“…At Yuanjia section, the PrecambrianCambrian boundary could be placed at the negative ␦ 13 C org excursion in the upper Liuchapo Formation (Guo et al, 2013) because this excursion may correlate with the ␦ 13 C carb and/or ␦ 13 C org negative excursions in the Daibu Member of the Zhujiaqing Formation at Xiaotan section, Yunnan Province Li et al, 2013a;Zhou et al, 1997) and in the lower part of the Yanjiahe Formation at Wuhe section, Three Gorges area (Cremonese et al, 2014;Ishikawa et al, 2008;Kikumoto et al, 2014) (Fig. 3b).…”