Titlebook: Geochemistry and Sedimentology of the Mediterranean Sea; E. M. Emelyanov,K. M. Shimkus Book 1986 Springer Science+Business Media Dordrecht

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The Geochemistry of Quaternary Sedimentogenesis and Diagenesis,e of discoasters (Cita et al., 1973); it is about 1.8 x 10 years BP, based on palaeomagnetic data (Ryan and Flood, 1973; Ryan, 1973). Continuous Quaternary sections can be divided into 3 biozones at Sites 132 and 125, based on the coccolithophorides (Stradner, 1973): (1) .. (0 — 0.58 x 10. years); (

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Main Features of the Geochemistry and Sedimentology of the Mediterranean Sea, but in other cases they are diluted. The transformation begins on the land when the denudation products are beginning to be transformed, continues in rivers and in the final basins of deposition (whilst in the water and on the sea floor), i.e. until the sediment reach a physical-chemical condition

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Book 1986Mediterranean Sea. For more than 20 years E.M. Emelyanov has examined the recent sedimentation of the Mediterranean Sea and K.M. Shimkus has studied the Quaternary and the earlier sedi- mentation of the area. The authors, scientific workers from the P.P. Shirshov Institute of Oceanology, USSR Academ

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Main Features of the Geochemistry and Sedimentology of the Mediterranean Sea,cess is intense* other times it becomes weaker.The marine areas (or the layers of water and sediment) where the processes of transformation of sedimentary material are most intensive, were called by E.M. Emelyanov “geochemical barrier zones (GBZ)”.

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Geochemistry and Sedimentology of the Mediterranean Sea978-94-009-4490-9