Various sedimentological and rock magnetic datasets from cores from the Yermak Plateau

The ratio of anhysteretic remanent susceptibility to bulk susceptibility was used for cross core correlation an tuning to a global oxygen isotope stack. This provided an age model independent of radicarbon ages and paleomagnetic data.

Physical properties were measured onboard RV Polarstern and at Stockholm University (Sweden). Rock- and paleomagnetic data were measured at Uppsala University (Sweden), Lund University (Sweden) and University of Bremen (Germany). Stable oxygen isotope data were measured at Stockholm University (Sweden).