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  • 1
    Book
    Book
    Bergen : John Grieg Forlag
    Type of Medium: Book
    Pages: 155 Seiten , Illustrationen, graphische Darstellungen
    ISBN: 8253302886
    Language: Norwegian
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  • 2
    Online Resource
    Online Resource
    Cambridge :Cambridge University Press,
    Keywords: Egypt -- Economic conditions. ; Electronic books.
    Description / Table of Contents: Seabed fluid flow involves the flow of gases and liquids through the seabed. This book describes the features and processes of seabed fluid flow and demonstrates its importance to human activities and natural environments. It is targeted at research scientists and professionals in the marine environment.
    Type of Medium: Online Resource
    Pages: 1 online resource (493 pages)
    Edition: 1st ed.
    ISBN: 9780511268366
    DDC: 551.468
    Language: English
    Note: Cover -- Half-title -- Title -- Copyright -- Contents -- Preface -- Acknowledgements -- Note on the accompanying website www.cambridge.org/0521819504 -- Maps on the accompanying website -- Contributed presentations on the accompanying website -- 1 Introduction to seabed fluid flow -- 2 Pockmarks, shallow gas, and seeps: an initial appraisal -- 2.1 THE SCOTIAN SHELF: THE EARLY YEARS -- 2.2 NORTH SEA POCKMARKS -- 2.2.1 History of discovery -- 2.2.2 Pockmark distribution -- 2.2.3 Pockmark size and density -- 2.2.4 Pockmark morphology -- Erosive nature -- Partial infilling -- Associated features -- BURIED ('FOSSIL') POCKMARKS -- DOMES -- 2.2.5 Evidence of gas -- The extent of shallow gas -- 2.3 DETAILED SURVEYS OF NORTH SEA POCKMARKS AND SEEPS -- 2.3.1 The South Fladen Pockmark Study Area -- Pockmark morphology and distribution -- Evidence of gas -- Evidence of pockmark growth and activity -- Post-glacial pockmark activity -- The Witch's Hole -- 2.3.2 Tommeliten: Norwegian Block 1/9 -- Geophysical reconnaissance and sediment sampling -- ROV surveys -- Gas -- 2.3.3 Norwegian Block 25/7 -- ROV surveys -- 2.3.4 The Holene: Norwegian Block 24/9 -- 2.3.5 The Norwegian Trench -- Top of the western slope: Norwegian Block 26/8 -- Bottom of the western slope: Norwegian Block 26/9 -- 2.3.6 Gullfaks -- Geophysical reconnaissance -- ROV surveys -- Sediment gases -- 2.3.7 Giant pockmarks: UK Block 15/25 -- Shallow gas -- Gas seeps -- Gas analyses -- Carbonates -- Benthic ecology -- 2.4 CONCLUSIONS -- 3 Seabed fluid flow around the world -- 3.1 INTRODUCTION -- 3.2 THE EASTERN ARCTIC -- 3.2.1 The Barents Sea -- Pockmarks and iceberg scours -- Giant blowout craters -- 3.2.2 Hakon Mosby Mud Volcano -- 3.3 SCANDINAVIA -- 3.3.1 Fjords in northern Norway -- Lyngenfjord: pockmarks, doming and high reflectivity -- 3.3.2 The Norwegian Sea -- 3.3.3 The Skagerrak. , 3.3.4 The Kattegat -- 3.4 THE BALTIC SEA -- 3.4.1 Eckernförde Bay -- 3.4.2 Stockholm Archipelago, Sweden -- 3.5 AROUND THE BRITISH ISLES -- 3.5.1 Pockmarks, domes, and seeps -- 3.5.2 'Freak' sandwaves -- 3.5.3 Methane-derived authigenic carbonate -- 3.5.4 The Atlantic Margin -- Carbonate mounds -- Rockall Trough - the Darwin Mounds -- 3.6 IBERIA -- 3.6.1 The Rías of Galicia, northwest Spain -- 3.6.2 Gulf of Cadiz -- The upper slope - gassy sediments and pockmarks -- The lower slope - mud diapirs, mud volcanoes, and gas hydrates -- 3.6.3 Ibiza -- 3.7 AFRICA -- 3.7.1 The Niger Delta and Fan -- 3.7.2 The continental