spliced record, Mg/Ca data available for box core, but authors did not calculate d18Osw

core (LPDf8072f4er): interpretation1_scope: '' has been replaced by 'isotope'
core (LPDf8072f4er): interpretation2_scope: '' has been replaced by 'isotope'
core (LPDf8072f4er): interpretation3_scope: '' has been replaced by 'isotope'

year (MAT65b2f38aca): The paleoData_values have changed

Column 'addRb8l1wX0n2VxjCG9g', with variable name 'age.rangeLow', was added to the dataset
Column 'addROfuPmngrdYmavCiE', with variable name 'ageEnsemble', was added to the dataset
Column 'addRq8NqT3h3n0nWNEuY', with variable name 'depth', was added to the dataset
Column 'addRqm79lrjPRHQGmIov', with variable name 'age', was added to the dataset
Column 'addRViezZ76tFTayUb75', with variable name 'age.rangeHigh', was added to the dataset
Column 'addRwlAGIFkt6MV26IMF', with variable name 'depth', was added to the dataset
Column 'MS04BLCB-chron-NA1', with variable name 'depth', was added to the dataset
Column 'MS04BLCB-chron-NA2', with variable name 'age.rangeLow', was added to the dataset
Column 'MS04BLCB-chron-NA3', with variable name 'age.rangeHigh', was added to the dataset
Column 'MS04BLCB-chron-NA4', with variable name 'age', was added to the dataset

age (chron15): chronData_units: 'yr BP' has been replaced by 'BP'

Black, D. E., Thunell, R. C., Kaplan, A., Peterson, L. C. and Tappa, E. J.: A 2000-year record of Caribbean and tropical North Atlantic hydrographic variability, Paleoceanography, 19(2), n/a–n/a, doi:10.1029/2003pa000982, 2004.

Black, D. E.: Eight Centuries of North Atlantic Ocean Atmosphere Variability, Science, 286(5445), 1709–1713, doi:10.1126/science.286.5445.1709, 1999.

N. pachyderma: 106-1000? not mentioned in paper, but from NOAA data sheet

A compilation of the _18O of modern Foraminifera, water temperature and salinity indicates that the isotopic composition of North Iceland Shelf Foraminifera is controlled primarily by temperature (Smith, 2001; Smith et al., in review). For example, Smith et al. (in review) found that a strong correlation (r21/40.74) exists between temperatures in the upper 50m of the water column and _18O of the planktonic species N. pachyderma (s). It is not surprising that foraminiferal _18O in this region is controlled primarily by temperature because modern hydrographic changes in North Iceland Shelf waters are dominated by temperature changes, with salinity playing a minor role (Smith, 2001; Smith et al., in review). The effects of temperature versus salinity on the _18O of North Iceland Shelf Foraminifera is discussed at length in a companion paper by Smith et al. (in review), which examines the same _18O records presented in this study.