Oceanographic processes and morphosedimentary products along the Iberian margins: A new multidisciplinary approach

Our understanding of bottom-currents and associated oceanographic processes (e.g., overflows, barotropic tidal currents) including intermittent processes (e.g., vertical eddies, deep sea storms, horizontal vortices, internal waves and tsunamis) is rapidly evolving. Many deep-water processes remain p...

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Autores: Hernández-Molina, Francisco J., Wåhlin, Anna, Bruno, Miguel, Ercilla, Gemma, Llave, Estefanía, Serra, Nuno, Rosón, Gabriel, Puig, Pere, Rebesco, Michele, Van Rooij, David, González-Pola, César, Sánchez, Francisco, Gómez-Ballesteros, María, Preu, Benedict, Schwenk, Tilmann, Hanebuth, T.J.J., Sánchez-Leal, Ricardo Félix, García-Lafuente, J.M., Brackenbridge, Rachel E., Juan, Carmen, Stow, Dorrik A. V., Sánchez-González, José María
Tipo de recurso: artículo
Estado:Versión aceptada para publicación
Fecha de publicación:2016
País:España
Institución:Consejo Superior de Investigaciones Científicas (CSIC)
Repositorio:DIGITAL.CSIC. Repositorio Institucional del CSIC
OAI Identifier:oai:digital.csic.es:10261/318862
Acceso en línea:http://hdl.handle.net/10261/318862
Access Level:acceso abierto
Palabra clave:Medio Marino
Centro Oceanográfico de Cádiz
Iberian margins
Oceanographic processes
Bottom currents
Sedimentary processes
Contourites
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spelling Oceanographic processes and morphosedimentary products along the Iberian margins: A new multidisciplinary approachHernández-Molina, Francisco J.Wåhlin, AnnaBruno, MiguelErcilla, GemmaLlave, EstefaníaSerra, NunoRosón, GabrielPuig, PereRebesco, MicheleVan Rooij, DavidGonzález-Pola, CésarSánchez, FranciscoGómez-Ballesteros, MaríaPreu, BenedictSchwenk, TilmannHanebuth, T.J.J.Sánchez-Leal, Ricardo FélixGarcía-Lafuente, J.M.Brackenbridge, Rachel E.Juan, CarmenStow, Dorrik A. V.Sánchez-González, José MaríaMedio MarinoCentro Oceanográfico de CádizIberian marginsOceanographic processesBottom currentsSedimentary processesContouritesOur understanding of bottom-currents and associated oceanographic processes (e.g., overflows, barotropic tidal currents) including intermittent processes (e.g., vertical eddies, deep sea storms, horizontal vortices, internal waves and tsunamis) is rapidly evolving. Many deep-water processes remain poorly understood due to limited direct observations, but can generate significant depositional and erosional features on both short and long term time scales. This paper represents a review work, which describes for the first time these oceanographic processes and examines their potential role in the sedimentary features along the Iberian continental margins. This review explores the implications of the studied processes, given their secondary role relative to other factors such as mass-transport and turbiditic processes, and highlights three major results: a) contourite depositional and erosional features are ubiquitous along the margins, indicating that bottom currents and associated oceanographic processes control the physiography and sedimentation; b) the position of interfaces between major water masses and their vertical and spatial variation in time specifically appears to exert primary control in determining major morphologic changes along the slope gradient, including the contourite terraces development; and c) contourites deposits exhibit greater variation than the established facies model suggests. Therefore, a consistent facies model however faces substantial challenges in terms of the wide range of oceanographic processes that can influence in their development. An integrated interpretation of these oceanographic processes requires an understanding of contourites, seafloor features, their spatial and temporal evolution, and the near-bottom flows that form them. This approach will synthesize oceanographic data, seafloor morphology, sediments and seismic images to improve our knowledge of permanent and intermittent processes around Iberia, and evaluate their conceptual and regional role in the margin's sedimentary evolution. Given their complexes, three-dimensional and temporally-variable nature, integration of these processes into sedimentary, oceanographic and climatological frameworks will require a multidisciplinary approach that includes Geology, Physical oceanography, Paleoceanography and Benthic Biology.SI202320232016info:eu-repo/semantics/articlehttp://purl.org/coar/resource_type/c_6501Postprintinfo:eu-repo/semantics/acceptedVersionhttp://hdl.handle.net/10261/318862reponame:DIGITAL.CSIC. Repositorio Institucional del CSICinstname:Consejo Superior de Investigaciones Científicas (CSIC)InglésCentro Oceanográfico de Cádizinfo:eu-repo/semantics/openAccessoai:digital.csic.es:10261/3188622026-05-22T06:33:51Z
dc.title.none.fl_str_mv Oceanographic processes and morphosedimentary products along the Iberian margins: A new multidisciplinary approach
title Oceanographic processes and morphosedimentary products along the Iberian margins: A new multidisciplinary approach
spellingShingle Oceanographic processes and morphosedimentary products along the Iberian margins: A new multidisciplinary approach
Hernández-Molina, Francisco J.
Medio Marino
Centro Oceanográfico de Cádiz
Iberian margins
Oceanographic processes
Bottom currents
Sedimentary processes
Contourites
title_short Oceanographic processes and morphosedimentary products along the Iberian margins: A new multidisciplinary approach
title_full Oceanographic processes and morphosedimentary products along the Iberian margins: A new multidisciplinary approach
title_fullStr Oceanographic processes and morphosedimentary products along the Iberian margins: A new multidisciplinary approach
title_full_unstemmed Oceanographic processes and morphosedimentary products along the Iberian margins: A new multidisciplinary approach
title_sort Oceanographic processes and morphosedimentary products along the Iberian margins: A new multidisciplinary approach
dc.creator.none.fl_str_mv Hernández-Molina, Francisco J.
