Benthic-pelagic uncoupling between the Northern Patagonian Frontal System and Patagonian scallop beds

Autores
Franco, Barbara Cristie; Palma, Elbio Daniel; Tonini, Mariano Hernan
Año de publicación
2014
Idioma
inglés
Tipo de recurso
artículo
Estado
versión publicada
Descripción
Availability of planktonic food in the bottom is the most important factor to explain the persistence and recurrent localization of Patagonian scallop (Zygochlamys patagonica) populations. The establishment of the scallop Sea Bay bed (SBB) has been related with food supply from the Northern Patagonian Frontal System (NPFS). In this article outputs from high resolution numerical models combined with particle tracking methods were used to identify for the first time potential physical mechanisms of food transfer. The model results showed no evidence of benthic-pelagic coupling between the NPFS and the SBB. They also revealed that the dominant instantaneous semidiurnal tidal currents and the mean N-NE flow on the inner-middle Patagonian shelf are the main dynamical mechanisms preventing particles released at the surface of the NPFS to reach the SBB area. Sensitivity studies changing the stochastic numerical method for solving the particle trajectories, the release month and location of the particles, the magnitude of the horizontal turbulent diffusion and the frequency of the wind forcing did not alter this conclusion significantly.
Fil: Franco, Barbara Cristie. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinacion Administrativa Ciudad Universitaria. Centro de Investigaciones del Mar y la Atmósfera; Argentina
Fil: Palma, Elbio Daniel. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Bahía Blanca. Instituto Argentino de Oceanografía (i); Argentina. Universidad Nacional del Sur. Departamento de Física; Argentina
Fil: Tonini, Mariano Hernan. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Bahía Blanca. Instituto Argentino de Oceanografía (i); Argentina. Universidad Nacional del Sur. Departamento de Física; Argentina
Materia
Benthic-Pelagic Coupling
Northern Patagonian Frontal System
Stochastic Processes
Scallop Beds
Nivel de accesibilidad
acceso abierto
Condiciones de uso
https://creativecommons.org/licenses/by-nc-nd/2.5/ar/
Repositorio
CONICET Digital (CONICET)
Institución
Consejo Nacional de Investigaciones Científicas y Técnicas
OAI Identificador
oai:ri.conicet.gov.ar:11336/4437
Acceder
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network_name_str CONICET Digital (CONICET)
spelling Benthic-pelagic uncoupling between the Northern Patagonian Frontal System and Patagonian scallop bedsFranco, Barbara CristiePalma, Elbio DanielTonini, Mariano HernanBenthic-Pelagic CouplingNorthern Patagonian Frontal SystemStochastic ProcessesScallop Bedshttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1Availability of planktonic food in the bottom is the most important factor to explain the persistence and recurrent localization of Patagonian scallop (Zygochlamys patagonica) populations. The establishment of the scallop Sea Bay bed (SBB) has been related with food supply from the Northern Patagonian Frontal System (NPFS). In this article outputs from high resolution numerical models combined with particle tracking methods were used to identify for the first time potential physical mechanisms of food transfer. The model results showed no evidence of benthic-pelagic coupling between the NPFS and the SBB. They also revealed that the dominant instantaneous semidiurnal tidal currents and the mean N-NE flow on the inner-middle Patagonian shelf are the main dynamical mechanisms preventing particles released at the surface of the NPFS to reach the SBB area. Sensitivity studies changing the stochastic numerical method for solving the particle trajectories, the release month and location of the particles, the magnitude of the horizontal turbulent diffusion and the frequency of the wind forcing did not alter this conclusion significantly.Fil: Franco, Barbara Cristie. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinacion Administrativa Ciudad Universitaria. Centro de Investigaciones del Mar y la Atmósfera; ArgentinaFil: Palma, Elbio Daniel. