Multiprep carbonate inlet system and the resulting CO  gas was analyzed with a Micromass Optima triple-collecting mass spectro- meter

The d18O  were tuned to the SST record by assigning the lowest (highest) d18O values of each year to the highest (lowest) SST. Age assignments were then linearly interpolated between these two annual anchor points using the Arand software package (P. Howell, personal commu- nication, 2002). A continuous monthly SST data set is available only as far back as 1970, so for age assignments before 1970 the lowest (highest) d18O and Sr/Ca values were assigned to March (August), March and August being the average times of highest and lowest SST, respectively, between 1970 and 1997

Composite of CO04BAFI01A and CO04BAFI02A

d18O (CO04BAFI00A): interpretation4_scope: '' has been replaced by 'isotope'
d18O (CO04BAFI01A): interpretation4_scope: '' has been replaced by 'isotope'
d18O (CO04BAFI02A): interpretation4_scope: '' has been replaced by 'isotope'

Column 'addRBaN96SJ9mYgsLt5p', with variable name 'yearEnsemble', was added to the dataset
Column 'addRwW2z1fFcIrAe1L9D', with variable name 'yearEnsemble', was added to the dataset

Bagnato, S., B.K. Linsley, S.S. Howe, G.M. Wellington, J. Salinger

Bagnato, S., Linsley, B. K., Howe, S. S., Wellington, G. M. and Salinger, J.: Evaluating the use of the massive coralDiploastrea helioporafor paleoclimate reconstruction, Paleoceanography, 19(1), n/a–n/a, doi:10.1029/2003pa000935, 2004.

automated carbonate device (Micromass Multiprep) attached to a mass spectrometer (Micromass Optima).

Age determination was carried out by matching the oxygen isotope record mainly reflects the seasonal SST cycle of 1a€“2 C at this location and indicates that the core provides a continuous record from 1957 to 1999.  Positive anomalies agreed with the timing of known El Nino events (when SSTs are cooler in this region)

oxygen isotope record mainly reflects the seasonal SST cycle of 1a€“2 C at this location

Age determination was carried out by matching the oxygen isotope record mainly reflects the seasonal SST cycle of 1–2 C at this location and indicates that the core provides a continuous record from 1957 to 1999.  Positive anomalies agreed with the timing of known El Nino events (when SSTs are cooler in this region)