“…Some studies have demonstrated that the oldest Quaternary deposits (fluvial sediments, named the Nanshe Formation) do not exceed 55 ka BP, based on radiocarbon, thermoluminescence (TL) dating, and stratigraphic relationships (Chen, 1984a;Li et al, 1987;Zong, 1987;Li et al, 1988;Sun et al, 2007;Zhou, 2008). Nevertheless, results from other dating methods, including electron spin resonance (ESR) and OSL, have shown that the oldest Quaternary sediments in the Lianjiang plain, the southeastern part of the Chaoshan plain, date back to more than 260 ka (Song et al, 2012;Tang et al, 2018). Yet, our understanding of the formation and evolution of the Chaoshan plain delta is still debated, owing to different dating methods that require further evaluation.…”