Version history for MNN1hLqGHovxO9RxzqWP - CO06QUNG
Version: 1.0.5
- lastVersion: 1.0.4
- curator: nicholas
- timestamp: 2025-04-17 20:03:58.11813 UTC
- changes:
- Paleo Column metadata:
- year (MAT85ba7be434): paleoData_isPrimary: NULL has been replaced by
‘TRUE’
- year (MAT85ba7be434): paleoData_primaryAgeColumn: NULL has been
replaced by ‘TRUE’
- d18O (Ocean2kHR_144): paleoData_isPrimary: NULL has been replaced by
‘FALSE’
- d18O (Ocean2kHR_144): paleoData_primaryAgeColumn: NULL has been
replaced by ‘FALSE’
- Sr/Ca (Ocean2kHR_145): paleoData_isPrimary: NULL has been replaced
by ‘FALSE’
- Sr/Ca (Ocean2kHR_145): paleoData_primaryAgeColumn: NULL has been
replaced by ‘FALSE’
- d13C (Ocean2kHR_146): paleoData_isPrimary: NULL has been replaced by
‘FALSE’
- d13C (Ocean2kHR_146): paleoData_primaryAgeColumn: NULL has been
replaced by ‘FALSE’
Version: 1.0.4
- lastVersion: 1.0.3
- curator: nicholas
- timestamp: 2025-04-11 16:13:37.087361 UTC
- changes:
- Paleo Interpretation metadata:
- year (MAT85ba7be434): interpretation1_scope: NULL has been replaced
by ‘climate’
- year (MAT85ba7be434): interpretation2_scope: NULL has been replaced
by ‘climate’
- d18O (Ocean2kHR_144): interpretation2_basis: ‘Coral d18O variations
are modestly correlated with SST variations over their common period of
overlap (1970? 1993), both in terms of the monthly and monthly anomaly
time series’ has been replaced by NULL
- d18O (Ocean2kHR_144): interpretation2_direction: ‘negative’ has been
replaced by NULL
- d18O (Ocean2kHR_144): interpretation2_inferredMaterial: ‘seawater’
has been replaced by NULL
- d18O (Ocean2kHR_144): interpretation2_integrationTime: ‘1’ has been
replaced by NULL
- d18O (Ocean2kHR_144): interpretation2_integrationTimeBasis: ‘Age
models were constructed using the AnalySeries program [Paillard et al.,
1996]. We used tie points to connect the lowest (highest) d18O values to
the warmest (coolest) temperatures in the instrumental SST record to
establish each year.The use of coral Sr/Ca values instead of coral d18O
values to construct the age model results produces a similar chronology.
The geochemical data were then interpolated to give monthly d18O values.
The geochemically based age models were confirmed via comparison with
ages determined by counting of skeletal density-band couplets in the
X-ray images of the coral slab.’ has been replaced by NULL
- d18O (Ocean2kHR_144): interpretation2_integrationTimeUnits: ‘month’
has been replaced by NULL
- d18O (Ocean2kHR_144): interpretation2_mathematicalRelation: ‘linear’
has been replaced by NULL
- d18O (Ocean2kHR_144): interpretation2_rank: ‘1’ has been replaced by
NULL
- d18O (Ocean2kHR_144): interpretation2_scope: ‘isotope’ has been
replaced by ‘climate’
- d18O (Ocean2kHR_144): interpretation2_seasonality: ‘subannual’ has
been replaced by NULL
- d18O (Ocean2kHR_144): interpretation2_variable: ‘temperature’ has
been replaced by NULL
- d18O (Ocean2kHR_144): interpretation2_variableGroup: ‘Temperature’
has been replaced by NULL
- d18O (Ocean2kHR_144): interpretation2_variableGroupDirection:
‘negative’ has been replaced by NULL
- d18O (Ocean2kHR_144): interpretation2_variableGroupOriginal:
‘T_water’ has been replaced by NULL
- d18O (Ocean2kHR_144): interpretation3_basis: ‘The monthly coral d18O
anomaly time series at Rabaul yields no significant correlation with the
instrumental SSS record, despite the fact that similar coral records
from Fiji [Le Bec et al., 2000] and Vanuatu [Kilbourne et al., 2004]
have been demonstrated to reflect SSS variations. It is possible that
the monthly coral d18O anomaly record does reflect local SSS variability
at Rabaul and the observed low correlation between these two variables
results from differences between the ship-track SSS record and the
actual SSS variability at Rabaul’ has been replaced by NULL
- d18O (Ocean2kHR_144): interpretation3_direction: ‘positive’ has been
replaced by NULL
- d18O (Ocean2kHR_144): interpretation3_inferredMaterial: ‘seawater’
has been replaced by NULL
- d18O (Ocean2kHR_144): interpretation3_integrationTime: ‘1’ has been
replaced by NULL
- d18O (Ocean2kHR_144): interpretation3_integrationTimeBasis: ‘Age
models were constructed using the AnalySeries program [Paillard et al.,
1996]. We used tie points to connect the lowest (highest) d18O values to
the warmest (coolest) temperatures in the instrumental SST record to
establish each year.The use of coral Sr/Ca values instead of coral d18O
values to construct the age model results produces a similar chronology.
