stratigraphic tie to piston core dated by varve counting and 210Pb

d2H (LS11KOMA01A): interpretation4_scope: '' has been replaced by 'isotope'

year (MAT15c72e1504): The paleoData_values have changed

Column 'addRAagtPWhfeYby7Kal', with variable name 'reject', was added to the dataset
Column 'addRB1Axpz0zqplKPugY', with variable name 'age.rangeHigh', was added to the dataset
Column 'addRJHcNM6ZGl5PETEmD', with variable name 'depth', was added to the dataset
Column 'addRsnH7jL7q35RvXNQG', with variable name 'ageEnsemble', was added to the dataset
Column 'addRsQCTxWhPj3pDHuQo', with variable name 'age', was added to the dataset
Column 'addRvU0U8UWN4Ks1bYX9', with variable name 'age.rangeLow', was added to the dataset
Column 'addRWKgqRZZrXttvXOWV', with variable name 'depth', was added to the dataset
Column 'LS11KOMA-chron-NA1', with variable name 'depth', was added to the dataset
Column 'LS11KOMA-chron-NA2', with variable name 'age.rangeLow', was added to the dataset
Column 'LS11KOMA-chron-NA3', with variable name 'age.rangeHigh', was added to the dataset
Column 'LS11KOMA-chron-NA4', with variable name 'age', was added to the dataset

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

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

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.

Delta Plus XL or Delta XP mass spectrometer (IRMS)

XRD undertaken; Microscopic observation of smear slides

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

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.