d18O (CO14CATI01A): interpretation1_variable: 'temperature and salinity' has been replaced by 'temperature'
d18O (CO14CATI01A): interpretation2_variable: 'T_water' has been replaced by 'temperature'
d18O (CO14CATI01A): interpretation3_variable: 'd18O_seawater' has been replaced by 'seawaterIsotope'
d18O (CO14CATI01B): interpretation1_variable: 'S' has been replaced by 'salinity'
d18O (CO14CATI01B): interpretation2_variable: 'd18O_seawater' has been replaced by 'seawaterIsotope'

d18O (CO14CATI01A): interpretation1_variable: 'temperature and salinity' has been replaced by 'temperature'
d18O (CO14CATI01A): interpretation2_variable: 'T_water' has been replaced by 'temperature'
d18O (CO14CATI01A): interpretation3_variable: 'd18O_seawater' has been replaced by 'seawaterIsotope'
d18O (CO14CATI01B): interpretation1_variable: 'S' has been replaced by 'salinity'
d18O (CO14CATI01B): interpretation2_variable: 'd18O_seawater' has been replaced by 'seawaterIsotope'

d18O (CO14CATI01A): paleoData_longName: '' has been replaced by 'AD'
d18O (CO14CATI01B): paleoData_longName: '' has been replaced by 'AD'
year (MAT707fd6cec5): paleoData_units: 'AD' has been replaced by 'yr AD'
year (MAT707fd6cec5): paleoData_longName: '' has been replaced by 'AD'
depth (MATa1d7413232): paleoData_longName: '' has been replaced by 'AD'

Cahyarini, S. Y., Pfeiffer, M., Nurhati, I. S., Aldrian, E., Dullo, W.-C. and Hetzinger, S.: Twentieth century sea surface temperature and salinity variations at Timor inferred from paired coral δ18O and Sr/Ca measurements, Journal of Geophysical Research: Oceans, 119(7), 4593–4604, doi:10.1002/2013jc009594, 2014.

Twentieth century sea surface temperature and salinity variations at Timor inferred from paired coral δ18O and Sr/Ca measurements

Cahyarini, S.Y.; Pfeiffer, M.; Nurhati, I.S.; Aldrian, E.; Dullo, W.-C.; Hetzinger, S.

We developed age models by visually comparing coral banding with seasonal d18O and d13C cycles. Dark regions of the coral X-ray positives corresponded with minima in d18O and d13C. We then associated local d18O and d13C minima with March, based on the mean Palau SSS and SST climatology. We converted samples to monthly resolution by performing linear interpolations between chronological anchor points.