“…With the advancement of analytical techniques in recent years, many studies have started to utilize inorganic geochemical analysis such as X‐ray fluorescence (XRF) to identify the elevated marine signals in overwash deposits (Dietz et al., 2022; H. F. Williams et al., 2022; Yang et al., 2020; Yao et al., 2018, 2020). In addition, analyses of stable isotopes of bulk sedimentary organic matter (e.g., 13 C and 15 N) (Jahan et al., 2021) and micropaleontological proxies (e.g., diatoms, phytoliths, palynomorphs, foraminifera) (e.g., K. B. Liu et al., 2008; Lul & Liu, 2005; Scott et al., 2003; Wang et al., 2019; Xian et al., 2022) have also been used in paleotempestological studies.…”