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Provedor de dados:  ArchiMer
País:  France
Título:  A benthic Si mass balance on the Congo margin: Origin of the 4000 m DSi anomaly and implications for the transfer of Si from land to ocean
Autores:  Ragueneau, O.
Regaudie-de-gioux, A.
Moriceau, B.
Gallinari, M.
Vangriesheim, Annick
Baurand, F.
Khripounoff, Alexis
Data:  2009-11
Ano:  2009
Palavras-chave:  Congo
Continental margin
Preservation
Dissolution
Biogenic silica
Resumo:  To elucidate the origin of the silicic acid (DSi) anomaly observed along the 4000 isobath on the Congo margin, we have established a benthic Si mass balance and performed direct measurements of biogenic silica (bSiO(2)) dissolution in the deep waters and in the sediments. Results strongly suggest that the anomaly originates from the sediments; the intensity of DSi recycling is consistent with the degradation of organic matter, as observed from Si:O-2 ratios in the benthic fluxes compared to that ratio observed in the anomalies. Strong imbalances, observed in both the Si and C mass balances, suggest that the biogenic matter that degrades and dissolves in these sediments near 4000 m does not come from pelagic sedimentation. It is probably not coming also from the deep channel, because observations were similar in the deep channel vicinity (site D) and further south, far from its influence (site C). The composition of the sediments, with an Si:C ratio close to that observed on continental shelves, suggests that this matter is coming from downslope transport. A first estimate of the magnitude of this flux at global scale, close to 12 T mol Si yr(-1), suggests that it may be an important path for transferring Si from land to ocean.
Tipo:  Text
Idioma:  Inglês
Identificador:  http://archimer.ifremer.fr/doc/2009/publication-7410.pdf

DOI:10.1016/j.dsr2.2009.04.003
Editor:  Elsevier
Relação:  http://archimer.ifremer.fr/doc/00000/7410/
Formato:  application/pdf
Fonte:  Deep Sea Research Part II: Topical Studies in Oceanography (0967-0645) (Elsevier), 2009-11 , Vol. 56 , N. 23 , P. 2197-2207
Direitos:  2009 Elsevier Ltd All rights reserved.
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