Seafloor geomorphology of the northern Argentine continental slope at 40-41° S mapped from high-resolution bathymetry
The southern sector of the northern Argentine continental margin (NACM), extending from 40 to 41° S, corresponds to a previously unmapped area of the South Atlantic Ocean in term of high-resolution bathymetry. Newly acquired high resolution data in the slope sector of the NACM between 900 and 5000 m...
Published in: | Journal of South American Earth Sciences |
---|---|
Main Authors: | , , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Pergamon-Elsevier Science Ltd
|
Subjects: | |
Online Access: | http://hdl.handle.net/11336/230838 |
_version_ | 1821713665249771520 |
---|---|
author | Principi, Sebastián Palma, Fermin Ignacio Bran, Donaldo Mauricio Bozzano, Graziella Isola, José Ignacio Ormazabal, Juan Pablo Esteban, Federico Damián Acosta, Luana Yazmin Tassone, Alejandro Alberto |
author_facet | Principi, Sebastián Palma, Fermin Ignacio Bran, Donaldo Mauricio Bozzano, Graziella Isola, José Ignacio Ormazabal, Juan Pablo Esteban, Federico Damián Acosta, Luana Yazmin Tassone, Alejandro Alberto |
author_sort | Principi, Sebastián |
collection | CONICET Digital (Consejo Nacional de Investigaciones Científicas y Técnicas) |
container_start_page | 104748 |
container_title | Journal of South American Earth Sciences |
container_volume | 134 |
description | The southern sector of the northern Argentine continental margin (NACM), extending from 40 to 41° S, corresponds to a previously unmapped area of the South Atlantic Ocean in term of high-resolution bathymetry. Newly acquired high resolution data in the slope sector of the NACM between 900 and 5000 m allowed us to carry out a geomorphological analysis by combining novel multibeam data with a very high-resolution 3D seismic-derived bathymetry. The resultant digital elevation model revealed the presence of a wide variety of seafloor features and allowed us to characterize them by a geomorphometric analysis. Along slope processes, produced by the interaction of contour currents with the seafloor, make up a large array of erosional and depositional elements on the slope, including a contourite terrace, scours, drift bodies and sediment waves, that as a whole form part of a Contourite Depositional System (CDS). Additionally, across slope processes are also present, and give origin to four deeply incised submarine canyons that intersect the CDS. Overall, this work reveals the geomorphological complexity of this sector of the NACM and serves as a reference point for further studies regarding the sedimentary processes and oceanographic dynamics acting in the continental slope. Fil: Principi, Sebastián. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Geociencias Básicas, Aplicadas y Ambientales de Buenos Aires. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Geociencias Básicas, Aplicadas y Ambientales de Buenos Aires; Argentina. YPF - Tecnología; Argentina Fil: Palma, Fermin Ignacio. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Geociencias Básicas, Aplicadas y Ambientales de Buenos Aires. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Geociencias Básicas, Aplicadas y ... |
format | Article in Journal/Newspaper |
genre | South Atlantic Ocean |
genre_facet | South Atlantic Ocean |
geographic | Argentina Argentine |
geographic_facet | Argentina Argentine |
id | ftconicet:oai:ri.conicet.gov.ar:11336/230838 |
institution | Open Polar |
language | English |
op_collection_id | ftconicet |
op_doi | https://doi.org/10.1016/j.jsames.2023.104748 |
op_relation | info:eu-repo/semantics/altIdentifier/url/https://linkinghub.elsevier.com/retrieve/pii/S0895981123005606 info:eu-repo/semantics/altIdentifier/doi/10.1016/j.jsames.2023.104748 http://hdl.handle.net/11336/230838 CONICET Digital CONICET |
op_rights | info:eu-repo/semantics/embargoedAccess https://creativecommons.org/licenses/by-nc-sa/2.5/ar/ |
publisher | Pergamon-Elsevier Science Ltd |
record_format | openpolar |
