Marine Zonage:
- continental shelf: the edge of a continent that is under water extending out to the shelf breakBy Chris_huh - Own work, Public Domain. |
- continental rise: the region at the base of the continental slope where the slope decreases to 1 degree extending to the abyssal plain.
- abyssal plain: a flat seafloor at depths of 3,000 to 6,000 feet.
Benthic and Pelagic regions: bottom
- benthic organisms: live on/ burrowed in the bottom
- some are sessile: attached and immobile (corals)
- or mobile: crawl around/ move
- pelagic organisms: live up in the water column (fish)
- subdivided according to size and swimming ability
- plankton: drifters
- phytoplankton: algae, tiny plants
- zooplankton: tiny animals and protozoans
- nekton: swim well enough against currents, fish, squid
- benthic zonation:
- intertidal zone: shallowest, tides
- subtidal: always submerged (coral reefs)
- deep ocean floor: bathyal, abyssal, halal zones
- pelagic zonation:
- neritic zone: the pelagic environment that lies above the continental shelf
- oceanic zone: pelagic waters after the shelf break
- photic zone: where light can penetrate
- aphasic zone: no light goes through, no photosynthesis
Oceanic zonation by By Photoguy2801 - Own work. |
Physical properties of water
Ocean water. By William Waterway. |
- humidity:
- prevents drying out or desiccation
- exposed respiratory surfaces (gills)
- external fertilization and development
- direct excretion of wastes
- high density:
- organisms and particles can be suspended or float
- rigid skeleton not necessary
- filter feeding is possible
- locomotion (swimming and drifting)
- high heat capacity:
- temperature of water remains stable
- high nutrient and mineral content:
- salts and nutrients readily available for absorption
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