Excess Ba enrichments show an increasing trend with depositional depth, with Ba excess contents of 0.031–0.109 wt% (averaging at 0.067 wt%) at Dazhuliushui, 0.028–0.171 wt% (averaging at 0.073 wt%) at Maluhe, 0.099–1.819 wt% (averaging at 0.725 wt%) at Caojiaping and 0.426–3.347 wt% (averaging at 1.561 wt%) at Sancha.
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Seawater barium and sulfide removal improved marine habitability for the Cambrian Explosion of early animals.
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