Fig. 9From: A ~180,000 years sedimentation history of a perialpine overdeepened glacial trough (Wehntal, N-Switzerland)Top results of luminescence dating plotted versus depth (with stretched core photo and stratigraphic units indicated on leftside). Black dots represent quartz OSL, red dots feldspars IRSL ages. Bottom correlation of the marine oxygen isotopes stages (MIS) as proxy for global ice volume (δ18O of benthic foraminifera; Bassinot et al. 1994)Back to article page