Version history for xpHL3Wn9kbEaJRpviF9x - CO04PFCH
Version: 1.0.6
- lastVersion: 1.0.5
- curator: nicholas
- timestamp: 2025-05-20 16:18:32.899099 UTC
- changes:
- Paleo Interpretation metadata:
- year (MAT7a32fff5e7): interpretation4_scope: NULL has been replaced
by ‘climate’
- depth (MATd4f8849f7d): interpretation4_scope: NULL has been replaced
by ‘climate’
Version: 1.0.5
- lastVersion: 1.0.4
- curator: nicholas
- timestamp: 2025-04-17 20:03:56.998051 UTC
- changes:
- Paleo Column metadata:
- d18O (CO04PFCH01A): paleoData_isPrimary: NULL has been replaced by
‘FALSE’
- d18O (CO04PFCH01A): paleoData_primaryAgeColumn: NULL has been
replaced by ‘FALSE’
- d18O (CO04PFCH02A): paleoData_isPrimary: NULL has been replaced by
‘FALSE’
- d18O (CO04PFCH02A): paleoData_primaryAgeColumn: NULL has been
replaced by ‘FALSE’
- year (MAT7a32fff5e7): paleoData_isPrimary: NULL has been replaced by
‘TRUE’
- year (MAT7a32fff5e7): paleoData_primaryAgeColumn: NULL has been
replaced by ‘TRUE’
- depth (MATd4f8849f7d): paleoData_isPrimary: NULL has been replaced
by ‘FALSE’
- depth (MATd4f8849f7d): paleoData_primaryAgeColumn: NULL has been
replaced by ‘FALSE’
Version: 1.0.4
- lastVersion: 1.0.3
- curator: nicholas
- timestamp: 2025-04-11 16:13:30.389905 UTC
- changes:
- Paleo Interpretation metadata:
- d18O (CO04PFCH01A): interpretation2_basis: ‘However, over the entire
time interval compared, maximum variations of mean summer SST are 1jC,
which would account for approximately 0.20x in coral y18O (Juillet-
Leclerc and Schmidt, 2001). Over the same period, mean summer coral y18O
varies by as much as 0.7x (piM) and 0.4x (COI-5) (Fig. 4); i.e., the
maximum SST contribution to the coral isotopic signal is 29% (piM) and
50% (COI-5)’ has been replaced by NULL
- d18O (CO04PFCH01A): interpretation2_direction: ‘decrease’ has been
replaced by NULL
- d18O (CO04PFCH01A): interpretation2_mathematicalRelation: ‘linear’
has been replaced by NULL
- d18O (CO04PFCH01A): interpretation2_rank: ‘2’ has been replaced by
NULL
- d18O (CO04PFCH01A): interpretation2_scope: ‘isotope’ has been
replaced by ‘climate’
- d18O (CO04PFCH01A): interpretation3_basis: ‘Core GIM correlates more
strongly with precipitation and OLR than COI-5 (Table 1). Note that
years of high rainfall coincide with years of large negative coral y18O
anomalies in the wet season (and high amplitudes of the annual cycle,’
has been replaced by NULL
- d18O (CO04PFCH01A): interpretation3_direction: ‘increase’ has been
replaced by NULL
- d18O (CO04PFCH01A): interpretation3_mathematicalRelation: ‘linear’
has been replaced by NULL
- d18O (CO04PFCH01A): interpretation3_rank: ‘1’ has been replaced by
NULL
- d18O (CO04PFCH01A): interpretation3_scope: ‘isotope’ has been
replaced by ‘climate’
- d18O (CO04PFCH01A): interpretation4_basis: NULL has been replaced by
‘However, over the entire time interval compared, maximum variations of
mean summer SST are 1jC, which would account for approximately 0.20x in
coral y18O (Juillet- Leclerc and Schmidt, 2001). Over the same period,
mean summer coral y18O varies by as much as 0.7x (piM) and 0.4x (COI-5)
(Fig. 4); i.e., the maximum SST contribution to the coral isotopic
signal is 29% (piM) and 50% (COI-5)’
- d18O (CO04PFCH01A): interpretation4_direction: NULL has been
replaced by ‘decrease’
- d18O (CO04PFCH01A): interpretation4_mathematicalRelation: NULL has
been replaced by ‘linear’
- d18O (CO04PFCH01A): interpretation4_rank: NULL has been replaced by
‘2’
- d18O (CO04PFCH01A): interpretation4_scope: NULL has been replaced by
‘isotope’
- d18O (CO04PFCH01A): interpretation5_basis: NULL has been replaced by
‘Core GIM correlates more strongly with precipitation and OLR than COI-5