slope of West Africa -- 3.8 THE MID-ATLANTIC RIDGE -- 3.9 THE ADRIATIC SEA -- 3.9.1 Seeps and carbonates of the northern Adriatic -- 3.9.2 Pockmarks, seeps, and mud diapirs in the central Adriatic -- Bonaccia gas field -- Jabuka Trough -- Offshore Ortona -- 3.10 THE EASTERN MEDITERRANEAN -- 3.10.1 Offshore Greece -- Prinos Bay -- Aetoliko Lagoon -- Active pockmarks and earthquakes -- Hydrothermal seeps -- 3.10.2 Mediterranean Ridge -- 3.10.3 The Anaximander Mountains -- 3.10.4 Eratosthenes Seamount -- 3.10.5 Nile Delta and Fan -- 3.11 THE BLACK SEA -- 3.11.1 Turkish Coast -- 3.11.2 Offshore Bulgaria -- 3.11.3 Northwestern Black Sea -- 3.11.4 Central and northern Black Sea -- Central Black Sea -- Sorokin Trough -- 3.11.5 The 'underwater swamps' of the east Black Sea abyssal plain -- 3.11.6 Offshore Georgia -- 3.12 INLAND SEAS OF EURASIA -- 3.12.1 The Caspian Sea -- 3.12.2 Lake Baikal -- 3.13 THE RED SEA -- 3.14 THE ARABIAN GULF -- 3.14.1 Setting -- 3.14.2 Seabed features -- Summary -- 3.14.3 Strait of Hormuz -- 3.15 THE INDIAN SUBCONTINENT -- 3.15.1 The Makran coast -- 3.15.2 The western coast of India -- 3.15.3 The eastern coast of the subcontinent -- 3.15.4 Indian Ocean vent fauna -- 3.16 SOUTH CHINA SEA -- 3.16.1 Offshore Brunei. , 3.16.2 Offshore Vietnam -- 3.16.3 Hong Kong -- 3.16.4 Taiwan -- 3.17 AUSTRALASIA -- 3.17.1 Sawu Sea -- 3.17.2 Timor Sea -- 3.17.3 New Britain and the Manus basins -- Matupi Harbour -- Manus Basin -- Eastern Manus Basin -- 3.17.4 New Zealand -- Poverty Bay -- Taupo Volcanic Zone -- 3.18 WESTERN PACIFIC -- 3.18.1 Silicic dome volcanism in the Mariana Back-arc Basin -- 3.18.2 Serpentine mud volcanoes near the Mariana Trench -- 3.18.3 The Yellow and East China seas -- 3.18.4 Offshore Korea -- 3.18.5 Japan -- Sagami Bay -- Kagoshima Bay -- Yuigahama Beach -- Subduction zones -- Gas hydrate resources -- 3.18.6 Sea of Okhotsk -- Northeast of Sakhalin Island -- West of the Kuril Islands -- The significance of the Sea of Okhotsk -- 3.18.7 Piip Submarine Volcano, east of Kamchatka -- 3.19 OFFSHORE ALASKA -- 3.19.1 Bering Sea -- Chirikov Basin and Norton Sound -- Navarin Basin -- Bering Sea pockmarks made by whales? -- 3.19.2 Gulf of Alaska -- Shelikoff Strait -- Alsek River Sediment Instability Area -- 3.19.3 The Aleutian Subduction Zone -- 3.20 BRITISH COLUMBIA -- 3.20.1 Queen Charlotte Sound -- 3.20.2 The Fraser Delta -- Evidence of gas -- ACOUSTIC TURBIDITY AND ENHANCED REFLECTIONS -- GAS IN CORES -- Gas-related features -- POCKMARKS -- SEABED DOMES -- 3.21 CASCADIA -- 3.21.1 Hydrate Ridge -- 3.21.2 Axial Seamount -- 3.22 CALIFORNIA -- 3.22.1 Northern California -- The Eel Shelf and Slope -- Klamath Delta -- 3.22.2 Monterey Bay -- 3.22.3 Big Sur -- 3.22.4 Santa Barbara Channel -- 3.22.5 Malibu Point -- 3.23 OCEAN SPREADING CENTRES OF THE EAST PACIFIC -- 3.23.1 Guaymas Basin, Gulf of California -- 3.24 CENTRAL AND SOUTH AMERICA -- 3.24.1 Costa Rica -- 3.24.2 Peru -- 3.24.3 The Argentine Basin -- 3.24.4 The Mouth of the Amazon -- 3.25 THE CARIBBEAN -- 3.25.1 Barbados Accretionary Wedge -- 3.25.2 Birth of Chatham Island, Trinidad -- 3.26 GULF OF MEXICO. , Migration and seabed features -- Cold-seep biological communities -- Fluids and hydrates -- Asphalt mud volcanoes -- The Florida Escarpment groundwater seeps -- 3.27 THE EASTERN SEABOARD, USA -- 3.27.1 Cape Lookout Bight -- 3.27.2 Atlantic Continental Margin -- Blake Ridge -- The Blake Ridge Diapir -- The Blake