O (Ocean2kHR_133): interpretation2_variableGroupOriginal:
‘T_water’ has been replaced by NULL
- d18O (Ocean2kHR_133): interpretation3_basis: ‘Comparison of the d180
with SST and rainfall records indicates a correlation of 0.71 and 0.54,
respectively, over the 13-year interval where data overlaps (Fig. 2).
Just as in the precipitation and SST comparison, the correlation is much
higher at the annual cycle (coherence of 0.95). There is also a slight
suggestion of coherence at the El Nino time scale, but the calibration
time series is too short to draw any definitive conclusions. Since the
0.71 correlation between SST and d180 explains only half the variance in
the SST record, other factors are obviously responsible for the d180
variations.’ has been replaced by NULL
- d18O (Ocean2kHR_133): interpretation3_direction: ‘positive’ has been
replaced by NULL
- d18O (Ocean2kHR_133): interpretation3_fraction: ‘0.29’ has been
replaced by NULL
- d18O (Ocean2kHR_133): interpretation3_inferredMaterial: ‘seawater’
has been replaced by NULL
- d18O (Ocean2kHR_133): interpretation3_integrationTime: ‘1-Jan’ has
been replaced by NULL
- d18O (Ocean2kHR_133): interpretation3_integrationTimeBasis:
‘Sampling resolution is four samples per year, one sample in the middle
of each density band. The 0.5 mm diameter, discrete point sampling
strategy used in this study creates samples that are a homogeneous
mixture of-26 (7 mm/year) to -20 (9 mm/year) days of skeletal growth,
assuming a linear extension rate. (Quinn et al, 1993). Isotope sampling
methods were also identical to Quinn et al. [1993], with new samples
being midway between the original samples reported in that study.’ has
been replaced by NULL
- d18O (Ocean2kHR_133): interpretation3_integrationTimeUncertainty: ‘1
year’ has been replaced by NULL
- d18O (Ocean2kHR_133):
interpretation3_integrationTimeUncertaintyType: ‘chronological and 230Th
dates’ has been replaced by NULL
- d18O (Ocean2kHR_133): interpretation3_integrationTimeUnits: ‘year’
has been replaced by NULL
- d18O (Ocean2kHR_133): interpretation3_mathematicalRelation: ‘linear’
has been replaced by NULL
- d18O (Ocean2kHR_133): interpretation3_rank: ‘2’ has been replaced by
NULL
- d18O (Ocean2kHR_133): interpretation3_scope: ‘isotope’ has been
replaced by ‘climate’
- d18O (Ocean2kHR_133): interpretation3_variable: ‘seawaterIsotope’
has been replaced by NULL
- d18O (Ocean2kHR_133): interpretation3_variableGroup:
‘EffectiveMoisture’ has been replaced by NULL
- d18O (Ocean2kHR_133): interpretation3_variableGroupDirection:
‘negative’ has been replaced by NULL
- d18O (Ocean2kHR_133): interpretation3_variableGroupOriginal:
‘d18O_seawater’ has been replaced by NULL
- d18O (Ocean2kHR_133): interpretation4_basis: NULL has been replaced
by ‘Comparison of the d180 with SST and rainfall records indicates a
correlation of 0.71 and 0.54, respectively, over the 13-year interval
where data overlaps (Fig. 2). Just as in the precipitation and SST
comparison, the correlation is much higher at the annual cycle
(coherence of 0.95). There is also a slight suggestion of coherence at
the El Nino time scale, but the calibration time series is too short to
draw any definitive conclusions. Since the 0.71 correlation between SST
and d180 explains only half the variance in the SST record, other
factors are obviously responsible for the d180 variations.’
- d18O (Ocean2kHR_133): interpretation4_direction: NULL has been
replaced by ‘negative’
- d18O (Ocean2kHR_133): interpretation4_inferredMaterial: NULL has
been replaced by ‘seawater’
- d18O (Ocean2kHR_133): interpretation4_integrationTime: NULL has been
replaced by ‘1-Jan’
- d18O (Ocean2kHR_133): interpretation4_integrationTimeBasis: NULL has
been replaced by ‘Sampling resolution is four samples per year, one
sample in the middle of each density band. The 0.5 mm diameter, discrete
point sampling strategy used in this study creates samples that are a
homogeneous mixture of-26 (7 mm/year) to -20 (9 mm/year) days of
skeletal growth, assuming a linear extension rate. (Quinn et al, 1993).
Isotope sampling methods were also identical to Quinn et al. [1993],
with new samples being midway between the original samples reported in
that study.’
