Version history for GtaQfVzeDU1H8ksSWa1m - CO96SWFB
Version: 1.0.6
- lastVersion: 1.0.5
- curator: nicholas
- timestamp: 2025-05-20 16:18:38.996904 UTC
- changes:
- Paleo Interpretation metadata:
- depth (MAT4b082cc2d4): interpretation4_scope: NULL has been replaced
by ‘climate’
- year (MAT7d0bc1f777): interpretation4_scope: NULL has been replaced
by ‘climate’
Version: 1.0.5
- lastVersion: 1.0.4
- curator: nicholas
- timestamp: 2025-04-17 20:04:03.520453 UTC
- changes:
- Paleo Column metadata:
- d18O (CO96SWFB01A): paleoData_isPrimary: NULL has been replaced by
‘FALSE’
- d18O (CO96SWFB01A): paleoData_primaryAgeColumn: NULL has been
replaced by ‘FALSE’
- depth (MAT4b082cc2d4): paleoData_isPrimary: NULL has been replaced
by ‘FALSE’
- depth (MAT4b082cc2d4): paleoData_primaryAgeColumn: NULL has been
replaced by ‘FALSE’
- year (MAT7d0bc1f777): paleoData_isPrimary: NULL has been replaced by
‘TRUE’
- year (MAT7d0bc1f777): paleoData_primaryAgeColumn: NULL has been
replaced by ‘TRUE’
Version: 1.0.4
- lastVersion: 1.0.3
- curator: nicholas
- timestamp: 2025-04-11 16:14:47.068085 UTC
- changes:
- Paleo Interpretation metadata:
- d18O (CO96SWFB01A): interpretation2_basis: ‘The higher skeletal d18O
value reflects the high d180 value of the Bay water itself (Lloyd, 1964;
Swart et al., 1989), which is enriched in d18O as a result of
evaporation and the input of 1so enriched freshwater from the Everglades
(Meyers et al., 1993). Salinity values are the highest during the
summer, as a result of evaporation, and lower during the winter when the
Bay becomes dominated by water from the Gulf of Mexico and the Florida
Reef Tract. These changes in salinity should be manifested in the 6180
of the coral, but as the maximum enrichment in the water occurs during
the warmest portion of the year (the summer), the temperature and
salinity effects tend to counteract each other, thereby reducing the
observed range of oxygen isotopic variation seen in the coral.’ has been
replaced by NULL
- d18O (CO96SWFB01A): interpretation2_direction: ‘positive’ has been
replaced by NULL
- d18O (CO96SWFB01A): interpretation2_inferredMaterial: ‘seawater’ has
been replaced by NULL
- d18O (CO96SWFB01A): interpretation2_integrationTime: ‘1’ has been
replaced by NULL
- d18O (CO96SWFB01A): interpretation2_integrationTimeBasis: ‘In South
Florida, the dense band forms in the late summer, but it is generally
thought that there is as much as a � two month variation in timing. By
counting the number of bands in a coral, the age can be assessed. Errors
in age interpretation arise when dense bands are indistinct or when
so-called “stress bands”, resulting from events such as temperature
extremes, occur. Generally speaking, a year in which a stress band forms
may actually contain two dense bands or a thicker dense band which is a
combination of the stress and normal dense band. Although it is possible
to misinterpret a stress band as an annual band, the annual bands can be
recognized by their regular spacing. Therefore, density changes can
still provide a clear annual chronology.’ has been replaced by NULL
- d18O (CO96SWFB01A): interpretation2_integrationTimeUncertainty:
‘subannual samples averaged to annual for archived data’ has been
replaced by NULL
- d18O (CO96SWFB01A): interpretation2_integrationTimeUncertaintyType:
‘chronological’ has been replaced by NULL
- d18O (CO96SWFB01A): interpretation2_integrationTimeUnits: ‘year’ has
been replaced by NULL
- d18O (CO96SWFB01A): interpretation2_mathematicalRelation: ‘linear’
has been replaced by NULL
- d18O (CO96SWFB01A): interpretation2_rank: ‘1’ has been replaced by
NULL
