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The rise of oxygen-driven arsenic cycling at ca. 2.48 Ga ArchiMer
Fru, Ernest Chi; Somogyi, Andrea; El Albani, Abderrazzak; Medjoubi, Kadda; Aubineau, Jeremie; Robbins, Leslie J.; Lalonde, Stefan; Konhauser, Kurt O..
The Great Oxidation Event (GOE) at 2.45 Ga facilitated the global expansion of oxidized compounds in seawater. Here, we demonstrate that the GOE coincided with a sharp increase in arsenate and arsenic sulfides in marine shales. The dramatic rise of these oxygen-sensitive tracers overlaps with the expansion of key arsenic oxidants, including oxygen, nitrate, and Mn(IV) oxides. The increase in arsenic sulfides by at least an order of magnitude after 2.45 Ga is consistent with the proposed transition to mid-depth continental-margin sulfide-rich waters following the GOE. At the same time, the strong increase in arsenate content, to similar to 60% of the total arsenic concentration in shales, suggests that the oxidative component of the arsenic cycle was...
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Ano: 2019 URL: https://archimer.ifremer.fr/doc/00637/74946/76142.pdf
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