Fig. 5: Lithology of 12-GC and 14-GC.
From: Seasonal sea-ice in the Arctic’s last ice area during the Early Holocene
Radiograph, core photo, XRF Ca/Ti (grey, 20-pt average in black) and bulk density (black) of (a) 12-GC and (b) 14-GC, including prominent sedimentary features (dropstones, cross-cutting, IRD/clasts). Key lithological boundaries can be correlated between 12-GC and 14-GC, for the respective depth of LU boundaries see Supplementary table 1. Uncalibrated radiocarbon ages and their respective depth are marked with yellow triangles. Red triangles mark outliers, which are excluded from the final age model.
