Benthic foraminifera and ostracoda in ODP Hole 107-650A, supplement to: Hieke, Werner; Glacon, Georgette; Hasegawa, Shiro; Müller, Carla; Peypouquet, Jean Pierre (1990): Sedimentation in the Marsili Basin during Quaternary (ODP Site 650, Tyrrhenian Sea). In: Kastens, KA; Mascle, J; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 107, 255-289

Werner Hieke, Georgette Glacon, Shiro Hasegawa, Carla Müller & Jean Pierre Peypouquet
Twenty-three sediment intervals from top of Site 650 down to 510 m below seafloor have been studied. Their thicknesses vary between 0.25 m and about 40 m. The studied deposits are turbidites or parts of them except one which is interpreted as an ash-fall layer.The composition of the turbidites signalizes sources from shallow water/coastal areas as well as from deep water levels. Repeated mobilization and displacement seems to have been common.Volcaniclastic material is the dominant...
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