R. E. Criss, Principles of Stable Isotope Distribution (Oxford Univ. Press, New York, 1999), p. 108.

ZK (07/01/2019): Pre-Holocene part of the D4 stal, NM: It looks like this one does now have data from the past 2k. I've made this the only primary timeseries. ZK (07/01/2019): Pre-Holocene part of the D4 stal. No data from the past 2000yrs

AA (3/5/19): No data from last 2000 yrs.

Yuan, D.: Timing, Duration, and Transitions of the Last Interglacial Asian Monsoon, Science, 304(5670), 575–578, doi:10.1126/science.1091220, 2004.

Yuan, D., H. Cheng, R.L. Edwards, C.A. Dykoski, M.J. Kelly, M. Zhang, J. Qing, Y. Lin, Y. Wang, J. Wu, J.A. Dorale, Z. An, and Y. Cai

d18O (SP04YUCN01A): interpretation3_scope: '' has been replaced by 'isotope'
d18O (SP04YUCN01A): interpretation4_scope: '' has been replaced by 'isotope'
d18O (SP04YUCN02A): interpretation4_scope: '' has been replaced by 'isotope'
d18O (SP04YUCN03A): interpretation3_scope: '' has been replaced by 'isotope'
d18O (SP04YUCN03A): interpretation4_scope: '' has been replaced by 'isotope'

on-line, automated, carbonate preparation system linked to a Finnigan Delta XL ratio mass spectrometer at the University of Massachusetts

; archiveType changed - was originally Speleothem (SP); archiveType changed - was originally Speleothem (SP)

relative portion of summer (SAM) vs winter rainfall

Thus, changes in convective intensity within the SASM/SACZ may significantly contribute to and reinforce the effect that the location of this system has on the d18O of precipitation.

Cruz, F. W., Burns, S. J., Karmann, I., Sharp, W. D., Vuille, M., Cardoso, A. O., Ferrari, J. A., Silva Dias, P. L. and Viana, O.: Insolation-driven changes in atmospheric circulation over the past 116,000 years in subtropical Brazil, Nature, 434(7029), 63–66, doi:10.1038/nature03365, 2005.

d18O (SP05CRBR01A): interpretation4_scope: '' has been replaced by 'isotope'

white, densely crystalline low-Mg calcite,  showing columnar-shape crystals in thin section

The d13C profile shows no correlation with d18O in any of the section profiles