(Table 1). Note that years of high rainfall coincide with years of large
negative coral y18O anomalies in the wet season (and high amplitudes of
the annual cycle,’
- d18O (CO04PFCH01A): interpretation5_direction: NULL has been
replaced by ‘increase’
- d18O (CO04PFCH01A): interpretation5_mathematicalRelation: NULL has
been replaced by ‘linear’
- d18O (CO04PFCH01A): interpretation5_rank: NULL has been replaced by
‘1’
- d18O (CO04PFCH01A): interpretation5_scope: NULL has been replaced by
‘isotope’
- d18O (CO04PFCH01A): interpretation6_scope: NULL has been replaced by
‘isotope’
- d18O (CO04PFCH02A): interpretation2_basis: ‘Core piM correlates more
strongly with precipitation and OLR than COI-5 (Table 1). Note that
years of high rainfall coincide with years of large negative coral y18O
anomalies in the wet season (and high amplitudes of the annual cycle,’
has been replaced by NULL
- d18O (CO04PFCH02A): interpretation2_direction: ‘positive’ has been
replaced by NULL
- d18O (CO04PFCH02A): interpretation2_inferredMaterial: ‘seawater’ has
been replaced by NULL
- d18O (CO04PFCH02A): interpretation2_integrationTime: ‘2’ has been
replaced by NULL
- d18O (CO04PFCH02A): interpretation2_integrationTimeBasis: ‘A simple
chronology based on these density bands in both corals temporally
aligned anomalous 18O-depleted years precisely in the same years (e.g.,
1972?1973, 1982? 1983). During these years, there were noted positive
precipitation and/or SST anomalies. We then assigned February 15 to the
most negative isotopic values. This is, on average, the wettest month.
We then interpolated linearly between the anchor points to obtain
bimonthly records of coral y18O.’ has been replaced by NULL
- d18O (CO04PFCH02A): interpretation2_integrationTimeUnits: ‘month’
has been replaced by NULL
- d18O (CO04PFCH02A): interpretation2_mathematicalRelation: ‘linear’
has been replaced by NULL
- d18O (CO04PFCH02A): interpretation2_rank: ‘1’ has been replaced by
NULL
- d18O (CO04PFCH02A): interpretation2_scope: ‘isotope’ has been
replaced by ‘climate’
- d18O (CO04PFCH02A): interpretation2_seasonality: ‘subannual’ has
been replaced by NULL
- d18O (CO04PFCH02A): interpretation2_variable: ‘seawaterIsotope’ has
been replaced by NULL
- d18O (CO04PFCH02A): interpretation2_variableGroup:
‘EffectiveMoisture’ has been replaced by NULL
- d18O (CO04PFCH02A): interpretation2_variableGroupDirection:
‘negative’ has been replaced by NULL
- d18O (CO04PFCH02A): interpretation2_variableGroupOriginal:
‘d18O_seawater’ has been replaced by NULL
- d18O (CO04PFCH02A): interpretation3_basis: ‘However, over the entire
time interval compared, maximum variations of mean summer SST are 1jC,
which would account for approximately 0.20x in coral y18O (Juillet-
Leclerc and Schmidt, 2001). Over the same period, mean summer coral y18O
varies by as much as 0.7x (piM) and 0.4x (COI-5) (Fig. 4); i.e., the
maximum SST contribution to the coral isotopic signal is 29% (piM) and
50% (COI-5).’ has been replaced by NULL
- d18O (CO04PFCH02A): interpretation3_direction: ‘negative’ has been
replaced by NULL
- d18O (CO04PFCH02A): interpretation3_inferredMaterial: ‘seawater’ has
been replaced by NULL
- d18O (CO04PFCH02A): interpretation3_integrationTime: ‘2’ has been
replaced by NULL
- d18O (CO04PFCH02A): interpretation3_integrationTimeBasis: ‘A simple
chronology based on these density bands in both corals temporally
aligned anomalous 18O-depleted years precisely in the same years (e.g.,
1972?1973, 1982? 1983). During these years, there were noted positive
precipitation and/or SST anomalies. We then assigned February 15 to the
most negative isotopic values. This is, on average, the wettest month.
