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...
- 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 |
dc.type.coar.fl_str_mv |
http://purl.org/coar/resource_type/c_2df8fbb1 |
dc.type.coar.spa.fl_str_mv |
http://purl.org/coar/resource_type/c_6501 |
dc.type.content.spa.fl_str_mv |
Text |
dc.type.driver.spa.fl_str_mv |
info:eu-repo/semantics/article |
dc.type.redcol.spa.fl_str_mv |
http://purl.org/redcol/resource_type/ART |
dc.type.version.spa.fl_str_mv |
info:eu-repo/semantics/acceptedVersion |
format |
http://purl.org/coar/resource_type/c_6501 |
status_str |
acceptedVersion |
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 |
dc.rights.accessrights.spa.fl_str_mv |
info:eu-repo/semantics/openAccess |
dc.rights.coar.spa.fl_str_mv |
http://purl.org/coar/access_right/c_abf2 |
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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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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 |