When this article was first published there was a plotting error in Figure 7. The revised plot is presented below and it should replace the original Figure 7. The implication of the error is that there is only a slight enrichment of Th over upper crustal values, and that the Th/Sc ratios for the proximal (Unit IIIb) varves are not significantly different from those of the distal (Unit IIIa) varves in Hanö Bay. However, this change does not influence the conclusions of the study. The authors regret this error. Figure 7. Bi-plot of Th/Sc ratios vs. Zr/Sc ratios, showing enrichment of Th for the lower proximal Baltic Ice Lake varves at Site M0064 (Unit IIIb). Diamictites of Unit IV and distal varves of Unit IIIa both have compositions near upper crustal values (McLennan, 2001) with Zr enrichment in the diamicton. The black line represents the typical compositional variability of fine-grained turbidites generated in active margin settings (from McLennan et al., 1993).