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Holocene morpho-sedimentary evolution of Marambaia Barrier Island (SE Brazil)

Published online by Cambridge University Press:  16 August 2021

Tatiana Pinheiro Dadalto Open the ORCID record for Tatiana Pinheiro Dadalto [Opens in a new window] ,
Breylla Campos Carvalho Open the ORCID record for Breylla Campos Carvalho [Opens in a new window] ,
Josefa Varela Guerra Open the ORCID record for Josefa Varela Guerra [Opens in a new window] ,
Antonio Tadeu dos Reis Open the ORCID record for Antonio Tadeu dos Reis [Opens in a new window]  and
Cleverson Guizan Silva Open the ORCID record for Cleverson Guizan Silva [Opens in a new window]
Tatiana Pinheiro Dadalto*
Affiliation:
Department of Geology, Fluminense Federal University, Niterói, Brazil Environmental Sciences Training Center, Federal University of Southern Bahia, Porto Seguro, Brazil
Breylla Campos Carvalho
Affiliation:
Department of Geological Oceanography, Rio de Janeiro State University, Rio de Janeiro, Brazil Coordenação de Estruturas Territoriais, Instituto Brasileiro de Geografia e Estatística, Rio de Janeiro, Brazil
Josefa Varela Guerra
Affiliation:
Department of Geological Oceanography, Rio de Janeiro State University, Rio de Janeiro, Brazil
Antonio Tadeu dos Reis
Affiliation:
Department of Geological Oceanography, Rio de Janeiro State University, Rio de Janeiro, Brazil
Cleverson Guizan Silva
Affiliation:
Department of Geology, Fluminense Federal University, Niterói, Brazil
*
*Corresponding author: tpdadalto@ufsb.edu.br
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Abstract

Barrier islands are sedimentary bodies susceptible to changes in sediment supply, dominant physical processes, and sea level. The aim of this work was to study the sedimentary processes that established Marambaia Barrier Island (SE Brazil) as an elongated sandy body that created Sepetiba Bay. For this purpose, barrier and back-barrier bay environments were analyzed using high-resolution satellite imagery, geophysical and topographic surveys, surface sediment samples and short cores, and radiocarbon and optically stimulated luminescence (OSL) dating techniques. Seven morpho-sedimentary domains were identified: coastal beach ridges, overland flow features, inter-ridge paleo lagoon, bayside beach ridges, marshlands, dune field and tidal wetlands. The results show that Marambaia Barrier Island evolved throughout the Holocene, first under normal regression conditions during sea-level rise, and then by forced regression as sea level lowered to its present position. Concurrent processes related to longshore drift, onshore transport, reworked barrier deposits, eolian transport, bay circulation, and pedogenesis influenced its morpho-sedimentary evolution. Morphological features such as truncated beach ridges, flying spits, and filled channels attest to the occurrence of alternating periods of erosion and accretion, evincing how the morphology of barrier island systems preserves an important archive of environmental changes.

Keywords

Holocene regressive barrier islandStratigraphic architectureGeochronologyOptically stimulated luminescenceSatellite imageryGround penetrating radar (GPR)Sepetiba Bay
Type
Research Article
Information
Quaternary Research , Volume 105 , January 2022 , pp. 182 - 200
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Copyright © University of Washington. Published by Cambridge University Press, 2021

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