year (MATa7e4c21c51): interpretation1_scope: '' has been replaced by 'climate'
year (MATa7e4c21c51): interpretation2_scope: '' has been replaced by 'climate'
year (MATa7e4c21c51): interpretation3_scope: '' has been replaced by 'climate'
depth (MATf33d41f775): interpretation1_scope: '' has been replaced by 'climate'
depth (MATf33d41f775): interpretation2_scope: '' has been replaced by 'climate'
depth (MATf33d41f775): interpretation3_scope: '' has been replaced by 'climate'
d18O (SP12FOAT01A): interpretation2_basis: 'The observed strong decrease in the ?18O by about 1.5? between 11 and 10 ka, for example, is rather a change of the source region than a pure temperature  effect. Based on this assumption, during the deglaciation the trajectories more frequently followed southerly routes. Towards the transition into the Holocene the main contribution of precipitation probably originated from more northern regions of the Atlantic, where the surface ocean is generally more depleted in 18O (LeGrande and Schmidt, 2006).' has been replaced by ''
d18O (SP12FOAT01A): interpretation2_direction: 'positive' has been replaced by ''
d18O (SP12FOAT01A): interpretation2_equilibriumEvidence: 'Owing to the low cave temperature kinetic isotope effects are minimal (Mangini et al., 2005; Vollweiler et al., 2006).' has been replaced by ''
d18O (SP12FOAT01A): interpretation2_inferredMaterial: 'groundwater d18O' has been replaced by ''
d18O (SP12FOAT01A): interpretation2_integrationTime: 'Average resolution of each stal 5.1 yr (SPA12), 3.5 yr (SPA128), 8 yr (SPA70), 4 yr (SPA127) and 1.6 yr (SPA133).' has been replaced by ''
d18O (SP12FOAT01A): interpretation2_integrationTimeBasis: 'iscam method (Fohlmeister et al., 2012), based on simulations and correlation calculations between pairs of climate  records (this is a stack of 5 records). Point-wise linear interpolation between data points. Typical age errors are smaller than 2%.' has been replaced by ''
d18O (SP12FOAT01A): interpretation2_integrationTimeUnits: 'year' has been replaced by ''
d18O (SP12FOAT01A): interpretation2_mathematicalRelation: 'nonlinear.' has been replaced by ''
d18O (SP12FOAT01A): interpretation2_rank: '1' has been replaced by ''
d18O (SP12FOAT01A): interpretation2_scope: 'isotope' has been replaced by 'climate'
d18O (SP12FOAT01A): interpretation2_seasonality: 'Sep-Feb' has been replaced by ''
d18O (SP12FOAT01A): interpretation2_variable: 'precipitationIsotope' has been replaced by ''
d18O (SP12FOAT01A): interpretation2_variableGroup: 'P_isotope' has been replaced by ''
d18O (SP12FOAT01A): interpretation2_variableGroupDirection: 'positive' has been replaced by ''
d18O (SP12FOAT01A): interpretation3_rank: '2' has been replaced by ''
d18O (SP12FOAT01A): interpretation3_scope: 'isotope' has been replaced by 'climate'
d18O (SP12FOAT01A): interpretation4_rank: '' has been replaced by '1'
d18O (SP12FOAT01A): interpretation4_basis: '' has been replaced by 'The observed strong decrease in the ?18O by about 1.5? between 11 and 10 ka, for example, is rather a change of the source region than a pure temperature  effect. Based on this assumption, during the deglaciation the trajectories more frequently followed southerly routes. Towards the transition into the Holocene the main contribution of precipitation probably originated from more northern regions of the Atlantic, where the surface ocean is generally more depleted in 18O (LeGrande and Schmidt, 2006).'
d18O (SP12FOAT01A): interpretation4_direction: '' has been replaced by 'positive'
d18O (SP12FOAT01A): interpretation4_equilibriumEvidence: '' has been replaced by 'Owing to the low cave temperature kinetic isotope effects are minimal (Mangini et al., 2005; Vollweiler et al., 2006).'
d18O (SP12FOAT01A): interpretation4_inferredMaterial: '' has been replaced by 'groundwater d18O'
d18O (SP12FOAT01A): interpretation4_integrationTime: '' has been replaced by 'Average resolution of each stal 5.1 yr (SPA12), 3.5 yr (SPA128), 8 yr (SPA70), 4 yr (SPA127) and 1.6 yr (SPA133).'
d18O (SP12FOAT01A): interpretation4_integrationTimeBasis: '' has been replaced by 'iscam method (Fohlmeister et al., 2012), based on simulations and correlation calculations between pairs of climate  records (this is a stack of 5 records). Point-wise linear interpolation between data points. Typical age errors are smaller than 2%.'
d18O (SP12FOAT01A): interpretation4_integrationTimeUnits: '' has been replaced by 'year'
d18O (SP12FOAT01A): interpretation4_mathematicalRelation: '' has been replaced by 'nonlinear.'
d18O (SP12FOAT01A): interpretation4_seasonality: '' has been replaced by 'Sep-Feb'
d18O (SP12FOAT01A): interpretation4_variable: '' has been replaced by 'precipitationIsotope'
d18O (SP12FOAT01A): interpretation4_variableGroup: '' has been replaced by 'P_isotope'
d18O (SP12FOAT01A): interpretation4_variableGroupDirection: '' has been replaced by 'positive'
d18O (SP12FOAT01A): interpretation5_rank: '' has been replaced by '2'
d18O (SP12FOAT01A): interpretation5_scope: '' has been replaced by 'isotope'
d18O (SP12FOAT01A): interpretation6_scope: '' has been replaced by 'isotope'