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Raimonet M., Ragueneau Olivier, Jacques V., Corvaisier R., Moriceau B., Khripounoff A., Pozzato L., Rabouille C. (2015). Rapid transport and high accumulation of amorphous silica in the Congo deep-sea fan : a preliminary budget. Journal of Marine Systems, 141 (SI), 71-79. ISSN 0924-7963

Lien direct chez l'éditeur doi:10.1016/j.jmarsys.2014.07.010

Titre
Rapid transport and high accumulation of amorphous silica in the Congo deep-sea fan : a preliminary budget
Année de publication2015
Type de documentArticle référencé dans le Web of Science WOS:000347868800007
AuteursRaimonet M., Ragueneau Olivier, Jacques V., Corvaisier R., Moriceau B., Khripounoff A., Pozzato L., Rabouille C.
SourceJournal of Marine Systems, 2015, 141 (SI), p. 71-79. ISSN 0924-7963
RésuméMechanisms controlling the transfer and retention of silicon (Si) along continental margins are poorly understood, but play a major role in the functioning of coastal ecosystems and the oceanic biological pump of carbon. Deep-sea fans are well recognized as carbon sink spots, but we lack knowledge about the importance of the fans in the global Si cycle. Here, we provide a first estimate of the role played by the Congo deep-sea fan, one of the biggest in the world, in the Si cycle. Sediment cores sampled in the deep-sea fan were analyzed to build a Si mass balance. An exceptionally high accumulation rate of amorphous silica aSiO(2) (2.29 +/- 0.58 mol Si m(-2) y(-1)) was found, due to a high sedimentation rate and the presence of aluminum in the sediments. Although favored by bioirrigation, recycling fluxes remained low (0.3 mol Si m(-2) y(-1)) and reconstructed input fluxes could only be explained by lateral inputs coming from the canyon. Preliminary calculations show that the rapid transport of aSiO(2) through the canyon and the excellent preservation efficiency in the sediments imply that 50% of aSiO(2) river inputs from the Congo River accumulate annually in the deep-sea fan. Si:C ratios in deep-sea fan sediments were very low (0.2) and only three times as high as those measured in the river itself, which suggests that material from the river and the continental shelf was delivered directly through the canyon, with very little time for Si and C cycle decoupling to take place.
Plan de classementLimnologie physique / Océanographie physique [032]
Descr. géo.CONGO FLEUVE
LocalisationFonds IRD
Identifiant IRDPAR00012705
Lien permanenthttp://www.documentation.ird.fr/hor/PAR00012705

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