Version history for 4eKXrgFThelRgVWLxd0K - CO03CHBU
Version: 1.0.6
lastVersion: 1.0.5
curator: nicholas
timestamp: 2025-05-20 16:18:31.868423 UTC
changes:
Paleo Interpretation metadata:
year (MAT471a9a9675): interpretation4_scope: NULL has been replaced
by ‘climate’
Version: 1.0.5
lastVersion: 1.0.4
curator: nicholas
timestamp: 2025-04-17 20:03:55.644729 UTC
changes:
Paleo Column metadata:
year (MAT471a9a9675): paleoData_isPrimary: NULL has been replaced by
‘TRUE’
year (MAT471a9a9675): paleoData_primaryAgeColumn: NULL has been
replaced by ‘TRUE’
d18O (Ocean2kHR_171): paleoData_isPrimary: NULL has been replaced by
‘FALSE’
d18O (Ocean2kHR_171): paleoData_primaryAgeColumn: NULL has been
replaced by ‘FALSE’
Version: 1.0.4
lastVersion: 1.0.3
curator: nicholas
timestamp: 2025-04-11 16:10:24.993122 UTC
changes:
Paleo Interpretation metadata:
year (MAT471a9a9675): interpretation1_scope: NULL has been replaced
by ‘climate’
year (MAT471a9a9675): interpretation2_scope: NULL has been replaced
by ‘climate’
year (MAT471a9a9675): interpretation3_scope: NULL has been replaced
by ‘climate’
d18O (Ocean2kHR_171): interpretation2_basis: ‘The annual variability
of the Bunaken coral d18O refects the seasonal cycle of both salinity
and temperature in the surrounding seawater. The characteristics and
correlations of the Bunaken Island coral d18O record strongly
suggestthat it monitors the air-sea interaction associatedwith Southeast
Asian summer monsoon.’ has been replaced by NULL
d18O (Ocean2kHR_171): interpretation2_direction: ‘positive’ has been
replaced by NULL
d18O (Ocean2kHR_171): interpretation2_inferredMaterial: ‘seawater’
has been replaced by NULL
d18O (Ocean2kHR_171): interpretation2_integrationTime: ‘1’ has been
replaced by NULL
d18O (Ocean2kHR_171): interpretation2_integrationTimeBasis:
‘anchoring seasonal maxima and minima of the d18O depth series to March
and October of each year. Crosschecks on the age assignments were
available through examination of the annual growth bands and the strong
semi-annual carbon isotope signal’ has been replaced by NULL
d18O (Ocean2kHR_171): interpretation2_integrationTimeUncertainty:
‘~1/4’ has been replaced by NULL
d18O (Ocean2kHR_171):
interpretation2_integrationTimeUncertaintyType: ‘chronological’ has been
replaced by NULL
d18O (Ocean2kHR_171): interpretation2_integrationTimeUnits: ‘month’
has been replaced by NULL
d18O (Ocean2kHR_171): interpretation2_mathematicalRelation: ‘linear’
has been replaced by NULL
d18O (Ocean2kHR_171): interpretation2_rank: ‘1’ has been replaced by
NULL
d18O (Ocean2kHR_171): interpretation2_scope: ‘isotope’ has been
replaced by ‘climate’
d18O (Ocean2kHR_171): interpretation2_seasonality: ‘subannual’ has
been replaced by NULL
d18O (Ocean2kHR_171): interpretation2_variable: ‘seawaterIsotope’
has been replaced by NULL
d18O (Ocean2kHR_171): interpretation2_variableGroup:
‘EffectiveMoisture’ has been replaced by NULL
d18O (Ocean2kHR_171): interpretation2_variableGroupDirection:
‘negative’ has been replaced by NULL
d18O (Ocean2kHR_171): interpretation2_variableGroupOriginal:
‘d18O_seawater’ has been replaced by NULL
d18O (Ocean2kHR_171): interpretation3_basis: ‘The annual variability
of the Bunaken coral d18O refects the seasonal cycle of both salinity
and temperature in the surrounding seawater: “in the Indonesian coral
records, coral d18O is more heavily infuenced by rainfall variability.”
