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  • 1
    Monograph available for loan
    Monograph available for loan
    Cambridge : Cambridge Univ. Press
    Call number: M 07.0041
    Description / Table of Contents: Contents: 1. Seabed fluid flow introduction; 2. Pockmarks, shallow gas and seeps: an initial appraisal; 3. Seabed fluid flow around the world; 4. The contexts of seabed fluid flow; 5. The nature and origins of flowing fluids; 6. Shallow gas and gas hydrates; 7. Migration and seabed features; 8. Seabed fluid flow and biology; 9. Seabed fluid flow and mineral precipitation; 10. Impacts on the hydrosphere and atmosphere; 11. Implications for man; References; Index.
    Type of Medium: Monograph available for loan
    Pages: xv, 475 S.
    ISBN: 0521819504
    Classification:
    Oceanology
    Location: Upper compact magazine
    Branch Library: GFZ Library
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  • 2
    Monograph available for loan
    Monograph available for loan
    London [u.a.] : Graham & Trotman
    Call number: AWI G4-92-0478
    Description / Table of Contents: Contents: Chapter 1 Seabed pockmarks and seepages: an introduction. - Chapter 2 Focus on North Sea pockmarks. - Chapter 3 Detailed surveys of North Sea pockmarks and seepages. - Chapter 4 Pockmarks around the world. - Chapter 5 A theory of pockmark formation. - Chapter 6 Submarine seepages. - Chapter 7 Features associated with seepage. - Chapter 8 Seepages and mineral precipitation. - Chapter 9 The ecology of pockmarks and seepages. - Chapter 10 Some implications and consequences of widespread seabed seepages. - Epilogue. - Appendix I Methane in seabed sediments. - Appendix II Survey techniques. - Appendix III Seabed relief maps and locations. - Glossary. - Index
    Description / Table of Contents: This original new work represents a major breakthrough in marine geology and ecology. The book examines the fact that gases are generated in, and fluids circulate through seabed sediments. The recognition of such a dynamic seabed environment has far-reaching implications for the understanding of sediment dynamics, marine biological productivity, mineral cycles, the CO2 budget, ferro-manganese nodule formation and carbonate formation. Seabed pockmarks are described, firstly from detailed studies conducted in the North Sea, and then with reference to pockmarks from many different parts of the world. The evidence presented is then used to explain their mode of formation. The discovery in pockmarks of a dense and varied fauna, and of methane-generated carbonate cements has led the authors to a comparison with seabed seepages in other marine geological contexts, including the hydrothermal seepages of ocean spreading centres, subduction zones, etc, where assemblages of seepage-dependent organisms have been found. The authors discuss their concept of a dynamic fluid circulation system in soft sediments, oceanic crust and sedimentary basins which result in the precipitation of minerals and the provision of nutrients to marine biological communities. Their findings may form the basis of a new understanding of ocean energy and nutrient budgets and the immense productivity of the world's seas and oceans. The book will be especially valuable to those interested in: sedimentology and marine geology, marine biology and ecology, marine and atmospheric pollution, offshore hydrocarbon exploration and exploitation, the floors of the world's seas and oceans in general.
    Type of Medium: Monograph available for loan
    Pages: xii, 293 S. : graph. Darst.
    Edition: 1. publ.
