Marine fronts at the continental shelves of austral South America: Physical and ecological processes

Neritic fronts are very abundant in austral South America, covering several scales of space and time. However, this region is poorly studied from a systemic point of view. Our main goal is to develop a holistic view of physical and ecological patterns and processes at austral South America, regardin...

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Autores principales: Acha, E.M., Mianzan, H.W., Guerrero, R.A., Favero, M., Bava, J.
Formato: JOUR
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Acceso en línea:http://hdl.handle.net/20.500.12110/paper_09247963_v44_n1-2_p83_Acha
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spelling todo:paper_09247963_v44_n1-2_p83_Acha2023-10-03T15:46:01Z Marine fronts at the continental shelves of austral South America: Physical and ecological processes Acha, E.M. Mianzan, H.W. Guerrero, R.A. Favero, M. Bava, J. 20-57° Lat. S 40-76° Long W Fronts Marine ecology Neritic province Physical oceanography Review South America Southeastern Pacific Southwestern Atlantic Chlorophyll Ecology Hydrographic surveys Ocean habitats Sea surface temperature Marine engineering biological oceanography continental shelf hydrographic survey oceanic front satellite imagery Atlantic Ocean Atlantic Ocean (Southwest) Pacific Ocean Pacific Ocean (Southeast) Argentina (fish) Aves Cephalopoda Invertebrata Pisces Neritic fronts are very abundant in austral South America, covering several scales of space and time. However, this region is poorly studied from a systemic point of view. Our main goal is to develop a holistic view of physical and ecological patterns and processes at austral South America, regarding frontal arrangements. Satellite information (sea surface temperature and chlorophyll concentration), and historical hydrographic data were employed to show fronts. We compiled all existing evidence (physical and biological) about fronts to identify regions defined by similar types of coastal fronts and to characterize them. Fronts in austral South America can be arranged in six zones according to their location, main forcing, key physical variables, seasonality, and enrichment mechanisms. Four zones, the Atlantic upwelling zone; the temperate estuarine zone; the Patagonian tidal zone and the Argentine shelf-break zone, occupy most of the Atlantic side. The Chile-Peru upwelling zone, on the Pacific, is the largest and best-known region. The Patagonian cold estuarine zone encompasses the tip of South America, connecting the Pacific and Atlantic oceans, and remains poorly studied. When observed at a continental scale, the Pacific coast dominated by two large frontal zones appears simplest than the Atlantic coast in terms of frontal richness. The extension of the continental shelf in the Atlantic coast allows for the development of a great diversity of mesoscale fronts. Though frontal zones we defined are extensive areas of the continental shelves, fronts inside the zones are comparatively small areas. Even so, they play a paramount role in ecological processes, allowing for high biological production; offering feeding and/or reproductive habitats for fishes, squids, and birds; acting as retention areas for larvae of benthic species; and promoting establishment of benthic invertebrates that benefit from the organic production in the frontal area. © 2003 Elsevier B.V. All rights reserved. JOUR info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by/2.5/ar http://hdl.handle.net/20.500.12110/paper_09247963_v44_n1-2_p83_Acha
institution Universidad de Buenos Aires
institution_str I-28
repository_str R-134
collection Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA)
topic 20-57° Lat. S
40-76° Long W
Fronts
Marine ecology
Neritic province
Physical oceanography
Review
South America
Southeastern Pacific
Southwestern Atlantic
Chlorophyll
Ecology
Hydrographic surveys
Ocean habitats
Sea surface temperature
Marine engineering
biological oceanography
continental shelf
hydrographic survey
oceanic front
satellite imagery
Atlantic Ocean
Atlantic Ocean (Southwest)
Pacific Ocean
Pacific Ocean (Southeast)
Argentina (fish)
Aves
Cephalopoda
Invertebrata
Pisces
spellingShingle 20-57° Lat. S
40-76° Long W
Fronts
Marine ecology
Neritic province
Physical oceanography
Review
South America
Southeastern Pacific
Southwestern Atlantic
Chlorophyll
Ecology
Hydrographic surveys
Ocean habitats
Sea surface temperature
Marine engineering
biological oceanography
continental shelf
hydrographic survey
oceanic front
satellite imagery
Atlantic Ocean
Atlantic Ocean (Southwest)
Pacific Ocean
Pacific Ocean (Southeast)
Argentina (fish)
Aves
Cephalopoda
Invertebrata
Pisces
Acha, E.M.
Mianzan, H.W.
Guerrero, R.A.
Favero, M.
Bava, J.
Marine fronts at the continental shelves of austral South America: Physical and ecological processes
topic_facet 20-57° Lat. S
40-76° Long W
Fronts
Marine ecology
Neritic province
Physical oceanography
Review
South America
Southeastern Pacific
Southwestern Atlantic
Chlorophyll
Ecology
Hydrographic surveys
Ocean habitats
Sea surface temperature
Marine engineering
biological oceanography
continental shelf
hydrographic survey
oceanic front
satellite imagery
Atlantic Ocean
Atlantic Ocean (Southwest)
Pacific Ocean
Pacific Ocean (Southeast)
Argentina (fish)
Aves
Cephalopoda
Invertebrata
Pisces
description Neritic fronts are very abundant in austral South America, covering several scales of space and time. However, this region is poorly studied from a systemic point of view. Our main goal is to develop a holistic view of physical and ecological patterns and processes at austral South America, regarding frontal arrangements. Satellite information (sea surface temperature and chlorophyll concentration), and historical hydrographic data were employed to show fronts. We compiled all existing evidence (physical and biological) about fronts to identify regions defined by similar types of coastal fronts and to characterize them. Fronts in austral South America can be arranged in six zones according to their location, main forcing, key physical variables, seasonality, and enrichment mechanisms. Four zones, the Atlantic upwelling zone; the temperate estuarine zone; the Patagonian tidal zone and the Argentine shelf-break zone, occupy most of the Atlantic side. The Chile-Peru upwelling zone, on the Pacific, is the largest and best-known region. The Patagonian cold estuarine zone encompasses the tip of South America, connecting the Pacific and Atlantic oceans, and remains poorly studied. When observed at a continental scale, the Pacific coast dominated by two large frontal zones appears simplest than the Atlantic coast in terms of frontal richness. The extension of the continental shelf in the Atlantic coast allows for the development of a great diversity of mesoscale fronts. Though frontal zones we defined are extensive areas of the continental shelves, fronts inside the zones are comparatively small areas. Even so, they play a paramount role in ecological processes, allowing for high biological production; offering feeding and/or reproductive habitats for fishes, squids, and birds; acting as retention areas for larvae of benthic species; and promoting establishment of benthic invertebrates that benefit from the organic production in the frontal area. © 2003 Elsevier B.V. All rights reserved.
format JOUR
author Acha, E.M.
Mianzan, H.W.
Guerrero, R.A.
Favero, M.
Bava, J.
author_facet Acha, E.M.
Mianzan, H.W.
Guerrero, R.A.
Favero, M.
Bava, J.
author_sort Acha, E.M.
title Marine fronts at the continental shelves of austral South America: Physical and ecological processes
title_short Marine fronts at the continental shelves of austral South America: Physical and ecological processes
title_full Marine fronts at the continental shelves of austral South America: Physical and ecological processes
title_fullStr Marine fronts at the continental shelves of austral South America: Physical and ecological processes
title_full_unstemmed Marine fronts at the continental shelves of austral South America: Physical and ecological processes
title_sort marine fronts at the continental shelves of austral south america: physical and ecological processes
url http://hdl.handle.net/20.500.12110/paper_09247963_v44_n1-2_p83_Acha
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