year (MATe843de3f7d): interpretation3_scope: '' has been replaced by 'climate'
depth (MATff68a2142b): interpretation3_scope: '' has been replaced by 'climate'

d18O (LS02BEPY): paleoData_isPrimary: '' has been replaced by 'FALSE'
d18O (LS02BEPY): paleoData_primaryAgeColumn: '' has been replaced by 'FALSE'
year (MATe843de3f7d): paleoData_isPrimary: '' has been replaced by 'TRUE'
year (MATe843de3f7d): paleoData_primaryAgeColumn: '' has been replaced by 'TRUE'
depth (MATff68a2142b): paleoData_isPrimary: '' has been replaced by 'FALSE'
depth (MATff68a2142b): paleoData_primaryAgeColumn: '' has been replaced by 'FALSE'

d18O (LS02BEPY): interpretation1_variable: 'lake overflow' has been replaced by 'hydrologicBalance'
d18O (LS02BEPY): interpretation2_variable: 'P_E' has been replaced by 'effectivePrecipitation'

d18O (LS02BEPY): interpretation1_variable: 'lake overflow' has been replaced by 'hydrologicBalance'
d18O (LS02BEPY): interpretation2_variable: 'P_E' has been replaced by 'effectivePrecipitation'

d18O (LS02BEPY): paleoData_longName: '' has been replaced by 'AD'
year (MATe843de3f7d): paleoData_units: 'AD' has been replaced by 'yr AD'
year (MATe843de3f7d): paleoData_longName: '' has been replaced by 'AD'
depth (MATff68a2142b): paleoData_longName: '' has been replaced by 'AD'

d18O (LS02BEPY): interpretation3_scope: '' has been replaced by 'isotope'
d18O (LS02BEPY): interpretation4_scope: '' has been replaced by 'isotope'

Benson, Larry , Kashgarian, Michaele , Rye, Robert , Lund, Steve , Paillet, Fred , Smoot, Joseph , Kester, Cynthia , Mensing, Scott , Meko, Dave , Lindstri¿½m, Susan

Benson, L., Kashgarian, M., Rye, R., Lund, S., Paillet, F., Smoot, J., Kester, C., Mensing, S., Meko, D. and Lindstroem, S.: Holocene multidecadal and multicentennial droughts affecting Northern California and Nevada, Quaternary Science Reviews, 21(4-6), 659–682, doi:10.1016/s0277-3791(01)00048-8, 2002.

Holocene multidecadal and multicentennial droughts affecting Northern California and Nevada

stronger zonal atmospheric circulation during the early Holocene remains the most plausable mechanism to explain the strong shifts in the d18O-MAT relation. Temperature equation applied to surface sediment yields essentially modern July temperatures|lake water d18O corresponds with pollen-inferred temperatures.