Determination of controls on Holocene barrier progradation through application of OSL dating: The Ilha Comprida Barrier example, Southeastern Brazil


Autoria(s): Guedes, Carlos Conforti Ferreira; Giannini, Paulo Cesar Fonseca; Sawakuchi, Andre Oliveira; DEWITT, R; Nascimento Junior, Daniel Rodrigues do; Aguiar, Vitor Ângelo Paulino de; ROSSI, M. G.
Contribuinte(s)

UNIVERSIDADE DE SÃO PAULO

Data(s)

20/10/2012

20/10/2012

2011

Resumo

Barrier development during the Holocene is studied using the example of the Ilha Comprida, Southeastern Brazil. Aerial photos, facies analysis, and optically stimulated luminescence dating are used to define the barrier emergence and evolution. Optically stimulated luminescence ages and facies successions indicate that the Ilha Comprida probably began as a Holocene transgressive barrier island 6000 years ago, just before the last relative sea-level maximum. Since then the barrier has progradated through the addition of curved beach ridges. Based on beach ridge alignments, six units of growth are identified with two growth directions, transverse and longitudinal. Rates of progradation with transverse growth vary from 0.13 to 4.6 m/year. Rates of longitudinal growth to NE range from 5.2 to 30 m/year. Variation in coastal progradation rates and sediment retention during the last 6000 years is compared with climate, physiography and relative sea-level changes. The physiography, represented by pre-Cenozoic hills, is the major control on sediment retention and alternation between longitudinal and transverse growth. Climate variations, such as the Little Ice Age event, apparently control the formation of ridges types: beach ridges, foredunes, and blowouts. These results allow the use of the Ilha Comprida Barrier as an example to analyze the major controls on barriers progradation. (C) 2011 Elsevier B.V. All rights reserved.

Fundacao de Amparo Pesquisa do Estado de Sao Paulo (FAPESP)[2001/01732-8]

Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)

Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)

Fundacao de Amparo Pesquisa do Estado de Sao Paulo (FAPESP)[2002/01016-3]

Fundacao de Amparo Pesquisa do Estado de Sao Paulo (FAPESP)[2007/51511-4]

Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)

Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq)[135013/2007-0]

Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)

Identificador

MARINE GEOLOGY, v.285, n.1/Abr, p.1-16, 2011

0025-3227

http://producao.usp.br/handle/BDPI/29592

10.1016/j.margeo.2011.04.005

http://dx.doi.org/10.1016/j.margeo.2011.04.005

Idioma(s)

eng

Publicador

ELSEVIER SCIENCE BV

Relação

Marine Geology

Direitos

restrictedAccess

Copyright ELSEVIER SCIENCE BV

Palavras-Chave #sediment accumulation #progradation rates #beach ridges #inlet dynamics #BEACH RIDGE PLAIN #SEA-LEVEL CHANGES #SOUTHERN BRAZIL #GUICHEN BAY #AUSTRALIA #CLIMATE #EVOLUTION #COASTLINE #FOREDUNES #SEDIMENTATION #Geosciences, Multidisciplinary #Oceanography
Tipo

article

original article

publishedVersion