Geomorphological and stratigraphic evolution of a fluvial incision in the coastal plain and inner continental shelf in southern Brazil

This paper describes the evolution of a sector of the southern coastal plain of the Pelotas Basin, southern Brazil, between the last Pleistocene sea-level lowstand and the Holocene highstand, based on geomorphology and high-resolution stratigraphy. A fluvial drainage system associated with an incise...

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Autores:
Barboza, Eduardo G.
Dillenburg, Sérgio R.
Lopes, Renato P.
Rosa, Maria Luiza C.C.
Caron, Felipe
Abreu, Vitor
Manzolli, Rogério P.
Nunes, José Carlos R.
Weschenfelder, Jair
Tomazelli, Luiz J.
Tipo de recurso:
Article of journal
Fecha de publicación:
2021
Institución:
Corporación Universidad de la Costa
Repositorio:
REDICUC - Repositorio CUC
Idioma:
eng
OAI Identifier:
oai:repositorio.cuc.edu.co:11323/8434
Acceso en línea:
https://hdl.handle.net/11323/8434
https://doi.org/10.1016/j.margeo.2021.106514
https://repositorio.cuc.edu.co/
Palabra clave:
Taim swamp
Paleo-drainage
Mirim Lagoon
Holocene/Late-Pleistocene
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Attribution-NonCommercial-NoDerivatives 4.0 International
id RCUC2_82434aa59d0af8b02700337592817f83
oai_identifier_str oai:repositorio.cuc.edu.co:11323/8434
network_acronym_str RCUC2
network_name_str REDICUC - Repositorio CUC
repository_id_str
dc.title.spa.fl_str_mv Geomorphological and stratigraphic evolution of a fluvial incision in the coastal plain and inner continental shelf in southern Brazil
title Geomorphological and stratigraphic evolution of a fluvial incision in the coastal plain and inner continental shelf in southern Brazil
spellingShingle Geomorphological and stratigraphic evolution of a fluvial incision in the coastal plain and inner continental shelf in southern Brazil
Taim swamp
Paleo-drainage
Mirim Lagoon
Holocene/Late-Pleistocene
title_short Geomorphological and stratigraphic evolution of a fluvial incision in the coastal plain and inner continental shelf in southern Brazil
title_full Geomorphological and stratigraphic evolution of a fluvial incision in the coastal plain and inner continental shelf in southern Brazil
title_fullStr Geomorphological and stratigraphic evolution of a fluvial incision in the coastal plain and inner continental shelf in southern Brazil
title_full_unstemmed Geomorphological and stratigraphic evolution of a fluvial incision in the coastal plain and inner continental shelf in southern Brazil
title_sort Geomorphological and stratigraphic evolution of a fluvial incision in the coastal plain and inner continental shelf in southern Brazil
dc.creator.fl_str_mv Barboza, Eduardo G.
Dillenburg, Sérgio R.
Lopes, Renato P.
Rosa, Maria Luiza C.C.
Caron, Felipe
Abreu, Vitor
Manzolli, Rogério P.
Nunes, José Carlos R.
Weschenfelder, Jair
Tomazelli, Luiz J.
dc.contributor.author.spa.fl_str_mv Barboza, Eduardo G.
Dillenburg, Sérgio R.
Lopes, Renato P.
Rosa, Maria Luiza C.C.
Caron, Felipe
Abreu, Vitor
Manzolli, Rogério P.
Nunes, José Carlos R.
Weschenfelder, Jair
Tomazelli, Luiz J.
dc.subject.spa.fl_str_mv Taim swamp
Paleo-drainage
Mirim Lagoon
Holocene/Late-Pleistocene
topic Taim swamp
Paleo-drainage
Mirim Lagoon
Holocene/Late-Pleistocene
description This paper describes the evolution of a sector of the southern coastal plain of the Pelotas Basin, southern Brazil, between the last Pleistocene sea-level lowstand and the Holocene highstand, based on geomorphology and high-resolution stratigraphy. A fluvial drainage system associated with an incised valley developed during the Last Glacial Maximum (LGM) was identified. Two highresolution 2D and 2.5D geophysical profiles using Ground-Penetrating Radar (GPR) show a Pleistocene fluvial system's former path, starting close to its present mouth inside Mirim Lagoon crossing the coastal barriers and reaching the inner continental shelf, covering some 60 km across the coastal plain. During the LGM, with the sea-level at −120 to −130 m and the coastline positioned close to the shelf edge (distant 200 km from the present coastline), the fluvial system excavated a ~31.5-m deep channel. Two cores, 36 and 32 m long, show that the paleochannel was filled with sedimentary deposits after 19.4 ka BP, and the facies succession represents the transition from fluvial, to estuarine, to the coastal barrier, and finally to inner shelf depositional environments, generated by processes connected to LGM and the Postglacial Marine Transgression (PMT). The study region behaved as a sediment by-pass zone, connecting the adjacent coastal plain's inner portion with the inner continental shelf. The studied area presents an unusual record of the LGM at a coastal plain domain.
