Version history for 2bMIZpJQr5xePS075xL8 - CO14CABT
Version: 1.0.5
- lastVersion: 1.0.4
- curator: nicholas
- timestamp: 2025-04-17 20:04:00.860571 UTC
- changes:
- Paleo Column metadata:
- d18O (CO14CABT01A): paleoData_isPrimary: NULL has been replaced by
‘FALSE’
- d18O (CO14CABT01A): paleoData_primaryAgeColumn: NULL has been
replaced by ‘FALSE’
- d18O (CO14CABT01B): paleoData_isPrimary: NULL has been replaced by
‘FALSE’
- d18O (CO14CABT01B): paleoData_primaryAgeColumn: NULL has been
replaced by ‘FALSE’
- d18O (CO14CABT01B2): paleoData_isPrimary: NULL has been replaced by
‘FALSE’
- d18O (CO14CABT01B2): paleoData_primaryAgeColumn: NULL has been
replaced by ‘FALSE’
- depth (MAT4739320cb9): paleoData_isPrimary: NULL has been replaced
by ‘FALSE’
- depth (MAT4739320cb9): paleoData_primaryAgeColumn: NULL has been
replaced by ‘FALSE’
- year (MAT65e08c7772): paleoData_isPrimary: NULL has been replaced by
‘TRUE’
- year (MAT65e08c7772): paleoData_primaryAgeColumn: NULL has been
replaced by ‘TRUE’
Version: 1.0.4
- lastVersion: 1.0.3
- curator: nicholas
- timestamp: 2025-04-11 16:13:39.162191 UTC
- changes:
- Paleo Interpretation metadata:
- d18O (CO14CABT01A): interpretation2_basis: ‘The full Butaritari
coral Sr/Ca and d18O (Figures 3b and 3c) are well correlated with SST
from the 2° x 2° grid cell centered on 4°N, 172°E in ERSSTv3b (R = 0.58
for Sr/Ca and 0.39 for d18O, p < 0.05 on detrended bimonthly data).’
has been replaced by NULL
- d18O (CO14CABT01A): interpretation2_direction: ‘negative’ has been
replaced by NULL
- d18O (CO14CABT01A): interpretation2_inferredMaterial: ‘seawater’ has
been replaced by NULL
- d18O (CO14CABT01A): interpretation2_integrationTime: ‘2’ has been
replaced by NULL
- d18O (CO14CABT01A): interpretation2_integrationTimeBasis: ‘Sr/Ca
data to monthly SST from the 2� � 2� grid square centered on 4�N, 172�E
from the extended reconstructed SST version 3b (ERSSTv3b) data product
[Smith et al., 2008; ttp://www.esrl.noaa.gov/psd] [?] Annual Sr/Ca
maxima were tied to the coolest points in the SST record using
Analyseries [Paillard et al., 1996]. The resulting spacing of Sr/Ca data
remained relatively constant throughout the record, and the chronology
was verified against growth band counts from the X-radiograph. After
converting depth to time in Analyseries, Sr/Ca were interpolated to six
equally spaced samples per year using ARAND time series analysis
software [Howell, 2001], corresponding to bimonthly resolution for the
length of the record.’ has been replaced by NULL
- d18O (CO14CABT01A): interpretation2_integrationTimeUnits: ‘months’
has been replaced by NULL
- d18O (CO14CABT01A): interpretation2_mathematicalRelation: ‘linear’
has been replaced by NULL
- d18O (CO14CABT01A): interpretation2_rank: ‘1’ has been replaced by
NULL
- d18O (CO14CABT01A): interpretation2_scope: ‘isotope’ has been
replaced by ‘climate’
- d18O (CO14CABT01A): interpretation2_seasonality: ‘subannual’ has
been replaced by NULL
- d18O (CO14CABT01A): interpretation2_variable: ‘temperature’ has been
replaced by NULL
- d18O (CO14CABT01A): interpretation2_variableGroup: ‘Temperature’ has
been replaced by NULL
- d18O (CO14CABT01A): interpretation2_variableGroupDirection:
‘negative’ has been replaced by NULL
