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Index >> Microbial Ecology of Different Ecosystems>> Structure of the Sea

Structure of the Sea

Structure of the Sea
The littoral (eulittoral) zone occurs at the seashore. This zone is subjected to alternate periods of flooding and drying at high and low tides respectively. The sublittoral zone extends from the low tide mark to the edge of the continental shelf. This region is also called as the neritic, or near shore zone. The term pelagic is used to designate open water or the high sea and includes portions of the neritic and the entirety of the oceanic province. The benthos or benthic region is the bottom, regardless of the overlying zone

The benthic region begins at the intertidal zone (littoral zone) and extends downwards. The continental shelf is a gently sloping benthic region that extends away from the land mass. At the continental shelf edge, the slope greatly increases. The continental slope, also known as the bathy region, drops down to the sea floor. The deep-sea floor is known as the abyssal plain and usually lies at about 4000m. The ocean floor is not flat but has deep ocean trenches and submarine ridges. The deep ocean trenches are called as the hadal region.

Structure of the sea

 

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