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High-resolution carbon-isotope (13C) profiles from shallow- and deep-water carbonates in the South Atlantic (Campos and Santos Basins) are here correlated to stratigraphically well-calibrated Tethyan sections, constraining the end of major evaporite deposition in the South Atlantic to the Early Aptian OAE 1a interval. The unusually extensive evaporite deposition would have reduced the global dissolved sulfate inventory, potentially increasing global preservation of organic matter by decreasing sulfate reduction, which could explain the coincidence in timing between OAE 1a and the dramatic negative sulfur-isotope excursion over this interval. Hence, in addition to the coeval eruption of the Ontong Java 22 Plateau, the opening of the South Atlantic may have played an important role in the genesis and character of OAE 1a

New age constraints on Aptian evaporites and carbonates from the South Atlantic: Implications for Oceanic Anoxic Event 1a