Sunday, July 12, 2009

Abyssal plains


Abyssal plains are flat or very gently sloping areas of the deepocean basin floor. They are among the Earth's flattest and smoothest regions and the least explored. Abyssal plains cover approximately 40% of the ocean floor and reach depths between 2,200 and 5,500 m (7,200 and 18,000 ft). They generally lie between the foot of a continental rise and a mid-oceanic ridge.

There are several distinct abyssal plains across the world's oceans. Each abyssalplain starts at a continental rise and continues until it reaches a mid-oceanic ridge, resuming on the other side. Mid-oceanic ridges are huge underwater mountain chains marking major plate boundaries. These ridges are also the primary source of sea floor spreading since they are slowly pulling apart. Since the continental slope and the ridges essentially form the edge of a deep bowl, some people refer to the abyssal plain as the ocean basin. Overall, the abyssalplain represents around 40% of the ocean floor.

Other components of abyssal plain sediment include wind-blown dust, volcanic ash, chemical precipitates, and occasional meteorite fragments. Abyssal plains are often littered with nodules of manganese containing varying amounts of iron, nickel, cobalt, and copper. These pea to potato-sized nodules form by direct preciption of mineralsfrom the sea-water onto a bone or rock fragment. Currently, deposits of manganese nodules are not being mined from the sea bed, but it is possible that they could be collected and used in the future.

Of the 15 billion tons of river-carried clay, sand, and gravel that are washed into the oceanseach year, only a fraction of this amount reaches the abyssal plains. The amount of biological sediment that reaches the bottom is similarly small. Thus, the rate of sediment accumulation on the abyssal plains is very slow, and in many areas, less than an inch of sediment accumulates per thousand years. Because of the slow rate of accumulation and the monotony of the topography, abyssal plains were once believed to be a stable, unchanging environment. However, deep ocean currents have been discovered that scour the ocean floor in places. Some currents have damaged trans-oceanic communication cables laid on these plains.

Although they are more common and widespread in the Atlantic and Indian ocean basins than in the Pacific, abyssal plains are found in all major ocean basins. Approximately 40% of the planet's ocean floor is covered by abyssal plains. The remainder of the ocean floor topography consists of hills, cone-shaped or flat-topped mountains, deep trenches, andmountain chain such as the mid-oceanic ridge systems.

The abyssal plains do not support a great abundance of aquatic life, though some species do survive in this relatively barren environment. Deep sea dredges have collected specimens of unusual-looking fish, worms, and clam-like creatures from these depths.




Saturday, July 11, 2009

continental slope

now let we see about another part in ocean environment that is continental slope and their environmental characteristics with species habitat

A continental slope is a relatively steep slope that extends from a depth of 100 to 200 meters at the edge of the continental shelf down to oceanic depths.the average angle of slope for a continental slope is 4 to 5 degree, although locally some parts are much steeper.


Because the continental slopes are more difficult to study than the continental shelves, less is known about them. the greater depth of water and the locally steep inclines on the continental slopes hinder rock dredging and drilling and make the results of seismic refraction and reflection harder to interpret.
Environment of the Continental Slope:
The deep waters of the Continental Slope are characterized by cold temperatures, low light conditions, and very high pressures. Sunlight does not penetrate to these depths, having been absorbed or reflected in the water above. In absorbing sunlight, surface waters are heated, while deeper waters stay cold, typically just a few degrees above freezing. Some mixing of the warm and cold waters occurs, generally in the top 100 m (330 ft) of the water column.
Adaptations to Life on the Slope:

Because of the cold environment, organisms that live at greater depths have slower metabo- lisms. As a result, they eat less frequently, are slower in digesting their food, and move more slowly.When these organisms are observed at depth with video equipment, they typically are seen sitting immobile on the bottom or floating with the current just off the bottom. Another consequence of slower metabolism is that the animals grow more slowly and attain greater ages than their counterparts that live in shallower waters. It has been determined that some deep-sea rockfish live more than 70 years. Many of the animals living in the perpetual darkness of these depths have developed light producing organs.Among organisms with these structures are shrimps and several fishes, includ- ing midshipman, flashlightfish, lampfish (fig.1), and headlightfish. Each species has its own
distinctive pattern of lights that serve various functions, such as communicating with members of their own kind (as in courtship), attracting food (Figure 1. Northern lampfish with light organs (small white circles) along its underside. This small fish, only about 6cm (2.5 in) long, also displays the dark coloration typical of many animals on deeper parts of the Continental Slope. )(like attracting moths to a flame), and avoiding being eaten (flashing a light in a predator’s eyes can give an animal a chance to get away). Another adaptation to the darkness is an absence of color diversity. With no light, colors can have no function. Therefore, animals living on the Continental Slope are generally either a dark color, like black or brown, or red (fig. 2). Among the fishes, rockfish and thornyheads are dominantly red. Red is also the basic color of many invertebrates, including certain crabs and shrimps. The red wavelengths of sunlight are absorbed in the water near the surface, and so do not penetrate to deeper areas. Because of this, red objects appear black at depth, (Figure 2. Because of the absence of light on the Continental Slope, animals living there are generally either a dark color, such as the sablefish (top), or red, such as the shortspine thornyhead (bottom)).

