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Pelagic zone

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Diagram of the layers of the pelagic zone.
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Diagram of the layers of the pelagic zone.

The pelagic zone is the part of the open sea or ocean comprising the water column, i.e. all of the sea other than that near the coast or the sea floor. In contrast, the demersal zone comprises the water that is near to (and thus is significantly affected by) the coast or the sea floor. The name is derived from the Greek πέλαγος (pélagos), which is roughly translated as "sea" but is more accurately translated as "open sea."

The pelagic zone (also known as the open-ocean zone) is further divided into a number of sub-zones, based on their different ecological characteristics (which is roughly a function of depth):

The epipelagic and (arguably) the mesopelagic zones together comprise the open ocean's photic zone. The remaining (lower) zones comprise the open ocean's aphotic zone.

The bathypelagic, abyssopelagic, and hadopelagic zones are very similar in character, and some marine biologists elide them into a single zone or consider the latter two to be the same. Some define the hadopelagic as waters below 6000 meters, whether in a trench or not.

In science fiction, a pelagic planet is a world covered mostly, or entirely, by oceans.

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