Clastic material
Clay, calcium carbonate, silica and organic material
Particle Formation in Oceans(enhance text by mouse over)
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Ocean circulation is driven by energy from the sun and the rotation of the Earth.
causes circulation of the atmosphere = winds
and variations in temperature and salinity of seawater -> temperature and salinity controls the water's density.
Due to the rotation of the earth, currents are deflected to the right in the northern hemisphere and to the left in the southern hemisphere. This effect is known as the "Coriolis force."
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How do essential nutrients like iron and other minerals get into vast watery stretches of the open ocean? According to one theory, large swirling currents, called eddies, pump nutrients from the depths up toward the sunlit surface, giving phytoplankton (microscopic marine plants) the ingredients they need to flourish. But a larger source of iron may be dust storms, which blow huge quantities of mineral-rich soil particles (called Aeolian dust) out to sea, particularly from desert regions in Africa and Asia. A team calling themselves the “Dust Busters” have designed
a device, mounted on a buoy that collects wind-blown particles in the
open ocean, to investigate the theory. Their first findings will be published
in the journal Deep-Sea Research. News from Oceanus |
The image shows Saharan dust swept off the west coast of Africa, then turned northwards on March 8, 2006. http://earthobservatory.nasa.gov/Newsroom/NewImages/images.php3?img_id=17207 NASA image courtesy Jeff Schmaltz, MODIS Land Rapid Response Team at NASA GSFC |

The
pelagic zone (also known as the open-ocean zone) is further divided into parts,
creating a number of sub-zones, based on their different ecological characteristics
(which is roughly a function of depth):
* Epipelagic (from the surface down to around 200 m) - the illuminated surface
zone where there is enough light for photosynthesis. Due to this, plants and
animals are largely concentrated in this zone. Here one will typically encounter
fish such as tuna and many sharks.
* Mesopelagic (from 200 m down to around 1000 m) - the twilight zone. Although
some light penetrates this deep, it is insufficient for photosynthesis. The
name stems from Greek ?????, middle.
* Bathypelagic (from 1000 m down to around 4000 m) - by this depth the ocean
is almost entirely dark (with only the occasional bioluminescent organism).
There are no living plants, and most animals survive by consuming the snow
of detritus falling from the zones above, or (like the marine hatchetfish)
by preying upon others. Giant squid live at this depth, and here they are
hunted by deep-diving sperm whales. From Greek ????? (bathys), deep.
* Abyssopelagic (from 4000 m down to above the ocean floor) - no light whatsoever
penetrates to this depth, and most creatures are blind and colourless. The
name is derived from the Greek ??????? (ábyssos), abyss, meaning bottomless
(a holdover from the times when the deep ocean was believed to be bottomless).
* Hadopelagic (the deep water in ocean trenches) - the name is derived from
Hades, the classical Greek underworld. This zone is 90% unknown and very few
species are known to live here (in the open areas). However, many organisms
live in hydrothermal vents in this and other zones.
Wednesday, 15 February 2006, 17:11:48
It was generally thought that organic particles sink vertically to the ocean
floor relatively rapidly. New studies show that particles are transported to
the deep ocean over thousands of years before being deposited on the seabed.
This may change our views of how the carbon cycle works (with relevance for
global climate) and how oil deposits form.
EurekAlert of 15 February 2006 at http://www.eurekalert.org/pub_releases/2006-02/uonu-toa021506.php
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