The characteristics and correlations of the Bunaken Island coral d18O
record strongly suggestthat it monitors the air-sea interaction
associatedwith Southeast Asian summer monsoon.’ has been replaced by
NULL
d18O (Ocean2kHR_171): interpretation3_direction: ‘negative’ has been
replaced by NULL
d18O (Ocean2kHR_171): interpretation3_inferredMaterial: ‘seawater’
has been replaced by NULL
d18O (Ocean2kHR_171): interpretation3_integrationTime: ‘1’ has been
replaced by NULL
d18O (Ocean2kHR_171): interpretation3_integrationTimeBasis:
‘anchoring seasonal maxima and minima of the d18O depth series to March
and October of each year. Crosschecks on the age assignments were
available through examination of the annual growth bands and the strong
semi-annual carbon isotope signal’ has been replaced by NULL
d18O (Ocean2kHR_171): interpretation3_integrationTimeUncertainty:
‘~1/4’ has been replaced by NULL
d18O (Ocean2kHR_171):
interpretation3_integrationTimeUncertaintyType: ‘chronological’ has been
replaced by NULL
d18O (Ocean2kHR_171): interpretation3_integrationTimeUnits: ‘month’
has been replaced by NULL
d18O (Ocean2kHR_171): interpretation3_mathematicalRelation: ‘linear’
has been replaced by NULL
d18O (Ocean2kHR_171): interpretation3_rank: ‘2’ has been replaced by
NULL
d18O (Ocean2kHR_171): interpretation3_scope: ‘isotope’ has been
replaced by ‘climate’
d18O (Ocean2kHR_171): interpretation3_variable: ‘temperature’ has
been replaced by NULL
d18O (Ocean2kHR_171): interpretation3_variableGroup: ‘Temperature’
has been replaced by NULL
d18O (Ocean2kHR_171): interpretation3_variableGroupDirection:
‘negative’ has been replaced by NULL
d18O (Ocean2kHR_171): interpretation3_variableGroupOriginal:
‘T_water’ has been replaced by NULL
d18O (Ocean2kHR_171): interpretation4_basis: NULL has been replaced
by ‘The annual variability of the Bunaken coral d18O refects the
seasonal cycle of both salinity and temperature in the surrounding
seawater. The characteristics and correlations of the Bunaken Island
coral d18O record strongly suggestthat it monitors the air-sea
interaction associatedwith Southeast Asian summer monsoon.’
d18O (Ocean2kHR_171): interpretation4_direction: NULL has been
replaced by ‘positive’
d18O (Ocean2kHR_171): interpretation4_inferredMaterial: NULL has
been replaced by ‘seawater’
d18O (Ocean2kHR_171): interpretation4_integrationTime: NULL has been
replaced by ‘1’
d18O (Ocean2kHR_171): interpretation4_integrationTimeBasis: NULL has
been replaced by ‘anchoring seasonal maxima and minima of the d18O depth
series to March and October of each year. Crosschecks on the age
assignments were available through examination of the annual growth
bands and the strong semi-annual carbon isotope signal’
d18O (Ocean2kHR_171): interpretation4_integrationTimeUncertainty:
NULL has been replaced by ‘~1/4’
d18O (Ocean2kHR_171):
interpretation4_integrationTimeUncertaintyType: NULL has been replaced
by ‘chronological’
d18O (Ocean2kHR_171): interpretation4_integrationTimeUnits: NULL has
been replaced by ‘month’
d18O (Ocean2kHR_171): interpretation4_mathematicalRelation: NULL has
been replaced by ‘linear’
d18O (Ocean2kHR_171): interpretation4_rank: NULL has been replaced
by ‘1’
d18O (Ocean2kHR_171): interpretation4_scope: NULL has been replaced
by ‘isotope’
d18O (Ocean2kHR_171): interpretation4_seasonality: NULL has been
replaced by ‘subannual’
d18O (Ocean2kHR_171): interpretation4_variable: NULL has been
replaced by ‘seawaterIsotope’
d18O (Ocean2kHR_171): interpretation4_variableGroup: NULL has been
replaced by ‘EffectiveMoisture’
d18O (Ocean2kHR_171): interpretation4_variableGroupDirection: NULL
has been replaced by ‘negative’
d18O (Ocean2kHR_171): interpretation4_variableGroupOriginal: NULL
has been replaced by ‘d18O_seawater’
d18O (Ocean2kHR_171): interpretation5_basis: NULL has been replaced
by ‘The annual variability of the Bunaken coral d18O refects the
seasonal cycle of both salinity and temperature in the surrounding
seawater: “in the Indonesian coral records, coral d18O is more heavily
infuenced by rainfall variability.” The characteristics and correlations
of the Bunaken Island coral d18O record strongly suggestthat it monitors
the air-sea interaction associatedwith Southeast Asian summer
monsoon.’
