Kilbourne 2004 has two paper that report on the same modern data

Malo Channel, Espiritu Santo Island - Stable Isotope and Elemental Data

d18O (Ocean2kHR_174): interpretation4_scope: '' has been replaced by 'isotope'
Sr/Ca (Ocean2kHR_175): interpretation3_scope: '' has been replaced by 'isotope'
Sr/Ca (Ocean2kHR_175): interpretation4_scope: '' has been replaced by 'isotope'
d13C (Ocean2kHR_176): interpretation2_scope: '' has been replaced by 'isotope'
d13C (Ocean2kHR_176): interpretation3_scope: '' has been replaced by 'isotope'

Column 'addR1WivGxDykQzAA6W0', with variable name 'yearEnsemble', was added to the dataset
Column 'addR2QZZLzDTu94FNCya', with variable name 'yearEnsemble', was added to the dataset

Kilbourne, K. H., Quinn, T. M., Taylor, F. W., Delcroix, T. and Gouriou, Y.: El Nino-Southern Oscillation-related salinity variations recorded in the skeletal geochemistry of aPoritescoral from Espiritu Santo, Vanuatu, Paleoceanography, 19(4), n/a–n/a, doi:10.1029/2004pa001033, 2004.

El Nino-Southern Oscillation-related salinity variations recorded in the skeletal geochemistry of a Porites coral from Espiritu Santo, Vanuatu

Malo Channel, Espiritu Santo Island, Vanuatu

used in Tierney et al, as a composite with HR_156; the original records are provided here rather than composites

Micromass Optima gas source mass spectrometer

0.038 per mil over 468 standards (NBS19)

0.04 per mil for d18O based on analyses of 657 (13.5%) rep- licate samples.

tied the annual minima in d18O to February (on average the warmest month) and maximum  d18O to August/September (on average the coolest months). And comparing the d18O  records to Nino3.4 (central equatorial Pacific region bounded by 5i¿½S?5i¿½N and 120i¿½?170i¿½W) SST anomaly (SSTa)

tied the annual minima in d18O to February (on average the warmest month) and maximum  d18O to August/September (on average the coolest months). And comparing the d18O  records to Nino3.4 (central equatorial Pacific region bounded by 5�S?5�N and 120�?170�W) SST anomaly (SSTa)