Quinn, T. M., Taylor, F. W., Crowley, T. J. and Link, S. M.: Evaluation of sampling resolution in coral stable isotope records: A case study using records from New Caledonia and Tarawa, Paleoceanography, 11(5), 529–542, doi:10.1029/96pa01859, 1996.

Finningan-MAT 251 mass spectrometer attached to an automated carousel

Siderastrea spp.,  the influence of salinity overwhelms the temperautre influence on the oxygen isotopic composition of corals

d18O (CO98SWPR01A): paleoData_isPrimary: '' has been replaced by 'FALSE'
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d18O (CO98SWPR01A): interpretation1_seasonality: 'annual' has been replaced by 'Annual'
d18O (CO98SWPR01A): interpretation1_variable: 'd18O_seawater' has been replaced by 'seawaterIsotope'

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Swart P. K., K. S. White, D. Enfield, R. E. Dodge, P. Milne

Swart, P. K., White, K. S., Enfield, D., Dodge, R. E. and Milne, P.: Stable oxygen isotopic composition of corals from the Gulf of Guinea as indicators of periods of extreme precipitation conditions in the sub-Sahara, Journal of Geophysical Research: Oceans, 103(C12), 27885–27891, doi:10.1029/98jc02404, 1998.

Oxygen isotope records in banded corals( i¿½!80) are mainly controlled by water composition (i.e., seawater salinity) and sea surface temperature (SST) at the time of accretion

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