- d18O (CO14CABT01A): interpretation2_variableGroupOriginal: ‘T_water’
has been replaced by NULL
- d18O (CO14CABT01A): interpretation3_direction: ‘positive’ has been
replaced by NULL
- d18O (CO14CABT01A): interpretation3_inferredMaterial: ‘seawater’ has
been replaced by NULL
- d18O (CO14CABT01A): interpretation3_integrationTime: ‘2’ has been
replaced by NULL
- d18O (CO14CABT01A): interpretation3_integrationTimeBasis: ‘Sr/Ca
data to monthly SST from the 2� � 2� grid square centered on 4�N, 172�E
from the extended reconstructed SST version 3b (ERSSTv3b) data product
[Smith et al., 2008; ttp://www.esrl.noaa.gov/psd] [?] Annual Sr/Ca
maxima were tied to the coolest points in the SST record using
Analyseries [Paillard et al., 1996]. The resulting spacing of Sr/Ca data
remained relatively constant throughout the record, and the chronology
was verified against growth band counts from the X-radiograph. After
converting depth to time in Analyseries, Sr/Ca were interpolated to six
equally spaced samples per year using ARAND time series analysis
software [Howell, 2001], corresponding to bimonthly resolution for the
length of the record.’ has been replaced by NULL
- d18O (CO14CABT01A): interpretation3_integrationTimeUnits: ‘months’
has been replaced by NULL
- d18O (CO14CABT01A): interpretation3_mathematicalRelation: ‘linear’
has been replaced by NULL
- d18O (CO14CABT01A): interpretation3_rank: ‘2’ has been replaced by
NULL
- d18O (CO14CABT01A): interpretation3_scope: ‘isotope’ has been
replaced by ‘climate’
- d18O (CO14CABT01A): interpretation3_variable: ‘seawaterIsotope’ has
been replaced by NULL
- d18O (CO14CABT01A): interpretation3_variableGroup:
‘EffectiveMoisture’ has been replaced by NULL
- d18O (CO14CABT01A): interpretation3_variableGroupDirection:
‘negative’ has been replaced by NULL
- d18O (CO14CABT01A): interpretation3_variableGroupOriginal:
‘d18O_seawater’ has been replaced by NULL
- d18O (CO14CABT01A): interpretation4_basis: NULL has been replaced by
‘The full Butaritari coral Sr/Ca and d18O (Figures 3b and 3c) are well
correlated with SST from the 2° x 2° grid cell centered on 4°N, 172°E in
ERSSTv3b (R = 0.58 for Sr/Ca and 0.39 for d18O, p < 0.05 on detrended
bimonthly data).’
- d18O (CO14CABT01A): interpretation4_direction: NULL has been
replaced by ‘negative’
- d18O (CO14CABT01A): interpretation4_inferredMaterial: NULL has been
replaced by ‘seawater’
- d18O (CO14CABT01A): interpretation4_integrationTime: NULL has been
replaced by ‘2’
- d18O (CO14CABT01A): interpretation4_integrationTimeBasis: NULL has
been replaced by ‘Sr/Ca data to monthly SST from the 2� � 2� grid square
centered on 4�N, 172�E from the extended reconstructed SST version 3b
(ERSSTv3b) data product [Smith et al., 2008;
ttp://www.esrl.noaa.gov/psd] [?] Annual Sr/Ca maxima were tied to the
coolest points in the SST record using Analyseries [Paillard et al.,
1996]. The resulting spacing of Sr/Ca data remained relatively constant
throughout the record, and the chronology was verified against growth
band counts from the X-radiograph. After converting depth to time in
Analyseries, Sr/Ca were interpolated to six equally spaced samples per
year using ARAND time series analysis software [Howell, 2001],
corresponding to bimonthly resolution for the length of the
record.’
