Plankton is the name for the trillions of tiny organisms that float in the world's oceans at the pelagic zone, within 656 ft (200 m) from the surface, where there is sufficient light for photosynthesis. Like every other ecosystem in the world, the basis of life in this zone are the photosynthetic bacteria (cyanobacteria), algae, and other autotrophs that soak up the sun's rays and reproduce by using trace amounts of carbon, nitrogen, phosphorous, and silicon from sea water as nutrients to divide and grow. These microorganisms exist in a boom-and-bust pattern, usually twice a year, when nutrients are plentiful and the organisms quickly reproduce.
There are five common levels of classification for these organisms, based on their size: nanoplankton (
Organisms included in this group, in approximate descending order of frequency, include the following:
- flagellate protists
- copepods (1 mm crustaceans)
- arrow worms
- ostracods (tiny seed-shaped crustaceans)
- tunicates (blob-like filter feeders that are actually primitive chordates)
- pteropods (planktonic gastropods)
- water fleas (crustaceans)
- pyrosomes (bioluminescent tunicates)
- and other small creatures.
At the highest level, rare large animals such as whales occasionally pass through this ecosystem and eat whatever organisms they can find. The combined annual prey of all whales in the world exceeds 100 million tons, which is greater than the total annual human consumption of seafood.
To humans, plankton is only indirectly meaningful because it serves as the primary food source of everything else in the ocean. Occasionally, some members of the collective, especially bacteria, are so visibly bioluminescent that "milky seas" — glowing water — are created. Areas as large as 6,000 square miles (15,540 square km) have been observed displaying the milky seas effect, and scientists are very interested in learning more about the conditions that give rise to this rare phenomenon.