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

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Acronym Participants GENAVIR GENAVIR 28 Zone Portuaire de Brégaillon B.P. 330 83507 La Seyne sur mer Cedex France Geological Survey of Ireland GSI 1 Beggars Bush, Haddington Road Dublin 4 Ireland GEOMAR Forschungszentrum für GEOMAR 1 Marine Geowissenschaften Wischhofstr. 1-3 24148 Kiel Germany Institut français de recherche pour IFREMER 16 l'exploitation de la mer BP70 29280 Plouzane France Institut Royales des Sciences IRSNB 2 Naturelles de Belgique Rue Vautier 19 9000 Bruxelles Belgium Institute for Applied Physics IAP 1 of the Russian Academy of Sciences Nishny Novgorod Russia Institute for Polar Ecology of Kiel University IPÖ 1 Wischhofstr. 1-3 24148 Kiel Germany Institute of Oceanology of the IOPAS 2 Polish Academy of Sciences P.B. 68 81-712 Sopot Poland International University Bremen IUB 7 Campusring 1 28759 Bremen Germany - 347 -
Acronym Participants iSiTEC GmbH ISITEC 1 Stresemannstr. 46 27570 Bremerhaven Germany Martin Ryan Marine Science Institute NUIG 3 National University of Ireland Galway Ireland Max Planck Institute for Marine Microbiology MPI 9 Celsiusstr. 1 28359 Bremen Germany Murmansk Marine Biological Institute MMBI 1 Vladimirskaya Str. 17 183010 Murmansk Russia OPTIMARE OPTIMARE 1 Coloradostr. 5 27580 Bremerhaven Germany P.P. Shirshov Institute of Oceanology SIO 1 of the Russian Academy of Sciences 23 Krasikova 117851 Moscow, Russia Reederei F. Laeisz GmbH FL 43 Barkhausenstr. 37 27568 Bremerhaven Germany Renard Centre of Marine Geology RCMG 2 Department of Geology and Soil Science University of Ghent Krijgslaan 281 S8 9000 Gent Belgium School of Ocean Sciences SOS 1 University of Wales Bangor Askew Street Menai Bridge, LL59 5AB United Kingdom - 348 -
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Preface The expedition ARK XIX/3 wi
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B. 1 Cruise leg ARK XIX/3b: An intr
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The ARK XIX/3 expedition A. 1 Itine
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positioning and navigation of the "
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was followed to obtain video materi
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On Friday morning the 20 th of June
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Fig. A1-2: The working area of the
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"Polarstern" (actual air temperatur
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6000" was still at depth "Polarster
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aseline navigation antennae which a
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Fig. A1-3: Entire cruise track of R
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At end of the leg pressure rising b
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The temperatures during the cruise
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Most frequent wind direction was so
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A. 3.1 High resolution seabed mappi
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On the other hand, the accuracy of
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The sampling campaign was also unde
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Hydrosweep DS2 is installed onboard
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Fig. A4.2-2: Normalized backscatter
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In addition to the micro bathymetry
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ackscatter value of -37.0dB, -38.9d
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athymetry and angular backscatter d
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A. 4.3 Sedimentary and hydrodynamic
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glacial periods. There is also evid
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Fig. A4.3.2-2: Visualisation of dif
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It seems that all the mounds along
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Visible calcareous fauna removed (b
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Fig. A4.3.3-2 Location of SAMS Phot
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Box Core Sample Log Sheet Station N
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A. 4.3.4 Influence of mound topogra
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A. 4.3.5 Photo lander deployment on
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- UMI data logger controlling a tra
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Fig. A4.3.5-3. Close-up view of the
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Lineated features are present NE of
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CARACOLE Cruise Report 30/07/2001 (
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intermediate nepheloid layers (Dick
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Fig. A4.4.1-2. Location of main stu
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A. 4.4.3 Biogeoprocesses along the
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in the database with the exact posi
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The areas with significant benthic
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predators and strong bottom current
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faunal distribution. Palaentologica
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ocks predate the last glaciation, s
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A. 4.4.6 Biological and geological
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Hovland M, Croker PF, Martin M (199
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Live fauna Sediments Live fauna and
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sites can subsequently be transport
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4) The NSOW has similar water mass
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0 100 200 300 400 500 600 700 800 P
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A. 4.8 Deep water coral ecology and
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and video observations made. On ret
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Fig. A4.8.2-2: This orange, planar
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Fig. A4.8.2-4: Feather-shaped alcyo
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Fig. A4.8.2-7: Top left) Yellow alc
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scour or demersal trawling. The gro
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survey at frequencies of 38, 70, 12
