d13C (Ocean2kHR_111): interpretation1_scope: '' has been replaced by 'climate'

Bunaken Island, Indonesia Coral Oxygen Isotope Data

Charles, Christopher D.;Cobb, Kim;Moore, Michael D.;Fairbanks, Richard G.

Monsoon–tropical ocean interaction in a network of coral records spanning the 20th century

Individual coral growth records. Composites used in database instead (following approach of original publication)

calcification rate measurements from individual samples

composite of individual samples, after standardization

West Australian coral growth records, 1900-2010

calcification (LPD1079b4bb): interpretation1_scope: '' has been replaced by 'climate'
calcification (LPD6c1fc0ed): interpretation1_scope: '' has been replaced by 'climate'
calcification (LPD81e7ab49): interpretation1_scope: '' has been replaced by 'climate'
calcification (LPDae761fd0): interpretation1_scope: '' has been replaced by 'climate'

Cooper, T. F.;O'Leary, R. A.;Lough, J. M.

Growth of Western Australian Corals in the Anthropocene

HVM, BM, 20/4/2016 Atlantic1578Kim2007_GeoB6007-2 Revised age model for GeoB6007-2 from Morley et al., (2011) was applied to GeoB6007-2 alkenone data from Kim et al., (2007).

MUE1998: Muller et al. 1998 sediment core top based calibration, n=370, R2=0.958); paleoData_units changed - was originally deg C; climateInterpretation_seasonality changed - was originally Annual

These are the original, not quality controlled data. O2kLR recommends only using the Quality controlled data.Dataset does not contain updated age constraints and does not combine data from nearby cores (age model is combined into one composite)

Kim, Jung-Hyun;Meggers, Helge;Rimbu, Norel;Lohmann, Gerrit;Freudenthal, Tim;Müller, Peter J.;Schneider, Ralph R.

Impacts of the North Atlantic gyre circulation on Holocene climate off northwest Africa

HVM, BM, 20/4/2016 Atlantic0487McGregor2007__GeoB6008-1, GeoB6008-2_ alkenone(Prahl et al., 1988)

PRA1988: E. huxleyi culture-based calibration. No RMSE is reported in the original publication, so a RMSE was calculated by taking a regression off of the five culture T-UK'37 datapoints reported in the publication.