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Antecedent topography controls preservation of latest Pleistocene-Holocene transgression record and clinoform development: the case of the São Francisco delta (eastern Brazil)

  • Adriane Gonçalves de Araújo Nunes Rangel
  • José Maria Landim DominguezEmail author
Original
  • 52 Downloads

Abstract

The present study used shallow high-resolution seismic surveys to characterize the architecture and stratigraphic evolution of the last depositional sequence of the São Francisco Delta (SFDS). The sequence was accumulated within a bathymetric low (BL) on the shelf located in front of the São Francisco river. This antecedent topography provided additional accommodation of tens of meters in comparison with the rest of the shelf. The BL and its sediment-trapping effect allowed the accumulation of a complete stratigraphic record of the eustatic sea-level rise since the Last Glacial Maximum (LGM). The SFDS comprises six stratigraphic units. Because cores and radiocarbon dates are not available for this study area, the depth of occurrence of the top and base of each unit and their lateral relationships with wave-cut terraces carved into the BL walls were used in an effort to tentatively tie the mapped units to known eustatic sea-level curves available in the literature. Results suggest that major episodes of accumulation occurred during intervals of reduced rates in sea-level rise. The lower five units mapped accumulated in a large bay-estuarine protected environment, which resulted from the inundation of the BL. Only the topmost unit (the present clinoform) accumulated in an open ocean environment when sea level reached approximately its present position after 8 ka and the whole shelf was flooded. The most important delta backstepping event was probably associated with Meltwater Pulse 1B, which followed the Younger Dryas and produced one of the most significant stratal surfaces of the SFDS. Among the existing wave-dominated deltas in the Brazilian coast only, the São Francisco was able to construct a well-developed sigmoidal muddy clinoform in an otherwise very shallow shelf subjected to high wave-energy levels. This was only possible because of the existence of a bathymetric low in front of the river mouth, which illustrates the role that antecedent topography might play in providing larger amount of available accommodation space called in this paper of additional accommodation.

Notes

Acknowledgments

AGAN Rangel and JML Dominguez also thank CNPq for a research fellowship. We would also like to express our gratitude to two anonymous reviewers, whose comments greatly improved the quality of the manuscript.

Funding information

This paper is a contribution of the following research grants: CAPES/PNPD (No. 2983/2010) and inctAmbTropic, CNPq/FAPESB Processes: 565054/2010-4, 8936/2011, and 465634/2014-1.

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Authors and Affiliations

  1. 1.Universidade Federal da BahiaSalvadorBrazil

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