Ridge Depression -- Cape Fear Slide -- 3.27.3 Chesapeake Bay -- 3.27.4 Active pockmarks, Gulf of Maine -- 3.28 THE GREAT LAKES -- 3.28.1 Ring-shaped depressions, Lake Superior -- 3.28.2 Pockmark-like depressions, Lake Michigan -- 3.29 EASTERN CANADA -- 3.29.1 The Scotian and Labrador shelves, and the Grand Banks -- 3.29.2 The Laurentian Fan -- 3.29.3 The Baffin Shelf -- Scott Inlet and Buchan Gulf -- Fresh water seeps, Cambridge Fjord -- 3.30 FINALE -- 4 The contexts of seabed fluid flow -- 4.1 INTRODUCTION -- 4.2 OCEANOGRAPHIC SETTINGS -- 4.2.1 Coastal settings -- 4.2.2 Continental shelves -- 4.2.3 Continental slopes and rises -- 4.2.4 Abyssal plains -- 4.3 PLATE TECTONICS SETTINGS -- 4.3.1 Divergent (constructive) plate boundaries -- 4.3.2 Convergent (destructive) plate boundaries -- Subduction zones and accretionary wedges -- Fore-arc basins -- Island arcs -- Back-arc basins -- 4.3.3 Transform plate boundaries -- 4.3.4 Intraplate igneous activity -- Sill intrusions in sedimentary basins -- Large sedimentary abyssal craters -- Hot spots and seamounts -- Subducting seamounts -- 4.3.5 Serpentinite seamounts -- 4.4 CONCLUSION -- 5 The nature and origins of flowing fluids -- 5.1 INTRODUCTION -- 5.2 HOT FLUIDS -- 5.2.1 Magma and volcanic fluids -- Steaming intrusions -- 5.2.2 Geothermal systems -- 5.2.3 Hydrothermal circulation systems -- The recharge zone -- The reaction zone - introducing supercritical water -- ROCK TYPE -- THE DEPTH OF THE REACTION ZONE -- Upflow and venting -- SEDIMENT CAPPING -- 5.2.4 Exothermic hydrothermal systems. , 5.3 WATER FLOWS -- 5.3.1 Submarine groundwater discharge (SGD) -- 5.3.2 Expelled pore water -- 5.4 PETROLEUM FLUIDS -- 5.4.1 Organic origins -- Assembling complex hydrocarbons -- Disassembling complex hydrocarbons -- 5.4.2 Microbial methane -- Burying the remains -- 5.4.3 Thermogenic hydrocarbons -- Petroleum -- Coal -- Escape from the kitchens -- 5.4.4 Hydrothermal and abiogenic petroleum -- Accelerated sediment maturity -- Post-magmatic inorganic synthesis -- Mantle-derived methane -- The Deep-Earth Gas hypothesis -- Biogenic vs abiogenic -- 5.5 DISCRIMINATING BETWEEN THE ORIGINS -- 6 Shallow gas and gas hydrates -- 6.1 INTRODUCTION -- 6.1.1 The character and formation of gas bubbles -- 6.2 GEOPHYSICAL INDICATORS OF SHALLOW GAS -- 6.2.1 The acoustic response of gas bubbles -- 6.2.2 Seismic evidence of gassy sediments -- Acoustic turbidity -- Enhanced reflections -- Intrasedimentary doming -- Pulldown -- Gas chimneys -- Bright spots -- Flat spots -- Acoustic blanking and columnar disturbances -- 6.2.3 Novel gas detection and mapping -- 3D-seismic techniques used for detection of hazardous gas -- High-resolution gravity -- 6.2.4 Seasonal shallow gas depth variations -- 6.3 GAS HYDRATES - A SPECIAL TYPE OF ACCUMULATION -- 6.3.1 Nature and formation -- The nature of occurrences -- Gas hydrate formation processes -- Gas hydrate formation at Hakon Mosby Mud Volcano -- The consequences of hydrate formation -- 6.3.2 Gas hydrates and fluid flow -- 6.3.3 The BSR -- ODP pioneers drilling through the BSR -- ODP LEG 146, CASCADIA ACCRETIONARY WEDGE -- ODP LEG 164, BLAKE OUTER RIDGE -- ODP LEG 204, HYDRATE RIDGE -- What is the BSR? -- 6.3.4 Other hydrate indicators -- 6.3.5 Dissociation -- 7 Migration and seabed features -- 7.1 INTRODUCTION -- 7.2 POCKMARKS AND RELATED FEATURES -- 7.2.1 Distribution -- 7.2.2 Pockmarks and fluid flow. , Action from above or below?.
