Magnetic susceptibility of sediment core LV76-21

The sediment magnetic susceptibility (MS) was measured onboard using a Satis Geo KM-7 kappameter at a resolution of 1 cm. Within 2 h after coring, the sediment core was split, and one half of core was used for the MS measurements. Values of the sediment MS are determined by concentration of terrigenous ferromagnetic material and of volcanogenic material as well.