d18O (LS11BIPU01a): interpretation1_seasonality: 'December - March (monsoon season)' has been replaced by 'Dec-Mar'
d18O (LS11BIPU01a): interpretation1_variable: 'd18O precipitation' has been replaced by 'precipitationIsotope'
d18O (LS11BIPU01a): interpretation2_variable: 'P_isotope' has been replaced by 'precipitationIsotope'
d18O (LS11BIPU01a): interpretation3_variable: 'T_lake' has been replaced by 'temperature'

d18O (LS11BIPU01a): interpretation1_seasonality: 'December - March (monsoon season)' has been replaced by 'Dec-Mar'
d18O (LS11BIPU01a): interpretation1_variable: 'd18O precipitation' has been replaced by 'precipitationIsotope'
d18O (LS11BIPU01a): interpretation2_variable: 'P_isotope' has been replaced by 'precipitationIsotope'
d18O (LS11BIPU01a): interpretation3_variable: 'T_lake' has been replaced by 'temperature'

d18O (LS11BIPU01a): paleoData_longName: '' has been replaced by 'AD'
depth (MATb2ca379d07): paleoData_longName: '' has been replaced by 'AD'
year (MATdcb959bd61): paleoData_units: 'AD' has been replaced by 'yr AD'
year (MATdcb959bd61): paleoData_longName: '' has been replaced by 'AD'

Bird, Broxton W. , Abbott, Mark B. , Rodbell, Donald T. , Vuille, Mathias

Bird, B. W., Abbott, M. B., Rodbell, D. T. and Vuille, M.: Holocene tropical South American hydroclimate revealed from a decadally resolved lake sediment δ18O record, Earth and Planetary Science Letters, 310(3-4), 192–202, doi:10.1016/j.epsl.2011.08.040, 2011.

Holocene tropical South American hydroclimate revealed from a decadally resolved lake sediment ?18O record

ASE200, HP 6890 GC, Finnigan MAT Delta+ XL mass spectrometer

Complete replacement of the winter Indian monsoon source with a southeasterly/northwesterly source would deplete ?Dwax by about 35?, which is the amplitude of change observed between the mega- droughts interval and the Holocene. / "Relatively depleted ?Dwax values at Lake Malawi from ~3.1 ka to present likely reflect the modern hydrological controls on ?Dprecip, with source changes constituting a more limited role than the amount effect and overall intensity of the hydrological cycle. "