We then interpolated linearly between the anchor points to obtain
bimonthly records of coral y18O.’ has been replaced by NULL
- d18O (CO04PFCH02A): interpretation3_integrationTimeUnits: ‘month’
has been replaced by NULL
- d18O (CO04PFCH02A): interpretation3_mathematicalRelation: ‘linear’
has been replaced by NULL
- d18O (CO04PFCH02A): interpretation3_rank: ‘2’ has been replaced by
NULL
- d18O (CO04PFCH02A): interpretation3_scope: ‘isotope’ has been
replaced by ‘climate’
- d18O (CO04PFCH02A): interpretation3_variable: ‘temperature’ has been
replaced by NULL
- d18O (CO04PFCH02A): interpretation3_variableGroup: ‘Temperature’ has
been replaced by NULL
- d18O (CO04PFCH02A): interpretation3_variableGroupDirection:
‘negative’ has been replaced by NULL
- d18O (CO04PFCH02A): interpretation3_variableGroupOriginal: ‘T_water’
has been replaced by NULL
- d18O (CO04PFCH02A): interpretation4_basis: NULL has been replaced by
‘Core piM correlates more strongly with precipitation and OLR than COI-5
(Table 1). Note that years of high rainfall coincide with years of large
negative coral y18O anomalies in the wet season (and high amplitudes of
the annual cycle,’
- d18O (CO04PFCH02A): interpretation4_direction: NULL has been
replaced by ‘positive’
- d18O (CO04PFCH02A): interpretation4_inferredMaterial: NULL has been
replaced by ‘seawater’
- d18O (CO04PFCH02A): interpretation4_integrationTime: NULL has been
replaced by ‘2’
- d18O (CO04PFCH02A): interpretation4_integrationTimeBasis: NULL has
been replaced by ‘A simple chronology based on these density bands in
both corals temporally aligned anomalous 18O-depleted years precisely in
the same years (e.g., 1972?1973, 1982? 1983). During these years, there
were noted positive precipitation and/or SST anomalies. We then assigned
February 15 to the most negative isotopic values. This is, on average,
the wettest month. We then interpolated linearly between the anchor
points to obtain bimonthly records of coral y18O.’
- d18O (CO04PFCH02A): interpretation4_integrationTimeUnits: NULL has
been replaced by ‘month’
- d18O (CO04PFCH02A): interpretation4_mathematicalRelation: NULL has
been replaced by ‘linear’
- d18O (CO04PFCH02A): interpretation4_rank: NULL has been replaced by
‘1’
- d18O (CO04PFCH02A): interpretation4_scope: NULL has been replaced by
‘isotope’
- d18O (CO04PFCH02A): interpretation4_seasonality: NULL has been
replaced by ‘subannual’
- d18O (CO04PFCH02A): interpretation4_variable: NULL has been replaced
by ‘seawaterIsotope’
- d18O (CO04PFCH02A): interpretation4_variableGroup: NULL has been
replaced by ‘EffectiveMoisture’
- d18O (CO04PFCH02A): interpretation4_variableGroupDirection: NULL has
been replaced by ‘negative’
- d18O (CO04PFCH02A): interpretation4_variableGroupOriginal: NULL has
been replaced by ‘d18O_seawater’
- d18O (CO04PFCH02A): interpretation5_basis: NULL has been replaced by
‘However, over the entire time interval compared, maximum variations of
mean summer SST are 1jC, which would account for approximately 0.20x in
coral y18O (Juillet- Leclerc and Schmidt, 2001). Over the same period,
mean summer coral y18O varies by as much as 0.7x (piM) and 0.4x (COI-5)
(Fig. 4); i.e., the maximum SST contribution to the coral isotopic
signal is 29% (piM) and 50% (COI-5).’
- d18O (CO04PFCH02A): interpretation5_direction: NULL has been
replaced by ‘negative’
- d18O (CO04PFCH02A): interpretation5_inferredMaterial: NULL has been
replaced by ‘seawater’
- d18O (CO04PFCH02A): interpretation5_integrationTime: NULL has been
replaced by ‘2’
- d18O (CO04PFCH02A): interpretation5_integrationTimeBasis: NULL has
been replaced by ‘A simple chronology based on these density bands in
both corals temporally aligned anomalous 18O-depleted years precisely in
the same years (e.g., 1972?1973, 1982? 1983). During these years, there
were noted positive precipitation and/or SST anomalies. We then assigned
February 15 to the most negative isotopic values. This is, on average,
the wettest month. We then interpolated linearly between the anchor
points to obtain bimonthly records of coral y18O.’