- d18O (CO96SWFB01A): interpretation2_scope: ‘isotope’ has been
replaced by ‘climate’
- d18O (CO96SWFB01A): interpretation2_seasonality: ‘Annual’ has been
replaced by NULL
- d18O (CO96SWFB01A): interpretation2_seasonalityOriginal: ‘Annual’
has been replaced by NULL
- d18O (CO96SWFB01A): interpretation2_variable: ‘seawaterIsotope’ has
been replaced by NULL
- d18O (CO96SWFB01A): interpretation2_variableGroup:
‘EffectiveMoisture’ has been replaced by NULL
- d18O (CO96SWFB01A): interpretation2_variableGroupDirection:
‘negative’ has been replaced by NULL
- d18O (CO96SWFB01A): interpretation2_variableGroupOriginal:
‘d18O_seawater’ has been replaced by NULL
- d18O (CO96SWFB01A): interpretation3_basis: ‘Temperature is not
significant (r= 0.08)’ has been replaced by NULL
- d18O (CO96SWFB01A): interpretation3_fraction: ‘0’ has been replaced
by NULL
- d18O (CO96SWFB01A): interpretation3_inferredMaterial: ‘seawater’ has
been replaced by NULL
- d18O (CO96SWFB01A): interpretation3_integrationTime: ‘1’ has been
replaced by NULL
- d18O (CO96SWFB01A): interpretation3_integrationTimeBasis: ‘In South
Florida, the dense band forms in the late summer, but it is generally
thought that there is as much as a � two month variation in timing. By
counting the number of bands in a coral, the age can be assessed. Errors
in age interpretation arise when dense bands are indistinct or when
so-called “stress bands”, resulting from events such as temperature
extremes, occur. Generally speaking, a year in which a stress band forms
may actually contain two dense bands or a thicker dense band which is a
combination of the stress and normal dense band. Although it is possible
to misinterpret a stress band as an annual band, the annual bands can be
recognized by their regular spacing. Therefore, density changes can
still provide a clear annual chronology.’ has been replaced by NULL
- d18O (CO96SWFB01A): interpretation3_integrationTimeUncertainty:
‘subannual samples averaged to annual for archived data’ has been
replaced by NULL
- d18O (CO96SWFB01A): interpretation3_integrationTimeUncertaintyType:
‘chronological’ has been replaced by NULL
- d18O (CO96SWFB01A): interpretation3_integrationTimeUnits: ‘year’ has
been replaced by NULL
- d18O (CO96SWFB01A): interpretation3_rank: ‘2’ has been replaced by
NULL
- d18O (CO96SWFB01A): interpretation3_scope: ‘isotope’ has been
replaced by ‘climate’
- d18O (CO96SWFB01A): interpretation3_variable: ‘temperature’ has been
replaced by NULL
- d18O (CO96SWFB01A): interpretation3_variableGroup: ‘Temperature’ has
been replaced by NULL
- d18O (CO96SWFB01A): interpretation3_variableGroupDirection:
‘negative’ has been replaced by NULL
- d18O (CO96SWFB01A): interpretation3_variableGroupOriginal: ‘T_water’
has been replaced by NULL
- d18O (CO96SWFB01A): interpretation4_basis: NULL has been replaced by
‘The higher skeletal d18O value reflects the high d180 value of the Bay
water itself (Lloyd, 1964; Swart et al., 1989), which is enriched in
d18O as a result of evaporation and the input of 1so enriched freshwater
from the Everglades (Meyers et al., 1993). Salinity values are the
highest during the summer, as a result of evaporation, and lower during
the winter when the Bay becomes dominated by water from the Gulf of
Mexico and the Florida Reef Tract. These changes in salinity should be
manifested in the 6180 of the coral, but as the maximum enrichment in
the water occurs during the warmest portion of the year (the summer),
the temperature and salinity effects tend to counteract each other,
thereby reducing the observed range of oxygen isotopic variation seen in
the coral.’
