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oceans, seafloor, and continental margins
oceans, seafloor, and continental margins

... siliceous and calcareous oozes, and red clays ...
Vol. 21, No. 2
Vol. 21, No. 2

... and synthesize key information/data. Due to the tight timelines and need to constrain its scope, our workshop focused primarily on fishing-related activities in the North Pacific. Clearly, however, within PICES we have considerable scientific understanding of other human activities that could be exp ...
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Alexei Platonov (1), José Manuel Redondo(1), Joan Graú

... of marine pollution and other types of marine and atmospheric phenomena. Since natural (caused by plankton, fish, etc.) and man-made oil slicks dampen the smallscale surface waves, which are responsible for the radar backscattering from the water surface, they are visible as dark patches or lines in ...
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... program has built a seamless global array of more than 3,500 free-drifting profiling floats, measuring the upper 2,000 meters of the ocean. This program, for the first time, allows continuous monitoring of ocean temperature, salinity and velocity concurrently and on a global scale, with all data rel ...
Translation Series No. 421
Translation Series No. 421

... Special experiments showed that prepared [predvaritelnye] membrane filters such as are used for filtering phytoplankton from fresh water,introdUced_errors when used to determine phytoplankton production in the sea, because these filters would let part of the small peridinean algae go through them, a ...
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The Ocean Planet - South Carolina Sea Grant Consortium
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... surface is covered by a layer of water known as the hydrosphere. Although scientists have found water ice on Mars and an ice crust has been discovered on Jupiter's moon Europa, it is no surprise that the Ocean Planet is the only planet presently known to mankind that is capable of supporting life—an ...
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Ambient Noise Measurement Using Naval Sensors

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... South Pacific, North and South Atlantic, Indian and Arctic Oceans and the Antarctic waters or seas. Scientists believe that the seas are as much as 500 million years old because animals that lived then occur as fossils in rocks which once were under ancient seas. There are several theories about the ...
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... in Europe. Here’s how we hypothesized they might have done so: We knew that surface water temperatures in the ocean affect the atmosphere - warmer ocean waters give heat to the atmosphere, making the air “lighter” or more buoyant, and reducing the air pressure. Similarly, colder surface waters cool ...
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... crack in the oceanic crust. At a mid-ocean ridge, molten material rises from the mantle and erupts. The molten material then spreads out, pushing older rock to both sides of the ridge. As the molten material cools, it forms a strip of solid rock in the center of the ridge. Then more molten material ...
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IOC/SCOR Workshop on Global Ocean Ecosystem Dynamics

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Oceanography - Flushing Community Schools
Oceanography - Flushing Community Schools

... ask good questions by asking who, what, when, where, why, and how. ...
Spatial Pattern of Bathymetry in Wangi
Spatial Pattern of Bathymetry in Wangi

... and depth of 200 meters. The condition of ocean floor topography on the areas of waters near the shore changes gradually from deep to steep. Moreover, the depth of the ocean floor As shown by the aforementioned figure, it is to outer island topography becomes steep with clear that the basic profile ...
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Marine habitats



The marine environment supplies many kinds of habitats that support marine life. Marine life depends in some way on the saltwater that is in the sea (the term marine comes from the Latin mare, meaning sea or ocean). A habitat is an ecological or environmental area inhabited by one or more living species.Marine habitats can be divided into coastal and open ocean habitats. Coastal habitats are found in the area that extends from as far as the tide comes in on the shoreline out to the edge of the continental shelf. Most marine life is found in coastal habitats, even though the shelf area occupies only seven percent of the total ocean area. Open ocean habitats are found in the deep ocean beyond the edge of the continental shelf.Alternatively, marine habitats can be divided into pelagic and demersal habitats. Pelagic habitats are found near the surface or in the open water column, away from the bottom of the ocean. Demersal habitats are near or on the bottom of the ocean. An organism living in a pelagic habitat is said to be a pelagic organism, as in pelagic fish. Similarly, an organism living in a demersal habitat is said to be a demersal organism, as in demersal fish. Pelagic habitats are intrinsically shifting and ephemeral, depending on what ocean currents are doing.Marine habitats can be modified by their inhabitants. Some marine organisms, like corals, kelp, mangroves and seagrasses, are ecosystem engineers which reshape the marine environment to the point where they create further habitat for other organisms.
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