- d18O (CO14CABT01A): interpretation4_integrationTimeUnits: NULL has
been replaced by ‘months’
- d18O (CO14CABT01A): interpretation4_mathematicalRelation: NULL has
been replaced by ‘linear’
- d18O (CO14CABT01A): interpretation4_rank: NULL has been replaced by
‘1’
- d18O (CO14CABT01A): interpretation4_scope: NULL has been replaced by
‘isotope’
- d18O (CO14CABT01A): interpretation4_seasonality: NULL has been
replaced by ‘subannual’
- d18O (CO14CABT01A): interpretation4_variable: NULL has been replaced
by ‘temperature’
- d18O (CO14CABT01A): interpretation4_variableGroup: NULL has been
replaced by ‘Temperature’
- d18O (CO14CABT01A): interpretation4_variableGroupDirection: NULL has
been replaced by ‘negative’
- d18O (CO14CABT01A): interpretation4_variableGroupOriginal: NULL has
been replaced by ‘T_water’
- d18O (CO14CABT01A): interpretation5_direction: NULL has been
replaced by ‘positive’
- d18O (CO14CABT01A): interpretation5_inferredMaterial: NULL has been
replaced by ‘seawater’
- d18O (CO14CABT01A): interpretation5_integrationTime: NULL has been
replaced by ‘2’
- d18O (CO14CABT01A): interpretation5_integrationTimeBasis: NULL has
been replaced by ‘Sr/Ca data to monthly SST from the 2� � 2� grid square
centered on 4�N, 172�E from the extended reconstructed SST version 3b
(ERSSTv3b) data product [Smith et al., 2008;
ttp://www.esrl.noaa.gov/psd] [?] Annual Sr/Ca maxima were tied to the
coolest points in the SST record using Analyseries [Paillard et al.,
1996]. The resulting spacing of Sr/Ca data remained relatively constant
throughout the record, and the chronology was verified against growth
band counts from the X-radiograph. After converting depth to time in
Analyseries, Sr/Ca were interpolated to six equally spaced samples per
year using ARAND time series analysis software [Howell, 2001],
corresponding to bimonthly resolution for the length of the
record.’
- d18O (CO14CABT01A): interpretation5_integrationTimeUnits: NULL has
been replaced by ‘months’
- d18O (CO14CABT01A): interpretation5_mathematicalRelation: NULL has
been replaced by ‘linear’
- d18O (CO14CABT01A): interpretation5_rank: NULL has been replaced by
‘2’
- d18O (CO14CABT01A): interpretation5_scope: NULL has been replaced by
‘isotope’
- d18O (CO14CABT01A): interpretation5_variable: NULL has been replaced
by ‘seawaterIsotope’
- d18O (CO14CABT01A): interpretation5_variableGroup: NULL has been
replaced by ‘EffectiveMoisture’
- d18O (CO14CABT01A): interpretation5_variableGroupDirection: NULL has
been replaced by ‘negative’
- d18O (CO14CABT01A): interpretation5_variableGroupOriginal: NULL has
been replaced by ‘d18O_seawater’
- d18O (CO14CABT01A): interpretation6_scope: NULL has been replaced by
‘isotope’
- d18O (CO14CABT01B): interpretation2_direction: ‘positive’ has been
replaced by NULL
- d18O (CO14CABT01B): interpretation2_inferredMaterial: ‘seawater’ has
been replaced by NULL
- d18O (CO14CABT01B): interpretation2_integrationTime: ‘2’ has been
replaced by NULL
- d18O (CO14CABT01B): interpretation2_integrationTimeBasis: ‘Sr/Ca
data to monthly SST from the 2� � 2� grid square centered on 4�N, 172�E
from the extended reconstructed SST version 3b (ERSSTv3b) data product
[Smith et al., 2008; ttp://www.esrl.noaa.gov/psd] [?] Annual Sr/Ca
maxima were tied to the coolest points in the SST record using