allowing red organisms to blend in with their dark surroundings. Most animals living on the Continental Slope are dark. Among the few exceptions is the deep-sea sole, which is mostly blue, with some black and brown. The water pressure on the sea floor at the top of the Continental Slope is more than 10 times higher than at the surface, and at the bottom of the slope the pressure can be more than 100 times higher than at the surface. To compensate for this difference in pressure, organisms have a large percentage of water in their tissues, bones, and shells that replaces other substances, such as gases and calcium. Owing to the high water content of their muscle tissues, many larger, older fish caught from deeper waters are limp and soft when brought to the surface. An example is the Dover sole, which as it grows and matures, moves deeper downslope, increasing the water content of its tissues. Because of their high water content, mature Dover sole brought to the surface become "jellied" and slimy, leading to one of the fish’s original names, "slime sole." Another such example is the shells of some deep-slope crabs, which are rigid at depth but are easily crushed when they are brought to the surface.

Different Slope Communities :

Fishes living at different depths on the Continental Slope have different life-histories. Species living near the top of the slope produce pelagic (open ocean) young that spend the first few months to years of life swimming in the upper water column and then settle out in relatively shallow water and migrate downslope as they grow and mature (fig. 3). Dover sole, sablefish, and rockfish (fig. 4) have this type of life history; however, most species living deeper, such as rattails, deep-sea soles, and slickheads, have young that live in the same depths as adults. Relatively few species occur at all or most depths on the Continental Slope. Species occu-pying (Figure 3. Juvenile rockfish swimming over Cordell Bank in the northern Gulf of the Farallones. Species of fish living near the top of the Continental Slope in the gulf produce pelagic (open-ocean) young that spend the first few months to years of life swimming in the upper water column and then settle out in relatively shallow water and migrate downslope as they grow and mature. )

one depth commonly are replaced by similar species at other depths. An exception is the eel-like hagfish, which is found at all depths on the slope. In general, the distribution of most (Figure 4. Ared-banded rockfish on the Continental Slope in the Gulf of the Farallones. Relatively few species of fish occur at all or most depths on the slope. Those occupying one depth commonly are replaced by similar species at other depths. For example, greenstriped and stripetail rockfishes live on muddy bottoms on the upper part of the slope, whereas at greater depth they are replaced by species of thornyheads. )

groups changes with increasing depth. For example, on the upper part of the slope, greenstriped and stripetail rockfishes live on muddy bottoms, whereas at greater depth, they are replaced by two species of thornyheads. Another example is skates, which are similar to rays. About five common species of skates live in the shallow waters of the slope, whereas three different species live at greater depths on the slope.

Fisheries :

Currently productive commercial fisheries on the Continental Slope off California’s coast catch Dover sole, sablefish, deep-living rockfishes, and thornyheads . Many of these fishes occupy similar habitats and generally are caught as a group. One increasingly active fishery is for rattails, a deep-living fish with a large head and a long tail that tapers to a point. Another fishery
exists for spot prawn, a rather large, spotted shrimp that lives on muddy bottoms along the slope. Smaller fisheries include one for a large shell-less snail (a nudibranch) that is sold for scientific research. One major fishery of note is for hagfish, the skin of which is used to make what are sold as "eel skin" wallets. Hagfish are not true eels but are a primitive group of fish that have no bones and no jaws. Instead of bones, they have cartilage, and instead of jaws, they have a large sucker-like mouth similar to that of a lamprey or a leech. Once attached, hagfish use a tongue with many tiny teeth to dig into their prey. Once inside, the prey is eaten from the inside out. Besides its unique method of eating, the hagfish has another interesting trait—it produces copious amounts of slime, probably used to discourage predators, and giving the fish its nickname, the "slime eel."















Continental shelf


where is continental shelf? what is continental shelf?, where it starts and where it ends, so we have lot of questions about continental shelf, lte we see about continental shelf and nature of continental shelf, species living in, and etc., first we see about different definitions for continental shelf


  • The continental shelf is an undersea extension which can stretch for many miles out to the sea in some cases. Many nations have asserted mineral and land rights to their associated continental shelves, since this region of the ocean is rich in natural resources such as marine life.

  • There are actually several parts to the continental shelf. The first part is the shelfitself, which starts below the shoreline of a continent. The shelf slopes gently as it stretches towards the deeper part of the ocean, until it reaches a certain point and drops off sharply, causing the waters above to rapidly become much deeper. This drop is called thecontinental break, and it occurs uniformly at around 460 feet (140 meters) of depth.t has been theorized that the continental break may mark the former sea level of the world's oceans.

  • the continental shelf, a shallow submarine platform at the edge of a continent inclines very gently seaward, generally at an angle 0.1 degeree.Continental shelves vary in width.on the pacific coast of north America the shelf is only a few kilometers wide. On the Pacific off Newfoundland in the Atlantic ocean it is about 500 kilometers.portions of the shelves in the Arctic Ocean off siberia and northern Europe are even wider. Water depth over a continental shelf tends to increase regularly away from land, with the outer edge of the shelf being about 100 to 200 meters below sea level.