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	Provedor de dados ArchiMer (2) Autor Grousset, Fe (2) Weber, O (2) Burdloff, D (1) Cortijo, E (1) Duprat, J (1) Herve, L (1) Huon, S (1) Jouanneau, Jm (1) Richter, T (1) Thomas, B (1) Mais... Palavra-chave Bay of Biscay (1) Climate and interannual variability (1) Climate dynamics (1) Fine-grained sediment (1) Golfe de Gascogne (1) Heavy metal (1) Métaux traces (1) Origin (1) Radiogenic isotope geochemistry (1) Rare earth element (1) Source (1) Sédiment fin (1) Terre rare (1) Mais... Tipo do documento Text (2) Ano 2001 (1) 1998 (1) País France (2) Idioma Inglês (2)		Ordenar por:  Relevância Autor Título Ano Registros recuperados: 2 Primeira ... 1 ... Última Pb, Zn, Cs, Sc and rare earth elements as tracers of the Loire and Gironde particles on the Biscay shelf (SW France) ArchiMer Jouanneau, Jm; Weber, O; Grousset, Fe; Thomas, B. The western Atlantic continental margin of the Bay of Biscay is characterised by a combined macro-tidal and a high energy environment. These conditions are responsible for the essentially sandy sedimentary cover along with well-defined fine deposit zones observed on the shelf. The main continental sources are the Loire, Gironde and Adour Rivers. It is estimated that 2.4 to 2.5 million tons of fine sediments are supplied annually to the ocean from these rivers of the French Atlantic coast. The Gironde and the Loire contribute with 84 % and the Gironde with 60 % of this amount. Previous studies of the distribution of the clay mineral assemblages and of oligo-elements have distinguished two provinces (north and south Biscay areas) according to these riverine... Tipo: Text Palavras-chave: Sédiment fin; Source; Métaux traces; Terre rare; Golfe de Gascogne; Fine-grained sediment; Origin; Heavy metal; Rare earth element; Bay of Biscay. Ano: 1998 URL: http://archimer.ifremer.fr/doc/00326/43682/43192.pdf Zooming in on Heinrich layers ArchiMer Grousset, Fe; Cortijo, E; Huon, S; Herve, L; Richter, T; Burdloff, D; Duprat, J; Weber, O. Theories explaining the origin of the abrupt, massive discharges of ice-rafted detritus (IRD) into the glacial North Atlantic (the Heinrich layers (HLs)) generally point to the Laurentide ice sheet as the sole source of these events, until it was found that the IRDs also originated from Icelandic and European ice sheets [Bond and Lotti, 1995; Snoeckx er al., 1999; Grousset et al., 2000]. This apparent contradiction must be reconciled as it raises fundamental questions about the mechanism(s) of HL origin. We have analyzed two similar to 12 cm thick HLs in an ultrahigh-resolution mode (1-2 century intervals) in a mid-Atlantic ridge piston core. The delta O-18 record (N. pachyderma left coiling) reveals strong excursions induced by the melting of the... Tipo: Text Palavras-chave: Climate and interannual variability; Climate dynamics; Radiogenic isotope geochemistry. Ano: 2001 URL: https://archimer.ifremer.fr/doc/00221/33190/31786.pdf Registros recuperados: 2 Primeira ... 1 ... Última

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