Showing papers by "Smail Mostefaoui published in 2019"
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TL;DR: The extreme 13C-depletions recorded in Neoarchean organic matter (OM) have commonly been interpreted as markers of methanotrophy using oxidants such as dioxygen, sulfate, nitrite/nitrate, and/or Fe3+-and Mn4+minerals as discussed by the authors.
22 citations