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  • 1
    In: Oceanography, Rockville, MD : The Oceanography Society, 1988, 22(2009), 1, Seite 92-109, 2377-617X
    In: volume:22
    In: year:2009
    In: number:1
    In: pages:92-109
    Description / Table of Contents: Submarine hydrocarbon seeps are geologically driven "hotspots" of increased biological activity on the seabed. As part of the HERMES project, several sites of natural hydrocarbon seepage in the European seas were investigated in detail, including mud volcanoes and pockmarks, in study areas extending from the Nordic margin, to the Gulf of Cádiz, to the Mediterranean and Black seas. High-resolution seabed maps and the main properties of key seep sites are presented here. Individual seeps show ecosystem zonation related to the strength of the methane flux and distinct biogeochemical processes in surface sediments. A feature common to many seeps is the formation of authigenic carbonate constructions. These constructions exhibit various morphologies ranging from large pavements and fragmented slabs to chimneys and mushroom-shaped mounds, and they form hard substrates colonized by fixed fauna. Gas hydrate dissociation could contribute to sustain seep chemosynthetic communities over several thousand years following large gas-release events.
    Type of Medium: Online Resource
    Pages: Ill., graph. Darst
    ISSN: 2377-617X
    Language: English
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  • 2
    In: Marine ecology progress series, Oldendorf/Luhe : Inter-Research, 1979, 382(2009), Seite 69-86, 1616-1599
    In: volume:382
    In: year:2009
    In: pages:69-86
    Description / Table of Contents: Submarine mud volcanism represents an important pathway for methane from deeper reservoirs to the surface, where it enters the benthic carbon cycle. To quantify overall methane release from the Captain Arutyunov mud volcano (CAMV) and to assess the contribution of macrobenthic seep organisms to the regulation of the benthic methane flux, we linked water column methane concentrations, seabed methane emission and pore water geochemistry to the spatial distribution of seep biota. Prominent organisms of the CAMV seep biota were 3 different species of frenulate tubeworms. Seabed methane emission ranged from 0.001 to 0.66 mmol m-2 d-1. Dense patches of tubeworms were associated with the lowest seabed methane emission. Elevated methane emission was associated with a sporadic distribution of tubeworms and the occurrence of numerous mud clasts. Despite the presence of a large subsurface methane reservoir, the estimated total methane release from CAMV was low (0.006 × 106 mol yr-1). In addition to direct methane consumption by Siboglinum poseidoni, the tubeworms likely contribute to the retention of methane carbon in the sediment by affecting bacterial communities in the proximity of the tubes. The siboglinids create new meso-scale habitats on the sediment surface, increasing habitat heterogeneity and introducing niches for bacterial communities.
    Type of Medium: Online Resource
    Pages: Ill., graph. Darst
    ISSN: 1616-1599
    Language: English
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  • 3
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] More than 50% of the Earth' s surface is sea floor below 3,000 m of water. Most of this major reservoir in the global carbon cycle and final repository for anthropogenic wastes is characterized by severe food limitation. Phytodetritus is the major food source for abyssal benthic ...
    Type of Medium: Electronic Resource
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  • 4
    Publication Date: 2020-02-12
    Description: In sedimentary environments microbial methanotrophy represents an important sink for methane before it leaves the seafloor and enters the water column. Using novel benthic observatories in conjunction with numerical modeling of pore water gradi- ents we investigated seabed methane emission rates at cold seep sites with underlying gas hydrates at the two contrasting regions Hydrate Ridge, (Cascadia margin), and the northern Gulf of Mexico. At both sites occurrence of microbial mats of the genus Beggiatoa apparently is coupled to the presence of shallow gas hydrates, the strength of sulfide flux and the velocity of advective pore water flow. However, type of vent- ing and biogeochemistry at both sites is highly different, which might affect seabed methane emission. At Hydrate Ridge characterized by active fluid and gas venting, seabed methane efflux from microbial mat sites varies from 1.9 to 11.5 mmol m − 2d − 1. Methane consuming efficiency at these sites is about 66 %. At Hydrate Ridge wefound a strong susceptibility of methane seepage from the availability of oxygen in the bottom contact water, emission rates of up to 113 mmol m − 2d − 1 were measured under anoxic conditions. At the Gulf of Mexico oil venting additionally to gas and fluid seepage introduces high amounts of organic carbon into the benthic system and wa- ter column. Seabed methane emission in this region is comparable to Hydrate Ridge and ranges from 0.3 to 7 mmol m − 2d − 1. Beside anaerobic methane oxidation, our measurements indicate a high potential capacity of aerobic methane oxidation in the benthic boundary layer. This layer potentially restrains seabed methane emission when anaerobic methane oxidation in the sediment becomes saturated or when methane is bypassing the sediment matrix along fractures and channels.
