(a) ARM and (b) IRM paleointensity determination from WIS.3. The AF intensity is depicted by the color of the points according to the color bar. We recovered the HC paleointensity by fitting to the data at coercivities >75 mT (gray line), which likely corresponds to the TRM carried predominantly by pyrrhotite. The shallower slope at coercivities between ∼25 mT and ∼75 mT likely corresponds to a pTRM carried predominantly by magnetite from which ARM and IRM paleointensities could not be reliably recovered.