GEOMORPHOLOGY OF THE NORTHERN OUTER CONTINENTAL SHELF OF RIO GRANDE DO NORTE AND IMPLICATIONS OF QUATERNARY SEA-LEVEL FLUCTUATIONS
outer shelf; paleoshorelines; reef; sea-level fluctuations; morphostratigraphy
Sea-level fluctuations are the main drivers of continental shelf evolution, particularly in mixed siliciclastic–carbonate settings where antecedent topography and sediment supply shape depositional patterns. The outer shelf of Rio Grande do Norte, northeastern Brazil, preserves incised valleys, terraces, paleoshorelines, and reefs linked to Quaternary sea-level changes. Using seismic, multibeam, backscatter, and satellite data, we correlate shelf morphology and stratigraphy with its outer evolution, in addition to implementing a new methodology for single-beam data processing. Results show that reefs developed on a Pleistocene basement bounded by a regressive surface of the Last Glacial Maximum and formed as Holocene transgressive buildups. Reefs colonized terraces and paleoshorelines, exhibiting backstepping morphologies associated with Meltwater Pulses. Collectively, the seabed features reveal a recurrent pattern of paleoshoreline generation driven by sea-level rise, incised-valley influence, and carbonate production on a mixed shelf.