Version history for PBWAsecE3wOhGEpJLXsk - SS05ROES
Version: 1.0.6
- lastVersion: 1.0.5
- curator: nicholas
- timestamp: 2025-04-17 20:05:05.699965 UTC
- changes:
- Paleo Column metadata:
- year (MAT2569a32240): paleoData_isPrimary: NULL has been replaced by
‘TRUE’
- year (MAT2569a32240): paleoData_primaryAgeColumn: NULL has been
replaced by ‘TRUE’
- d18O (Ocean2kHR_112): paleoData_isPrimary: NULL has been replaced by
‘FALSE’
- d18O (Ocean2kHR_112): paleoData_primaryAgeColumn: NULL has been
replaced by ‘FALSE’
- Sr/Ca (Ocean2kHR_113): paleoData_isPrimary: NULL has been replaced
by ‘FALSE’
- Sr/Ca (Ocean2kHR_113): paleoData_primaryAgeColumn: NULL has been
replaced by ‘FALSE’
Version: 1.0.5
- lastVersion: 1.0.4
- curator: nicholas
- timestamp: 2025-04-11 16:27:24.140553 UTC
- changes:
- Paleo Interpretation metadata:
- d18O (Ocean2kHR_112): interpretation2_basis: ‘bohm 2000
10.1016/S0016-7037(99)00408-1’ has been replaced by NULL
- d18O (Ocean2kHR_112): interpretation2_direction: ‘negative’ has been
replaced by NULL
- d18O (Ocean2kHR_112): interpretation2_equilibriumEvidence: ‘mode of
skeleton formation of Ceratoporella nicholsoni suggest that these
sponges precipitate aragonite close to isotopic equilibrium (bohm,
2000).’ has been replaced by NULL
- d18O (Ocean2kHR_112): interpretation2_inferredMaterial: ‘seawater’
has been replaced by NULL
- d18O (Ocean2kHR_112): interpretation2_integrationTime: ‘1’ has been
replaced by NULL
- d18O (Ocean2kHR_112): interpretation2_integrationTimeBasis:
‘sclerosponges were dated using U/Th radiometric techniques and then
analyzed using high resolution micromilling for oxygen isotope analysis
via isotope ratio mass spectrometry and laser ablation sampling for
Sr/Ca analysis via ICP-MS. Constant-growth age models constructed from
U/Th dating indicate growth rates of 145 mmy1 for the Exuma sclerosponge
and 172 mmy1 for the TOTO sclerosponge (auxiliary material1). The
radiometric age model of the TOTO sclerosponge was tuned to annual Sr/
Ca variations after Swart et al. [2002], however because tuned age
models and constant growth models are within 5% [Swart et al., 2002],
the U/Th constant growth model was used for the Exuma sclerosponge.’ has
been replaced by NULL
- d18O (Ocean2kHR_112): interpretation2_integrationTimeUncertainty:
‘subannual samples averaged to annual for archived data’ has been
replaced by NULL
- d18O (Ocean2kHR_112):
interpretation2_integrationTimeUncertaintyType: ‘U/Th dating and Sr/Ca
for annual cycles to define chronology’ has been replaced by NULL
- d18O (Ocean2kHR_112): interpretation2_integrationTimeUnits: ‘year’
has been replaced by NULL
- d18O (Ocean2kHR_112): interpretation2_mathematicalRelation: ‘linear’
has been replaced by NULL
- d18O (Ocean2kHR_112): interpretation2_rank: ‘1’ has been replaced by
NULL
- d18O (Ocean2kHR_112): interpretation2_scope: ‘isotope’ has been
replaced by ‘climate’
- d18O (Ocean2kHR_112): interpretation2_variable: ‘temperature’ has
been replaced by NULL
- d18O (Ocean2kHR_112): interpretation2_variableGroup: ‘Temperature’
has been replaced by NULL
- d18O (Ocean2kHR_112): interpretation2_variableGroupDirection:
‘negative’ has been replaced by NULL
- d18O (Ocean2kHR_112): interpretation2_variableGroupOriginal:
‘T_water’ has been replaced by NULL
- d18O (Ocean2kHR_112): interpretation3_basis: ‘Oxygen isotope values
(d18O) are measured in %VPDB for aragonite and % SMOW for water. Ratios
of Sr/Ca are measured in mmolmol1, temperature (T) is in C, and salinity
(S) is in psu. Equation (3) is constructed from surface waters (<50
m) of the return flow of the N. Atlantic Gyre between 45N and 31N.
