d18O (WEB0e874eb3): interpretation1_basis: 'Salinity variability for the past half century are qualitatively captured in the Palaui Diploastrea δ18Oc, showing a freshening trend consistent with Porites δ18Oc, instrumental SSS, and coral-based records within the IndoPaciﬁc region. However, a robust Diploastrea δ18Oc and SSS calibration at interannual timescales was not achieved as a result of the competing SST and SSS inﬂuences dampening the δ18Oc signal and compounding effects of continuing coral calciﬁcation during different seasons. Diploastrea δ18Oc should be useful in places where there is high salinity range (mean annual salinity >~1.5 psu) and where SST and SSS signals combine to enlarge the δ18Oc amplitude as previously investigated in the central and South Paciﬁc regions.' has been replaced by ''
d18O (WEB0e874eb3): interpretation1_direction: 'positive' has been replaced by ''
d18O (WEB0e874eb3): interpretation1_rank: '1' has been replaced by ''
d18O (WEB0e874eb3): interpretation1_scope: 'isotope' has been replaced by 'climate'
d18O (WEB0e874eb3): interpretation1_seasonality: 'subannual' has been replaced by ''
d18O (WEB0e874eb3): interpretation1_variable: 'seawaterIsotope' has been replaced by ''
d18O (WEB0e874eb3): interpretation1_variableGroup: 'EffectiveMoisture' has been replaced by ''
d18O (WEB0e874eb3): interpretation1_variableGroupDirection: 'negative' has been replaced by ''
d18O (WEB0e874eb3): interpretation1_variableGroupOriginal: 'd18O_seawater' has been replaced by ''
d18O (WEB0e874eb3): interpretation2_direction: 'negative' has been replaced by ''
d18O (WEB0e874eb3): interpretation2_rank: '2' has been replaced by ''
d18O (WEB0e874eb3): interpretation2_scope: 'isotope' has been replaced by 'climate'
d18O (WEB0e874eb3): interpretation2_variable: 'temperature' has been replaced by ''
d18O (WEB0e874eb3): interpretation2_variableGroup: 'Temperature' has been replaced by ''
d18O (WEB0e874eb3): interpretation2_variableGroupDirection: 'negative' has been replaced by ''
d18O (WEB0e874eb3): interpretation2_variableGroupOriginal: 'T_water' has been replaced by ''
d18O (WEB0e874eb3): interpretation3_scope: '' has been replaced by 'climate'
d18O (WEB0e874eb3): interpretation4_basis: '' has been replaced by 'Salinity variability for the past half century are qualitatively captured in the Palaui Diploastrea δ18Oc, showing a freshening trend consistent with Porites δ18Oc, instrumental SSS, and coral-based records within the IndoPaciﬁc region. However, a robust Diploastrea δ18Oc and SSS calibration at interannual timescales was not achieved as a result of the competing SST and SSS inﬂuences dampening the δ18Oc signal and compounding effects of continuing coral calciﬁcation during different seasons. Diploastrea δ18Oc should be useful in places where there is high salinity range (mean annual salinity >~1.5 psu) and where SST and SSS signals combine to enlarge the δ18Oc amplitude as previously investigated in the central and South Paciﬁc regions.'
d18O (WEB0e874eb3): interpretation4_direction: '' has been replaced by 'positive'
d18O (WEB0e874eb3): interpretation4_rank: '' has been replaced by '1'
d18O (WEB0e874eb3): interpretation4_scope: '' has been replaced by 'isotope'
d18O (WEB0e874eb3): interpretation4_seasonality: '' has been replaced by 'subannual'
d18O (WEB0e874eb3): interpretation4_variable: '' has been replaced by 'seawaterIsotope'
d18O (WEB0e874eb3): interpretation4_variableGroup: '' has been replaced by 'EffectiveMoisture'
d18O (WEB0e874eb3): interpretation4_variableGroupDirection: '' has been replaced by 'negative'
d18O (WEB0e874eb3): interpretation4_variableGroupOriginal: '' has been replaced by 'd18O_seawater'
d18O (WEB0e874eb3): interpretation5_direction: '' has been replaced by 'negative'
d18O (WEB0e874eb3): interpretation5_rank: '' has been replaced by '2'
d18O (WEB0e874eb3): interpretation5_scope: '' has been replaced by 'isotope'
d18O (WEB0e874eb3): interpretation5_variable: '' has been replaced by 'temperature'
d18O (WEB0e874eb3): interpretation5_variableGroup: '' has been replaced by 'Temperature'
d18O (WEB0e874eb3): interpretation5_variableGroupDirection: '' has been replaced by 'negative'
d18O (WEB0e874eb3): interpretation5_variableGroupOriginal: '' has been replaced by 'T_water'
d18O (WEB0e874eb3): interpretation6_scope: '' has been replaced by 'isotope'
Sr/Ca (WEB1b49cf10): interpretation1_scope: '' has been replaced by 'climate'
Sr/Ca (WEB1b49cf10): interpretation2_scope: '' has been replaced by 'climate'
Sr/Ca (WEB1b49cf10): interpretation3_scope: '' has been replaced by 'climate'
Sr/Ca (WEB1b49cf10): interpretation4_scope: '' has been replaced by 'isotope'
Sr/Ca (WEB1b49cf10): interpretation5_scope: '' has been replaced by 'isotope'
Sr/Ca (WEB1b49cf10): interpretation6_scope: '' has been replaced by 'isotope'
