year (MAT0ee6aa23ee): The paleoData_values have changed

Column 'addR31C5QbCde6vZUKKY', with variable name 'ageEnsemble', was added to the dataset
Column 'addR4GyJOyGDz6lzP487', with variable name 'depth', was added to the dataset
Column 'addR7rlWCH8c8nOnjQ93', with variable name 'age.rangeHigh', was added to the dataset
Column 'addRcegFbslNEiDKi8al', with variable name 'age.rangeLow', was added to the dataset
Column 'addRijr7IUY1nlaKb9F5', with variable name 'depth', was added to the dataset
Column 'addRnQ1NTF5NRy24R02i', with variable name 'age', was added to the dataset
Column 'LS14FEZA-chron-NA1', with variable name 'depth', was added to the dataset
Column 'LS14FEZA-chron-NA2', with variable name 'age.rangeLow', was added to the dataset
Column 'LS14FEZA-chron-NA3', with variable name 'age.rangeHigh', was added to the dataset
Column 'LS14FEZA-chron-NA4', with variable name 'age', was added to the dataset

age14C (chron2): The chronData_values have changed
age14Cuncertainty (chron3): The chronData_values have changed

Feakins, Sarah J. , Kirby, Matthew E. , Cheetham, Michael I. , Ibarra, Yadira , Zimmerman, Susan R.H.

Feakins, S. J., Kirby, M. E., Cheetham, M. I., Ibarra, Y. and Zimmerman, S. R. H.: Fluctuation in leaf wax D/H ratio from a southern California lake records significant variability in isotopes in precipitation during the late Holocene, Organic Geochemistry, 66, 48–59, doi:10.1016/j.orggeochem.2013.10.015, 2014.

Agilent 6890 GC, pyrolysis at 1440C, Thermo Scientific DeltaV Plus

SASM precipitation that falls on the Altiplano is ultimately derived from Atlantic Ocean moisture that has been transported across the Amazon Basin and lifted over the eastern cordillera of the Andes. Altiplano ?Dp thus integrates upstream effects including rainout and moisture recycling over the Amazon Basin, altitude effects associated with upslope moisture transport, and local effects such as the intensity of precipitation (?amount effect?) (Dansgaard, 1964). ... "Increased rainout along this trajectory, as well as increased local precipitation in the Andes, results in more depleted ?Dp, consistent with the continentality and amount effects that dominate ?Dp variability throughout most of tropical South America (Vuille et al., 2003). Accordingly, the intensity of the SASM is significantly negatively correlated with ?18O (and correspondingly ?D) of modern precipitation in the Cen- tral Andes, as well as throughout much of southern tropical South America (Vuille and Werner, 2005).