Fig. 10From: Unmixing biogenic and terrigenous magnetic mineral components in red clay of the Pacific Ocean using principal component analyses of first-order reversal curve diagrams and paleoenvironmental implicationsPaleopositions of the core KR13-02 PC06 site superimposed on the present-day bathymetry. The backtrack path was calculated with the GPlates software (Seton et al. 2012)Back to article page