spelling | ftconicet:oai:ri.conicet.gov.ar:11336/230838 2025-01-17T00:50:12+00:00 Seafloor geomorphology of the northern Argentine continental slope at 40-41° S mapped from high-resolution bathymetry Principi, Sebastián Palma, Fermin Ignacio Bran, Donaldo Mauricio Bozzano, Graziella Isola, José Ignacio Ormazabal, Juan Pablo Esteban, Federico Damián Acosta, Luana Yazmin Tassone, Alejandro Alberto application/pdf http://hdl.handle.net/11336/230838 eng eng Pergamon-Elsevier Science Ltd info:eu-repo/semantics/altIdentifier/url/https://linkinghub.elsevier.com/retrieve/pii/S0895981123005606 info:eu-repo/semantics/altIdentifier/doi/10.1016/j.jsames.2023.104748 http://hdl.handle.net/11336/230838 CONICET Digital CONICET info:eu-repo/semantics/embargoedAccess https://creativecommons.org/licenses/by-nc-sa/2.5/ar/ ARGENTINE CONTINENTAL MARGIN CONTOURITE DRIFTS MARINE GEOMORPHOLOGY SEAFLOOR MAPPING SEDIMENT WAVES SUBMARINE CANYON SW ATLANTIC https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 info:eu-repo/semantics/article info:ar-repo/semantics/artículo info:eu-repo/semantics/publishedVersion ftconicet https://doi.org/10.1016/j.jsames.2023.104748 2024-10-04T09:34:17Z The southern sector of the northern Argentine continental margin (NACM), extending from 40 to 41° S, corresponds to a previously unmapped area of the South Atlantic Ocean in term of high-resolution bathymetry. Newly acquired high resolution data in the slope sector of the NACM between 900 and 5000 m allowed us to carry out a geomorphological analysis by combining novel multibeam data with a very high-resolution 3D seismic-derived bathymetry. The resultant digital elevation model revealed the presence of a wide variety of seafloor features and allowed us to characterize them by a geomorphometric analysis. Along slope processes, produced by the interaction of contour currents with the seafloor, make up a large array of erosional and depositional elements on the slope, including a contourite terrace, scours, drift bodies and sediment waves, that as a whole form part of a Contourite Depositional System (CDS). Additionally, across slope processes are also present, and give origin to four deeply incised submarine canyons that intersect the CDS. Overall, this work reveals the geomorphological complexity of this sector of the NACM and serves as a reference point for further studies regarding the sedimentary processes and oceanographic dynamics acting in the continental slope. Fil: Principi, Sebastián. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Geociencias Básicas, Aplicadas y Ambientales de Buenos Aires. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Geociencias Básicas, Aplicadas y Ambientales de Buenos Aires; Argentina. YPF - Tecnología; Argentina Fil: Palma, Fermin Ignacio. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Geociencias Básicas, Aplicadas y Ambientales de Buenos Aires. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Geociencias Básicas, Aplicadas y ... Article in Journal/Newspaper South Atlantic Ocean CONICET Digital (Consejo Nacional de Investigaciones Científicas y Técnicas) Argentina Argentine Journal of South American Earth Sciences 134 104748 |
spellingShingle | ARGENTINE CONTINENTAL MARGIN CONTOURITE DRIFTS MARINE GEOMORPHOLOGY SEAFLOOR MAPPING SEDIMENT WAVES SUBMARINE CANYON SW ATLANTIC https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 Principi, Sebastián Palma, Fermin Ignacio Bran, Donaldo Mauricio Bozzano, Graziella Isola, José Ignacio Ormazabal, Juan Pablo Esteban, Federico Damián Acosta, Luana Yazmin Tassone, Alejandro Alberto Seafloor geomorphology of the northern Argentine continental slope at 40-41° S mapped from high-resolution bathymetry |
title | Seafloor geomorphology of the northern Argentine continental slope at 40-41° S mapped from high-resolution bathymetry |
title_full | Seafloor geomorphology of the northern Argentine continental slope at 40-41° S mapped from high-resolution bathymetry |
title_fullStr | Seafloor geomorphology of the northern Argentine continental slope at 40-41° S mapped from high-resolution bathymetry |
title_full_unstemmed | Seafloor geomorphology of the northern Argentine continental slope at 40-41° S mapped from high-resolution bathymetry |
title_short | Seafloor geomorphology of the northern Argentine continental slope at 40-41° S mapped from high-resolution bathymetry |
title_sort | seafloor geomorphology of the northern argentine continental slope at 40-41° s mapped from high-resolution bathymetry |
topic | ARGENTINE CONTINENTAL MARGIN CONTOURITE DRIFTS MARINE GEOMORPHOLOGY SEAFLOOR MAPPING SEDIMENT WAVES SUBMARINE CANYON SW ATLANTIC https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 |
topic_facet | ARGENTINE CONTINENTAL MARGIN CONTOURITE DRIFTS MARINE GEOMORPHOLOGY SEAFLOOR MAPPING SEDIMENT WAVES SUBMARINE CANYON SW ATLANTIC https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 |
url | http://hdl.handle.net/11336/230838 |