Reference : Vivianite formation and distribution in Lake Baikal sediments
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Physical, chemical, mathematical & earth Sciences : Multidisciplinary, general & others
Physical, chemical, mathematical & earth Sciences : Earth sciences & physical geography
Vivianite formation and distribution in Lake Baikal sediments
Fagel, Nathalie mailto [Université de Liège - ULiège > Département de géologie > Géochim. sédiment. - Sédiment. mar. & continent. du quatern. >]
Alleman, L. Y. [> > > >]
Granina, L. [> > > >]
Hatert, Frédéric mailto [Université de Liège - ULiège > Département de géologie > Minéralogie et cristallochimie >]
Thamo-Bozso, Edith [> > > >]
Cloots, Rudi mailto [Université de Liège - ULiège > > Chimie inorganique structurale >]
André, Luc [Université de Liège - ULiège > > Géochim. sédiment. - Sédiment. mar. & continent. du quatern. >]
Global and Planetary Change
Elsevier Science Bv
Yes (verified by ORBi)
[en] Lake Baikal ; Late Quaternary ; sediment ; vivianite ; geochemistry
[en] In an effort to better understand vivianite formation processes, four Lake Baikal sediment cores spanning two to four interglacial stages in the northern, central and southern basins and under various biogeochemical environments are scrutinized. The vivianite-rich layers were detected by anomalous P-enrichments in bulk geochemistry and visually by observations on X-radiographs. The millimetric concretions of vivianite were isolated by sieving and analysed by X-ray diffraction, scanning electron microscope (SEM), microprobe, infrared spectroscopy, inductively coupled plasma atomic emission spectrometry and mass spectrometry (ICP-AES, ICP-MS). All the vivianites display similar morphological, mineralogical and geochemical signature, suggesting a common diagenetic origin. Their geochemical signature is sensitive to secondary alteration where vivianite concretions are gradually transformed from the rim to the center into an amorphous santabarbaraite phase with a decreasing Mn content. We analysed the spatial and temporal distribution of the concretions in order to determine the primary parameters controlling the vivianite formation, e.g., lithology, sedimentation rates, and porewater chemistry. We conclude that vivianite formation in Lake Baikal is mainly controlled by porewater chemistry and sedimentation rates, and it is not a proxy for lacustrine paleoproductivity. Vivianite accumulation is not restricted to areas of slow sedimentation rates (e.g., Academician and Continent ridges). At the site of relatively fast sedimentation rate, i.e., the Posolsky Bank near the Selenga Delta, vivianite production may be more or less related to the Selenga River inputs. It could be also indirectly related to the past intensive methane escapes from the sediments. While reflecting an early diagenetic signal, the source of P and Fe porewater for vivianites genesis is still unclear. (C) 2004 Elsevier B.V. All rights reserved.
Commission européenne : Direction générale de la Recherche ; Fonds de la Recherche Scientifique (Communauté française de Belgique) - F.R.S.-FNRS
The Authors thank Elsevier for their authorization.

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