year (MATb8b3cd2a90): paleoData_isPrimary: '' has been replaced by 'TRUE'
year (MATb8b3cd2a90): paleoData_primaryAgeColumn: '' has been replaced by 'TRUE'
d18O (Ocean2kHR_011): paleoData_isPrimary: '' has been replaced by 'FALSE'
d18O (Ocean2kHR_011): paleoData_primaryAgeColumn: '' has been replaced by 'FALSE'

d18O (Ocean2kHR_011): interpretation1_seasonality: 'not applicable (subannually resolved)' has been replaced by 'subannual'
d18O (Ocean2kHR_011): interpretation1_variable: 'temperature and salinity' has been replaced by 'temperature'
d18O (Ocean2kHR_011): interpretation2_variable: 'T_water' has been replaced by 'temperature'
d18O (Ocean2kHR_011): interpretation3_seasonality: 'monsoon season' has been replaced by 'Wet Season'
d18O (Ocean2kHR_011): interpretation3_variable: 'd18O_seawater' has been replaced by 'seawaterIsotope'

d18O (Ocean2kHR_011): interpretation1_seasonality: 'not applicable (subannually resolved)' has been replaced by 'subannual'
d18O (Ocean2kHR_011): interpretation1_variable: 'temperature and salinity' has been replaced by 'temperature'
d18O (Ocean2kHR_011): interpretation2_variable: 'T_water' has been replaced by 'temperature'
d18O (Ocean2kHR_011): interpretation3_seasonality: 'monsoon season' has been replaced by 'Wet Season'
d18O (Ocean2kHR_011): interpretation3_variable: 'd18O_seawater' has been replaced by 'seawaterIsotope'

year (MATb8b3cd2a90): paleoData_units: 'AD' has been replaced by 'yr AD'
year (MATb8b3cd2a90): paleoData_longName: '' has been replaced by 'AD'
d18O (Ocean2kHR_011): paleoData_longName: '' has been replaced by 'AD'

Charles, C.D., D.E.Hunter, and R.G.Fairbanks.

Charles, C. D.: Interaction Between the ENSO and the Asian Monsoon in a Coral Record of Tropical Climate, Science, 277(5328), 925–928, doi:10.1126/science.277.5328.925, 1997.

Interaction Between the ENSO and the Asian Monsoon in a Coral Record of Tropical Climate

Beau Vallon Bay, Mahe Island, Republic of the Seychelles

The chronology is then established by associating each maximum and minimum in d18O with each minimum (August) maximum (March) in the SST record (Figure2), assuming a constant linear extension rate between these 2 months