d18O (LS14YAHA01a): interpretation1_variable: 'P/E' has been replaced by 'effectivePrecipitation'
d18O (LS14YAHA01a): interpretation2_variable: 'P_E' has been replaced by 'effectivePrecipitation'
d18O (LS14YAHA02a): interpretation1_variable: 'M' has been replaced by 'effectivePrecipitation'
d18O (LS14YAHA02a): interpretation2_variable: 'P_E' has been replaced by 'effectivePrecipitation'

d18O (LS14YAHA01a): interpretation1_variable: 'P/E' has been replaced by 'effectivePrecipitation'
d18O (LS14YAHA01a): interpretation2_variable: 'P_E' has been replaced by 'effectivePrecipitation'
d18O (LS14YAHA02a): interpretation1_variable: 'M' has been replaced by 'effectivePrecipitation'
d18O (LS14YAHA02a): interpretation2_variable: 'P_E' has been replaced by 'effectivePrecipitation'

d18O (LS14YAHA01a): paleoData_longName: '' has been replaced by 'AD'
d18O (LS14YAHA02a): paleoData_longName: '' has been replaced by 'AD'
depth (LS14YAHA02adepth): paleoData_longName: '' has been replaced by 'AD'
year (LS14YAHA02ayear): paleoData_units: 'AD' has been replaced by 'yr AD'
year (LS14YAHA02ayear): paleoData_longName: '' has been replaced by 'AD'
depth (MAT713c9c0063): paleoData_longName: '' has been replaced by 'AD'
year (MATc4d3657706): paleoData_units: 'AD' has been replaced by 'yr AD'
year (MATc4d3657706): paleoData_longName: '' has been replaced by 'AD'

Yan, D. and Wuennemann, B.: Late Quaternary water depth changes in Hala Lake, northeastern Tibetan Plateau, derived from ostracod assemblages and sediment properties in multiple sediment records, Quaternary Science Reviews, 95, 95–114, doi:10.1016/j.quascirev.2014.04.030, 2014.

Late Quaternary water depth changes in Hala Lake, northeastern Tibetan Plateau, derived from ostracod assemblages and sediment properties in multiple sediment records

El Junco Lake is presumed to have remained fresh and therefore its lake-water dD value is dictated solely by the isotopic composition of precipitation, and the relative rates of evaporation and precipitation. More negative lake-water dD values reflect a greater rate of rainfall relative to evaporation during wet periods. Conclusions of the paper are about moisture balance (P-E) in the tropical Pacific.