Correction to Arsenic in a Speleothem from Central China: Stadial-Interstadial Variations and Implications

摘要

The concentration values on the y-axes of the Al and Mn plots of Figure 3 were accidently amplified and the corrected Figure 3 is given here. Because Figure 3 is used in the paper to indicate that (l) aluminum, manganese, and iron are transported largely in particulate phases in karst groundwater at the study site, and (2) iron concentrations in the karst groundwaters at the study site are much lower than in hydrothermal spring outlets in the Cezallier area of the French Massif Central, the corrected concentration values for Al and Mn do not impact any discussion or conclusions of the paper.