“…The biotic turnover, ecological crisis, and environmental background across the Tr–J transition have drawn significant attention over the last decades (Barash, 2015; Hesselbo et al, 2007). The impact of the end‐Triassic mass extinction on marine organisms has been extensively documented (e.g., radiolarians, Hallam, 2002; foraminifera, Michalík et al, 2007; ammonites and brachiopods, Tomašových & Siblík, 2007; corals and calcisponges, Stanley Jr. et al, 2018; bivalves, Atkinson et al, 2019). Bio‐ and chemo‐stratigraphic data and stratigraphic correlations of sea‐level changes, ocean acidification and release of greenhouse gases (e.g., CO 2 , CH 4 ) suggest this event to be triggered by the breakup of Pangea and particularly by the eruptions of the Central Atlantic Magmatic Province (CAMP) at that time (Marzoli et al, 2004; Van de Schootbrugge et al, 2009; Whiteside et al, 2010; Ruhl et al, 2011, Ruhl et al, 2020; Percival et al, 2017; Capriolo et al, 2020; He et al, 2020).…”