The geochemical data were then interpolated to give monthly d18O values.
The geochemically based age models were confirmed via comparison with
ages determined by counting of skeletal density-band couplets in the
X-ray images of the coral slab.’ has been replaced by NULL
- d18O (Ocean2kHR_144): interpretation3_integrationTimeUnits: ‘month’
has been replaced by NULL
- d18O (Ocean2kHR_144): interpretation3_mathematicalRelation: ‘linear’
has been replaced by NULL
- d18O (Ocean2kHR_144): interpretation3_rank: ‘2’ has been replaced by
NULL
- d18O (Ocean2kHR_144): interpretation3_scope: ‘isotope’ has been
replaced by ‘climate’
- d18O (Ocean2kHR_144): interpretation3_variable: ‘seawaterIsotope’
has been replaced by NULL
- d18O (Ocean2kHR_144): interpretation3_variableGroup:
‘EffectiveMoisture’ has been replaced by NULL
- d18O (Ocean2kHR_144): interpretation3_variableGroupDirection:
‘negative’ has been replaced by NULL
- d18O (Ocean2kHR_144): interpretation3_variableGroupOriginal:
‘d18O_seawater’ has been replaced by NULL
- d18O (Ocean2kHR_144): interpretation4_basis: NULL has been replaced
by ‘Coral d18O variations are modestly correlated with SST variations
over their common period of overlap (1970? 1993), both in terms of the
monthly and monthly anomaly time series’
- d18O (Ocean2kHR_144): interpretation4_direction: NULL has been
replaced by ‘negative’
- d18O (Ocean2kHR_144): interpretation4_inferredMaterial: NULL has
been replaced by ‘seawater’
- d18O (Ocean2kHR_144): interpretation4_integrationTime: NULL has been
replaced by ‘1’
- d18O (Ocean2kHR_144): interpretation4_integrationTimeBasis: NULL has
been replaced by ‘Age models were constructed using the AnalySeries
program [Paillard et al., 1996]. We used tie points to connect the
lowest (highest) d18O values to the warmest (coolest) temperatures in
the instrumental SST record to establish each year.The use of coral
Sr/Ca values instead of coral d18O values to construct the age model
results produces a similar chronology. The geochemical data were then
interpolated to give monthly d18O values. The geochemically based age
models were confirmed via comparison with ages determined by counting of
skeletal density-band couplets in the X-ray images of the coral
slab.’
