Updated lipdverse database entry with a changed file.

Column 'addRc5MmtHacWZXGR92G', with variable name 'yearEnsemble', was added to the dataset
Column 'addRhJ6b7ya7P4uWd33Y', with variable name 'yearEnsemble', was added to the dataset

Cole, J. E.: Tropical Pacific Forcing of Decadal SST Variability in the Western Indian Ocean over the Past Two Centuries, Science, 287(5453), 617–619, doi:10.1126/science.287.5453.617, 2000.

American Association for the Advancement of Science (AAAS)

Tropical Pacific Forcing of Decadal SST Variability in the Western Indian Ocean over the Past Two Centuries

Auer, Gerald , Piller, Werner E. , Reuter, Markus , Harzhauser, Mathias

Auer, G., Piller, W. E., Reuter, M. and Harzhauser, M.: Correlating carbon and oxygen isotope events in early to middle Miocene shallow marine carbonates in the Mediterranean region using orbitally tuned chemostratigraphy and lithostratigraphy, Paleoceanography, 30(4), 332–352, doi:10.1002/2014pa002716, 2015.

X-radiographs were assessed from the skeleton slices to expose density banding. Chronologies were achieved by counting the well-developed density couplets. BDA 210 revealed continuous growth between 1825 and 1993, whereas BDA 215 and BDA 221 contain hiatuses. The bases of the colonies, which were separated from the upper living parts by algal growth, were 14C dated by AMS in the Leibnitz Laboratory in Kiel. Precision of Dating came to  30 years. The stratigraphy obtained from 14C dating was confirmed by the strong correspondence of the present proxy time series with a continuous 800-year coral skeletal chronology from Bermuda, presented by Patzold et al. (1998; see Fig. 3c).

chronological and radiocarbon dating 30 years

Finnigan MAT 251 micro-mass spectrometer with an automatic carbonate preparation device (Kiel Device).

; climateInterpretation_seasonality changed - was originally -12 -11 -10 -9 -8 1 2 3 4 5 6 7; archiveType changed - was originally Coral (CO)

d18O (3 yr mean) calibration to SST (3 yr mean). SST is inferred from air temperature