Shallow seas cover the continental shelves. These sunlit, or neritic, waters are where the oceans are most productive, where biomass is highest and where all the major sea fisheries of the world take their catches. The shallow seas include warm tropical waters, temperate seas like those round the UK and the chilly waters of the Arctic and Southern Oceans.
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Home of the giant octopus
Nutrient-rich waters along the Pacific coast support life large and small.
Ocean food chain
The rich warm, shallow waters off the Scilly Isles attract a wealth of marine life.
Life in a marina
Travel beneath the surface of a marina to see what flourishes under the gleaming yachts.
Pied kingfisher
Cape gannet
Kittiwake
South polar skua
Adelie penguin
Chinstrap penguin
Emperor penguin
Humboldt penguin
King penguin
Magellanic penguin
Snares crested penguin
Wandering albatross
Waved albatross
Antarctic fur seal
Brown fur seal
Crabeater seal
Galápagos fur seal
Grey seal
Leopard seal
Otter
Polar bear
Sea otter
Southern Elephant Seal
Southern sea lion
Weddell seal
Amazonian manatee
Dugong
Blue whale
Common bottlenose dolphin
Grey whale
Humpback whale
Killer whale
Pantropical spotted dolphin
Peale's dolphin
The neritic zone, also called the sublittoral zone, is the part of the ocean extending from the low tide mark to the edge of the continental shelf, with a relatively shallow depth extending to about 200 meters (100 fathoms). The neritic zone has generally well-oxygenated water, low water pressure, and relatively stable temperature and salinity levels. These, combined with presence of light and the resulting photosynthetic life, such as phytoplankton and floating sargassum, make the neritic zone the location of the majority of sea life.
Zooplankton, free-floating creatures ranging from microscopic foraminiferans to small fish and shrimp, live in this zone, and together with the phytoplankton form the base of the food pyramid that supports most of the world's great fishing areas.
At the edge of the neritic zone the continental shelves end, rapidly descending to the deeper oceanic crust and the pelagic zone.
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