During transport between these latitudes, this water mass begins
adopting the properties of the SMW [Krauss, 1986; Ottens, 1991]. By
combining and rearranging these equations to reconstruct the salinity
record preserved in Bahamas sclerosponges,’ has been replaced by
NULL
- d18O (Ocean2kHR_112): interpretation3_direction: ‘negative’ has been
replaced by NULL
- d18O (Ocean2kHR_112): interpretation3_equilibriumEvidence: ‘mode of
skeleton formation of Ceratoporella nicholsoni suggest that these
sponges precipitate aragonite close to isotopic equilibrium (bohm,
2000).’ has been replaced by NULL
- d18O (Ocean2kHR_112): interpretation3_inferredMaterial: ‘seawater’
has been replaced by NULL
- d18O (Ocean2kHR_112): interpretation3_integrationTime: ‘1’ has been
replaced by NULL
- d18O (Ocean2kHR_112): interpretation3_integrationTimeBasis:
‘sclerosponges were dated using U/Th radiometric techniques and then
analyzed using high resolution micromilling for oxygen isotope analysis
via isotope ratio mass spectrometry and laser ablation sampling for
Sr/Ca analysis via ICP-MS. Constant-growth age models constructed from
U/Th dating indicate growth rates of 145 mmy1 for the Exuma sclerosponge
and 172 mmy1 for the TOTO sclerosponge (auxiliary material1). The
radiometric age model of the TOTO sclerosponge was tuned to annual Sr/
Ca variations after Swart et al. [2002], however because tuned age
models and constant growth models are within 5% [Swart et al., 2002],
the U/Th constant growth model was used for the Exuma sclerosponge.’ has
been replaced by NULL
- d18O (Ocean2kHR_112): interpretation3_integrationTimeUncertainty:
‘subannual samples averaged to annual for archived data’ has been
replaced by NULL
- d18O (Ocean2kHR_112):
interpretation3_integrationTimeUncertaintyType: ‘U/Th dating and Sr/Ca
for annual cycles to define chronology’ has been replaced by NULL
- d18O (Ocean2kHR_112): interpretation3_integrationTimeUnits: ‘year’
has been replaced by NULL
- d18O (Ocean2kHR_112): interpretation3_mathematicalRelation: ‘linear’
has been replaced by NULL
- d18O (Ocean2kHR_112): interpretation3_rank: ‘2’ has been replaced by
NULL
- d18O (Ocean2kHR_112): interpretation3_scope: ‘isotope’ has been
replaced by ‘climate’
- d18O (Ocean2kHR_112): interpretation3_variable: ‘salinity’ has been
replaced by NULL
- d18O (Ocean2kHR_112): interpretation3_variableGroup:
‘EffectiveMoisture’ has been replaced by NULL
- d18O (Ocean2kHR_112): interpretation3_variableGroupDirection:
‘negative’ has been replaced by NULL
- d18O (Ocean2kHR_112): interpretation3_variableGroupOriginal:
‘salinity_seawater’ has been replaced by NULL
- d18O (Ocean2kHR_112): interpretation4_rank: NULL has been replaced
by ‘1’
- d18O (Ocean2kHR_112): interpretation4_basis: NULL has been replaced
by ‘bohm 2000 10.1016/S0016-7037(99)00408-1’
- d18O (Ocean2kHR_112): interpretation4_direction: NULL has been
replaced by ‘negative’
- d18O (Ocean2kHR_112): interpretation4_equilibriumEvidence: NULL has
been replaced by ‘mode of skeleton formation of Ceratoporella nicholsoni
suggest that these sponges precipitate aragonite close to isotopic
equilibrium (bohm, 2000).’
- d18O (Ocean2kHR_112): interpretation4_inferredMaterial: NULL has
been replaced by ‘seawater’
- d18O (Ocean2kHR_112): interpretation4_integrationTime: NULL has been
replaced by ‘1’
- d18O (Ocean2kHR_112): interpretation4_integrationTimeBasis: NULL has
been replaced by ‘sclerosponges were dated using U/Th radiometric
techniques and then analyzed using high resolution micromilling for
oxygen isotope analysis via isotope ratio mass spectrometry and laser
ablation sampling for Sr/Ca analysis via ICP-MS. Constant-growth age
models constructed from U/Th dating indicate growth rates of 145 mmy1
for the Exuma sclerosponge and 172 mmy1 for the TOTO sclerosponge
(auxiliary material1). The radiometric age model of the TOTO
sclerosponge was tuned to annual Sr/ Ca variations after Swart et
al. [2002], however because tuned age models and constant growth models
are within 5% [Swart et al., 2002], the U/Th constant growth model was
used for the Exuma sclerosponge.’
