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

We used a combination of rockmagnetic, sedimentological and oxygen isotope data to put three new sediment cores in the context of the regional stratigraphy. 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).



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