Process control in the geneses and evolution of a lagoon-barrier system inside of the patos lagoon, south of Brazil

The origin and geological evolution of a complex of a beach ridgeplain in the Feitoria lagoon-barrier, located on the western margin of the southern cell Patos lagoon, Brazil was influenced by the interactions between the alocyclic (climate change and relative sea level) and autocyclic (sediment sup...

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Autores:
Portantiolo Manzolli, Rogerio
Portz, Luana Carla
De Bitencourt Borges, Volney Junior
Amabile Leal, Renato
Martins Marques, Eduardo
Biancini Da Silva, Anderson
Guimarães Barboza, Eduardo
Caron, Felipe
Alcantara Carrio, Javier
Oliveira Sawakuchi, Andre
Tipo de recurso:
Article of journal
Fecha de publicación:
2018
Institución:
Corporación Universidad de la Costa
Repositorio:
REDICUC - Repositorio CUC
Idioma:
eng
OAI Identifier:
oai:repositorio.cuc.edu.co:11323/1506
Acceso en línea:
https://hdl.handle.net/11323/1506
https://doi.org/10.2112/SI85-131.1
https://repositorio.cuc.edu.co/
Palabra clave:
Barrier-lagoon system into lagoon
Beach-ridge plain
Coastal evolution
GPR
Rights
openAccess
License
Atribución – No comercial – Compartir igual
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dc.title.eng.fl_str_mv Process control in the geneses and evolution of a lagoon-barrier system inside of the patos lagoon, south of Brazil
title Process control in the geneses and evolution of a lagoon-barrier system inside of the patos lagoon, south of Brazil
spellingShingle Process control in the geneses and evolution of a lagoon-barrier system inside of the patos lagoon, south of Brazil
Barrier-lagoon system into lagoon
Beach-ridge plain
Coastal evolution
GPR
title_short Process control in the geneses and evolution of a lagoon-barrier system inside of the patos lagoon, south of Brazil
title_full Process control in the geneses and evolution of a lagoon-barrier system inside of the patos lagoon, south of Brazil
title_fullStr Process control in the geneses and evolution of a lagoon-barrier system inside of the patos lagoon, south of Brazil
title_full_unstemmed Process control in the geneses and evolution of a lagoon-barrier system inside of the patos lagoon, south of Brazil
title_sort Process control in the geneses and evolution of a lagoon-barrier system inside of the patos lagoon, south of Brazil
dc.creator.fl_str_mv Portantiolo Manzolli, Rogerio
Portz, Luana Carla
De Bitencourt Borges, Volney Junior
Amabile Leal, Renato
Martins Marques, Eduardo
Biancini Da Silva, Anderson
Guimarães Barboza, Eduardo
Caron, Felipe
Alcantara Carrio, Javier
Oliveira Sawakuchi, Andre
dc.contributor.author.spa.fl_str_mv Portantiolo Manzolli, Rogerio
Portz, Luana Carla
De Bitencourt Borges, Volney Junior
Amabile Leal, Renato
Martins Marques, Eduardo
Biancini Da Silva, Anderson
Guimarães Barboza, Eduardo
Caron, Felipe
Alcantara Carrio, Javier
Oliveira Sawakuchi, Andre
dc.subject.eng.fl_str_mv Barrier-lagoon system into lagoon
Beach-ridge plain
Coastal evolution
GPR
topic Barrier-lagoon system into lagoon
Beach-ridge plain
Coastal evolution
GPR
description The origin and geological evolution of a complex of a beach ridgeplain in the Feitoria lagoon-barrier, located on the western margin of the southern cell Patos lagoon, Brazil was influenced by the interactions between the alocyclic (climate change and relative sea level) and autocyclic (sediment supply, waves, longshore drift and storm surges) forcing. The study of this regressive beach ridgeplain included the analysis of orthophotos; topographic detail (PRO-XRS Trimble®-post-processed); and shallow geophysical data with Ground Penetrating Radar (GPR), 150, 200 and 400 MHz antennae, combined with facies analysis and radiocarbon dating (AMS) and Optically Stimulated Luminescence (OSL) from shallow borehole samples. The analysis of orthophotos allowed for the definition of at least nine morphologically distinct series of progradation, marked by truncations of progressive orientation changes. The integration of topographically corrected GPR data, sedimentary records, and geochronological data determined the beginning of the progradation occurred at 7.2 kaBP. At the beginning of progradation, the low tide terrace was at the height of 1.9m (EGM96) Above the Sea Current Level (ASCL). The swash zone was in the 2.5m, and the crest reached 4.3m ASCL. Currently, the low tide terrace quota is -0.4m, the swash zone to 0.3m and the crest reaches 2.1m ASCL. Among other factors, the fall of the lagoon base levels was associated with sea level fall during the Holocene regression. However, crest construction control is dependent on the lagoon base level oscillation, which in turn is controlled by the precipitation regime and storms surges. Moreover, these results suggest that the orientation of the ridges was controlled by changes in the internal lagoon hydrodynamics, due to the progressive narrowing of the lagoon connection with the open ocean.
