“…Geochemistry is a powerful tool in reconstructing the sediment sources (detrital vs. endogenic or continental vs. marine) and transport paths of mass flow units. Applications of geochemistry in submarine paleoseismology include the analyses of inorganic tracers (Chagué‐Goff et al., 2017; Goff et al., 2018; Polonia, Panieri, et al., 2013; Schwestermann et al., 2020; Yakupoğlu et al., 2019), radionuclides (Çağatay et al., 2012; McHugh, Kanamatsu, Seeber, Bopp, Cormier, & Usami, 2016; McHugh, Seeber, et al., 2020; Sakuna‐Schwartz et al., 2015), organic carbon (Bao et al., 2018) and organic contaminants (e.g., PAHs Giuliani et al., 2017; Pongpiachan & Schwarzer 2013; Tipmanee et al., 2012). The same tracers are widely used also in tsunami research onshore and in the marine environment (Chagué‐Goff et al., 2017 and references therein).…”