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

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sedimentological parameters. During <strong>ARK</strong> <strong>XIX</strong>/3c <strong>the</strong> number of permanent stations<br />

was increased to a total of 15 stations by introducing additional sampling sites along a<br />

latitudinal transect following <strong>the</strong> 2500 m water depth isobath (Fig. C1).<br />

To characterise and quantify organic matter fluxes to <strong>the</strong> seafloor, we use moorings<br />

carrying sedimentation traps, which were replaced during <strong>ARK</strong> <strong>XIX</strong>/3c (see Chapter C.<br />

1). <strong>The</strong> exchange of solutes between <strong>the</strong> sediments and <strong>the</strong> overlaying waters as well<br />

as <strong>the</strong> bottom currents were studied to investigate major processes at <strong>the</strong> sedimentwater-interface.<br />

A micro-profiler, being positioned and activated by <strong>the</strong> ROV, was used<br />

to assess <strong>the</strong> oxygen consumption by <strong>the</strong> benthic community (see Chapter C. 2).<br />

Gradients in oxygen were also measured from bottom water samples in order to<br />

quantify interfacial solute fluxes (including nutrients) and metabolic rates in <strong>the</strong> benthic<br />

boundary layer. <strong>The</strong>se investigations were completed by <strong>the</strong> use of an acoustical<br />

current meter, handled by <strong>the</strong> ROV.<br />

Fig. C1: Deep-sea long-term station AWI-"Hausgarten", west off Spitsbergen<br />

(: sampling sites; : experimental areas; : optical surveys).<br />

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