publishDate 2018
dc.date.accessioned.none.fl_str_mv 2018-11-20T20:31:52Z
dc.date.available.none.fl_str_mv 2018-11-20T20:31:52Z
dc.date.issued.none.fl_str_mv 2018-02-10
dc.type.spa.fl_str_mv Artículo de revista
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dc.type.content.spa.fl_str_mv Text
dc.type.driver.spa.fl_str_mv info:eu-repo/semantics/article
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dc.identifier.issn.spa.fl_str_mv 07490208
dc.identifier.uri.spa.fl_str_mv https://hdl.handle.net/11323/1506
dc.identifier.doi.spa.fl_str_mv https://doi.org/10.2112/SI85-131.1
dc.identifier.instname.spa.fl_str_mv Corporación Universidad de la Costa
dc.identifier.reponame.spa.fl_str_mv REDICUC - Repositorio CUC
dc.identifier.repourl.spa.fl_str_mv https://repositorio.cuc.edu.co/
identifier_str_mv 07490208
Corporación Universidad de la Costa
REDICUC - Repositorio CUC
url https://hdl.handle.net/11323/1506
https://doi.org/10.2112/SI85-131.1
https://repositorio.cuc.edu.co/
dc.language.iso.none.fl_str_mv eng
language eng
dc.rights.spa.fl_str_mv Atribución – No comercial – Compartir igual
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rights_invalid_str_mv Atribución – No comercial – Compartir igual
http://purl.org/coar/access_right/c_abf2
eu_rights_str_mv openAccess
dc.publisher.spa.fl_str_mv Journal Of Coastal Research
institution Corporación Universidad de la Costa
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spelling Portantiolo Manzolli, RogerioPortz, Luana CarlaDe Bitencourt Borges, Volney JuniorAmabile Leal, RenatoMartins Marques, EduardoBiancini Da Silva, AndersonGuimarães Barboza, EduardoCaron, FelipeAlcantara Carrio, JavierOliveira Sawakuchi, Andre2018-11-20T20:31:52Z2018-11-20T20:31:52Z2018-02-1007490208https://hdl.handle.net/11323/1506https://doi.org/10.2112/SI85-131.1Corporación Universidad de la CostaREDICUC - Repositorio CUChttps://repositorio.cuc.edu.co/The origin and geological evolution of a complex of a beach ridgeplain in the Feitoria lagoon-barrier, located on the western margin of the southern cell Patos lagoon, Brazil was influenced by the interactions between the alocyclic (climate change and relative sea level) and autocyclic (sediment supply, waves, longshore drift and storm surges) forcing. The study of this regressive beach ridgeplain included the analysis of orthophotos; topographic detail (PRO-XRS Trimble®-post-processed); and shallow geophysical data with Ground Penetrating Radar (GPR), 150, 200 and 400 MHz antennae, combined with facies analysis and radiocarbon dating (AMS) and Optically Stimulated Luminescence (OSL) from shallow borehole samples. The analysis of orthophotos allowed for the definition of at least nine morphologically distinct series of progradation, marked by truncations of progressive orientation changes. The integration of topographically corrected GPR data, sedimentary records, and geochronological data determined the beginning of the progradation occurred at 7.2 kaBP. At the beginning of progradation, the low tide terrace was