Titlebook: Marine Geochemistry; Horst D. Schulz,Matthias Zabel Textbook 20001st edition Springer-Verlag Berlin Heidelberg 2000 Fühdiagenese.Ocean.Oze

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Sulfate Reduction in Marine Sediments,neralization of organic matter and oxidation of methane in different depositional environments and discuss the often observed discrepancy between sulfate reduction rates deduced from radiotracer methods and those calculated from pore-water concentration profiles and/or solid-phase sulfur data.

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Manganese: Predominant Role of Nodules and Crusts,iving an average Mn/Fe ratio of 0.02. It also occurs in two valency states whose stability boundary lies within the range of the natural environment. Fe oxy-hydroxides have a high adsorption capacity and large surface area. Goethite has a pH. of 7.1 and can adsorb both cations and anions (e.g. REE, P, Mo, W etc.).

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