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

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Considering <strong>the</strong> observed 5000 m² video and still photo material of Milkov et al. which<br />

covered 0.5 % of <strong>the</strong> edifice of <strong>the</strong> mud volcano [3], it should be emphasised that <strong>the</strong><br />

new data set is 20 times more extensive and covers more than 10% of <strong>the</strong> sea-floor<br />

area. Fig. B5.4-4 represents <strong>the</strong> tracks of <strong>the</strong> mosaics and shows <strong>the</strong> full extend of <strong>the</strong><br />

video mosaicking surveys.<br />

HMMV Mosaicking Tracks 2003<br />

0 1 00 200 300 Met ers<br />

Fig. B5.4-4: Frames of <strong>the</strong> video mosaicking images during <strong>the</strong> cruise PS64.<br />

This very successful data collection will deliver an insight into <strong>the</strong> habitats of <strong>the</strong><br />

Håkon Mosby Mud Volcano better than before. <strong>The</strong> mosaics will be analysed for<br />

habitat types according to Milkov et al., 1999: smooth mud, mud <strong>with</strong> holes, mud <strong>with</strong><br />

ripples, mud <strong>with</strong> relief, seafloor <strong>with</strong> bacterial mats (Beggiatoa), seafloor <strong>with</strong><br />

tubeworms (Pogonophora) <strong>with</strong> a comparable method like in Bergmann (this issue).<br />

References:<br />

[1] Pollio, J. (1968): Stereo-photographic mapping from submersibles. In SPIE: Vol. 12, pp 67-<br />

71. U.S. Naval Oceanographic Office, Deep Vehicle Branch.<br />

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