- d18O (Ocean2kHR_133): interpretation4_integrationTimeUncertainty:
NULL has been replaced by ‘1 year’
- d18O (Ocean2kHR_133):
interpretation4_integrationTimeUncertaintyType: NULL has been replaced
by ‘chronological and 230Th dates’
- d18O (Ocean2kHR_133): interpretation4_integrationTimeUnits: NULL has
been replaced by ‘year’
- d18O (Ocean2kHR_133): interpretation4_mathematicalRelation: NULL has
been replaced by ‘linear’
- d18O (Ocean2kHR_133): interpretation4_rank: NULL has been replaced
by ‘1’
- d18O (Ocean2kHR_133): interpretation4_scope: NULL has been replaced
by ‘isotope’
- d18O (Ocean2kHR_133): interpretation4_seasonality: NULL has been
replaced by ‘subannual’
- d18O (Ocean2kHR_133): interpretation4_variable: NULL has been
replaced by ‘temperature’
- d18O (Ocean2kHR_133): interpretation4_variableGroup: NULL has been
replaced by ‘Temperature’
- d18O (Ocean2kHR_133): interpretation4_variableGroupDirection: NULL
has been replaced by ‘negative’
- d18O (Ocean2kHR_133): interpretation4_variableGroupOriginal: NULL
has been replaced by ‘T_water’
- d18O (Ocean2kHR_133): interpretation5_basis: NULL has been replaced
by ‘Comparison of the d180 with SST and rainfall records indicates a
correlation of 0.71 and 0.54, respectively, over the 13-year interval
where data overlaps (Fig. 2). Just as in the precipitation and SST
comparison, the correlation is much higher at the annual cycle
(coherence of 0.95). There is also a slight suggestion of coherence at
the El Nino time scale, but the calibration time series is too short to
draw any definitive conclusions. Since the 0.71 correlation between SST
and d180 explains only half the variance in the SST record, other
factors are obviously responsible for the d180 variations.’
- d18O (Ocean2kHR_133): interpretation5_direction: NULL has been
replaced by ‘positive’
- d18O (Ocean2kHR_133): interpretation5_fraction: NULL has been
replaced by ‘0.29’
- d18O (Ocean2kHR_133): interpretation5_inferredMaterial: NULL has
been replaced by ‘seawater’
- d18O (Ocean2kHR_133): interpretation5_integrationTime: NULL has been
replaced by ‘1-Jan’
- d18O (Ocean2kHR_133): interpretation5_integrationTimeBasis: NULL has
been replaced by ‘Sampling resolution is four samples per year, one
sample in the middle of each density band. The 0.5 mm diameter, discrete
point sampling strategy used in this study creates samples that are a
homogeneous mixture of-26 (7 mm/year) to -20 (9 mm/year) days of
skeletal growth, assuming a linear extension rate. (Quinn et al, 1993).
Isotope sampling methods were also identical to Quinn et al. [1993],
with new samples being midway between the original samples reported in
that study.’
- d18O (Ocean2kHR_133): interpretation5_integrationTimeUncertainty:
NULL has been replaced by ‘1 year’
- d18O (Ocean2kHR_133):
interpretation5_integrationTimeUncertaintyType: NULL has been replaced
by ‘chronological and 230Th dates’
- d18O (Ocean2kHR_133): interpretation5_integrationTimeUnits: NULL has
been replaced by ‘year’
- d18O (Ocean2kHR_133): interpretation5_mathematicalRelation: NULL has
been replaced by ‘linear’
- d18O (Ocean2kHR_133): interpretation5_rank: NULL has been replaced
by ‘2’
- d18O (Ocean2kHR_133): interpretation5_scope: NULL has been replaced
by ‘isotope’
- d18O (Ocean2kHR_133): interpretation5_variable: NULL has been
replaced by ‘seawaterIsotope’
- d18O (Ocean2kHR_133): interpretation5_variableGroup: NULL has been
replaced by ‘EffectiveMoisture’
- d18O (Ocean2kHR_133): interpretation5_variableGroupDirection: NULL
has been replaced by ‘negative’
- d18O (Ocean2kHR_133): interpretation5_variableGroupOriginal: NULL
has been replaced by ‘d18O_seawater’
- d18O (Ocean2kHR_133): interpretation6_scope: NULL has been replaced
by ‘isotope’
Version: 1.0.3
- lastVersion: 1.0.2
- curator: nicholas
- timestamp: 2025-04-09 20:50:20.28846 UTC
- notes: Updated lipdverse database entry with a changed
file.
- changes:
- Paleo Interpretation metadata:
- d18O (Ocean2kHR_133): interpretation1_seasonality: ‘annual’ has been
replaced by ‘Annual’
- d18O (Ocean2kHR_133): interpretation1_variable: ‘temperature and
salinity’ has been replaced by ‘temperature’
- d18O (Ocean2kHR_133): interpretation2_variable: ‘T_water’ has been
replaced by ‘temperature’
- d18O (Ocean2kHR_133): interpretation3_variable: ‘d18O_seawater’ has
been replaced by ‘seawaterIsotope’
Version: 1.0.2
- lastVersion: 1.0.1
- curator: nicholas
- timestamp: 2025-04-09 17:39:02.201831 UTC
- notes: Changes made as part of LiPDverse vocabulary
standardization process
- changes:
- Paleo Interpretation metadata:
- d18O (Ocean2kHR_133): interpretation1_seasonality: ‘annual’ has been
replaced by ‘Annual’
- d18O (Ocean2kHR_133): interpretation1_variable: ‘temperature and
salinity’ has been replaced by ‘temperature’
- d18O (Ocean2kHR_133): interpretation2_variable: ‘T_water’ has been
replaced by ‘temperature’
- d18O (Ocean2kHR_133): interpretation3_variable: ‘d18O_seawater’ has
been replaced by ‘seawaterIsotope’
Version: 1.0.1
- lastVersion: 1.0.0
- curator: nicholas
- timestamp: 2025-04-08 17:32:35.356367 UTC
- notes: Changes made as part of LiPDverse vocabulary
standardization process
- changes:
- Paleo Column metadata:
- year (MAT76b067a764): paleoData_units: ‘AD’ has been replaced by ‘yr
AD’
- year (MAT76b067a764): paleoData_longName: NULL has been replaced by
‘AD’
- d18O (Ocean2kHR_133): paleoData_longName: NULL has been replaced by
‘AD’