d18O (Ocean2kHR_112): interpretation2_basis: 'bohm 2000 10.1016/S0016-7037(99)00408-1' has been replaced by ''
d18O (Ocean2kHR_112): interpretation2_direction: 'negative' has been replaced by ''
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 has been replaced by ''
d18O (Ocean2kHR_112): interpretation2_inferredMaterial: 'seawater' has been replaced by ''
d18O (Ocean2kHR_112): interpretation2_integrationTime: '1' has been replaced by ''
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 has been replaced by ''
d18O (Ocean2kHR_112): interpretation2_integrationTimeUncertainty: 'subannual samples averaged to annual for archived data' has been replaced by ''
d18O (Ocean2kHR_112): interpretation2_integrationTimeUncertaintyType: 'U/Th dating and Sr/Ca for annual cycles to define chronology' has been replaced by ''
d18O (Ocean2kHR_112): interpretation2_integrationTimeUnits: 'year' has been replaced by ''
d18O (Ocean2kHR_112): interpretation2_mathematicalRelation: 'linear' has been replaced by ''
d18O (Ocean2kHR_112): interpretation2_rank: '1' has been replaced by ''
d18O (Ocean2kHR_112): interpretation2_scope: 'isotope' has been replaced by 'climate'
d18O (Ocean2kHR_112): interpretation2_variable: 'temperature' has been replaced by ''
d18O (Ocean2kHR_112): interpretation2_variableGroup: 'Temperature' has been replaced by ''
d18O (Ocean2kHR_112): interpretation2_variableGroupDirection: 'negative' has been replaced by ''
d18O (Ocean2kHR_112): interpretation2_variableGroupOriginal: 'T_water' has been replaced by ''
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 ''
d18O (Ocean2kHR_112): interpretation3_direction: 'negative' has been replaced by ''
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 ''
d18O (Ocean2kHR_112): interpretation3_inferredMaterial: 'seawater' has been replaced by ''
d18O (Ocean2kHR_112): interpretation3_integrationTime: '1' has been replaced by ''
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 ''
d18O (Ocean2kHR_112): interpretation3_integrationTimeUncertainty: 'subannual samples averaged to annual for archived data' has been replaced by ''
d18O (Ocean2kHR_112): interpretation3_integrationTimeUncertaintyType: 'U/Th dating and Sr/Ca for annual cycles to define chronology' has been replaced by ''
d18O (Ocean2kHR_112): interpretation3_integrationTimeUnits: 'year' has been replaced by ''
d18O (Ocean2kHR_112): interpretation3_mathematicalRelation: 'linear' has been replaced by ''
d18O (Ocean2kHR_112): interpretation3_rank: '2' has been replaced by ''
d18O (Ocean2kHR_112): interpretation3_scope: 'isotope' has been replaced by 'climate'
d18O (Ocean2kHR_112): interpretation3_variable: 'salinity' has been replaced by ''
d18O (Ocean2kHR_112): interpretation3_variableGroup: 'EffectiveMoisture' has been replaced by ''
d18O (Ocean2kHR_112): interpretation3_variableGroupDirection: 'negative' has been replaced by ''
d18O (Ocean2kHR_112): interpretation3_variableGroupOriginal: 'salinity_seawater' has been replaced by ''
d18O (Ocean2kHR_112): interpretation4_rank: '' has been replaced by '1'
d18O (Ocean2kHR_112): interpretation4_basis: '' has been replaced by 'bohm 2000 10.1016/S0016-7037(99)00408-1'
d18O (Ocean2kHR_112): interpretation4_direction: '' has been replaced by 'negative'
d18O (Ocean2kHR_112): interpretation4_equilibriumEvidence: '' 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: '' has been replaced by 'seawater'
d18O (Ocean2kHR_112): interpretation4_integrationTime: '' has been replaced by '1'
d18O (Ocean2kHR_112): interpretation4_integrationTimeBasis: '' 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: '' has been replaced by 'subannual samples averaged to annual for archived data'
d18O (Ocean2kHR_112): interpretation4_integrationTimeUncertaintyType: '' has been replaced by 'U/Th dating and Sr/Ca for annual cycles to define chronology'
d18O (Ocean2kHR_112): interpretation4_integrationTimeUnits: '' has been replaced by 'year'
d18O (Ocean2kHR_112): interpretation4_mathematicalRelation: '' has been replaced by 'linear'
d18O (Ocean2kHR_112): interpretation4_variable: '' has been replaced by 'temperature'
d18O (Ocean2kHR_112): interpretation4_variableGroup: '' has been replaced by 'Temperature'
d18O (Ocean2kHR_112): interpretation4_variableGroupDirection: '' has been replaced by 'negative'
d18O (Ocean2kHR_112): interpretation4_variableGroupOriginal: '' has been replaced by 'T_water'
d18O (Ocean2kHR_112): interpretation5_basis: '' 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: '' has been replaced by 'negative'
d18O (Ocean2kHR_112): interpretation5_equilibriumEvidence: '' 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: '' has been replaced by 'seawater'
d18O (Ocean2kHR_112): interpretation5_integrationTime: '' has been replaced by '1'
d18O (Ocean2kHR_112): interpretation5_integrationTimeBasis: '' 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: '' has been replaced by 'subannual samples averaged to annual for archived data'
d18O (Ocean2kHR_112): interpretation5_integrationTimeUncertaintyType: '' has been replaced by 'U/Th dating and Sr/Ca for annual cycles to define chronology'
d18O (Ocean2kHR_112): interpretation5_integrationTimeUnits: '' has been replaced by 'year'
d18O (Ocean2kHR_112): interpretation5_mathematicalRelation: '' has been replaced by 'linear'
d18O (Ocean2kHR_112): interpretation5_rank: '' has been replaced by '2'
d18O (Ocean2kHR_112): interpretation5_scope: '' has been replaced by 'isotope'
d18O (Ocean2kHR_112): interpretation5_variable: '' has been replaced by 'salinity'
d18O (Ocean2kHR_112): interpretation5_variableGroup: '' has been replaced by 'EffectiveMoisture'
d18O (Ocean2kHR_112): interpretation5_variableGroupDirection: '' has been replaced by 'negative'
d18O (Ocean2kHR_112): interpretation5_variableGroupOriginal: '' has been replaced by 'salinity_seawater'
d18O (Ocean2kHR_112): interpretation6_scope: '' has been replaced by 'isotope'
Sr/Ca (Ocean2kHR_113): interpretation2_inferredMaterial: 'seawater' has been replaced by ''
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: '' has been replaced by 'seawater'
Sr/Ca (Ocean2kHR_113): interpretation5_scope: '' has been replaced by 'isotope'
Sr/Ca (Ocean2kHR_113): interpretation6_scope: '' has been replaced by 'isotope'