Analyseries [Paillard et al., 1996]. The resulting spacing of Sr/Ca data
remained relatively constant throughout the record, and the chronology
was verified against growth band counts from the X-radiograph. After
converting depth to time in Analyseries, Sr/Ca were interpolated to six
equally spaced samples per year using ARAND time series analysis
software [Howell, 2001], corresponding to bimonthly resolution for the
length of the record.’ has been replaced by NULL
- d18O (CO14CABT01B): interpretation2_integrationTimeUnits: ‘months’
has been replaced by NULL
- d18O (CO14CABT01B): interpretation2_mathematicalRelation: ‘linear’
has been replaced by NULL
- d18O (CO14CABT01B): interpretation2_rank: ‘1’ has been replaced by
NULL
- d18O (CO14CABT01B): interpretation2_scope: ‘isotope’ has been
replaced by ‘climate’
- d18O (CO14CABT01B): interpretation2_seasonality: ‘subannual’ has
been replaced by NULL
- d18O (CO14CABT01B): interpretation2_variable: ‘seawaterIsotope’ has
been replaced by NULL
- d18O (CO14CABT01B): interpretation2_variableGroup:
‘EffectiveMoisture’ has been replaced by NULL
- d18O (CO14CABT01B): interpretation2_variableGroupDirection:
‘negative’ has been replaced by NULL
- d18O (CO14CABT01B): interpretation2_variableGroupOriginal:
‘d18O_seawater’ has been replaced by NULL
- d18O (CO14CABT01B): interpretation3_scope: NULL has been replaced by
‘climate’
- d18O (CO14CABT01B): interpretation4_direction: NULL has been
replaced by ‘positive’
- d18O (CO14CABT01B): interpretation4_inferredMaterial: NULL has been
replaced by ‘seawater’
- d18O (CO14CABT01B): interpretation4_integrationTime: NULL has been
replaced by ‘2’
- d18O (CO14CABT01B): interpretation4_integrationTimeBasis: NULL has
been replaced by ‘Sr/Ca data to monthly SST from the 2� � 2� grid square
centered on 4�N, 172�E from the extended reconstructed SST version 3b
(ERSSTv3b) data product [Smith et al., 2008;
ttp://www.esrl.noaa.gov/psd] [?] Annual Sr/Ca maxima were tied to the
coolest points in the SST record using Analyseries [Paillard et al.,
1996]. The resulting spacing of Sr/Ca data remained relatively constant
throughout the record, and the chronology was verified against growth
band counts from the X-radiograph. After converting depth to time in
Analyseries, Sr/Ca were interpolated to six equally spaced samples per
year using ARAND time series analysis software [Howell, 2001],
corresponding to bimonthly resolution for the length of the
record.’
- d18O (CO14CABT01B): interpretation4_integrationTimeUnits: NULL has
been replaced by ‘months’
- d18O (CO14CABT01B): interpretation4_mathematicalRelation: NULL has
been replaced by ‘linear’
- d18O (CO14CABT01B): interpretation4_rank: NULL has been replaced by
‘1’
- d18O (CO14CABT01B): interpretation4_scope: NULL has been replaced by
‘isotope’
- d18O (CO14CABT01B): interpretation4_seasonality: NULL has been
replaced by ‘subannual’
- d18O (CO14CABT01B): interpretation4_variable: NULL has been replaced
by ‘seawaterIsotope’
- d18O (CO14CABT01B): interpretation4_variableGroup: NULL has been
replaced by ‘EffectiveMoisture’
- d18O (CO14CABT01B): interpretation4_variableGroupDirection: NULL has
been replaced by ‘negative’
- d18O (CO14CABT01B): interpretation4_variableGroupOriginal: NULL has
