The slow decomposition of organic molecules by enzymes is known as
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Arthropods are key factors influencing comminution and mineralization. Decomposition most commonly is measured as respiration rate, as the ratio of litter input to litter standing crop, or as the rate of litter disappearance. Isotopic tracers also provide data on decomposition rate. Decomposition rate typically is higher in mesic than in arid ecosystems.
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