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Bahía Blanca. Instituto Argentino de Oceanografía (i); Argentina. Universidad Nacional del Sur. Departamento de Física; ArgentinaFil: Tonini, Mariano Hernan. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Bahía Blanca. Instituto Argentino de Oceanografía (i); Argentina. Universidad Nacional del Sur. Departamento de Física; ArgentinaElsevier2014-12info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/4437Franco, Barbara Cristie; Palma, Elbio Daniel; Tonini, Mariano Hernan; Benthic-pelagic uncoupling between the Northern Patagonian Frontal System and Patagonian scallop beds; Elsevier; Estuarine Coastal and Shelf Science; 153; 12-2014; 145-1550272-7714enginfo:eu-repo/semantics/altIdentifier/url/http://www.sciencedirect.com/science/article/pii/S0272771414003771info:eu-repo/semantics/altIdentifier/doi/10.1016/j.ecss.2014.12.006info:eu-repo/semantics/altIdentifier/issn/0272-7714info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-nd/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-29T10:02:18Zoai:ri.conicet.gov.ar:11336/4437instacron:CONICETInstitucionalhttp://ri.conicet.gov.ar/Organismo científico-tecnológicoNo correspondehttp://ri.conicet.gov.ar/oai/requestdasensio@conicet.gov.ar; lcarlino@conicet.gov.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:34982025-09-29 10:02:18.834CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse
dc.title.none.fl_str_mv Benthic-pelagic uncoupling between the Northern Patagonian Frontal System and Patagonian scallop beds
title Benthic-pelagic uncoupling between the Northern Patagonian Frontal System and Patagonian scallop beds
spellingShingle Benthic-pelagic uncoupling between the Northern Patagonian Frontal System and Patagonian scallop beds
Franco, Barbara Cristie
Benthic-Pelagic Coupling
Northern Patagonian Frontal System
Stochastic Processes
Scallop Beds
title_short Benthic-pelagic uncoupling between the Northern Patagonian Frontal System and Patagonian scallop beds
title_full Benthic-pelagic uncoupling between the Northern Patagonian Frontal System and Patagonian scallop beds
title_fullStr Benthic-pelagic uncoupling between the Northern Patagonian Frontal System and Patagonian scallop beds
title_full_unstemmed Benthic-pelagic uncoupling between the Northern Patagonian Frontal System and Patagonian scallop beds
title_sort Benthic-pelagic uncoupling between the Northern Patagonian Frontal System and Patagonian scallop beds
dc.creator.none.fl_str_mv Franco, Barbara Cristie
Palma, Elbio Daniel
Tonini, Mariano Hernan
author Franco, Barbara Cristie
author_facet Franco, Barbara Cristie
Palma, Elbio Daniel
Tonini, Mariano Hernan
author_role author
author2 Palma, Elbio Daniel
Tonini, Mariano Hernan
author2_role author
author
dc.subject.none.fl_str_mv Benthic-Pelagic Coupling
Northern Patagonian Frontal System
Stochastic Processes
Scallop Beds
topic Benthic-Pelagic Coupling
Northern Patagonian Frontal System
Stochastic Processes
Scallop Beds
purl_subject.fl_str_mv https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
dc.description.none.fl_txt_mv Availability of planktonic food in the bottom is the most important factor to explain the persistence and recurrent localization of Patagonian scallop (Zygochlamys patagonica) populations. The establishment of the scallop Sea Bay bed (SBB) has been related with food supply from the Northern Patagonian Frontal System (NPFS). In this article outputs from high resolution numerical models combined with particle tracking methods were used to identify for the first time potential physical mechanisms of food transfer. The model results showed no evidence of benthic-pelagic coupling between the NPFS and the SBB. They also revealed that the dominant instantaneous semidiurnal tidal currents and the mean N-NE flow on the inner-middle Patagonian shelf are the main dynamical mechanisms preventing particles released at the surface of the NPFS to reach the SBB area. Sensitivity studies changing the stochastic numerical method for solving the particle trajectories, the release month and location of the particles, the magnitude of the horizontal turbulent diffusion and the frequency of the wind forcing did not alter this conclusion significantly.