- d18O (CO96SWFB01A): interpretation4_direction: NULL has been
replaced by ‘positive’
- d18O (CO96SWFB01A): interpretation4_inferredMaterial: NULL has been
replaced by ‘seawater’
- d18O (CO96SWFB01A): interpretation4_integrationTime: NULL has been
replaced by ‘1’
- d18O (CO96SWFB01A): interpretation4_integrationTimeBasis: NULL has
been replaced by ‘In South Florida, the dense band forms in the late
summer, but it is generally thought that there is as much as a � two
month variation in timing. By counting the number of bands in a coral,
the age can be assessed. Errors in age interpretation arise when dense
bands are indistinct or when so-called “stress bands”, resulting from
events such as temperature extremes, occur. Generally speaking, a year
in which a stress band forms may actually contain two dense bands or a
thicker dense band which is a combination of the stress and normal dense
band. Although it is possible to misinterpret a stress band as an annual
band, the annual bands can be recognized by their regular spacing.
Therefore, density changes can still provide a clear annual
chronology.’
- d18O (CO96SWFB01A): interpretation4_integrationTimeUncertainty: NULL
has been replaced by ‘subannual samples averaged to annual for archived
data’
- d18O (CO96SWFB01A): interpretation4_integrationTimeUncertaintyType:
NULL has been replaced by ‘chronological’
- d18O (CO96SWFB01A): interpretation4_integrationTimeUnits: NULL has
been replaced by ‘year’
- d18O (CO96SWFB01A): interpretation4_mathematicalRelation: NULL has
been replaced by ‘linear’
- d18O (CO96SWFB01A): interpretation4_rank: NULL has been replaced by
‘1’
- d18O (CO96SWFB01A): interpretation4_scope: NULL has been replaced by
‘isotope’
- d18O (CO96SWFB01A): interpretation4_seasonality: NULL has been
replaced by ‘Annual’
- d18O (CO96SWFB01A): interpretation4_seasonalityOriginal: NULL has
been replaced by ‘Annual’
- d18O (CO96SWFB01A): interpretation4_variable: NULL has been replaced
by ‘seawaterIsotope’
- d18O (CO96SWFB01A): interpretation4_variableGroup: NULL has been
replaced by ‘EffectiveMoisture’
- d18O (CO96SWFB01A): interpretation4_variableGroupDirection: NULL has
been replaced by ‘negative’
- d18O (CO96SWFB01A): interpretation4_variableGroupOriginal: NULL has
been replaced by ‘d18O_seawater’
- d18O (CO96SWFB01A): interpretation5_basis: NULL has been replaced by
‘Temperature is not significant (r= 0.08)’
- d18O (CO96SWFB01A): interpretation5_fraction: NULL has been replaced
by ‘0’
- d18O (CO96SWFB01A): interpretation5_inferredMaterial: NULL has been
replaced by ‘seawater’
- d18O (CO96SWFB01A): interpretation5_integrationTime: NULL has been
replaced by ‘1’
- d18O (CO96SWFB01A): interpretation5_integrationTimeBasis: NULL has
been replaced by ‘In South Florida, the dense band forms in the late
summer, but it is generally thought that there is as much as a � two
month variation in timing. By counting the number of bands in a coral,
the age can be assessed. Errors in age interpretation arise when dense
bands are indistinct or when so-called “stress bands”, resulting from
events such as temperature extremes, occur. Generally speaking, a year
in which a stress band forms may actually contain two dense bands or a
thicker dense band which is a combination of the stress and normal dense
band. Although it is possible to misinterpret a stress band as an annual
band, the annual bands can be recognized by their regular spacing.
Therefore, density changes can still provide a clear annual
chronology.’