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  • 3
    Online Resource
    Online Resource
    Dordrecht :Springer Netherlands,
    Keywords: Deep sea corals. ; Coral reefs and islands. ; Marine biodiversity. ; Electronic books.
    Description / Table of Contents: This volume provides a comprehensive and thorough scientific analysis and documentation of deep-water coral reefs around the world, highlighting the general geological implications for the understanding of ancient coral and carbonate reefs.
    Type of Medium: Online Resource
    Pages: 1 online resource (299 pages)
    Edition: 1st ed.
    ISBN: 9781402084607
    Series Statement: Springer Praxis Bks.
    DDC: 577.789
    Language: English
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  • 4
    Keywords: Meeresboden ; Geomorphologie ; Unterwasserquelle ; Meeresboden ; Hydrothermalquelle ; Cold Seep ; Gashydrate ; Gasblase ; Ausgasung ; Meeresboden ; Erdöl ; Quelle ; Austritt ; Meeresökosystem ; Geoökosystem ; Meeresboden ; Extremophiler Mikroorganismus ; Biogeochemie ; Aquatisches Ökosystem ; Carbonate ; Methan ; Biomineralisation
    Type of Medium: Book
    Pages: XII, 293 S , Ill., graph. Darst., Kt
    ISBN: 0860109488
    DDC: 551.46'08
    Language: English
    Note: Literaturangaben
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  • 5
    Book
    Book
    Chichester, UK : Praxis Publishing | Dordrecht : Springer
    Keywords: Deep-sea corals ; Coral reefs and islands ; Marine biodiversity ; Coral reefs and islands ; Coral reef ecology ; Tiefsee ; Korallenriff ; Biodiversität ; Atlantischer Ozean Nord ; Lophelia ; Calciumcarbonat ; Kaltwasser ; Schlammhügel ; Bioherm ; Korallenriff ; Ökosystem ; Meeresbiologie ; Kaltwasser ; Lophelia
    Type of Medium: Book
    Pages: xxvi, 278 Seiten , Illustrationen, Diagramme
    ISBN: 1402084617 , 9781402084614
    Series Statement: Springer Praxis books in life sciences incorporating aquatic and marine sciences
    DDC: 593.6/1779
    RVK:
    Language: English
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  • 6
    Book
    Book
    Cambridge [u.a.] : Cambridge Univ. Press
    Keywords: Ocean bottom ; Marine sediments Gas content ; Upwelling (Oceanography) ; Deep-sea ecology ; Ocean bottom ; Marine sediments Gas content ; Upwelling (Oceanography) ; Deep-sea ecology ; Meeresboden ; Meeressediment ; Meeresökologie ; Meeresboden ; Hydrothermalquelle ; Cold Seep ; Meeresgeologie ; Meeressediment ; Gashydrate ; Methan ; Ausbruch ; Meeresboden ; Meeressediment ; Meeresökologie ; Meeresboden ; Hydrothermalquelle ; Cold Seep ; Meeresgeologie ; Meeressediment ; Gashydrate ; Methan ; Ausbruch
    Type of Medium: Book
    Pages: XV, 475 S. , Ill., graph. Darst., Kt. , 26cm
    Edition: 1. publ.
    ISBN: 0521114209 , 9780521114202 , 0521819504 , 9780521819503
    DDC: 551.468
    RVK:
    RVK:
    Language: English
    Note: Literaturverz. S. 387 - 441 , Includes bibliographical references and index. - Formerly CIP
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  • 7
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Terra nova 2 (1990), S. 0 
    ISSN: 1365-3121
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: Buried carbonate reefs are favoured hydrocarbon prospecting targets, mainly due to their high porosity and potential for containing large quantities of petroleum. The question of the true relationship between reef structure and the internally trapped fluids (hydrocarbons) is here raised as one of cause - and effect. In other words, which came first, the hydrocarbons or the carbonate reef itself?Modern bioherms and seabed carbonate reefs in, amongst other locations, the North Sea and the Gulf of Mexico, are shown to form in close association with active hydrocarbon seepages. Mainly based on results from ecological studies at deep-ocean vent communities, a new model for carbonate reef formation is promoted: that such reefs form at locations containing high concentrations of bacteria and other microorganisms suspended in the water column as a result of seeping fluids (solutions and gases) that provide some of the energy basis and carbon source for ecosystems independently of photosynthesis. Therefore, on burial and effective sealing (‘capping’), these carbonate reefs become hydrocarbon reservoirs, trapping and accumulating the very minerals on which they - in the first place - were dependent.
