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Preface The expedition ARK XIX/3 with the German icebreaking RV ...

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and is probably a reflection of <strong>the</strong> abundance of life form here (and now largely<br />

destroyed).<br />

<strong>The</strong> o<strong>the</strong>r important discovery that deserves a special mention is <strong>the</strong> nature of <strong>the</strong><br />

numerous scarps that are found along this margin. <strong>The</strong>se have been imaged both on<br />

TOBI side-scan sonar and by <strong>the</strong> Geological Survey of Ireland multibeam dataset.<br />

<strong>The</strong>se scarps extend for 10s of km and often feature <strong>the</strong> growth of carbonate mounds.<br />

<strong>The</strong> coincidence of <strong>the</strong>se scarps <strong>with</strong> boundary faults and hydrocarbon reservoirs has<br />

lead to <strong>the</strong> speculation that <strong>the</strong>se may be <strong>the</strong> sites of cold seeps that have developed<br />

into carbonate mounds. As a result of this cruise we can now dismiss this hypo<strong>the</strong>sis.<br />

<strong>The</strong> scarps are obviously erosional features <strong>with</strong> scarp faces revealing consolidated<br />

Quaternary sediments that has <strong>the</strong>n become colonised by suspension feeders. <strong>The</strong>re<br />

was absolutely no evidence of hydrocarbon seepage. Fur<strong>the</strong>rmore, where carbonate<br />

mounds grow on this scarp <strong>the</strong>y grow on <strong>the</strong> tops of <strong>the</strong> scarps, due to enhanced<br />

hydrodynamics and not from <strong>the</strong> base up due to a process of feeding by cold seeps.<br />

Although this is a negative conclusion, in many senses this is one of <strong>the</strong> most<br />

significant finds of <strong>the</strong> entire cruise.<br />

References<br />

Akhmetzhanov AM, Kenyon NH, Ivanov MK, Wheeler A, Shashkin PV, van Weering TCE<br />

(2003) Giant carbonate mounds and current swept seafloors on <strong>the</strong> slopes of <strong>the</strong> sou<strong>the</strong>rn<br />

Rockall Trough In: Mienert J, Weaver P (eds) European Margin Sediment Dynamics: Sidescan<br />

Sonar and Seismic Images, Springer-Verlag, p.203-210<br />

Croker PF, de Haas H, Huvenne VAI, Wheeler AJ (2003) <strong>The</strong> 2002 TOBI sidescan survey of<br />

carbonate mounds in <strong>the</strong> Rockall and Porcupine basins. 46th Annual Irish Geological<br />

Research Meeting, Ulster Museum, Belfast, 21st-23rd February 2003.<br />

Dando PR, Hovland M (1992) Environmental effects of submarine seeping natural gas.<br />

Continental Shelf Research 12: 1197-1207.<br />

Dickson RR, McCave IN (1986) Nepheloid layers on <strong>the</strong> continental slope west of Porcupine<br />

Bank. Deep-Sea Research 33: 791-818.<br />

de Haas H, Huvenne V, Wheeler A, Unnithan V, shipboard scientific crew (2002) M2002<br />

Cruise report (R.V. Pelagia Cruise 64PE197): A TOBI Side Scan Sonar Survey of Cold<br />

Water Coral Carbonate Mounds in <strong>the</strong> Rockall Trough and Porcupine Sea Bight - Texel-<br />

Southampton-Galway, 21 June – 14 July 2002. Royal Ne<strong>the</strong>rlands of Sea Research,<br />

Texel, <strong>The</strong> Ne<strong>the</strong>rlands, 2002.<br />

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