Wåhlin, Anna
Bruno, Miguel
Ercilla, Gemma
Llave, Estefanía
Serra, Nuno
Rosón, Gabriel
Puig, Pere
Rebesco, Michele
Van Rooij, David
González-Pola, César
Sánchez, Francisco
Gómez-Ballesteros, María
Preu, Benedict
Schwenk, Tilmann
Hanebuth, T.J.J.
Sánchez-Leal, Ricardo Félix
García-Lafuente, J.M.
Brackenbridge, Rachel E.
Juan, Carmen
Stow, Dorrik A. V.
Sánchez-González, José María
author Hernández-Molina, Francisco J.
author_facet Hernández-Molina, Francisco J.
Wåhlin, Anna
Bruno, Miguel
Ercilla, Gemma
Llave, Estefanía
Serra, Nuno
Rosón, Gabriel
Puig, Pere
Rebesco, Michele
Van Rooij, David
González-Pola, César
Sánchez, Francisco
Gómez-Ballesteros, María
Preu, Benedict
Schwenk, Tilmann
Hanebuth, T.J.J.
Sánchez-Leal, Ricardo Félix
García-Lafuente, J.M.
Brackenbridge, Rachel E.
Juan, Carmen
Stow, Dorrik A. V.
Sánchez-González, José María
author_role author
author2 Wåhlin, Anna
Bruno, Miguel
Ercilla, Gemma
Llave, Estefanía
Serra, Nuno
Rosón, Gabriel
Puig, Pere
Rebesco, Michele
Van Rooij, David
González-Pola, César
Sánchez, Francisco
Gómez-Ballesteros, María
Preu, Benedict
Schwenk, Tilmann
Hanebuth, T.J.J.
Sánchez-Leal, Ricardo Félix
García-Lafuente, J.M.
Brackenbridge, Rachel E.
Juan, Carmen
Stow, Dorrik A. V.
Sánchez-González, José María
author2_role author
author
author
author
author
author
author
author
author
author
author
author
author
author
author
author
author
author
author
author
author
dc.subject.none.fl_str_mv Medio Marino
Centro Oceanográfico de Cádiz
Iberian margins
Oceanographic processes
Bottom currents
Sedimentary processes
Contourites
topic Medio Marino
Centro Oceanográfico de Cádiz
Iberian margins
Oceanographic processes
Bottom currents
Sedimentary processes
Contourites
description Our understanding of bottom-currents and associated oceanographic processes (e.g., overflows, barotropic tidal currents) including intermittent processes (e.g., vertical eddies, deep sea storms, horizontal vortices, internal waves and tsunamis) is rapidly evolving. Many deep-water processes remain poorly understood due to limited direct observations, but can generate significant depositional and erosional features on both short and long term time scales. This paper represents a review work, which describes for the first time these oceanographic processes and examines their potential role in the sedimentary features along the Iberian continental margins. This review explores the implications of the studied processes, given their secondary role relative to other factors such as mass-transport and turbiditic processes, and highlights three major results: a) contourite depositional and erosional features are ubiquitous along the margins, indicating that bottom currents and associated oceanographic processes control the physiography and sedimentation; b) the position of interfaces between major water masses and their vertical and spatial variation in time specifically appears to exert primary control in determining major morphologic changes along the slope gradient, including the contourite terraces development; and c) contourites deposits exhibit greater variation than the established facies model suggests. Therefore, a consistent facies model however faces substantial challenges in terms of the wide range of oceanographic processes that can influence in their development. An integrated interpretation of these oceanographic processes requires an understanding of contourites, seafloor features, their spatial and temporal evolution, and the near-bottom flows that form them. This approach will synthesize oceanographic data, seafloor morphology, sediments and seismic images to improve our knowledge of permanent and intermittent processes around Iberia, and evaluate their conceptual and regional role in the margin's sedimentary evolution. Given their complexes, three-dimensional and temporally-variable nature, integration of these processes into sedimentary, oceanographic and climatological frameworks will require a multidisciplinary approach that includes Geology, Physical oceanography, Paleoceanography and Benthic Biology.
publishDate 2016
dc.date.none.fl_str_mv 2016
2023
2023
dc.type.none.fl_str_mv info:eu-repo/semantics/article
http://purl.org/coar/resource_type/c_6501
Postprint
info:eu-repo/semantics/acceptedVersion
format article
status_str acceptedVersion
dc.identifier.none.fl_str_mv http://hdl.handle.net/10261/318862
url http://hdl.handle.net/10261/318862
dc.language.none.fl_str_mv Inglés
language_invalid_str_mv Inglés
dc.relation.none.fl_str_mv Centro Oceanográfico de Cádiz
dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
eu_rights_str_mv openAccess
dc.source.none.fl_str_mv reponame:DIGITAL.CSIC. Repositorio Institucional del CSIC
instname:Consejo Superior de Investigaciones Científicas (CSIC)
instname_str Consejo Superior de Investigaciones Científicas (CSIC)
reponame_str DIGITAL.CSIC. Repositorio Institucional del CSIC
collection DIGITAL.CSIC. Repositorio Institucional del CSIC
repository.name.fl_str_mv
repository.mail.fl_str_mv
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