Fig. 7From: Palaeomagnetic and mineral magnetic analyses of the Deckenschotter of northern Switzerland and southern GermanyTimes of geomagnetic polarity changes as shown in the Astronomically Tuned Neogene Time Scale ATNTS2020 (Raffi et al., 2020). The LR04 oxygen isotope fractionation curve and corresponding marine isotope stages (Lisiecki and Raymo, 2005) provide indications on warmer periodsBack to article page