AN APPROACH TO THE CONTRIBUTION OF ANTHROPOGENIC ACTIONS FOR THE ARARUAMA LAGOONAL SYSTEM (SE BRAZIL) GEOMORPHOLOGICAL EVOLUTION

The first studies regarding the constitution of the Araruama lagoonal system, located in the Rio de Janeiro state (SE Brazil), were carried out by Alberto Ribeiro Lamego. This author supported the thesis that it had resulted from the formation of a sand barrier (called Massambaba) due to the longitu...

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Main Authors: OLEGÁRIO NELSON AZEVEDO PEREIRA, MARIA ANTONIETA DA CONCEIÇÃO RODRIGUES, JOÃO MANUEL ALVEIRINHO DIAS
Format: Article
Language:English
Published: Universidade do Estado do Rio de Janeiro 2018-06-01
Series:Journal of Sedimentary Environments
Subjects:
Online Access:https://www.e-publicacoes.uerj.br/index.php/jse/article/view/35533
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spelling doaj-b672cba15fb844eea71ca61e193fb1bc2020-11-25T00:29:51ZengUniversidade do Estado do Rio de JaneiroJournal of Sedimentary Environments 2447-94622447-94622018-06-0132108120https://doi.org/10.12957/jse.2018.35533AN APPROACH TO THE CONTRIBUTION OF ANTHROPOGENIC ACTIONS FOR THE ARARUAMA LAGOONAL SYSTEM (SE BRAZIL) GEOMORPHOLOGICAL EVOLUTIONOLEGÁRIO NELSON AZEVEDO PEREIRA0MARIA ANTONIETA DA CONCEIÇÃO RODRIGUES1JOÃO MANUEL ALVEIRINHO DIAS2Universidade do Estado do Rio de Janeiro, Programa de Pós-Graduação em Meio Ambiente, Rio de Janeiro, Brazil. Universidade do Estado do Rio de Janeiro, Faculdade de Geologia, Rio de Janeiro, Brazil. Universidade do Algarve, CIMA (Centro de Investigação Marinha e Ambiental), Faro, Portugal. The first studies regarding the constitution of the Araruama lagoonal system, located in the Rio de Janeiro state (SE Brazil), were carried out by Alberto Ribeiro Lamego. This author supported the thesis that it had resulted from the formation of a sand barrier (called Massambaba) due to the longitudinal transport of large quantities of sediments through coastal drift currents, and the growth of spits parallel to the shoreline. However, most recent studies largely rejected it, sustaining that the confinement of this hydric environment was the result of the growth of two sand barriers during the Pleistocene and Holocene times (120.000 to 7.000 years before present - BP) due to the sea level changes. The hypothesis that we suggest, is that both propositions are acceptable and complementary. This study aims to demonstrate that, despite the opinions on the formation of the double sand barrier, deposition of sediments by coastal drift currents at the end of the Holocene, and especially in recent chronologies, also contributed to the establishment of this lagoon system. In our opinion, the increased sediment supplies due to human activities contributed to the formation of the inner spits and the nearby sea sandbar. Its orientation was influenced by the existence of the island of Cabo Frio, that allowed the formation of the tombolo that almost connected it to the continent. Through the analysis of historical and cartographic documents related to the colonization and economic exploitation of the region, it is evident that the anthropogenic actions played a significant role in the sandy spits formation. Of these, special emphasis is placed on the agriculture and deforestation that contributed to the increase of sedimentary accumulation. This work demonstrate that the analysis of historical documents can provide information and contribute to the understanding of recent coastal developments.https://www.e-publicacoes.uerj.br/index.php/jse/article/view/35533environmental historycoastal environmentslagoonal formationinteraction man-natureanthropogenic activities
collection DOAJ
language English
format Article
sources DOAJ