publishDate 2021
dc.date.accessioned.none.fl_str_mv 2021-06-29T21:34:03Z
dc.date.available.none.fl_str_mv 2021-06-29T21:34:03Z
dc.date.issued.none.fl_str_mv 2021
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.uri.spa.fl_str_mv https://hdl.handle.net/11323/8434
dc.identifier.doi.spa.fl_str_mv https://doi.org/10.1016/j.margeo.2021.106514
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/
url https://hdl.handle.net/11323/8434
https://doi.org/10.1016/j.margeo.2021.106514
https://repositorio.cuc.edu.co/
identifier_str_mv Corporación Universidad de la Costa
REDICUC - Repositorio CUC
dc.language.iso.none.fl_str_mv eng
language eng
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spelling Barboza, Eduardo G.Dillenburg, Sérgio R.Lopes, Renato P.Rosa, Maria Luiza C.C.Caron, FelipeAbreu, VitorManzolli, Rogério P.Nunes, José Carlos R.Weschenfelder, JairTomazelli, Luiz J.2021-06-29T21:34:03Z2021-06-29T21:34:03Z2021https://hdl.handle.net/11323/8434https://doi.org/10.1016/j.margeo.2021.106514Corporación Universidad de la CostaREDICUC - Repositorio CUChttps://repositorio.cuc.edu.co/This paper describes the evolution of a sector of the southern coastal plain of the Pelotas Basin, southern Brazil, between the last Pleistocene sea-level lowstand and the Holocene highstand, based on geomorphology and high-resolution stratigraphy. A fluvial drainage system associated with an incised valley developed during the Last Glacial Maximum (LGM) was identified. Two highresolution 2D and 2.5D geophysical profiles using Ground-Penetrating Radar (GPR) show a Pleistocene fluvial system's former path, starting close to its present mouth inside Mirim Lagoon crossing the coastal barriers and reaching the inner continental shelf, covering some 60 km across the coastal plain. During the LGM, with the sea-level at −120 to −130 m and the coastline positioned close to the shelf edge (distant 200 km from the present coastline), the fluvial system excavated a ~31.5-m deep channel. Two cores, 36 and 32 m long, show that the paleochannel was filled with sedimentary deposits after 19.4 ka BP, and the facies succession represents the transition from fluvial, to estuarine, to the coastal barrier, and finally to inner shelf depositional environments, generated by processes connected to LGM and the Postglacial Marine Transgression (PMT). The study region behaved as a sediment by-pass zone, connecting the adjacent coastal plain's inner portion with the inner continental shelf. The studied area presents an unusual record of the LGM at a coastal plain domain.Barboza, Eduardo G.Dillenburg, Sérgio R.Lopes, Renato P.Rosa, Maria Luiza C.C.Caron, FelipeAbreu, VitorManzolli, Rogério P.Nunes, José Carlos R.Weschenfelder, JairTomazelli, Luiz J.application/pdfengAttribution-NonCommercial-NoDerivatives 4.0 Internationalhttp://creativecommons.org/licenses/by-nc-nd/4.0/info:eu-repo/semantics/openAccesshttp://purl.org/coar/access_right/c_abf2Marine Geologyhttps://www.sciencedirect.com/science/article/abs/pii/S0025322721000967Taim swampPaleo-drainageMirim LagoonHolocene/Late-PleistoceneGeomorphological and stratigraphic evolution of a fluvial incision in the coastal plain and inner continental shelf in southern 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/acceptedVersionJ.G.N. Abreu, L.J. 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