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"Belgica mounds" - Porcupine Seabig
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"Twin mounds" - Porcupine Bank 14°
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corals were alive, relatively abund
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Network Setup for Tests The setup f
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are only initial testings and much
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pressure produced as a consequence
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surrounded by elevated sediment fea
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B. 2 Microbathymetry on ROV "Victor
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Pitch correction Due to assembling
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Maps Complete area Håkon Mosby Mud
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B. 3 Geochemistry, geophysics and s
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Heat Flow HMMV 2m # # # # # # # # #
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Lat_dec. Lon_dec Name k T_0m PS64/s
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Temperature / Gravity Corer # GC9 #
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Table B3.2-1: Technical specificati
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Sound velocity: As the cores all co
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Fig. B3.3-1: Display of a 4 km long
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sediment cores varies between 166 t
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Fig. B3.4-1b: Lithological descript
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Fig. B3.4-1d: Lithological descript
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Fig. B3.4-1f: Lithological descript
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hydrotroilite and gas hydrate, this
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As an example, a echo sounder image
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B. 5 Biological investigations at t
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- How much methane is oxidized aero
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profiler). Bottom water samples hav
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the water column was measured using
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1 kg of tubeworms in wet weight. Th
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B. 5.2 Microscale analysis of the s
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Laboratory measurements Central sit
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O2, CO3-- (mM) Beggiatoa mats, 30/0
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Photograph of the sulfide oxidising
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Central area No measurements could
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the temperature profile showed adve
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B. 5.3 Methane in gas hydrate beari
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The deployments covered 3 (5) diffe
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flows at the Håkon Mosby Mud Volca
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The quality of the mosaics depends
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[2] Vincent AG, Pessel N, Borgetto
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References Milkov, A., Vogt, P., Ch
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ROV "Victor 6000" The ROV "Victor 6
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has spent in organising the coring
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A multiple corer was used to retrie
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At the position of the moorings a C
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Micro profiles of O 2 but also of p
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The current regime luff and lee sid
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2° 3° 4° N2 5° PS64/481 PS64/48
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station IRD archive liner bulk x-ra
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C. 4 Marine Geology Kukina, N. Majo
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2° 3° 4° 5° 6° PS64/481 79°20
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Appendix 1: List of samples for fut
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material via the Transpolar Drift t
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ounding processes as well. One poss
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The most frequent rock type is sand
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Eastern Greenland, Iceland and Scan
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C. 6 Debris on the seafloor at “H
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Results A summary of the results is
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enthic community are of crucial imp
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frame showed no obvious colonisatio
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subsamples (area of 400 - 800 cm 2
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using shipboard techniques - provid
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Tab C11-1: Stationlist of in situ m
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Tab. C11-2: In-situ measurements of
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Tab. C11-2: In-situ measurements of
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Climate models predict that global
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90 mean copepod densities/ 10 cm 2
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- Molecular phylogeny and phylogeog
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Species Stations Tmetonyx sp.1 326-
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was used to terminate and sample th
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openings of 45° at both sides the
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Station Date Time PositionLat Posit
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Page 297 and 298: Station Date Time PositionLat Posit
Page 347: E. Participating institutes / compa
Page 351 and 352: F. Participants F. 1 Participants A
Page 353 and 354: F. 2 Participants ARK XIX/3b Armand
Page 355 and 356: F. 3 Participants ARK XIX/3c Bauerf
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Preface The expedition ARK XIX/3 with the German icebreaking RV ...

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