author OLEGÁRIO NELSON AZEVEDO PEREIRA
MARIA ANTONIETA DA CONCEIÇÃO RODRIGUES
JOÃO MANUEL ALVEIRINHO DIAS
spellingShingle OLEGÁRIO NELSON AZEVEDO PEREIRA
MARIA ANTONIETA DA CONCEIÇÃO RODRIGUES
JOÃO MANUEL ALVEIRINHO DIAS
AN APPROACH TO THE CONTRIBUTION OF ANTHROPOGENIC ACTIONS FOR THE ARARUAMA LAGOONAL SYSTEM (SE BRAZIL) GEOMORPHOLOGICAL EVOLUTION
Journal of Sedimentary Environments
environmental history
coastal environments
lagoonal formation
interaction man-nature
anthropogenic activities
author_facet OLEGÁRIO NELSON AZEVEDO PEREIRA
MARIA ANTONIETA DA CONCEIÇÃO RODRIGUES
JOÃO MANUEL ALVEIRINHO DIAS
author_sort OLEGÁRIO NELSON AZEVEDO PEREIRA
title AN APPROACH TO THE CONTRIBUTION OF ANTHROPOGENIC ACTIONS FOR THE ARARUAMA LAGOONAL SYSTEM (SE BRAZIL) GEOMORPHOLOGICAL EVOLUTION
title_short AN APPROACH TO THE CONTRIBUTION OF ANTHROPOGENIC ACTIONS FOR THE ARARUAMA LAGOONAL SYSTEM (SE BRAZIL) GEOMORPHOLOGICAL EVOLUTION
title_full AN APPROACH TO THE CONTRIBUTION OF ANTHROPOGENIC ACTIONS FOR THE ARARUAMA LAGOONAL SYSTEM (SE BRAZIL) GEOMORPHOLOGICAL EVOLUTION
title_fullStr AN APPROACH TO THE CONTRIBUTION OF ANTHROPOGENIC ACTIONS FOR THE ARARUAMA LAGOONAL SYSTEM (SE BRAZIL) GEOMORPHOLOGICAL EVOLUTION
title_full_unstemmed AN APPROACH TO THE CONTRIBUTION OF ANTHROPOGENIC ACTIONS FOR THE ARARUAMA LAGOONAL SYSTEM (SE BRAZIL) GEOMORPHOLOGICAL EVOLUTION
title_sort approach to the contribution of anthropogenic actions for the araruama lagoonal system (se brazil) geomorphological evolution
publisher Universidade do Estado do Rio de Janeiro
series Journal of Sedimentary Environments
issn 2447-9462
2447-9462
publishDate 2018-06-01
description The first studies regarding the constitution of the Araruama lagoonal system, located in the Rio de Janeiro state (SE Brazil), were carried out by Alberto Ribeiro Lamego. This author supported the thesis that it had resulted from the formation of a sand barrier (called Massambaba) due to the longitudinal transport of large quantities of sediments through coastal drift currents, and the growth of spits parallel to the shoreline. However, most recent studies largely rejected it, sustaining that the confinement of this hydric environment was the result of the growth of two sand barriers during the Pleistocene and Holocene times (120.000 to 7.000 years before present - BP) due to the sea level changes. The hypothesis that we suggest, is that both propositions are acceptable and complementary. This study aims to demonstrate that, despite the opinions on the formation of the double sand barrier, deposition of sediments by coastal drift currents at the end of the Holocene, and especially in recent chronologies, also contributed to the establishment of this lagoon system. In our opinion, the increased sediment supplies due to human activities contributed to the formation of the inner spits and the nearby sea sandbar. Its orientation was influenced by the existence of the island of Cabo Frio, that allowed the formation of the tombolo that almost connected it to the continent. Through the analysis of historical and cartographic documents related to the colonization and economic exploitation of the region, it is evident that the anthropogenic actions played a significant role in the sandy spits formation. Of these, special emphasis is placed on the agriculture and deforestation that contributed to the increase of sedimentary accumulation. This work demonstrate that the analysis of historical documents can provide information and contribute to the understanding of recent coastal developments.
topic environmental history
coastal environments
lagoonal formation
interaction man-nature
anthropogenic activities
url https://www.e-publicacoes.uerj.br/index.php/jse/article/view/35533
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