d18O (LS12ANYE): 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 weighted  precipitation-?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 has been replaced by ''
d18O (LS12ANYE): interpretation2_direction: 'negative' has been replaced by ''
d18O (LS12ANYE): interpretation2_inferredMaterial: 'lake water' has been replaced by ''
d18O (LS12ANYE): interpretation2_integrationTime: '5-100' has been replaced by ''
d18O (LS12ANYE): interpretation2_integrationTimeUncertaintyType: 'chronological' has been replaced by ''
d18O (LS12ANYE): interpretation2_integrationTimeUnits: 'years' has been replaced by ''
d18O (LS12ANYE): interpretation2_rank: '1' has been replaced by ''
d18O (LS12ANYE): interpretation2_scope: 'isotope' has been replaced by 'climate'
d18O (LS12ANYE): interpretation2_variable: 'effectivePrecipitation' has been replaced by ''
d18O (LS12ANYE): interpretation2_variableGroup: 'EffectiveMoisture' has been replaced by ''
d18O (LS12ANYE): interpretation2_variableGroupDirection: 'negative' has been replaced by ''
d18O (LS12ANYE): interpretation2_variableGroupOriginal: 'P_E' has been replaced by ''
d18O (LS12ANYE): interpretation3_basis: 'Variations in Yellow Lake past lake-water-?18O are interpreted in two ways. When the basin was over-flowing, past lake-water-?18O values are interpreted similarly to  Bison Lake that is in terms of the seasonal balance of precipitation.  When the basin closed, past lake-water-?18O values are interpreted  as secondary effects of summer evaporation: higher lake-water ?18O values reflect more summer evaporation, or less effective moisture  (precipitation?evaporation), whereas lower values reflect less evapo-  ration, or increased effective moisture.' has been replaced by ''
d18O (LS12ANYE): interpretation3_inferredMaterial: 'lake water' has been replaced by ''
d18O (LS12ANYE): interpretation3_integrationTime: '5-100' has been replaced by ''
d18O (LS12ANYE): interpretation3_integrationTimeUncertaintyType: 'chronological' has been replaced by ''
d18O (LS12ANYE): interpretation3_integrationTimeUnits: 'years' has been replaced by ''
d18O (LS12ANYE): interpretation3_mathematicalRelation: 'increase' has been replaced by ''
d18O (LS12ANYE): interpretation3_rank: '2' has been replaced by ''
d18O (LS12ANYE): interpretation3_scope: 'isotope' has been replaced by 'climate'
d18O (LS12ANYE): interpretation3_seasonality: 'Summer' has been replaced by ''
d18O (LS12ANYE): interpretation3_variable: 'effectivePrecipitation' has been replaced by ''
d18O (LS12ANYE): interpretation3_variableGroup: 'EffectiveMoisture' has been replaced by ''
d18O (LS12ANYE): interpretation3_variableGroupDirection: 'negative' has been replaced by ''
d18O (LS12ANYE): interpretation3_variableGroupOriginal: 'P_E' has been replaced by ''
d18O (LS12ANYE): 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 weighted  precipitation-?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 (LS12ANYE): interpretation4_direction: '' has been replaced by 'negative'
d18O (LS12ANYE): interpretation4_inferredMaterial: '' has been replaced by 'lake water'
d18O (LS12ANYE): interpretation4_integrationTime: '' has been replaced by '5-100'
d18O (LS12ANYE): interpretation4_integrationTimeUncertaintyType: '' has been replaced by 'chronological'
d18O (LS12ANYE): interpretation4_integrationTimeUnits: '' has been replaced by 'years'
d18O (LS12ANYE): interpretation4_rank: '' has been replaced by '1'
d18O (LS12ANYE): interpretation4_scope: '' has been replaced by 'isotope'
d18O (LS12ANYE): interpretation4_variable: '' has been replaced by 'effectivePrecipitation'
d18O (LS12ANYE): interpretation4_variableGroup: '' has been replaced by 'EffectiveMoisture'
d18O (LS12ANYE): interpretation4_variableGroupDirection: '' has been replaced by 'negative'
d18O (LS12ANYE): interpretation4_variableGroupOriginal: '' has been replaced by 'P_E'
d18O (LS12ANYE): interpretation5_basis: '' has been replaced by 'Variations in Yellow Lake past lake-water-?18O are interpreted in two ways. When the basin was over-flowing, past lake-water-?18O values are interpreted similarly to  Bison Lake that is in terms of the seasonal balance of precipitation.  When the basin closed, past lake-water-?18O values are interpreted  as secondary effects of summer evaporation: higher lake-water ?18O values reflect more summer evaporation, or less effective moisture  (precipitation?evaporation), whereas lower values reflect less evapo-  ration, or increased effective moisture.'
d18O (LS12ANYE): interpretation5_inferredMaterial: '' has been replaced by 'lake water'
d18O (LS12ANYE): interpretation5_integrationTime: '' has been replaced by '5-100'
d18O (LS12ANYE): interpretation5_integrationTimeUncertaintyType: '' has been replaced by 'chronological'
d18O (LS12ANYE): interpretation5_integrationTimeUnits: '' has been replaced by 'years'
d18O (LS12ANYE): interpretation5_mathematicalRelation: '' has been replaced by 'increase'
d18O (LS12ANYE): interpretation5_rank: '' has been replaced by '2'
d18O (LS12ANYE): interpretation5_scope: '' has been replaced by 'isotope'
d18O (LS12ANYE): interpretation5_seasonality: '' has been replaced by 'Summer'
d18O (LS12ANYE): interpretation5_variable: '' has been replaced by 'effectivePrecipitation'
d18O (LS12ANYE): interpretation5_variableGroup: '' has been replaced by 'EffectiveMoisture'
d18O (LS12ANYE): interpretation5_variableGroupDirection: '' has been replaced by 'negative'
d18O (LS12ANYE): interpretation5_variableGroupOriginal: '' has been replaced by 'P_E'
d18O (LS12ANYE): interpretation6_scope: '' has been replaced by 'isotope'
year (MAT3277152d67): interpretation1_scope: '' has been replaced by 'climate'
year (MAT3277152d67): interpretation2_scope: '' has been replaced by 'climate'
year (MAT3277152d67): interpretation3_scope: '' has been replaced by 'climate'
depth (MAT5e1d4452c1): interpretation1_scope: '' has been replaced by 'climate'
depth (MAT5e1d4452c1): interpretation2_scope: '' has been replaced by 'climate'
depth (MAT5e1d4452c1): interpretation3_scope: '' has been replaced by 'climate'