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FIGURE 8 Bioturbation structures in bottom-current-affected settings. (A) Hiatus horizon covered
with mud pebbles, representing the base of the Late Pleistocene within the Iceland Shetland
Channel in 1,100 m water depth. British Geological Survey core 60-05/50 (60 49.7 0 N,
4 12.5 0 W), 346-358 cm (for details, see Akhurst et al., 2002 ). The mud clasts (mc), one with
Zoophycos ( Z ), are embedded in coarse sand (S) that in turn rests on mud with autochthonous Zoo-
phycos ( Z a ). The minimum amount of erosion is 40 cm, based on the burrowing depth of the
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