Geochemistry of an exotic sediment layer
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A. HΓΌbner; G.J. De Lange; J. Dittmer; P. Halbach
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Article
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2003
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Elsevier Science
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English
β 533 KB
In a gravity core from the eastern Mediterranean Sea, a chemically and mineralogically distinct, 5.5-cm-thick layer is present above sapropel S-1 and overlain by hemipelagic marls. Calcite is completely absent in this exotic layer, dolomite is present only in small amounts, and the Cr concentrations