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2. Underwater towed video (A to F) and grab sampling (G to I) of Codling Fault mound targets. A. Semi-exposed nodules and pavement (P1); B. Semi-exposed hardgrounds (P2); C. Pavement stacking (P3); D. Reduced surface sediment (P4) E. Large exposed hardgounds (P5) F. Exposed colonised and non-colonised hardgrounds (P6); G. G103, H. G107, I. G109-a hardground colonised by a Nemertesia hydroid (black arrow); Unlabelled scale bars = 25cm; The locations for underwater still images and sampling stations are given in Fig. 3.1 and Table 3.1. 

2. Underwater towed video (A to F) and grab sampling (G to I) of Codling Fault mound targets. A. Semi-exposed nodules and pavement (P1); B. Semi-exposed hardgrounds (P2); C. Pavement stacking (P3); D. Reduced surface sediment (P4) E. Large exposed hardgounds (P5) F. Exposed colonised and non-colonised hardgrounds (P6); G. G103, H. G107, I. G109-a hardground colonised by a Nemertesia hydroid (black arrow); Unlabelled scale bars = 25cm; The locations for underwater still images and sampling stations are given in Fig. 3.1 and Table 3.1. 

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Cycling of organic carbon in marine sediments is of fundamental importance for marine ecosystem function, for marine and atmospheric chemistry, for the petroleum and natural gas industry, and for paleoclimatic and paleoenvironmental studies. While most of this carbon is derived from marine and terrestrial sources, significant improvements in mappin...