Abstract
Black shales from the Cenomanian/Turonian Boundary Event show a remarkable enrichment in trace metals (Cd, Ag, Zn, Sb, Mo, V, Cu, etc.) relative to normal shales, Lower Toarcian black shales from SW Germany or TOC-rich sediments from recent upwelling areas. If these enrichments are authigenic in origin, trace metals may serve as indicators for the paleoenvironmental conditions during deposition of black shales. Low sediment accumulation rates, a comparably low organic primary productivity and enhanced preservation of TOC due to anaerobic conditions in the water column then are indicated for the Cenomanian/Turonian time interval.
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© 1986 Springer-Verlag
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Brumsack, HJ. (1986). Trace metal accumulation in black shales from the Cenomanian/Turonian Boundary Event. In: Walliser, O.H. (eds) Global Bio-Events. Lecture Notes in Earth Sciences, vol 8. Springer, Berlin, Heidelberg. https://doi.org/10.1007/BFb0010216
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DOI: https://doi.org/10.1007/BFb0010216
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