Please use this identifier to cite or link to this item: http://hdl.handle.net/2445/155942
Title: Settling particle fluxes across the continental margin of the Gulf of Lion: the role of dense shelf water cascading
Author: Pasqual Mas, Catalina
Sànchez Vidal, Anna
Zúñiga, Diana
Calafat Frau, Antoni
Canals Artigas, Miquel
Durrieu de Madron, Xavier
Puig, Pere
Heussner, Serge
Palanques Monteys, Albert
Delsaut, N.
Keywords: Biogeoquímica
Mediterrània (Mar)
Biogeochemistry
Mediterranean Sea
Issue Date: 2010
Publisher: European Geosciences Union (EGU)
Abstract: Settling 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
Note: Reproducció del document publicat a: https://doi.org/10.5194/bg-7-217-2010
It is part of: Biogeosciences, 2010, vol. 7, p. 217-231
URI: http://hdl.handle.net/2445/155942
Related resource: https://doi.org/10.5194/bg-7-217-2010
ISSN: 1726-4170
Appears in Collections:Articles publicats en revistes (Dinàmica de la Terra i l'Oceà)

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