Down-core variations of anhysteretic remanent magnetisation and simplified lithological description of the investigated cores.

Conceptual intercorrelation between ARM and simplified lithology and correlation to the δ18O record from ODP Site 677 (Shackleton et al., 1990), assuming that clay-rich layers with high magnetic concentration represent glacial periods, and that diatomaceous layers with low magnetic concentration represent interglacial periods. Numbers in the δ18O record represent marine isotope stages (MIS).