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Epipelagic Zone

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The oceanic zone is made up of three main zones. The epipelagic zone, the mesopelagic zone, and the bathypelagic zone. The epipelagic zone is the surface layer of the ocean, and this where most of the ocean life lives. The mesopelagic zone is the layer of the ocean below the epipelagic zone. Not a lot of sunlight penetrates this area of the ocean. The zone under the mesopelagic zone is the bathypelagic zone. No sunlight reaches this zone. Together all of these zones make up the oceanic zone. The surface layer of the ocean is the epipelagic zone. This zone is from the surface of the ocean to about 200 meters down. Since this zone is close to the surface the currents move at a fast speed. These currents carry nutrients throughout the zone. This zone has most of the life in the ocean because the sunlight penetrates the water here. The animals that live here range from whales to small phytoplankton. These phytoplankton use the nutrients in the water and the sunlight to produce their own food. This is how the phytoplankton survived, the phytoplankton themselves were used as food for other animals. Some of these animals that eat the plankton are small fish but not only fish eat them whales also eat them. The temperature of the water ranges from …show more content…

This zone is also called the midnight or dark zone because no light will ever reach this far down. The only light is from bioluminescent animals that make their own light. The temperature down there usually stays between 35-39 degrees fahrenheit. This zone ranged from 1,000 to 4,000 meters down in the ocean. The pressure is about 5,800 psi. The food source here is limited to the debris of dead material that sinks from the above zones. A lot of animals stay still to conserve energy. Unlike other zones where animals travel between zones, the animals in the bathypelagic zone usually stay in this zone. The water here moves extremely slow and there is some downward current due to

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