“…The paucity of sulfides in the Ben Lawers Schist, and in barite beds M6 and M7 in the uppermost part of the Ben Eagach Schist (Fig. 2b and 4a), is consistent with increased oxygenation of the sea bed at this time, possibly corresponding to one of the episodic ocean oxygenation events that occurred in the Ediacaran (Yuan et al, 2022).…”