    Type: info:eu-repo/semantics/conferenceObject
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  • 5
    Publication Date: 2020-02-24
    Description: In this paper we provide an overview of new knowledge on oxygen depletion (hypoxia) and related phenomena in aquatic systems resulting from the EU-FP7 project HYPOX (“In situ monitoring of oxygen depletion in hypoxic ecosystems of coastal and open seas, and landlocked water bodies”, www.hypox.net). In view of the anticipated oxygen loss in aquatic systems due to eutrophication and climate change, HYPOX was set up to improve capacities to monitor hypoxia as well as to understand its causes and consequences. Temporal dynamics and spatial patterns of hypoxia were analyzed in field studies in various aquatic environments, including the Baltic Sea, the Black Sea, Scottish and Scandinavian fjords, Ionian Sea lagoons and embayments, and Swiss lakes. Examples of episodic and rapid (hours) occurrences of hypoxia, as well as seasonal changes in bottom-water oxygenation in stratified systems, are discussed. Geologically driven hypoxia caused by gas seepage is demonstrated. Using novel technologies, temporal and spatial patterns of watercolumn oxygenation, from basin-scale seasonal patterns to meter-scale sub-micromolar oxygen distributions, were resolved. Existing multidecadal monitoring data were used to demonstrate the imprint of climate change and eutrophication on long-term oxygen distributions. Organic and inorganic proxies were used to extend investigations on past oxygen conditions to centennial and even longer timescales that cannot be resolved by monitoring. The effects of hypoxia on faunal communities and biogeochemical processes were also addressed in the project. An investigation of benthic fauna is presented as an example of hypoxia-devastated benthic communities that slowly recover upon a reduction in eutrophication in a system where naturally occurring hypoxia overlaps with anthropogenic hypoxia. Biogeochemical investigations reveal that oxygen intrusions have a strong effect on the microbially mediated redox cycling of elements. Observations and modeling studies of the sediments demonstrate the effect of seasonally changing oxygen conditions on benthic mineralization pathways and fluxes. Data quality and access are crucial in hypoxia research. Technical issues are therefore also addressed, including the availability of suitable sensor technology to resolve the gradual changes in bottom-water oxygen in marine systems that can be expected as a result of climate change. Using cabled observatories as examples, we show how the benefit of continuous oxygen monitoring can be maximized by adopting proper quality control. Finally, we discuss strategies for state-of-the-art data archiving and dissemination in compliance with global standards, and how ocean observations can contribute to global earth observation attempts.
    Description: Published
    Description: 1215-1259
    Description: 7A. Geofisica di esplorazione
    Description: JCR Journal
    Description: open
    Keywords: Hypoxia, oceans, gas ; 03. Hydrosphere::03.04. Chemical and biological::03.04.01. Biogeochemical cycles
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 6
    Publication Date: 2019-07-17
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , peerRev
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  • 7
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    In:  EPIC3Journal of the marine biological association of the united kingdom:, 76, pp. 327-344
    Publication Date: 2014-09-17
    Description: The size distribution of benthic nematodes was investigated along different gradients of food availability in various regions of the NE Atlantic: I. across the continental margin and II. with increasing distance from the continental rise. An overall trend for miniaturization with increasing distance from the food source was found. However, a series of physical, chemical and biological factors clearly lead to variations in nematode size structure. Moreover, our results indicate that seasonally varying food supply or a periodically pulsed input of organic matter to the sea floor affects nematode size spectra. The hypothesis is proposed that the life cycle of deep-sea nematode species and hence the size structure of their populations are related to seasonal energy availability. This dependence might result in one-year life spans of deep-sea nematodes and probably other meiofauna.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
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  • 8
    Publication Date: 2019-07-17
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , peerRev
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  • 9
    Publication Date: 2014-09-17
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
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  • 10
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    In:  EPIC3Meteor-Berichte:, 96(3), pp. 43-45
    Publication Date: 2014-09-17
    Repository Name: EPIC Alfred Wegener Institut
    Type: Miscellaneous , notRev
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