- d18O (Ocean2kHR_144): interpretation4_integrationTimeUnits: NULL has
been replaced by ‘month’
- d18O (Ocean2kHR_144): interpretation4_mathematicalRelation: NULL has
been replaced by ‘linear’
- d18O (Ocean2kHR_144): interpretation4_rank: NULL has been replaced
by ‘1’
- d18O (Ocean2kHR_144): interpretation4_scope: NULL has been replaced
by ‘isotope’
- d18O (Ocean2kHR_144): interpretation4_seasonality: NULL has been
replaced by ‘subannual’
- d18O (Ocean2kHR_144): interpretation4_variable: NULL has been
replaced by ‘temperature’
- d18O (Ocean2kHR_144): interpretation4_variableGroup: NULL has been
replaced by ‘Temperature’
- d18O (Ocean2kHR_144): interpretation4_variableGroupDirection: NULL
has been replaced by ‘negative’
- d18O (Ocean2kHR_144): interpretation4_variableGroupOriginal: NULL
has been replaced by ‘T_water’
- d18O (Ocean2kHR_144): interpretation5_basis: NULL has been replaced
by ‘The monthly coral d18O anomaly time series at Rabaul yields no
significant correlation with the instrumental SSS record, despite the
fact that similar coral records from Fiji [Le Bec et al., 2000] and
Vanuatu [Kilbourne et al., 2004] have been demonstrated to reflect SSS
variations. It is possible that the monthly coral d18O anomaly record
does reflect local SSS variability at Rabaul and the observed low
correlation between these two variables results from differences between
the ship-track SSS record and the actual SSS variability at Rabaul’
- d18O (Ocean2kHR_144): interpretation5_direction: NULL has been
replaced by ‘positive’
- d18O (Ocean2kHR_144): interpretation5_inferredMaterial: NULL has
been replaced by ‘seawater’
- d18O (Ocean2kHR_144): interpretation5_integrationTime: NULL has been
replaced by ‘1’
- d18O (Ocean2kHR_144): interpretation5_integrationTimeBasis: NULL has
been replaced by ‘Age models were constructed using the AnalySeries
program [Paillard et al., 1996]. We used tie points to connect the
lowest (highest) d18O values to the warmest (coolest) temperatures in
the instrumental SST record to establish each year.The use of coral
Sr/Ca values instead of coral d18O values to construct the age model
results produces a similar chronology. The geochemical data were then
interpolated to give monthly d18O values. The geochemically based age
models were confirmed via comparison with ages determined by counting of
skeletal density-band couplets in the X-ray images of the coral
slab.’
- d18O (Ocean2kHR_144): interpretation5_integrationTimeUnits: NULL has
been replaced by ‘month’
- d18O (Ocean2kHR_144): interpretation5_mathematicalRelation: NULL has
been replaced by ‘linear’
- d18O (Ocean2kHR_144): interpretation5_rank: NULL has been replaced
by ‘2’
- d18O (Ocean2kHR_144): interpretation5_scope: NULL has been replaced
by ‘isotope’
- d18O (Ocean2kHR_144): interpretation5_variable: NULL has been
replaced by ‘seawaterIsotope’
- d18O (Ocean2kHR_144): interpretation5_variableGroup: NULL has been
replaced by ‘EffectiveMoisture’
- d18O (Ocean2kHR_144): interpretation5_variableGroupDirection: NULL
has been replaced by ‘negative’
- d18O (Ocean2kHR_144): interpretation5_variableGroupOriginal: NULL
has been replaced by ‘d18O_seawater’
- d18O (Ocean2kHR_144): interpretation6_scope: NULL has been replaced
by ‘isotope’
- Sr/Ca (Ocean2kHR_145): interpretation2_inferredMaterial: ‘seawater’
has been replaced by NULL
- Sr/Ca (Ocean2kHR_145): interpretation2_scope: ‘isotope’ has been
replaced by ‘climate’
- Sr/Ca (Ocean2kHR_145): interpretation2_seasonality: ‘subannual’ has
been replaced by NULL
- Sr/Ca (Ocean2kHR_145): interpretation3_scope: NULL has been replaced
by ‘climate’
