|Author(s)||Fru Ernest Chi1, Somogyi Andrea2, El Albani Abderrazzak3, Medjoubi Kadda2, Aubineau Jeremie3, Robbins Leslie J.4, Lalonde Stefan5, Konhauser Kurt O.4|
|Affiliation(s)||1 : Cardiff Univ, Coll Phys Sci & Engn, Sch Earth & Ocean Sci, Ctr Geobiol & Geochem, Cardiff CF10 3AT, S Glam, Wales.
2 : LOrme Merisiers St Aubin, Synchrotron SOLEIL, Nanoscopium Beamline, BP 48, F-91192 Gif Sur Yvette, France.
3 : Univ Poitiers, CNRS, UMR 7285, Inst Chim Milieux & Mat Poitiers, 5 Rue Albert Turpin,Bat B35, F-86073 Poitiers, France.
4 : Univ Alberta, Dept Earth & Atmospher Sci, Edmonton, AB T6G 2E3, Canada.
5 : Univ Bretagne Occidentale, CNRS, UMR6538, European Inst Marine Studies,Lab Geosci Ocean, F-29280 Plouzane, France.
|Source||Geology (0091-7613) (Geological Soc Amer, Inc), 2019-03 , Vol. 47 , N. 3 , P. 243-246|
|WOS© Times Cited||16|
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 established for the first time in Earth's history. These data highlight the global emergence of a new selective pressure on the survival of marine microbial communities across the GOE, the widespread appearance of toxic, oxidized chemical species such as arsenate in seawater.
Fru Ernest Chi, Somogyi Andrea, El Albani Abderrazzak, Medjoubi Kadda, Aubineau Jeremie, Robbins Leslie J., Lalonde Stefan, Konhauser Kurt O. (2019). The rise of oxygen-driven arsenic cycling at ca. 2.48 Ga. Geology, 47(3), 243-246. Publisher's official version : https://doi.org/10.1130/G45676.1 , Open Access version : https://archimer.ifremer.fr/doc/00637/74946/