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Early diagenetic sediment processes generate iron and manganese oxide layers in the sediments of Lake Baikal, Siberia

Distinct layers of iron(III) and manganese(IV) (Fe/Mn) oxides are found buried within the reducing part of the sediments in Lake Baikal and cause considerable complexity and steep vertical gradients with respect to the redox sequence. For the on-site investigation of the responsible biogeochemical processes,

Authors:   Natascha T Torres; Lawrence M Och; Peter C Hauser; Gerhard Furrer; Helmut Brandl; Elena Vologina; Michael Sturm; Helmut Bürgmann; Beat Mueller
Journal:   Journal of Environmental Monitoring
DOI:   10.1039/C3EM00676J
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