The bathyal zone or bathypelagic – from Greek βαθύς (bathýs), deep – (also known as midnight zone) is the part of the pelagic zone that extends from a depth of 1000 to 4000 meters (3300 to 13000 feet) below the ocean surface. It lies between the mesopelagic above, and the abyssopelagic below. The average temperature hovers at about 4 °C (39 °F). Although larger by volume than the euphotic zone, the bathyal zone is less densely populated. Sunlight does not reach this zone, meaning primary production, if any, is almost nonexistent. There are no known plants because of the lack of sunlight necessary for photosynthesis. It is known as the midnight zone because of this feature. Because of the lack of light, some species do not have eyes, however those possessing eyes in this zone include the viperfish and the frill shark. Many forms of nekton live in the bathyal zone, such as squid, large whales, and octopuses. In the bathyal, some of the world's largest whales feed. Sponges, brachiopods, sea stars, and echinoids are also common in the bathyal zone. Animals in the bathyal zone are not threatened by predators that can see them, so they do not have powerful muscles. This zone is difficult for fish to live in, since it is especially hard to find nutrients. They have become very energy efficient, and many have slow metabolic rates to conserve energy. The fish are characterized by weak muscles, soft skin and slimy bodies. The adaptations of some of the fish that live there include small eyes and transparent skin.
Except where the ocean is exceptionally deep, the bathyal zone extends to the benthic zone on the ocean bed of that part of the continental slope that lies between 1000 and 4000 meters deep. The bathyal zone contains sharks, squid, octopus, and different species of fish.
- Enig, C. C. (1997). Bathyal zones on the Mediterranean continental slope: An attempt. Research on marine benthos: 9th Iberian Symposium on Studies of Marine Benthos. Madrid: MAPA, SGT. pp. 23–33. ISBN 8449102995.
- Bathyal zone (oceanography) Encyclopædia Britannica Online. 21 March 2009.
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