d18O (LS15ABSH01a): interpretation1_variable: 'Evaporation' has been replaced by 'evaporation'
d18O (LS15ABSH01a): interpretation2_variable: 'I_E' has been replaced by 'hydrologicBalance'
d18O (LS15ABSH01a): interpretation3_variable: 'T_water' has been replaced by 'temperature'

d18O (LS15ABSH01a): interpretation1_variable: 'Evaporation' has been replaced by 'evaporation'
d18O (LS15ABSH01a): interpretation2_variable: 'I_E' has been replaced by 'hydrologicBalance'
d18O (LS15ABSH01a): interpretation3_variable: 'T_water' has been replaced by 'temperature'

d18O (LS15ABSH01a): paleoData_longName: '' has been replaced by 'AD'
depth (MAT6eacdefa6e): paleoData_longName: '' has been replaced by 'AD'
year (MAT91072c2c75): paleoData_units: 'AD' has been replaced by 'yr AD'
year (MAT91072c2c75): paleoData_longName: '' has been replaced by 'AD'

Abu-Zied, R. H. and Bantan, R. A.: Palaeoenvironment, palaeoclimate and sea-level changes in the Shuaiba Lagoon during the late Holocene (last 3.6 ka), eastern Red Sea coast, Saudi Arabia, The Holocene, 25(8), 1301–1312, doi:10.1177/0959683615584204, 2015.

Palaeoenvironment, palaeoclimate and sea-level changes in the Shuaiba Lagoon during the late Holocene (last 3.6 ka), eastern Red Sea coast, Saudi Arabia

"We used a Thermo Scientificdegrees Trace gas chromato graph equipped with an Rxi5ms column (30 m degrees 0.25 mm, film thickness 1 permilm) and a programmable temperature va porizing (PTV) injector operated in solvent split mode with an evaporation temperature of 60 permil C. The GC was con nected via a GC Isolink with pyrolysis/combustion furnace (at 1400/1000 permilC) and a Conflo IV interface to a DeltaVPlus isotope ratio mass spectrometer. The H+3 factor (Sessions et al., 2001) was determined daily to test measurement linearity of the system and accounted for 5.8 ppm mvpermil1 on average. Reference peaks of H2 bracket nalkanoic acid peaks during the course of a GCIRMS run; two of these peaks were used for the standardization of the isotopic analysis, while the remainders were treated as unknowns to assess pre cision. Except for the case of coelution, precision of these replicates was better than 0.6 permil."