Lumin (GBRCD.JU08KES02.Lumin): interpretation1_scope: '' has been replaced by 'climate'

Individual record that makes up part of KI Master record. Core collection depth differs between Jupiter et al. (2008) and Jupiter (2006).

Luminescence age model from minimum density matched to minimum winter SSTs (first week of August based on IGOSS weekly SST November 1981 to December 2004). Trace elements time series created by matching SrCa maxima & minima with IGOSS weekly SST records 1981 to 2004, and the average week of SST maxima and minima used for pre-1981 data. Data interpolated to 52 points per year.

Laser 50 x 500 μm rectangle on the coral surface. 390 λ excitation/490 λ emission was measured at 0.25 mm increments. No analytical precision data available.

ArF excimer laser (193 nm wavelength) attached to a modified VG Elemental PQ2+ or Varian 820

notes: 'Individual record that makes up part of KI Master record. Lumin data is 1976-2003; no lumin data available for part of 1987-1988. BaCa data is 1968-2002.' has been replaced by 'Individual record that makes up part of KI Master record. Lumin data is 1976-2003; no Lumin data available for part of 1987-1988. BaCa data is 1968-2002.'

year (GBRCD.JU08KES03.year): paleoData_isPrimary: 'FALSE' has been replaced by 'TRUE'

notes: 'Individual record that makes up part of KI Master record. No luminescence data available for part of 1987-1988. BaCa data from 1968-2002.' has been replaced by 'Individual record that makes up part of KI Master record. Lumin data is 1976-2003; no lumin data available for part of 1987-1988. BaCa data is 1968-2002.'
originalDataUrl: '' has been replaced by 'https://doi.org/10.25921/2syx-b667'

geo_notes: 'Not applicable' has been replaced by 'Collection depth is "N/A".'

BaCa (GBRCD.JU08KES03.BaCa): paleoData_description: 'Barium/Calcium 
 For laser ablation datasets this is a measure of the total Ba/Ca using the count intensities of the Ba137 isotope.' has been replaced by 'Barium/Calcium. 
 For laser ablation datasets this is a measure of the total Ba/Ca using the count intensities of the Ba137 isotope.'