“…The Pirabas Formation (Maury, 1925), which is of early Miocene, Aquitanian to early Burdigalian, N4 to N5 to middle Miocene, Langhian N8-N9 plankton foraminiferal biozones (Blow, 1969) (Aguilera et al, 2020a, b and references therein), consists of carbonate to mixed siliciclastic-carbonate deposits associated to shallow-water coastal settings (grainstone and consolidated packstone, stratified wackestone to packstone, and laminated mudstone) (Rossetti et al, 2013 and references therein). In addition, littoral facies (shoreface/foreshore), marginal lagoons, restricted platform environments (gray to olive mudstone and conglomeratic sandstone), and mangrove estuarine lagoons (dark mudstone, massive or laminated) have been recorded (Lima et al, 2020a, b). A diverse fossil fauna that is rich in microfossils (foraminifera, ostracodes) and macrofossils (mollusks, bryozoans, corals, echinoderms, decapods, fishes, cetaceans, and sirenids has been described (Aguilera et al, 2020a, b; Lima et al, 2020a, b).…”