- d18O (CO96SWFB01A): interpretation5_integrationTimeUncertainty: NULL
has been replaced by ‘subannual samples averaged to annual for archived
data’
- d18O (CO96SWFB01A): interpretation5_integrationTimeUncertaintyType:
NULL has been replaced by ‘chronological’
- d18O (CO96SWFB01A): interpretation5_integrationTimeUnits: NULL has
been replaced by ‘year’
- d18O (CO96SWFB01A): interpretation5_rank: NULL has been replaced by
‘2’
- d18O (CO96SWFB01A): interpretation5_scope: NULL has been replaced by
‘isotope’
- d18O (CO96SWFB01A): interpretation5_variable: NULL has been replaced
by ‘temperature’
- d18O (CO96SWFB01A): interpretation5_variableGroup: NULL has been
replaced by ‘Temperature’
- d18O (CO96SWFB01A): interpretation5_variableGroupDirection: NULL has
been replaced by ‘negative’
- d18O (CO96SWFB01A): interpretation5_variableGroupOriginal: NULL has
been replaced by ‘T_water’
- d18O (CO96SWFB01A): interpretation6_scope: NULL has been replaced by
‘isotope’
- depth (MAT4b082cc2d4): interpretation1_scope: NULL has been replaced
by ‘climate’
- depth (MAT4b082cc2d4): interpretation2_scope: NULL has been replaced
by ‘climate’
- depth (MAT4b082cc2d4): interpretation3_scope: NULL has been replaced
by ‘climate’
- year (MAT7d0bc1f777): interpretation1_scope: NULL has been replaced
by ‘climate’
- year (MAT7d0bc1f777): interpretation2_scope: NULL has been replaced
by ‘climate’
- year (MAT7d0bc1f777): interpretation3_scope: NULL has been replaced
by ‘climate’
Version: 1.0.3
- lastVersion: 1.0.2
- curator: nicholas
- timestamp: 2025-04-09 20:50:25.503945 UTC
- notes: Updated lipdverse database entry with a changed
file.
- changes:
- Paleo Interpretation metadata:
- d18O (CO96SWFB01A): interpretation1_variable: ‘S’ has been replaced
by ‘salinity’
- d18O (CO96SWFB01A): interpretation2_seasonality: ‘annual’ has been
replaced by ‘Annual’
- d18O (CO96SWFB01A): interpretation2_variable: ‘d18O_seawater’ has
been replaced by ‘seawaterIsotope’
- d18O (CO96SWFB01A): interpretation3_variable: ‘T_water’ has been
replaced by ‘temperature’
Version: 1.0.2
- lastVersion: 1.0.1
- curator: nicholas
- timestamp: 2025-04-09 17:39:02.538838 UTC
- notes: Changes made as part of LiPDverse vocabulary
standardization process
- changes:
- Paleo Interpretation metadata:
- d18O (CO96SWFB01A): interpretation1_variable: ‘S’ has been replaced
by ‘salinity’
- d18O (CO96SWFB01A): interpretation2_seasonality: ‘annual’ has been
replaced by ‘Annual’
- d18O (CO96SWFB01A): interpretation2_variable: ‘d18O_seawater’ has
been replaced by ‘seawaterIsotope’
- d18O (CO96SWFB01A): interpretation3_variable: ‘T_water’ has been
replaced by ‘temperature’
Version: 1.0.1
- lastVersion: 1.0.0
- curator: nicholas
- timestamp: 2025-04-08 17:32:35.557636 UTC
- notes: Changes made as part of LiPDverse vocabulary
standardization process
- changes:
- Paleo Column metadata:
- d18O (CO96SWFB01A): paleoData_longName: NULL has been replaced by
‘AD’
- depth (MAT4b082cc2d4): paleoData_longName: NULL has been replaced by
‘AD’
- year (MAT7d0bc1f777): paleoData_units: ‘AD’ has been replaced by ‘yr
AD’
- year (MAT7d0bc1f777): paleoData_longName: NULL has been replaced by
‘AD’