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The Gulf of St. Lawrence: A Unique Ecosystem
The Gulf of St. Lawrence: A Unique Ecosystem

... probable sources (i.e. industrial plants). The most abundant contaminants appear to be PCBs and other organochlorine pesticides because they do not easily biodegrade. It is interesting that although the production and use of most of these compounds has been prohibited for several decades they are st ...
Status and trends of, and threats to, deep seabed genetic
Status and trends of, and threats to, deep seabed genetic

... The present document has been written in response to paragraph 54 of decision VII/5. It presents information on the methods for the identification, assessment and monitoring of genetic resources in the deep seabed beyond the limits of national jurisdiction; compiles and synthesizes information on th ...
Past and present natural methane seepage on the northern
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Underwater Domains in Yellowstone Lake Hydrothermal Vent
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Sulphur Emission and Transformations at Deep Sea Hydrothermal

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Reader Chapter 2 In chapter 2 and 3 you can read more about the
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... north. Weikert (1987) indicated that the habitat becomes more hostile to planktonic life as depth increases and with distance from the Gulf of Aden, which is the source of plankton, and thus the number of species decreases with depth and towards the Gulfs of Suez and Aqaba. For example, in calanoid ...
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... You will see the true face of the ocean floor Covered by sediments, gravel, silt and mud Sediment particles from land, from biological activity, and even from space Sediments can help us define what occurred in recent history in the ocean basin Sediment thickest at continental margins Thinnest over ...
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Relative Abundance and Diversity of Bacterial Methanotrophs at the

... level fluctuations (Droz et al., 2003). These sedimentary inputs flow 760 km off the Congo-Angola margin along the presentday active channel-levee system, which ends with lobe-shaped sedimentary deposits called the recent lobe complex (Savoye et al., 2009). The accumulated sediments (1.25 × 106 t of ...
Fundamental Characteristics of Hydrothermal Submarine Systems
Fundamental Characteristics of Hydrothermal Submarine Systems

... is the principal agent of energy and mass transfer from the Earth=s crust to the ocean and one of the primary modes of interaction between the solid earth and the ocean/ atmosphere system. The fluid discharged from seafloor geothermal reservoirs cools the submarine hot rock, builds mineral deposits, ...
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... environments and most of the abyssal seafloor is highly stable for long periods of time, but evidence accumulated since 1960s has shown that the deep sea is in fact a dynamic environment: in some regions and especially along continental margins sediment instability, strong bottom current, dense wat ...
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... particular, is more or less entirely controlled by the presence or absence of hypoxia/anoxia. Current evidence suggests that the spatial and temporal extent of oxygen deficiency has increased over the past decades. In the light of historical work, it is also likely that reference conditions defined ...
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Cold seep



A cold seep (sometimes called a cold vent) is an area of the ocean floor where hydrogen sulfide, methane and other hydrocarbon-rich fluid seepage occurs, often in the form of a brine pool. ""Cold"" does not mean that the temperature of the seepage is lower than that of the surrounding sea water. On the contrary, its temperature is often slightly higher. Cold seeps constitute a biome supporting several endemic species.Cold seeps develop unique topography over time, where reactions between methane and seawater create carbonate rock formations and reefs. These reactions may also be dependent on bacterial activity. Ikaite, a hydrous calcium carbonate, can be associated with oxidizing methane at cold seeps.
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