Methodology in Smittenberg and Sachs, 2007, Journal of Chromatography, 1169:70-76

d2H (LPD292174f8): interpretation2_scope: '' has been replaced by 'isotope'
d2H (LPD292174f8): interpretation3_scope: '' has been replaced by 'isotope'

year (MAT3e773ec33c): The paleoData_values have changed

Column 'addRdY8lwp7leV85Y6oR', with variable name 'ageEnsemble', was added to the dataset
Column 'addREMtuKnwhKeTMdaFq', with variable name 'age.rangeLow', was added to the dataset
Column 'addRsfWzkguNJJbwD7Ce', with variable name 'age.rangeHigh', was added to the dataset
Column 'addRV0p7GgrZtjsVCfF8', with variable name 'depth', was added to the dataset
Column 'addRZH1Gxl8gA9uDeH2i', with variable name 'age', was added to the dataset
Column 'addRzlhAa1QJmTSG1QVg', with variable name 'depth', was added to the dataset
Column 'LS09SASP-chron-NA1', with variable name 'depth', was added to the dataset
Column 'LS09SASP-chron-NA2', with variable name 'age.rangeLow', was added to the dataset
Column 'LS09SASP-chron-NA3', with variable name 'age.rangeHigh', was added to the dataset
Column 'LS09SASP-chron-NA4', with variable name 'age', was added to the dataset

Costech Zero Blank Auto Sampler-Thermo/Finnigan TC/EA-Thermo Delta V Plus IRMS via Conflo III combustion interface

Sachs and Sachse 2008, GCA , 72:793-806. Conclusions of the paper are about moisture balance (P-E) in the tropical Pacific.

Sachs and Sachse 2008, GCA , 72:793-806; "dD values of lipids...were closely correlated with salinity, owing to a decrease in D/H fractionation between lipids and source water as salinity increases. TLE dD values can therefore be used as a salinity indicator in hypersaline evnrionments such as those at Christmas Island".

ageUncertainty (85% atmosphere, 15% marine model)

the only uncertainty information I have been able to find is as follows "The average standard deviation (sigma) of all measured samples was 3.8?" from Sachse and Sachs (2008) GCA, 72:793-806 (this paper was referenced in the method section of the main publication)