Column 'RkAJDUldOBROKb3nx', with variable name 'reject', was added to the dataset
Column 'LS11KOMA-chron-NA1', with variable name 'reject', was removed from the dataset

d2H (LS11KOMA01A): interpretation1_seasonality: 'DJF' has been replaced by 'Dec-Feb'
d2H (LS11KOMA01A): interpretation1_variable: 'Source and intensity' has been replaced by 'precipitationIsotope'
d2H (LS11KOMA01A): interpretation2_seasonality: 'annual' has been replaced by 'Annual'
d2H (LS11KOMA01A): interpretation2_variable: 'P_isotope' has been replaced by 'precipitationIsotope'
d2H (LS11KOMA01A): interpretation3_seasonality: 'annual' has been replaced by 'Annual'
d2H (LS11KOMA01A): interpretation3_variable: 'P_amount' has been replaced by 'precipitation'

d2H (LS11KOMA01A): paleoData_longName: '' has been replaced by 'AD'
year (MAT15c72e1504): paleoData_units: 'AD' has been replaced by 'yr AD'
year (MAT15c72e1504): paleoData_longName: '' has been replaced by 'AD'
depth (MAT3c131c959e): paleoData_longName: '' has been replaced by 'AD'

Konecky, Bronwen L. , Russell, James M. , Johnson, Thomas C. , Brown, Erik T. , Berke, Melissa A. , Werne, Josef P. , Huang, Yongsong

Konecky, B. L., Russell, J. M., Johnson, T. C., Brown, E. T., Berke, M. A., Werne, J. P. and Huang, Y.: Atmospheric circulation patterns during late Pleistocene climate changes at Lake Malawi, Africa, Earth and Planetary Science Letters, 312(3-4), 318–326, doi:10.1016/j.epsl.2011.10.020, 2011.

Atmospheric circulation patterns during late Pleistocene climate changes at Lake Malawi, Africa

The isotopic composition of this calcite [endogenic calcite in macrophyte coatings] is approximately in equilibrium with lake waters,

Delta Plus XL or Delta XP mass spectrometer (IRMS)

XRD undertaken; Microscopic observation of smear slides

The isotopic composition of the Triassic limestone bedrock is characterized by relatively low oxygen isotope values (between -4.0 and -6.0%; average d18Ocalcite = -5.3%)...samples from units 6, 5 and 3 show d18Ocalcite values (-7.1% to -3.2%) similar to the isotopic signal of the bedrock (-4.6% to -5.2%), indicating a dominant clastic origin of the carbonate.