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Plankton Planet

The world would be a barren place without these ubiquitous plants at the bottom of the food chain

By definition, plankton are waterborne animals or plants that cannot swim against an ambient current. For the most part they float, although some can maneuver as long as they “go with the flow.” Phytoplankton are single-celled plants. The largest can be divided into three groups: coccolithophorids, diatoms, and dinoflagellates. The exterior of the coccolithophorid at right, a Syracolithus quadriperforatus, is made of calcium carbonate, the stuff of chalk. By contrast, the shell of the diatom Cyclotella pseudostelligera is silica, the material that makes up sand, glass, and quartz. Coccolithophorids and dinoflagellates are largely marine plants, meaning they live in salt water. Diatoms exist in both fresh and brackish environments. The oldest diatom fossils are about 140 million years old, leading some scientists to speculate that they evolved along with the ascent of terrestrial grasses, which released silica into the sea after separating it from minerals.SEM scan

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When 19th-century British biologist Thomas Henry Huxley first put seafloor mud under a microscope, he found tiny round and oval particles in abundance. Not knowing what they were, he dubbed them coccoliths, based on the Greek words for “seed” and “stone.” Only later would scientists learn that coccoliths are calcite plates that surround some species of phytoplankton like armor. Today, more than 100 years after Huxley, teams of researchers are still unraveling the role phytoplankton play in creating the air we breathe, the food we eat, the fuel we burn, even the ground we walk on.

Phytoplankton can be found floating in just about every ocean, lake, and river in the world. But scientists are looking mostly at saltwater species, which, taken together, may have influenced life on Earth more than any other group of organisms. Plankton are literally at the bottom of the food chain, a source of nourishment ...

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