Abstract:Abstract. The Aptian–Albian interval is characterized by significant
paleoclimatic, paleoceanographic, and paleogeographic changes, which in turn
affected the distribution and evolution of marine ecosystems. Despite the
importance of such studies, there have been few correlations between
Aptian–Albian sections of the Tethys Sea and those of the South Atlantic
Ocean. This interval, including the Aptian–Albian transition, is preserved
in the deposits of the Riachuelo Formation (Sergipe–Alagoas Basin, Brazil)
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