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About Rot
Decomposition or rot is the process by which dead organic substances are damage down into simpler organic or inorganic matter such as carbon dioxide, water, simple sugars and mineral salts. The process is a part of the nutrient cycle and is valuable for recycling the finite issue that occupies physical song in the biosphere. Bodies of bustling organisms start to decompose suddenly after death. Animals, such as earthworms, also back decompose the organic materials. Organisms that attain this are known as decomposers or detritivores. Although no two organisms decompose in the thesame way, they whatever undergo the similar sequential stages of decomposition. The science which studies decomposition is generally referred to as taphonomy from the Greek word taphos, meaning tomb. Decomposition can furthermore be a gradual process for organisms that have lengthy periods of dormancy.
One can differentiate abiotic decomposition from biotic decomposition (biodegradation). The former means “the degradation of a substance by chemical or bodily processes”, e.g., hydrolysis; the latter means “the metabolic assay of materials into simpler components by full of life organisms”, typically by microorganisms.