at the height of 1.9m (EGM96) Above the Sea Current Level (ASCL). The swash zone was in the 2.5m, and the crest reached 4.3m ASCL. Currently, the low tide terrace quota is -0.4m, the swash zone to 0.3m and the crest reaches 2.1m ASCL. Among other factors, the fall of the lagoon base levels was associated with sea level fall during the Holocene regression. However, crest construction control is dependent on the lagoon base level oscillation, which in turn is controlled by the precipitation regime and storms surges. Moreover, these results suggest that the orientation of the ridges was controlled by changes in the internal lagoon hydrodynamics, due to the progressive narrowing of the lagoon connection with the open ocean.Portantiolo Manzolli, Rogerio-0000-0002-0223-5634-600Portz, Luana Carla-0000-0001-9232-8086-600De Bitencourt Borges, Volney Junior-75969dc0-7cef-42bc-9093-f6b47283cf65-0Amabile Leal, Renato-828a6871-7c1d-413c-8756-d5523a825c30-0Martins Marques, Eduardo-1c37171f-489d-4ff0-8eb4-d3f8498b76e0-0Biancini Da Silva, Anderson-e105b896-3ac4-42e5-b6ec-acbb48ac6eaf-0Guimarães Barboza, Eduardo-346b833b-c4d6-49a4-a4dc-25fd91326f63-0Caron, Felipe-7afa47f6-6236-40a3-836b-79067674491c-0Alcantara Carrio, Javier-383e9689-8093-46ea-a1ab-ccbc2bf38f69-0Oliveira Sawakuchi, Andre-bfdde8cc-0326-4020-8a53-1f49363cfc2d-0engJournal Of Coastal ResearchAtribución – No comercial – Compartir igualinfo:eu-repo/semantics/openAccesshttp://purl.org/coar/access_right/c_abf2Barrier-lagoon system into lagoonBeach-ridge plainCoastal evolutionGPRProcess control in the geneses and evolution of a lagoon-barrier system inside of the patos lagoon, south of BrazilArtículo de revistahttp://purl.org/coar/resource_type/c_6501http://purl.org/coar/resource_type/c_2df8fbb1Textinfo:eu-repo/semantics/articlehttp://purl.org/redcol/resource_type/ARTinfo:eu-repo/semantics/acceptedVersionPublicationORIGINALProcess Control In The Geneses And Evolution.pdfProcess Control In The Geneses And Evolution.pdfapplication/pdf182509https://repositorio.cuc.edu.co/bitstreams/b7a26ca5-0425-4a40-a770-6b9c04d0ecd2/download59c4c9ec15de6672f4a589554998830cMD51LICENSElicense.txtlicense.txttext/plain; charset=utf-81748https://repositorio.cuc.edu.co/bitstreams/9c4f3429-2518-4081-b3f0-311daa063259/download8a4605be74aa9ea9d79846c1fba20a33MD52THUMBNAILProcess Control In The Geneses And Evolution.pdf.jpgProcess Control In The Geneses And Evolution.pdf.jpgimage/jpeg58292https://repositorio.cuc.edu.co/bitstreams/efbc7f6d-4b58-40c2-8edc-de750cdf784f/downloada3bde24c9694afeccfff8f8e6634978bMD54TEXTProcess Control In The Geneses And Evolution.pdf.txtProcess Control In The Geneses And Evolution.pdf.txttext/plain2379https://repositorio.cuc.edu.co/bitstreams/be5e6616-e863-4364-ac7a-ef628b57b3cb/download3a334a789a5e7e04a564147b7b8653feMD5511323/1506oai:repositorio.cuc.edu.co:11323/15062024-09-17 10:46:31.257open.accesshttps://repositorio.cuc.edu.coRepositorio de la Universidad de la Costa CUCrepdigital@cuc.edu.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