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dc.creatorBorges de Bitencourt, Volney Junior
dc.creatorDillenburg, Sergio
dc.creatorGuimarães Barboza, Eduardo
dc.creatorRosa, Maria Luiza
dc.creatorManzolli, Rogerio Portantiolo
dc.date.accessioned2020-09-29T19:20:00Z
dc.date.available2020-09-29T19:20:00Z
dc.date.issued2020-05-05
dc.identifier.issn1519-1540
dc.identifier.issn2236-5664
dc.identifier.urihttps://hdl.handle.net/11323/7132
dc.description.abstractNeste trabalho, investigou-se com detalhe a barreira holocênica do litoral médio do Rio Grande do Sul (RS), entre as localidades do Estreito e de Bacupari. Este trecho do litoral corresponde a mais expressiva projeção costeira de larga-escala da costa do RS. Dados geofísicos (Georadar) e geomorfológicos superficiais permitiram importantes descobertas. Na porção sul da projeção costeira, entre o Estreito e o setor norte da Lagoa do Peixe, a barreira holocênica exibe um comportamento evolutivo dominantemente retrogradacional (provavelmente desde 6 ka até o presente), o qual foi determinado por um longo período de balanço negativo de sedimentos. Já na porção norte da projeção, entre o Balneário Mostardense e Bacupari, a barreira mostra uma inversão de comportamento retrogradacional para progradacional. Tal mudança evolutiva, expressa numa progradação que varia de 230 a 1800 m, é possivelmente oriunda de uma alteração no balanço de sedimentos (balanço negativo para positivo) que pode ter ocorrido somente há alguns séculos, ou mesmo poucos milênios. A mudança para um padrão de empilhamento progradacional mostrou-se crescente em dimensão (extensão do registro progradacional) do meio para o norte da projeção costeira. É possível sugerir que essas tendências evolutivas em escala geológica (10²-10³ anos) vão continuar no decorrer das próximas décadas. Informações acerca do comportamento evolutivo da linha de costa nos últimos séculos e milênios podem servir como subsídios do meio físico na gestão costeira do litoral médio do RS.spa
dc.description.abstractIn this work, the Holocene barrier of the middle coast of Rio Grande do Sul (RS), located between Estreito and Bacupari, was investigated in detail. This stretch of the coast corresponds to the most expressive large-scale coastal projection of the RS coast. Important discoveries were made through subsurface geophysical (GPR) and surfi cial geomorphology data. In the southern portion of the projection, between Estreito and the northern sector of Lagoa do Peixe, the Holocene barrier exhibits a predominantly retrogradational evolutionary behavior (probably from 6 ka and the present), which was determined by a negative sediment budget in the long term. On the other hand, in the northern portion of the projection, between Balneário Mostardense and Bacupari, the barrier shows a reversal from retrogradational to progradational behavior. Such evolutionary change, expressed in a progradation ranging from 230 to 1800 m, is possibly attributed to a change in the sediment budget (negative to positive budget) that may have occurred only a few centuries ago, or even a few millennia. The reversal towards a progradational stacking pattern showed an increase in size (length of the progradational record) from the middle to the north of the coastal projection. It is possible to suggest that these evolutionary trends on a geological scale (10²-10³ years) will continue over the next decades. Information about the coastline evolutionary trends in the last centuries and millennia can be useful as subsidies for the coastal management of the middle coast of RS.spa
dc.language.isoporspa
dc.publisherCorporación Universidad de la Costaspa
dc.rightsCC0 1.0 Universal*
dc.rights.urihttp://creativecommons.org/publicdomain/zero/1.0/*
dc.sourceRevista Brasileira de Geomorfologiaspa
dc.subjectGeoradar (GPR)spa
dc.subjectEvolução Costeiraspa
dc.subjectBalanço sedimentarspa
dc.subjectGround penetrating radar (GPR)spa
dc.subjectCoastal evolutionspa
dc.subjectSediment budgetspa
dc.subjectGISspa
dc.titlePadrões de empilhamento estratigráfico e seus reflexos na morfologia da barreira costeira holocênica no litoral médio do Rio Grande do Sul, Brasilspa
dc.title.alternativeStratigraphic stacking patterns and their reflections on the holocene coastal barrier morphology of the middle Coast of Rio Grande Do Sul, Brazilspa
dc.typearticlespa
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