Fig. 6From: Benthic foraminifera in a deep-sea high-energy environment: the Moira Mounds (Porcupine Seabight, SW of Ireland)Total organic carbon (TOC) content in box core (BC) surface sediments. Orange bars: living coral and dead coral facies; brown bars: sand and biogenic gravel facies; purple bars: sand and dropstone faciesBack to article page