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Possible diagenetic mobilization of barium in sapropelic sediment from the eastern Mediterranean

✍ Scribed by Bertil J.H. van Os; Jack J. Middelburg; Gert J. de Lange


Publisher
Elsevier Science
Year
1991
Tongue
English
Weight
837 KB
Volume
100
Category
Article
ISSN
0025-3227

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Geochemistry of an exotic sediment layer
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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