- d18O (Ocean2kHR_112): interpretation4_integrationTimeUncertainty:
NULL has been replaced by ‘subannual samples averaged to annual for
archived data’
- d18O (Ocean2kHR_112):
interpretation4_integrationTimeUncertaintyType: NULL has been replaced
by ‘U/Th dating and Sr/Ca for annual cycles to define chronology’
- d18O (Ocean2kHR_112): interpretation4_integrationTimeUnits: NULL has
been replaced by ‘year’
- d18O (Ocean2kHR_112): interpretation4_mathematicalRelation: NULL has
been replaced by ‘linear’
- d18O (Ocean2kHR_112): interpretation4_variable: NULL has been
replaced by ‘temperature’
- d18O (Ocean2kHR_112): interpretation4_variableGroup: NULL has been
replaced by ‘Temperature’
- d18O (Ocean2kHR_112): interpretation4_variableGroupDirection: NULL
has been replaced by ‘negative’
- d18O (Ocean2kHR_112): interpretation4_variableGroupOriginal: NULL
has been replaced by ‘T_water’
- d18O (Ocean2kHR_112): interpretation5_basis: NULL has been replaced
by ‘Oxygen isotope values (d18O) are measured in %VPDB for aragonite and
% SMOW for water. Ratios of Sr/Ca are measured in mmolmol1, temperature
(T) is in C, and salinity (S) is in psu. Equation (3) is constructed
from surface waters (<50 m) of the return flow of the N. Atlantic
Gyre between 45N and 31N. During transport between these latitudes, this
water mass begins adopting the properties of the SMW [Krauss, 1986;
Ottens, 1991]. By combining and rearranging these equations to
reconstruct the salinity record preserved in Bahamas
sclerosponges,’
- d18O (Ocean2kHR_112): interpretation5_direction: NULL has been
replaced by ‘negative’
- d18O (Ocean2kHR_112): interpretation5_equilibriumEvidence: NULL has
been replaced by ‘mode of skeleton formation of Ceratoporella nicholsoni
suggest that these sponges precipitate aragonite close to isotopic
equilibrium (bohm, 2000).’
- d18O (Ocean2kHR_112): interpretation5_inferredMaterial: NULL has
been replaced by ‘seawater’
- d18O (Ocean2kHR_112): interpretation5_integrationTime: NULL has been
replaced by ‘1’
- d18O (Ocean2kHR_112): interpretation5_integrationTimeBasis: NULL has
been replaced by ‘sclerosponges were dated using U/Th radiometric
techniques and then analyzed using high resolution micromilling for
oxygen isotope analysis via isotope ratio mass spectrometry and laser
ablation sampling for Sr/Ca analysis via ICP-MS. Constant-growth age
models constructed from U/Th dating indicate growth rates of 145 mmy1
for the Exuma sclerosponge and 172 mmy1 for the TOTO sclerosponge
(auxiliary material1). The radiometric age model of the TOTO
sclerosponge was tuned to annual Sr/ Ca variations after Swart et
al. [2002], however because tuned age models and constant growth models
are within 5% [Swart et al., 2002], the U/Th constant growth model was
used for the Exuma sclerosponge.’