Fil: Franco, Barbara Cristie. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinacion Administrativa Ciudad Universitaria. Centro de Investigaciones del Mar y la Atmósfera; Argentina
Fil: Palma, Elbio Daniel. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Bahía Blanca. Instituto Argentino de Oceanografía (i); Argentina. Universidad Nacional del Sur. Departamento de Física; Argentina
Fil: Tonini, Mariano Hernan. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Bahía Blanca. Instituto Argentino de Oceanografía (i); Argentina. Universidad Nacional del Sur. Departamento de Física; Argentina
description Availability of planktonic food in the bottom is the most important factor to explain the persistence and recurrent localization of Patagonian scallop (Zygochlamys patagonica) populations. The establishment of the scallop Sea Bay bed (SBB) has been related with food supply from the Northern Patagonian Frontal System (NPFS). In this article outputs from high resolution numerical models combined with particle tracking methods were used to identify for the first time potential physical mechanisms of food transfer. The model results showed no evidence of benthic-pelagic coupling between the NPFS and the SBB. They also revealed that the dominant instantaneous semidiurnal tidal currents and the mean N-NE flow on the inner-middle Patagonian shelf are the main dynamical mechanisms preventing particles released at the surface of the NPFS to reach the SBB area. Sensitivity studies changing the stochastic numerical method for solving the particle trajectories, the release month and location of the particles, the magnitude of the horizontal turbulent diffusion and the frequency of the wind forcing did not alter this conclusion significantly.
publishDate 2014
dc.date.none.fl_str_mv 2014-12
dc.type.none.fl_str_mv info:eu-repo/semantics/article
info:eu-repo/semantics/publishedVersion
http://purl.org/coar/resource_type/c_6501
info:ar-repo/semantics/articulo
format article
status_str publishedVersion
dc.identifier.none.fl_str_mv http://hdl.handle.net/11336/4437
Franco, Barbara Cristie; Palma, Elbio Daniel; Tonini, Mariano Hernan; Benthic-pelagic uncoupling between the Northern Patagonian Frontal System and Patagonian scallop beds; Elsevier; Estuarine Coastal and Shelf Science; 153; 12-2014; 145-155
0272-7714
url http://hdl.handle.net/11336/4437
identifier_str_mv Franco, Barbara Cristie; Palma, Elbio Daniel; Tonini, Mariano Hernan; Benthic-pelagic uncoupling between the Northern Patagonian Frontal System and Patagonian scallop beds; Elsevier; Estuarine Coastal and Shelf Science; 153; 12-2014; 145-155
0272-7714
dc.language.none.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv info:eu-repo/semantics/altIdentifier/url/http://www.sciencedirect.com/science/article/pii/S0272771414003771
info:eu-repo/semantics/altIdentifier/doi/10.1016/j.ecss.2014.12.006
info:eu-repo/semantics/altIdentifier/issn/0272-7714
dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
https://creativecommons.org/licenses/by-nc-nd/2.5/ar/
eu_rights_str_mv openAccess
rights_invalid_str_mv https://creativecommons.org/licenses/by-nc-nd/2.5/ar/
dc.format.none.fl_str_mv application/pdf
application/pdf
application/pdf
application/pdf
dc.publisher.none.fl_str_mv Elsevier
publisher.none.fl_str_mv Elsevier
dc.source.none.fl_str_mv reponame:CONICET Digital (CONICET)
instname:Consejo Nacional de Investigaciones Científicas y Técnicas
reponame_str CONICET Digital (CONICET)
collection CONICET Digital (CONICET)
instname_str Consejo Nacional de Investigaciones Científicas y Técnicas
repository.name.fl_str_mv CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicas
repository.mail.fl_str_mv dasensio@conicet.gov.ar; lcarlino@conicet.gov.ar
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score 13.070432

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