- d18O (CO04PFCH02A): interpretation5_integrationTimeUnits: NULL has
been replaced by ‘month’
- d18O (CO04PFCH02A): interpretation5_mathematicalRelation: NULL has
been replaced by ‘linear’
- d18O (CO04PFCH02A): interpretation5_rank: NULL has been replaced by
‘2’
- d18O (CO04PFCH02A): interpretation5_scope: NULL has been replaced by
‘isotope’
- d18O (CO04PFCH02A): interpretation5_variable: NULL has been replaced
by ‘temperature’
- d18O (CO04PFCH02A): interpretation5_variableGroup: NULL has been
replaced by ‘Temperature’
- d18O (CO04PFCH02A): interpretation5_variableGroupDirection: NULL has
been replaced by ‘negative’
- d18O (CO04PFCH02A): interpretation5_variableGroupOriginal: NULL has
been replaced by ‘T_water’
- d18O (CO04PFCH02A): interpretation6_scope: NULL has been replaced by
‘isotope’
- year (MAT7a32fff5e7): interpretation1_scope: NULL has been replaced
by ‘climate’
- year (MAT7a32fff5e7): interpretation2_scope: NULL has been replaced
by ‘climate’
- year (MAT7a32fff5e7): interpretation3_scope: NULL has been replaced
by ‘climate’
- depth (MATd4f8849f7d): interpretation1_scope: NULL has been replaced
by ‘climate’
- depth (MATd4f8849f7d): interpretation2_scope: NULL has been replaced
by ‘climate’
- depth (MATd4f8849f7d): interpretation3_scope: NULL has been replaced
by ‘climate’
Version: 1.0.3
- lastVersion: 1.0.2
- curator: nicholas
- timestamp: 2025-04-08 23:21:06.780056 UTC
- notes: Updated lipdverse database entry with a changed
file.
- changes:
- Paleo Interpretation metadata:
- d18O (CO04PFCH01A): interpretation1_variable: ‘temperature and
salinity’ has been replaced by ‘temperature’
- d18O (CO04PFCH02A): interpretation1_variable: ‘temperature and
salinity’ has been replaced by ‘temperature’
- d18O (CO04PFCH02A): interpretation2_variable: ‘d18O_seawater’ has
been replaced by ‘seawaterIsotope’
- d18O (CO04PFCH02A): interpretation3_variable: ‘T_water’ has been
replaced by ‘temperature’
Version: 1.0.2
- lastVersion: 1.0.1
- curator: nicholas
- timestamp: 2025-04-08 23:21:06.298187 UTC
- notes: Changes made as part of LiPDverse vocabulary
standardization process
- changes:
- Paleo Interpretation metadata:
- d18O (CO04PFCH01A): interpretation1_variable: ‘temperature and
salinity’ has been replaced by ‘temperature’
- d18O (CO04PFCH02A): interpretation1_variable: ‘temperature and
salinity’ has been replaced by ‘temperature’
- d18O (CO04PFCH02A): interpretation2_variable: ‘d18O_seawater’ has
been replaced by ‘seawaterIsotope’
- d18O (CO04PFCH02A): interpretation3_variable: ‘T_water’ has been
replaced by ‘temperature’
Version: 1.0.1
- lastVersion: 1.0.0
- curator: nicholas
- timestamp: 2025-04-08 17:30:22.222855 UTC
- notes: Changes made as part of LiPDverse vocabulary
standardization process
- changes:
- Paleo Column metadata:
- d18O (CO04PFCH01A): paleoData_longName: NULL has been replaced by
‘AD’
- d18O (CO04PFCH02A): paleoData_longName: NULL has been replaced by
‘AD’
- year (MAT7a32fff5e7): paleoData_units: ‘AD’ has been replaced by ‘yr
AD’
- year (MAT7a32fff5e7): paleoData_longName: NULL has been replaced by
‘AD’
- depth (MATd4f8849f7d): paleoData_longName: NULL has been replaced by
‘AD’