English   español  
Please use this identifier to cite or link to this item: http://hdl.handle.net/10261/27159
Share/Impact:
Statistics
logo share SHARE logo core CORE   Add this article to your Mendeley library MendeleyBASE

Visualizar otros formatos: MARC | Dublin Core | RDF | ORE | MODS | METS | DIDL
Exportar a otros formatos:

DC FieldValueLanguage
dc.contributor.authorPasqual, Catalina-
dc.contributor.authorSánchez-Vidal, Anna-
dc.contributor.authorZúñiga, Diana-
dc.contributor.authorCalafat, Antoni-
dc.contributor.authorCanals, Miquel-
dc.contributor.authorDurrieu de Madron, Xavier-
dc.contributor.authorPuig, Pere-
dc.contributor.authorHeussner, Serge-
dc.contributor.authorPalanques, Albert-
dc.contributor.authorDelsaut, N.-
dc.date.accessioned2010-08-18T08:54:53Z-
dc.date.available2010-08-18T08:54:53Z-
dc.date.issued2010-01-
dc.identifier.citationBiogeosciences 7(1): 217-231 (2010)en_US
dc.identifier.issn1726-4170-
dc.identifier.urihttp://hdl.handle.net/10261/27159-
dc.description15 páginas, 8 figuras, 3 tablas.en_US
dc.description.abstractSettling particles were collected using sediment traps deployed along three transects in the Lacaze-Duthiers and Cap de Creus canyons and the adjacent southern open slope from October 2005 to October 2006. The settling material was analyzed to obtain total mass fluxes and main constituent contents (organic matter, opal, calcium carbonate, and siliciclastics). Cascades of dense shelf water from the continental shelf edge to the lower continental slope occurred from January to March 2006. They were traced through strong negative near-bottom temperature anomalies and increased current speeds, and generated two intense pulses of mass fluxes in January and March 2006. This oceanographic phenomenon appeared as the major physical forcing of settling particles at almost all stations, and caused both high seasonal variability in mass fluxes and important qualitative changes in settling material. Fluxes during the dense shelf water cascading (DSWC) event ranged from 90.1 g m−2 d−1 at the middle Cap de Creus canyon (1000 m) to 3.2 g m−2 d−1 at the canyon mouth (1900 m). Fractions of organic matter, opal and calcium carbonate components increased seaward, thus diminishing the siliciclastic fraction. Temporal variability of the major components was larger in the canyon mouth and open slope sites, due to the mixed impact of dense shelf water cascading processes and the pelagic biological production. Results indicate that the cascading event remobilized and homogenized large amounts of material down canyon and southwardly along the continental slope contributing to a better understanding of the off-shelf particle transport and the internal dynamics of DSWC events.en_US
dc.description.sponsorshipThis research has been supported by HERMES (GOCE-CT-2005-511234-1), SESAME (GOCE-036949), HERMIONE (FP7-ENV-2008-1-226354), and GRACCIE (CSD2007-00067, Consolider-Ingenio Program) research projects, a Generalitat de Catalunya “Grups de Recerca Consolidats” grant (2009 SGR-1305) and a FP7 Marie Curie Reintegration Grant (PERG04-GA-2008-239175). C. Pasqual is supported by an F.P.U. grant from the Spanish government.en_US
dc.format.extent6033820 bytes-
dc.format.mimetypeapplication/pdf-
dc.language.isoengen_US
dc.publisherCopernicus Publicationsen_US
dc.relationinfo:eu-repo/grantAgreement/EC/FP7/226354-
dc.relation.isversionofPublisher’s version-
dc.rightsopenAccessen_US
dc.titleFlux and composition of settling particles across the continental margin of the Gulf of Lion: the role of dense shelf water cascadingen_US
dc.typeartículoen_US
dc.identifier.doi10.5194/bg-7-217-2010-
dc.description.peerreviewedPeer revieweden_US
dc.relation.publisherversionhttp://dx.doi.org/10.5194/bg-7-217-2010en_US
Appears in Collections:(ICM) Artículos
(IIM) Artículos
Files in This Item:
File Description SizeFormat 
bg-7-217-2010.pdf5,89 MBAdobe PDFThumbnail
View/Open
Show simple item record
 

Related articles:


WARNING: Items in Digital.CSIC are protected by copyright, with all rights reserved, unless otherwise indicated.