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Living diatoms make up a significant portion of the Earth's biomass : they generate about click to 50 percent of the oxygen produced on the planet each year, [8] [9] take in over 6. Diatoms are unicellular : they occur either as solitary cells or in colonieswhich can take the shape of ribbons, fans, zigzags, or stars. Individual cells range in size from 2 to micrometers. A unique feature of diatom anatomy is that Cfll are surrounded by a cell wall made of silica hydrated silicon dioxidecalled a frustule.
Movement in diatoms primarily occurs passively as a result of both water currents and wind-induced water turbulence ; however, male gametes of centric diatoms have flagellapermitting active movement for seeking female gametes. Similar to plantsdiatoms convert light energy to chemical energy by photosynthesisalthough this shared autotrophy evolved independently in both lineages. Unusually for autotrophic organisms, diatoms possess a urea cyclea feature that they share with animalsalthough this cycle is used to different metabolic ends in diatoms.
The family Rhopalodiaceae also possess a cyanobacterial endosymbiont called a spheroid body. This endosymbiont has lost its photosynthetic properties, but has kept its ability to perform nitrogen fixationallowing the diatom to fix atmospheric nitrogen.
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The study of diatoms is a branch of phycology. Diatoms are classified as eukaryotesorganisms with a membrane-bound cell nucleusPlnt separates them from the prokaryotes archaea and bacteria. Diatoms are a type of plankton called phytoplanktonthe most common of the plankton types.
Diatoms also grow attached to benthic substrates, floating debris, and on macrophytes. They comprise an integral component of the periphyton community. Several systems for classifying the individual diatom species exist.
Fossil evidence suggests that diatoms originated during or before the early Jurassic periodwhich was about to million years ago. The oldest fossil evidence for diatoms is a specimen of extant genus Hemiaulus in Late Jurassic aged amber from Thailand. Diatoms are used to monitor past and present environmental conditions, and are commonly used in studies of water quality. Diatomaceous earth diatomite is a collection of diatom shells found in the earth's crust.
Diatomaceous earth is used for a variety of purposes including for water filtration, as a mild abrasive, in cat litter, and as a dynamite stabilizer. Diatoms are generally 2 to micrometers in size, [13] with a few larger species. Their yellowish-brown chloroplaststhe site of photosynthesis, are typical of heterokontshaving four Lab Report On Plant Cell Walls and containing pigments such as the carotenoid fucoxanthin. Individuals usually lack flagellabut they are present in male gametes of the centric diatoms and have the usual heterokont structure, including the hairs mastigonemes characteristic in other groups.
Diatoms are often referred as "jewels of the sea" or "living opals" due to their optical properties. Diatoms build intricate hard but porous cell walls called frustules composed primarily of silica. The cell itself consists of two halves, each containing an essentially flat plate, or valve and marginal connecting, or girdle band. One half, the hypothecais slightly smaller than the other half, the epitheca. Diatom morphology varies.]
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