    Type of Medium: Electronic Resource
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  • 8
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Sedimentology 31 (1984), S. 0 
    ISSN: 1365-3091
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: This paper presents the results of a comparative study of pockmarks and associated features appearing on both sides of the North Atlantic: on the Scotian Shelf off Nova Scotia and in the northern North Sea. Pockmarks are formed in seabed material consisting of soft silty clay. The seismic, sonar and lithologic characteristics of the sediments on the Scotian Shelf are remarkably similar to those found in the northern North Sea. Sediment clouds suspended in the water column immediately over the seabed have previously been observed on side-scan records associated with gas-charged sediments on corresponding shallow-seismic records. These and similar observations strongly suggest that most pockmarks are caused by gas efflux through the seafloor. However, the detailed mechanism of formation and the origin of the gas in the sediments is still unknown.
    Type of Medium: Electronic Resource
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  • 9
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 357 (1992), S. 119-119 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] SIR - The remarkable photograph (S. V. Boletzky et al. Nature 356, 199; 1992) of a cirrate octopod hovering at a water depth of 2.88 metres off Lifou Island in the southwestern Pacific raises the question of why the animal prefers transition into a pumpkin shape as a defence mechanism. The answer ...
    Type of Medium: Electronic Resource
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  • 10
    Publication Date: 2024-02-16
    Description: Gullfaks is one of the four major Norwegian oil and gas fields, located in the northeastern edge of the North Sea Plateau. Tommeliten lies in the greater Ekofisk area in the central North Sea. During the cruises HE 208 and AL 267 several seep locations of the North Sea were visited. At the Heincke seep at Gullfaks, sediments were sampled in May 2004 (HE 208) using a video-guided multiple corer system (MUC; Octopus, Kiel). The samples were recovered from an area densely covered with bacterial mats where gas ebullition was observed. The coarse sands limited MUC penetration depth to maximal 30 centimeters and the highly permeable sands did not allow for a high-resolution, vertical subsampling because of pore water loss. The gas flare mapping and videographic observation at Tommeliten indicated an area of gas emission with a few small patches of bacterial mats with diameters 〈50 cm from most of which a single stream of gas bubbles emerged. The patches were spaced apart by 10-100 m. Sampling of sediments covered by bacterial mats was only possible with 3 small push cores (3.8 cm diameter) mounted to ROV Cherokee. These cores were sampled in 3 cm intervals. Lipid biomarker extraction from 10 -17 g wet sediment was carried out as described in detail elsewhere (Elvert et al., 2003; doi:10.1080/01490450303894). Briefly, defined concentrations of cholestane, nonadecanol and nonadecanolic acid with known delta 13C-values were added to the sediments prior to extraction as internal standards for the hydrocarbon, alcohol and fatty acid fraction, respectively. Total lipid extracts were obtained from the sediment by ultrasonification with organic solvents of decreasing polarity. Esterified fatty acids (FAs) were cleaved from the glycerol head group by saponification with methanolic KOH solution. From this mixture, the neutral fraction was extracted with hexane. After subsequent acidification, FAs were extracted with hexane. For analysis, FAs were methylated using BF3 in methanol yielding fatty acid methyl esters (FAMES). The fixation for total cell counts and CARD-FISH were performed on-board directly after sampling. For both methods, sediments were fixed in formaldehyde solution. After two hours, aliquots for CARD-FISH staining were washed with 1* PBS (10mmol/l sodium phosphate solution, 130mmol/l NaCl, adjusted to a pH of 7.2) and finally stored in a 1:1 PBS:ethanol solution at -20°C until further processing. Samples for total cell counts were stored in formalin at 4°C until analysis. For sandy samples, the total cell count/CARD-FISH protocol was optimized to separate sand particles from the cells. Cells were dislodged from sediment grains and brought into solution with the supernatant by sonicating each sample onice for 2 minutes at 50W. This procedure was repeated four times and supernatants were combined. The sediment samples were brought to a final dilution of 1:2000 to 1:4000 and filtered onto 0.2µm GTTP filters (Millipore, Eschbonn, Germany).
    Type: Dataset
    Format: application/zip, 2 datasets
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