d18O (CO99LICL01A): paleoData_longName: '' has been replaced by 'AD'
d18O (CO99LICL02A): paleoData_longName: '' has been replaced by 'AD'
d18O (CO99LICL03A): paleoData_longName: '' has been replaced by 'AD'
year (MAT58797073a9): paleoData_units: 'AD' has been replaced by 'yr AD'
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year (MATd01867a5fa): paleoData_units: 'AD' has been replaced by 'yr AD'
year (MATd01867a5fa): paleoData_longName: '' has been replaced by 'AD'
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Linsley B. K., L. Ren, R. B. Dunbar, S. S. Howe

Linsley, B. K., Messier, R. G. and Dunbar, R. B.: Assessing between-colony oxygen isotope variability in the coral Porites lobata at Clipperton Atoll, Coral Reefs, 18(1), 13–27, doi:10.1007/s003380050148, 1999.

El Ni�o Southern Oscillation (ENSO) and decadal-scale climate variability at 10�N in the eastern Pacific from 1893 to 1994: A coral-based reconstruction from Clipperton Atoll

NOTED from downloading Swart1999 data, it is very different from Swart1996 even though the paper says it was the same coral, core, and data, not sure why, will have to contact Peter Swart to ask and look at Healy thesis. This coral species is Solenastrea bournoni, one not used in coral climate reconstructions, and it is located in a complex system of Florida Bay where waters from the Everglades enter the ocean and ther eare high rates of evaporation. The d18O system is not additive but subtractive for SSS and SST. Swart 1999 revisited this coral colony and they collect a new core from the same colony. Hudson 1989 gives a map with the coral location, which is 24degrees 55 minutes, and ~80 degrees and between 40 and 50 minutes, about 44 minutes nu my eye. Swart 1999 NOAA has different corrdinates for this coral 25 0N, 80 36W, Looking at Google earth and Hudsons map, the Swart 1999 corrdinates incorrect, they should be 24 degrees 55 minutes N, and ~80 degrees, 43.5 minutes W