year (LPD9b7b0312): paleoData_isPrimary: '' has been replaced by 'TRUE'
year (LPD9b7b0312): paleoData_primaryAgeColumn: '' has been replaced by 'TRUE'
depth (MAT7d1ee4077b): paleoData_isPrimary: '' has been replaced by 'FALSE'
depth (MAT7d1ee4077b): paleoData_primaryAgeColumn: '' has been replaced by 'FALSE'
d18O (SP05CRBR01A): paleoData_isPrimary: '' has been replaced by 'FALSE'
d18O (SP05CRBR01A): paleoData_primaryAgeColumn: '' has been replaced by 'FALSE'

d18O (SP05CRBR01A): interpretation1_seasonality: 'annual' has been replaced by 'Annual'
d18O (SP05CRBR01A): interpretation1_variable: 'P' has been replaced by 'precipitation'
d18O (SP05CRBR01A): interpretation2_seasonality: 'DJF' has been replaced by 'Dec-Feb'
d18O (SP05CRBR01A): interpretation2_variable: 'P_isotope' has been replaced by 'precipitationIsotope'

d18O (SP05CRBR01A): interpretation1_seasonality: 'annual' has been replaced by 'Annual'
d18O (SP05CRBR01A): interpretation1_variable: 'P' has been replaced by 'precipitation'
d18O (SP05CRBR01A): interpretation2_seasonality: 'DJF' has been replaced by 'Dec-Feb'
d18O (SP05CRBR01A): interpretation2_variable: 'P_isotope' has been replaced by 'precipitationIsotope'

year (LPD9b7b0312): paleoData_units: 'AD' has been replaced by 'yr AD'
year (LPD9b7b0312): paleoData_longName: '' has been replaced by 'AD'
depth (MAT7d1ee4077b): paleoData_longName: '' has been replaced by 'AD'
d18O (SP05CRBR01A): paleoData_longName: '' has been replaced by 'AD'

d18O (SP05CRBR01A): interpretation4_scope: '' has been replaced by 'isotope'

Cruz, F. W., Burns, S. J., Karmann, I., Sharp, W. D., Vuille, M., Cardoso, A. O., Ferrari, J. A., Silva Dias, P. L. and Viana, O.: Insolation-driven changes in atmospheric circulation over the past 116,000 years in subtropical Brazil, Nature, 434(7029), 63–66, doi:10.1038/nature03365, 2005.

The d13C profile shows no correlation with d18O in any of the section profiles

white, densely crystalline low-Mg calcite,  showing columnar-shape crystals in thin section

the relationship between temperature and isotopic composition results from a mixing of different types of precipitation that varies with temperature.