d18O (CO13HENG01A): interpretation1_variable: 'temperature and salinity' has been replaced by 'temperature'
d18O (CO13HENG01A): interpretation2_variable: 'd18O_seawater' has been replaced by 'seawaterIsotope'
d18O (CO13HENG01A): interpretation3_variable: 'T_water' has been replaced by 'temperature'
d18O (CO13HENG02A): interpretation1_variable: 'temperature and salinity' has been replaced by 'temperature'
d18O (CO13HENG02A): interpretation2_variable: 'd18O_seawater' has been replaced by 'seawaterIsotope'
d18O (CO13HENG02A): interpretation3_variable: 'T_water' has been replaced by 'temperature'
d18O (CO13HENG03A): interpretation1_variable: 'temperature and salinity' has been replaced by 'temperature'
d18O (CO13HENG03A): interpretation2_variable: 'd18O_seawater' has been replaced by 'seawaterIsotope'
d18O (CO13HENG03A): interpretation3_variable: 'T_water' has been replaced by 'temperature'

d18O (CO13HENG01A): paleoData_longName: '' has been replaced by 'AD'
d18O (CO13HENG02A): paleoData_longName: '' has been replaced by 'AD'
d18O (CO13HENG03A): paleoData_longName: '' has been replaced by 'AD'
year (MAT37c78e7b7c): paleoData_units: 'AD' has been replaced by 'yr AD'
year (MAT37c78e7b7c): paleoData_longName: '' has been replaced by 'AD'
year (MAT6f97b4c7b7): paleoData_units: 'AD' has been replaced by 'yr AD'
year (MAT6f97b4c7b7): paleoData_longName: '' has been replaced by 'AD'
year (MAT7e393cba74): paleoData_units: 'AD' has been replaced by 'yr AD'
year (MAT7e393cba74): paleoData_longName: '' has been replaced by 'AD'

Hereid, K. A., Quinn, T. M., Taylor, F. W., Shen, C.-C., Lawrence Edwards, R. and Cheng, H.: Coral record of reduced El Nino activity in the early 15th to middle 17th centuries, Geology, 41(1), 51–54, doi:10.1130/g33510.1, 2012.

Sr/Ca data to monthly SST from the 2i¿½ i¿½ 2i¿½ grid square centered on 4i¿½N, 172i¿½E from the extended reconstructed SST version 3b (ERSSTv3b) data product [Smith et al., 2008; ttp://www.esrl.noaa.gov/psd] [?] Annual Sr/Ca maxima were tied to the coolest points in the SST record using Analyseries [Paillard et al., 1996]. The resulting spacing of Sr/Ca data remained relatively constant throughout the record, and the chronology was verified against growth band counts from the X-radiograph. After converting depth to time in Analyseries, Sr/Ca were interpolated to six equally spaced samples per year using ARAND time series analysis software [Howell, 2001], corresponding  to bimonthly resolution for the length of the record.