d18O (Ocean2kHR_171): interpretation5_direction: NULL has been
replaced by ‘negative’
d18O (Ocean2kHR_171): interpretation5_inferredMaterial: NULL has
been replaced by ‘seawater’
d18O (Ocean2kHR_171): interpretation5_integrationTime: NULL has been
replaced by ‘1’
d18O (Ocean2kHR_171): interpretation5_integrationTimeBasis: NULL has
been replaced by ‘anchoring seasonal maxima and minima of the d18O depth
series to March and October of each year. Crosschecks on the age
assignments were available through examination of the annual growth
bands and the strong semi-annual carbon isotope signal’
d18O (Ocean2kHR_171): interpretation5_integrationTimeUncertainty:
NULL has been replaced by ‘~1/4’
d18O (Ocean2kHR_171):
interpretation5_integrationTimeUncertaintyType: NULL has been replaced
by ‘chronological’
d18O (Ocean2kHR_171): interpretation5_integrationTimeUnits: NULL has
been replaced by ‘month’
d18O (Ocean2kHR_171): interpretation5_mathematicalRelation: NULL has
been replaced by ‘linear’
d18O (Ocean2kHR_171): interpretation5_rank: NULL has been replaced
by ‘2’
d18O (Ocean2kHR_171): interpretation5_scope: NULL has been replaced
by ‘isotope’
d18O (Ocean2kHR_171): interpretation5_variable: NULL has been
replaced by ‘temperature’
d18O (Ocean2kHR_171): interpretation5_variableGroup: NULL has been
replaced by ‘Temperature’
d18O (Ocean2kHR_171): interpretation5_variableGroupDirection: NULL
has been replaced by ‘negative’
d18O (Ocean2kHR_171): interpretation5_variableGroupOriginal: NULL
has been replaced by ‘T_water’
d18O (Ocean2kHR_171): interpretation6_scope: NULL has been replaced
by ‘isotope’
Version: 1.0.3
lastVersion: 1.0.2
curator: nicholas
timestamp: 2025-04-08 23:01:44.676332 UTC
notes: Updated lipdverse database entry with a changed
file.
changes:
Paleo Interpretation metadata:
d18O (Ocean2kHR_171): interpretation1_seasonality: ‘not applicable
(subannually resolved)’ has been replaced by ‘subannual’
d18O (Ocean2kHR_171): interpretation1_variable: ‘temperature and
salinity’ has been replaced by ‘temperature’
d18O (Ocean2kHR_171): interpretation2_variable: ‘d18O_seawater’ has
been replaced by ‘seawaterIsotope’
d18O (Ocean2kHR_171): interpretation3_variable: ‘T_water’ has been
replaced by ‘temperature’
Version: 1.0.2
lastVersion: 1.0.1
curator: nicholas
timestamp: 2025-04-08 23:01:44.088541 UTC
notes: Changes made as part of LiPDverse vocabulary
standardization process
changes:
Paleo Interpretation metadata:
d18O (Ocean2kHR_171): interpretation1_seasonality: ‘not applicable
(subannually resolved)’ has been replaced by ‘subannual’
d18O (Ocean2kHR_171): interpretation1_variable: ‘temperature and
salinity’ has been replaced by ‘temperature’
d18O (Ocean2kHR_171): interpretation2_variable: ‘d18O_seawater’ has
been replaced by ‘seawaterIsotope’
d18O (Ocean2kHR_171): interpretation3_variable: ‘T_water’ has been
replaced by ‘temperature’
Version: 1.0.1
lastVersion: 1.0.0
curator: nicholas
timestamp: 2025-04-08 17:30:20.994094 UTC
notes: Changes made as part of LiPDverse vocabulary
standardization process
changes:
Paleo Column metadata:
year (MAT471a9a9675): paleoData_units: ‘AD’ has been replaced by ‘yr
AD’
year (MAT471a9a9675): paleoData_longName: NULL has been replaced by
‘AD’
d18O (Ocean2kHR_171): paleoData_longName: NULL has been replaced by
‘AD’