- Sr/Ca (Ocean2kHR_145): interpretation4_inferredMaterial: NULL has
been replaced by ‘seawater’
- Sr/Ca (Ocean2kHR_145): interpretation4_scope: NULL has been replaced
by ‘isotope’
- Sr/Ca (Ocean2kHR_145): interpretation4_seasonality: NULL has been
replaced by ‘subannual’
- Sr/Ca (Ocean2kHR_145): interpretation5_scope: NULL has been replaced
by ‘isotope’
- Sr/Ca (Ocean2kHR_145): interpretation6_scope: NULL has been replaced
by ‘isotope’
- d13C (Ocean2kHR_146): interpretation1_inferredMaterial: ‘seawater’
has been replaced by NULL
- d13C (Ocean2kHR_146): interpretation1_scope: ‘isotope’ has been
replaced by ‘climate’
- d13C (Ocean2kHR_146): interpretation1_seasonality: ‘subannual’ has
been replaced by NULL
- d13C (Ocean2kHR_146): interpretation2_scope: NULL has been replaced
by ‘climate’
- d13C (Ocean2kHR_146): interpretation3_scope: NULL has been replaced
by ‘climate’
- d13C (Ocean2kHR_146): interpretation4_inferredMaterial: NULL has
been replaced by ‘seawater’
- d13C (Ocean2kHR_146): interpretation4_scope: NULL has been replaced
by ‘isotope’
- d13C (Ocean2kHR_146): interpretation4_seasonality: NULL has been
replaced by ‘subannual’
- d13C (Ocean2kHR_146): interpretation5_scope: NULL has been replaced
by ‘isotope’
- d13C (Ocean2kHR_146): interpretation6_scope: NULL has been replaced
by ‘isotope’
Version: 1.0.3
- lastVersion: 1.0.2
- curator: nicholas
- timestamp: 2025-04-09 20:49:57.583714 UTC
- notes: Updated lipdverse database entry with a changed
file.
- changes:
- Paleo Interpretation metadata:
- d18O (Ocean2kHR_144): interpretation1_seasonality: ‘not applicable
(subannually resolved)’ has been replaced by ‘subannual’
- d18O (Ocean2kHR_144): interpretation1_variable: ‘temperature and
salinity’ has been replaced by ‘temperature’
- d18O (Ocean2kHR_144): interpretation2_variable: ‘T_water’ has been
replaced by ‘temperature’
- d18O (Ocean2kHR_144): interpretation3_variable: ‘d18O_seawater’ has
been replaced by ‘seawaterIsotope’
- Sr/Ca (Ocean2kHR_145): interpretation1_seasonality: ‘not applicable
(subannually resolved)’ has been replaced by ‘subannual’
- Sr/Ca (Ocean2kHR_145): interpretation1_variable: ‘T’ has been
replaced by ‘temperature’
Version: 1.0.2
- lastVersion: 1.0.1
- curator: nicholas
- timestamp: 2025-04-09 17:26:03.859419 UTC
- notes: Changes made as part of LiPDverse vocabulary
standardization process
- changes:
- Paleo Interpretation metadata:
- d18O (Ocean2kHR_144): interpretation1_seasonality: ‘not applicable
(subannually resolved)’ has been replaced by ‘subannual’
- d18O (Ocean2kHR_144): interpretation1_variable: ‘temperature and
salinity’ has been replaced by ‘temperature’
- d18O (Ocean2kHR_144): interpretation2_variable: ‘T_water’ has been
replaced by ‘temperature’
- d18O (Ocean2kHR_144): interpretation3_variable: ‘d18O_seawater’ has
been replaced by ‘seawaterIsotope’
- Sr/Ca (Ocean2kHR_145): interpretation1_seasonality: ‘not applicable
(subannually resolved)’ has been replaced by ‘subannual’
- Sr/Ca (Ocean2kHR_145): interpretation1_variable: ‘T’ has been
replaced by ‘temperature’
Version: 1.0.1
- lastVersion: 1.0.0
- curator: nicholas
- timestamp: 2025-04-08 17:30:23.402555 UTC
- notes: Changes made as part of LiPDverse vocabulary
standardization process
- changes:
- Paleo Column metadata:
- year (MAT85ba7be434): paleoData_units: ‘AD’ has been replaced by ‘yr
AD’
- year (MAT85ba7be434): paleoData_longName: NULL has been replaced by
‘AD’
- d18O (Ocean2kHR_144): paleoData_longName: NULL has been replaced by
‘AD’
- Sr/Ca (Ocean2kHR_145): paleoData_longName: NULL has been replaced by
‘AD’
- d13C (Ocean2kHR_146): paleoData_longName: NULL has been replaced by
‘AD’