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

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250<br />

4,0<br />

]<br />

200<br />

3,0<br />

150<br />

100<br />

2,0<br />

50<br />

1,0<br />

0<br />

0 5 10<br />

t [h]<br />

0,0<br />

0 2 4 6 8 10<br />

t (h)<br />

Fig. B3.5-2: Oxygen (left) and methane (right) concentrations in teh chamber water of an<br />

incubation on a Beggiatoa mat.<br />

Macrofauna<br />

In addition, <strong>the</strong> following questions were addressed:<br />

Does <strong>the</strong> macrofauna at HMMV play an as important role for habitat structure as it<br />

does at „normal“ continental slope settings ?<br />

Does <strong>the</strong> macrofauna utilize <strong>the</strong> methane - based food chain (stable isotope<br />

analysis)?<br />

How does <strong>the</strong> mud/ fluid flow affect <strong>the</strong> community structure of larger organisms<br />

(Macrofauna) in terms of biomass and diversity ?.<br />

In order to address <strong>the</strong>se questions, <strong>the</strong> sediments retrieved <strong>with</strong> <strong>the</strong> benthic<br />

chambers were sieved (250 µm) and <strong>the</strong> remaining organisms preserved in 4 %<br />

buffered formaldehyde. In <strong>the</strong> home laboratory, <strong>the</strong> samples will be sorted, identified<br />

to <strong>the</strong> lowest taxonomic level possible. Subsequently, <strong>the</strong> 13 C signatures of each<br />

single specimen will be determined.<br />

B. 5.4 Video Mosaicking on Håkon Mosby Mud Volcano<br />

Jerosch, K., Vincent, A.G., Schlüter, M.<br />

Introduction<br />

Geo-referenced video mosaicking of <strong>the</strong> sea floor is useful to many applications. In<br />

our case, we use it to gain an understanding of <strong>the</strong> oceans’ biological and<br />

sedimentological entities – especially <strong>the</strong> distribution of different habitats and mud<br />

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