- d18O (Ocean2kHR_112): interpretation5_integrationTimeUncertainty:
NULL has been replaced by ‘subannual samples averaged to annual for
archived data’
- d18O (Ocean2kHR_112):
interpretation5_integrationTimeUncertaintyType: NULL has been replaced
by ‘U/Th dating and Sr/Ca for annual cycles to define chronology’
- d18O (Ocean2kHR_112): interpretation5_integrationTimeUnits: NULL has
been replaced by ‘year’
- d18O (Ocean2kHR_112): interpretation5_mathematicalRelation: NULL has
been replaced by ‘linear’
- d18O (Ocean2kHR_112): interpretation5_rank: NULL has been replaced
by ‘2’
- d18O (Ocean2kHR_112): interpretation5_scope: NULL has been replaced
by ‘isotope’
- d18O (Ocean2kHR_112): interpretation5_variable: NULL has been
replaced by ‘salinity’
- d18O (Ocean2kHR_112): interpretation5_variableGroup: NULL has been
replaced by ‘EffectiveMoisture’
- d18O (Ocean2kHR_112): interpretation5_variableGroupDirection: NULL
has been replaced by ‘negative’
- d18O (Ocean2kHR_112): interpretation5_variableGroupOriginal: NULL
has been replaced by ‘salinity_seawater’
- d18O (Ocean2kHR_112): interpretation6_scope: NULL has been replaced
by ‘isotope’
- Sr/Ca (Ocean2kHR_113): interpretation2_inferredMaterial: ‘seawater’
has been replaced by NULL
- Sr/Ca (Ocean2kHR_113): interpretation2_scope: ‘isotope’ has been
replaced by ‘climate’
- Sr/Ca (Ocean2kHR_113): interpretation3_scope: ‘isotope’ has been
replaced by ‘climate’
- Sr/Ca (Ocean2kHR_113): interpretation4_inferredMaterial: NULL has
been replaced by ‘seawater’
- Sr/Ca (Ocean2kHR_113): interpretation5_scope: NULL has been replaced
by ‘isotope’
- Sr/Ca (Ocean2kHR_113): interpretation6_scope: NULL has been replaced
by ‘isotope’
Version: 1.0.4
- lastVersion: 1.0.3
- curator: nicholas
- timestamp: 2025-04-09 21:54:37.317095 UTC
- notes: Updated lipdverse database entry with a changed
file.
- changes:
- Paleo Interpretation metadata:
- d18O (Ocean2kHR_112): interpretation1_seasonality: ‘annual’ has been
replaced by ‘Annual’
- d18O (Ocean2kHR_112): interpretation1_variable: ‘temperature and
salinity’ has been replaced by ‘temperature’
- d18O (Ocean2kHR_112): interpretation2_variable: ‘T_water’ has been
replaced by ‘temperature’
- d18O (Ocean2kHR_112): interpretation3_variable: ‘salinity_seawater’
has been replaced by ‘salinity’
- Sr/Ca (Ocean2kHR_113): interpretation1_seasonality: ‘annual’ has
been replaced by ‘Annual’
- Sr/Ca (Ocean2kHR_113): interpretation1_variable: ‘T’ has been
replaced by ‘temperature’
Version: 1.0.3
- lastVersion: 1.0.2
- curator: nicholas
- timestamp: 2025-04-09 20:28:12.743031 UTC
- notes: Changes made as part of LiPDverse vocabulary
standardization process
- changes:
- Paleo Interpretation metadata:
- d18O (Ocean2kHR_112): interpretation1_seasonality: ‘annual’ has been
replaced by ‘Annual’
- d18O (Ocean2kHR_112): interpretation1_variable: ‘temperature and
salinity’ has been replaced by ‘temperature’
- d18O (Ocean2kHR_112): interpretation2_variable: ‘T_water’ has been
replaced by ‘temperature’
- d18O (Ocean2kHR_112): interpretation3_variable: ‘salinity_seawater’
has been replaced by ‘salinity’
- Sr/Ca (Ocean2kHR_113): interpretation1_seasonality: ‘annual’ has
been replaced by ‘Annual’
- Sr/Ca (Ocean2kHR_113): interpretation1_variable: ‘T’ has been
replaced by ‘temperature’
Version: 1.0.2
- lastVersion: 1.0.1
- curator: nicholas
- timestamp: 2025-04-08 17:34:54.075094 UTC
- notes: Changes made as part of LiPDverse vocabulary
standardization process
- changes:
- Paleo Column metadata:
- year (MAT2569a32240): paleoData_units: ‘AD’ has been replaced by ‘yr
AD’
- year (MAT2569a32240): paleoData_longName: NULL has been replaced by
‘AD’
- d18O (Ocean2kHR_112): paleoData_longName: NULL has been replaced by
‘AD’
- Sr/Ca (Ocean2kHR_113): paleoData_longName: NULL has been replaced by
‘AD’
Version: 1.0.1
- lastVersion: 1.0.0
- curator: nicholas
- timestamp: 2022-08-16 23:29:50 UTC
- changes:
- Paleo Interpretation metadata:
- d18O (Ocean2kHR_112): interpretation4_scope: NULL has been replaced
by ‘isotope’
- Sr/Ca (Ocean2kHR_113): interpretation3_scope: NULL has been replaced
by ‘isotope’
- Sr/Ca (Ocean2kHR_113): interpretation4_scope: NULL has been replaced
by ‘isotope’