Sr/Ca (WEB34c958f0): interpretation1_scope: '' has been replaced by 'climate'
Sr/Ca (WEB34c958f0): interpretation2_scope: '' has been replaced by 'climate'
Sr/Ca (WEB34c958f0): interpretation3_scope: '' has been replaced by 'climate'
Sr/Ca (WEB34c958f0): interpretation4_scope: '' has been replaced by 'isotope'
Sr/Ca (WEB34c958f0): interpretation5_scope: '' has been replaced by 'isotope'
Sr/Ca (WEB34c958f0): interpretation6_scope: '' has been replaced by 'isotope'
d18O (WEB9aced55a): interpretation1_basis: 'Salinity variability for the past half century are qualitatively captured in the Palaui Diploastrea δ18Oc, showing a freshening trend consistent with Porites δ18Oc, instrumental SSS, and coral-based records within the IndoPaciﬁc region. However, a robust Diploastrea δ18Oc and SSS calibration at interannual timescales was not achieved as a result of the competing SST and SSS inﬂuences dampening the δ18Oc signal and compounding effects of continuing coral calciﬁcation during different seasons. Diploastrea δ18Oc should be useful in places where there is high salinity range (mean annual salinity >~1.5 psu) and where SST and SSS signals combine to enlarge the δ18Oc amplitude as previously investigated in the central and South Paciﬁc regions.' has been replaced by ''
d18O (WEB9aced55a): interpretation1_direction: 'positive' has been replaced by ''
d18O (WEB9aced55a): interpretation1_rank: '1' has been replaced by ''
d18O (WEB9aced55a): interpretation1_scope: 'isotope' has been replaced by 'climate'
d18O (WEB9aced55a): interpretation1_seasonality: 'subannual' has been replaced by ''
d18O (WEB9aced55a): interpretation1_variable: 'seawaterIsotope' has been replaced by ''
d18O (WEB9aced55a): interpretation1_variableGroup: 'EffectiveMoisture' has been replaced by ''
d18O (WEB9aced55a): interpretation1_variableGroupDirection: 'negative' has been replaced by ''
d18O (WEB9aced55a): interpretation1_variableGroupOriginal: 'd18O_seawater' has been replaced by ''
d18O (WEB9aced55a): interpretation2_direction: 'negative' has been replaced by ''
d18O (WEB9aced55a): interpretation2_rank: '2' has been replaced by ''
d18O (WEB9aced55a): interpretation2_scope: 'isotope' has been replaced by 'climate'
d18O (WEB9aced55a): interpretation2_variable: 'temperature' has been replaced by ''
d18O (WEB9aced55a): interpretation2_variableGroup: 'Temperature' has been replaced by ''
d18O (WEB9aced55a): interpretation2_variableGroupDirection: 'negative' has been replaced by ''
d18O (WEB9aced55a): interpretation2_variableGroupOriginal: 'T_water' has been replaced by ''
d18O (WEB9aced55a): interpretation3_scope: '' has been replaced by 'climate'
d18O (WEB9aced55a): interpretation4_basis: '' has been replaced by 'Salinity variability for the past half century are qualitatively captured in the Palaui Diploastrea δ18Oc, showing a freshening trend consistent with Porites δ18Oc, instrumental SSS, and coral-based records within the IndoPaciﬁc region. However, a robust Diploastrea δ18Oc and SSS calibration at interannual timescales was not achieved as a result of the competing SST and SSS inﬂuences dampening the δ18Oc signal and compounding effects of continuing coral calciﬁcation during different seasons. Diploastrea δ18Oc should be useful in places where there is high salinity range (mean annual salinity >~1.5 psu) and where SST and SSS signals combine to enlarge the δ18Oc amplitude as previously investigated in the central and South Paciﬁc regions.'
d18O (WEB9aced55a): interpretation4_direction: '' has been replaced by 'positive'
d18O (WEB9aced55a): interpretation4_rank: '' has been replaced by '1'
d18O (WEB9aced55a): interpretation4_scope: '' has been replaced by 'isotope'
d18O (WEB9aced55a): interpretation4_seasonality: '' has been replaced by 'subannual'
d18O (WEB9aced55a): interpretation4_variable: '' has been replaced by 'seawaterIsotope'
d18O (WEB9aced55a): interpretation4_variableGroup: '' has been replaced by 'EffectiveMoisture'
d18O (WEB9aced55a): interpretation4_variableGroupDirection: '' has been replaced by 'negative'
d18O (WEB9aced55a): interpretation4_variableGroupOriginal: '' has been replaced by 'd18O_seawater'
d18O (WEB9aced55a): interpretation5_direction: '' has been replaced by 'negative'
d18O (WEB9aced55a): interpretation5_rank: '' has been replaced by '2'
d18O (WEB9aced55a): interpretation5_scope: '' has been replaced by 'isotope'
d18O (WEB9aced55a): interpretation5_variable: '' has been replaced by 'temperature'
d18O (WEB9aced55a): interpretation5_variableGroup: '' has been replaced by 'Temperature'
d18O (WEB9aced55a): interpretation5_variableGroupDirection: '' has been replaced by 'negative'
d18O (WEB9aced55a): interpretation5_variableGroupOriginal: '' has been replaced by 'T_water'
d18O (WEB9aced55a): interpretation6_scope: '' has been replaced by 'isotope'