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Diatomite rock sample from Sisquoc Formation Scanning electron micrograph of diatomaceous earth. Diatomaceous earth (/ ËŒ d aɪ. É™ t É™ ˈ m eɪ ʃ É™ s / DY-É™-tÉ™-MAY-shÉ™s), also known as diatomite (/ d aɪ ˈ æ t É™ m aɪ t / dy-AT-É™-myte), celite, or kieselguhr, is a naturally occurring, soft, siliceous sedimentary rock that can be crumbled into a fine white to off-white powder.
The frustule is composed almost purely of silica, made from silicic acid, and is coated with a layer of organic substance, which was referred to in the early literature on diatoms as pectin, a fiber most commonly found in cell walls of plants. [1] [2] This layer is actually composed of several types of polysaccharides. [3]
This image of diatomaceous earth particles in water is at a scale of 6.236 pixels/μm, the entire image covers a region of approximately 1.13 by 0.69 mm Main article: Microfossil Microfossils are fossils that are generally between 0.001mm and 1 mm in size, [ 1 ] the study of which requires the use of light or electron microscopy .
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Diatomaceous earth (diatomite) is a collection of diatom shells found in the Earth's crust. They are soft, silica-containing sedimentary rocks which are easily crumbled into a fine powder and typically have a particle size of 10 to 200 μm.
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