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.
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.
The shallow offshore sea goes through its own seasons. In spring, plankton blooms in the warming waters, the basis of a classic food chain which feeds a succession of marine life. Shoals of herring attract larger predators, including the grey seals that thrive in the rich waters of the Atlantic coast.
Ice trap
Water from the depths turns to ice and traps everything that cannot escape.
Water from the depths turns to ice and traps everything that cannot escape.
Finger of death
Winter reaches down into the depths as an icy brinicle is formed.
Winter reaches down into the depths as an icy brinicle is formed.
Plankton world
A floating community of animals and plants comes in all shapes and sizes.
A floating community of animals and plants comes in all shapes and sizes.
Antarctic fur seal
Brown fur seal
Common seal
Crabeater seal
Galápagos fur seal
Grey seal
Leopard seal
Mediterranean monk seal
Otter
Polar bear
Ringed seal
Sea otter
Southern Elephant Seal
Southern sea lion
Steller sea lion
Walrus
Weddell seal
Amazonian manatee
Dugong
Atlantic spotted dolphin
Beluga whale
Blue whale
Bowhead whale
Common bottlenose dolphin
Grey whale
Harbour porpoise
Humpback whale
Indo-Pacific bottlenose dolphin
Killer whale
Narwhal
Northern bottlenose whale
Pantropical spotted dolphin
Peale's dolphin
Southern right whale
Spotted dolphins
White whales
Adelie penguin
African penguin
Chinstrap penguin
Emperor penguin
Humboldt penguin
King penguin
Macaroni penguin
Magellanic penguin
Snares crested penguin
Spectacled eider
Pied kingfisher
Cape gannet
Northern gannet
Socotra cormorant
Arctic skua
Arctic tern
Auks
Great black-backed gull
Guillemot
Guillemots
Herring gull
Kittiwake
Lesser black-backed gull
Plovers and lapwings
Puffin
Skimmers
South polar skua
Thick-billed guillemot
Herons, egrets and bitterns
Fulmar
Galápagos petrel
Manx shearwater
Shearwaters
Short-tailed shearwater
Snow petrel
Storm petrel
Wandering albatross
Waved albatross
Plesiosaurs
Pliosaurs
Banded sea krait
Black-banded sea krait
Marine iguana
Green sea turtle
Olive ridley turtle
Sea turtles
Whale shark
Manta ray
Rays, skates and sawfish
Stingrays
Cartilaginous fish
Sharks
Ground sharks
Hammerhead sharks
Lemon shark
Requiem sharks
Tiger shark
Basking shark
Great white shark
Mackerel sharks
Three-spined stickleback
Atlantic salmon
Atlantic salmon and trout
Salmon family
Leafy sea dragon
Seahorses and pipefish
Weedy sea dragon
Anglerfish
Catfish
Eeltail catfish
Herring and sardine family
Herrings and anchovies
Peruvian anchoveta
Flying fish
Needlefish and flying fish
Gobies
Perch-like fishes
Ray-finned fishes
The neritic zone, also called coastal waters, the coastal ocean or 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 (110 fathoms or 667 feet). 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 slope begins, descending from the continental shelf to the abyssal plain and the pelagic zone.
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