been replaced by ‘d18O_seawater’
- d18O (CO14CABT01B): interpretation5_scope: NULL has been replaced by
‘isotope’
- d18O (CO14CABT01B): interpretation6_scope: NULL has been replaced by
‘isotope’
- d18O (CO14CABT01B2): interpretation2_direction: ‘positive’ has been
replaced by NULL
- d18O (CO14CABT01B2): interpretation2_inferredMaterial: ‘seawater’
has been replaced by NULL
- d18O (CO14CABT01B2): interpretation2_integrationTime: ‘2’ has been
replaced by NULL
- d18O (CO14CABT01B2): interpretation2_integrationTimeBasis: ‘Sr/Ca
data to monthly SST from the 2� � 2� grid square centered on 4�N, 172�E
from the extended reconstructed SST version 3b (ERSSTv3b) data product
[Smith et al., 2008; ttp://www.esrl.noaa.gov/psd] [?] Annual Sr/Ca
maxima were tied to the coolest points in the SST record using
Analyseries [Paillard et al., 1996]. The resulting spacing of Sr/Ca data
remained relatively constant throughout the record, and the chronology
was verified against growth band counts from the X-radiograph. After
converting depth to time in Analyseries, Sr/Ca were interpolated to six
equally spaced samples per year using ARAND time series analysis
software [Howell, 2001], corresponding to bimonthly resolution for the
length of the record.’ has been replaced by NULL
- d18O (CO14CABT01B2): interpretation2_integrationTimeUnits: ‘months’
has been replaced by NULL
- d18O (CO14CABT01B2): interpretation2_mathematicalRelation: ‘linear’
has been replaced by NULL
- d18O (CO14CABT01B2): interpretation2_rank: ‘1’ has been replaced by
NULL
- d18O (CO14CABT01B2): interpretation2_scope: ‘isotope’ has been
replaced by ‘climate’
- d18O (CO14CABT01B2): interpretation2_seasonality: ‘subannual’ has
been replaced by NULL
- d18O (CO14CABT01B2): interpretation2_variable: ‘seawaterIsotope’ has
been replaced by NULL
- d18O (CO14CABT01B2): interpretation2_variableGroup:
‘EffectiveMoisture’ has been replaced by NULL
- d18O (CO14CABT01B2): interpretation2_variableGroupDirection:
‘negative’ has been replaced by NULL
- d18O (CO14CABT01B2): interpretation2_variableGroupOriginal:
‘d18O_seawater’ has been replaced by NULL
- d18O (CO14CABT01B2): interpretation3_scope: NULL has been replaced
by ‘climate’
- d18O (CO14CABT01B2): interpretation4_direction: NULL has been
replaced by ‘positive’
- d18O (CO14CABT01B2): interpretation4_inferredMaterial: NULL has been
replaced by ‘seawater’
- d18O (CO14CABT01B2): interpretation4_integrationTime: NULL has been
replaced by ‘2’
- d18O (CO14CABT01B2): interpretation4_integrationTimeBasis: NULL has
been replaced by ‘Sr/Ca data to monthly SST from the 2� � 2� grid square
centered on 4�N, 172�E from the extended reconstructed SST version 3b
(ERSSTv3b) data product [Smith et al., 2008;
ttp://www.esrl.noaa.gov/psd] [?] Annual Sr/Ca maxima were tied to the
coolest points in the SST record using Analyseries [Paillard et al.,
1996]. The resulting spacing of Sr/Ca data remained relatively constant
throughout the record, and the chronology was verified against growth
band counts from the X-radiograph. After converting depth to time in
Analyseries, Sr/Ca were interpolated to six equally spaced samples per
year using ARAND time series analysis software [Howell, 2001],
corresponding to bimonthly resolution for the length of the
record.’
