d18O (LS12ANBI): interpretation2_basis: 'Drought periods (i.e., drier winters and/or a more rain-dominated seasonal precipitation balance) generally correspond with higher calcite d18O values, and vice-versa;although lake-water values are currently observed to change  through the ice-free season from ?16.7? to ?13.5? (n= 10), the late summer values are artificially elevated (inset of Fig. 3.).The lower, early summer values are similar to average weightedprecipitation-?18O, and similar to values inferred from near-surface  calcite-?18O prior to 1953 (see Fig. 3 in Anderson, 2011). It is on this basis that variations in through-flowing Bison Lake water-?18O are interpreted as precipitation-?18O and changes in the ratio of the seasonal precipitation balance between snowfall-dominated ?18O) and rainfall-dominated (higher ?18O).' has been replaced by ''
d18O (LS12ANBI): interpretation2_direction: 'positive' has been replaced by ''
d18O (LS12ANBI): interpretation2_inferredMaterial: 'lake water' has been replaced by ''
d18O (LS12ANBI): interpretation2_integrationTime: '5-100' has been replaced by ''
d18O (LS12ANBI): interpretation2_integrationTimeUncertaintyType: 'chronological' has been replaced by ''
d18O (LS12ANBI): interpretation2_integrationTimeUnits: 'years' has been replaced by ''
d18O (LS12ANBI): interpretation2_rank: '1' has been replaced by ''
d18O (LS12ANBI): interpretation2_scope: 'isotope' has been replaced by 'climate'
d18O (LS12ANBI): interpretation2_variable: 'precipitationIsotope' has been replaced by ''
d18O (LS12ANBI): interpretation2_variableGroup: 'P_isotope' has been replaced by ''
d18O (LS12ANBI): interpretation2_variableGroupDirection: 'positive' has been replaced by ''
d18O (LS12ANBI): interpretation3_scope: '' has been replaced by 'climate'
d18O (LS12ANBI): interpretation4_basis: '' has been replaced by 'Drought periods (i.e., drier winters and/or a more rain-dominated seasonal precipitation balance) generally correspond with higher calcite d18O values, and vice-versa;although lake-water values are currently observed to change  through the ice-free season from ?16.7? to ?13.5? (n= 10), the late summer values are artificially elevated (inset of Fig. 3.).The lower, early summer values are similar to average weightedprecipitation-?18O, and similar to values inferred from near-surface  calcite-?18O prior to 1953 (see Fig. 3 in Anderson, 2011). It is on this basis that variations in through-flowing Bison Lake water-?18O are interpreted as precipitation-?18O and changes in the ratio of the seasonal precipitation balance between snowfall-dominated ?18O) and rainfall-dominated (higher ?18O).'
d18O (LS12ANBI): interpretation4_direction: '' has been replaced by 'positive'
d18O (LS12ANBI): interpretation4_inferredMaterial: '' has been replaced by 'lake water'
d18O (LS12ANBI): interpretation4_integrationTime: '' has been replaced by '5-100'
d18O (LS12ANBI): interpretation4_integrationTimeUncertaintyType: '' has been replaced by 'chronological'
d18O (LS12ANBI): interpretation4_integrationTimeUnits: '' has been replaced by 'years'
d18O (LS12ANBI): interpretation4_rank: '' has been replaced by '1'
d18O (LS12ANBI): interpretation4_scope: '' has been replaced by 'isotope'
d18O (LS12ANBI): interpretation4_variable: '' has been replaced by 'precipitationIsotope'
d18O (LS12ANBI): interpretation4_variableGroup: '' has been replaced by 'P_isotope'
d18O (LS12ANBI): interpretation4_variableGroupDirection: '' has been replaced by 'positive'
d18O (LS12ANBI): interpretation5_scope: '' has been replaced by 'isotope'
d18O (LS12ANBI): interpretation6_scope: '' has been replaced by 'isotope'
depth (MAT59872767a4): interpretation1_scope: '' has been replaced by 'climate'
depth (MAT59872767a4): interpretation2_scope: '' has been replaced by 'climate'
year (MATa6bb957328): interpretation1_scope: '' has been replaced by 'climate'
year (MATa6bb957328): interpretation2_scope: '' has been replaced by 'climate'