    ISBN: 0860109488
    Branch Library: AWI Library
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  • 3
    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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  • 4
    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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  • 5
    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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  • 6
    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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  • 7
    Publication Date: 2024-02-16
    Keywords: 10-methyl-Hexadecanoic acid; 10-methyl-Hexadecanoic acid, δ13C; AL267; AL267_1274-MUC; Alkor (1990); anteiso-fatty acid C15:0; anteiso-fatty acid C15:0, δ13C; anteiso-fatty acid C17:0; anteiso-fatty acid C17:0, δ13C; Archaeol; Archaeol, δ13C; Bishomohopanol, δ13C; cy-fatty acids C17:0w5,6; cy-fatty acids C17:0w5,6, δ13C; Date/Time of event; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Diplopterol; Diplopterol, δ13C; Event label; fatty acid C16:1w5; fatty acid C16:1w5cis; fatty acid C18:1w7cis; fatty acid C18:1w9cis; Gas chromatography; HE180; HE180/1904; HE208; HE208/766; Heincke; iso-fatty acid C15:0; iso-fatty acid C15:0, δ13C; iso-fatty acid C17:0; iso-fatty acid C17:0, δ13C; Isoprene-fatty acid C19:0; Isoprene-fatty acid C19:0, δ13C; Kvitebjorn; Latitude of event; Longitude of event; MUC; MultiCorer; Multicorer with television; n-fatty acid C14:0; n-fatty acid C14:0, δ13C; n-fatty acid C15:0; n-fatty acid C15:0, δ13C; n-fatty acid C16:0; n-fatty acid C16:0, δ13C; n-fatty acid C16:1w7cis, δ13C; n-fatty acid C17:0, δ13C; n-fatty acid C18:0; n-fatty acid C18:0, δ13C; n-fatty acid C18:1w7cis, δ13C; n-fatty acid C18:1w9cis, δ13C; North Sea; Sample comment; sn2-Hydroxyarchaeol; sn2-Hydroxyarchaeol, δ13C; TVMUC; VC; Vibro corer
    Type: Dataset
    Format: text/tab-separated-values, 105 data points
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  • 8
    Publication Date: 2024-02-16
    Keywords: AL267; AL267_1274-MUC; Alkor (1990); Anaerobic methanotrophic archaea-1, targeted with ANME-1-350 oligonucleotide FISH-probe; Anaerobic methanotrophic archaea-2a, targeted with ANME-2a-647 oligonucleotide FISH-probe; Anaerobic methanotrophic archaea-2a, targeted with ANME-2c-622 oligonucleotide FISH-probe; Anaerobic methanotrophic archaea-3, targeted with ANME-3-1249 oligonucleotide FISH-probe; Archaea; Area/locality; Bacteria; Catalysed reporter deposition-fluorescence in situ hybridization (CARD-FISH); Date/Time of event; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Desulfusarcina/Desulfococcus, targeted with DSS658 oligonucleotide FISH-probe; Event label; HE208; HE208/766; HE208/771; Heincke; Kvitebjorn; Latitude of event; Longitude of event; MUC; MultiCorer; Multicorer with television; North Sea; Prokaryotes, abundance as single cells; Sample comment; Standard deviation; TVMUC
    Type: Dataset
    Format: text/tab-separated-values, 161 data points
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  • 9
    Publication Date: 2003-01-01
    Description: During a regional seismic interpretation study of leakage anomalies in the northern North Sea, mounds and zones with a highly chaotic seismic reflection pattern in the Tertiary Hordaland Group were repeatedly observed located above gas chimneys in the Cretaceous succession. The chaotic seismic reflection pattern was interpreted as mobilized sediments. These mud diapirs are large and massive, the largest being 100 km long and 40 km wide. Vertical injections of gas, oil and formation water are interpreted to have triggered the diapirs. On the eastern side of the Viking Graben, another much smaller type of mud diapir was observed. These near-circular mud diapirs are typically 1-3 km in diameter in the horizontal plane. Limited fluid injection from intra-Hordaland Group sands, through sand injection zones, into the upper Hordaland Group is interpreted to have triggered the near-circular diapirs. This observed external' type of mobilization was generated at shallow burial (〈1000 m) and should be discriminated from the more common internal' type of mud diapirism that is generated in deep basins (〉3000 m). The suggested model has implications for the understanding of the palaeofluid system, sand distribution, stratigraphic prediction within the chaotic zone, seismic imaging, and seismic interpretation of the hydrocarbon plumbing' system.
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  • 10
    Publication Date: 2012-05-13
    Print ISSN: 0276-0460
    Electronic ISSN: 1432-1157
    Topics: Geosciences
    Published by Springer
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