- d18O (CO14CABT01B2): interpretation4_integrationTimeUnits: NULL has
been replaced by ‘months’
- d18O (CO14CABT01B2): interpretation4_mathematicalRelation: NULL has
been replaced by ‘linear’
- d18O (CO14CABT01B2): interpretation4_rank: NULL has been replaced by
‘1’
- d18O (CO14CABT01B2): interpretation4_scope: NULL has been replaced
by ‘isotope’
- d18O (CO14CABT01B2): interpretation4_seasonality: NULL has been
replaced by ‘subannual’
- d18O (CO14CABT01B2): interpretation4_variable: NULL has been
replaced by ‘seawaterIsotope’
- d18O (CO14CABT01B2): interpretation4_variableGroup: NULL has been
replaced by ‘EffectiveMoisture’
- d18O (CO14CABT01B2): interpretation4_variableGroupDirection: NULL
has been replaced by ‘negative’
- d18O (CO14CABT01B2): interpretation4_variableGroupOriginal: NULL has
been replaced by ‘d18O_seawater’
- d18O (CO14CABT01B2): interpretation5_scope: NULL has been replaced
by ‘isotope’
- d18O (CO14CABT01B2): interpretation6_scope: NULL has been replaced
by ‘isotope’
- depth (MAT4739320cb9): interpretation1_scope: NULL has been replaced
by ‘climate’
- depth (MAT4739320cb9): interpretation2_scope: NULL has been replaced
by ‘climate’
- year (MAT65e08c7772): interpretation1_scope: NULL has been replaced
by ‘climate’
- year (MAT65e08c7772): interpretation2_scope: NULL has been replaced
by ‘climate’
Version: 1.0.3
- lastVersion: 1.0.2
- curator: nicholas
- timestamp: 2025-04-09 21:04:55.869309 UTC
- notes: Updated lipdverse database entry with a changed
file.
- changes:
- Paleo Interpretation metadata:
- d18O (CO14CABT01A): interpretation1_variable: ‘temperature and
salinity’ has been replaced by ‘temperature’
- d18O (CO14CABT01A): interpretation2_variable: ‘T_water’ has been
replaced by ‘temperature’
- d18O (CO14CABT01A): interpretation3_variable: ‘d18O_seawater’ has
been replaced by ‘seawaterIsotope’
- d18O (CO14CABT01B): interpretation1_variable: ‘S’ has been replaced
by ‘salinity’
- d18O (CO14CABT01B): interpretation2_variable: ‘d18O_seawater’ has
been replaced by ‘seawaterIsotope’
- d18O (CO14CABT01B2): interpretation1_variable: ‘S’ has been replaced
by ‘salinity’
- d18O (CO14CABT01B2): interpretation2_variable: ‘d18O_seawater’ has
been replaced by ‘seawaterIsotope’
Version: 1.0.2
- lastVersion: 1.0.1
- curator: nicholas
- timestamp: 2025-04-09 17:37:33.960296 UTC
- notes: Changes made as part of LiPDverse vocabulary
standardization process
- changes:
- Paleo Interpretation metadata:
- d18O (CO14CABT01A): interpretation1_variable: ‘temperature and
salinity’ has been replaced by ‘temperature’
- d18O (CO14CABT01A): interpretation2_variable: ‘T_water’ has been
replaced by ‘temperature’
- d18O (CO14CABT01A): interpretation3_variable: ‘d18O_seawater’ has
been replaced by ‘seawaterIsotope’
- d18O (CO14CABT01B): interpretation1_variable: ‘S’ has been replaced
by ‘salinity’
- d18O (CO14CABT01B): interpretation2_variable: ‘d18O_seawater’ has
been replaced by ‘seawaterIsotope’
- d18O (CO14CABT01B2): interpretation1_variable: ‘S’ has been replaced
by ‘salinity’
- d18O (CO14CABT01B2): interpretation2_variable: ‘d18O_seawater’ has
been replaced by ‘seawaterIsotope’
Version: 1.0.1
- lastVersion: 1.0.0
- curator: nicholas
- timestamp: 2025-04-08 17:30:25.454229 UTC
- notes: Changes made as part of LiPDverse vocabulary
standardization process
- changes:
- Paleo Column metadata:
- d18O (CO14CABT01A): paleoData_longName: NULL has been replaced by
‘AD’
- d18O (CO14CABT01B): paleoData_longName: NULL has been replaced by
‘AD’
- d18O (CO14CABT01B2): paleoData_longName: NULL has been replaced by
‘AD’
- depth (MAT4739320cb9): paleoData_longName: NULL has been replaced by
‘AD’
- year (MAT65e08c7772): paleoData_units: ‘AD’ has been replaced by ‘yr
AD’
- year (MAT65e08c7772): paleoData_longName: NULL has been replaced by
‘AD’