Decomposition
Decomposition is a biological process that involves the breakdown of organic materials into simpler organic and inorganic matter. This process is carried out by decomposers, which include bacteria, fungi, and other organisms. Decomposition is a vital process in the ecosystem as it helps in the recycling of nutrients.
Overview[edit | edit source]
Decomposition is a complex process that involves several stages. The first stage is the initial decay, where the organic materials are broken down by bacteria and fungi. This is followed by the decomposition of the more resistant materials, such as cellulose and lignin. The final stage is the humification, where the decomposed materials are converted into humus, a stable organic matter that is beneficial to the soil.
Decomposition is influenced by several factors, including temperature, moisture, and the presence of oxygen. The rate of decomposition is faster in warm, moist, and oxygen-rich environments.
Role in the Ecosystem[edit | edit source]
Decomposition plays a crucial role in the ecosystem. It helps in the recycling of nutrients, which are essential for the growth and development of plants. By breaking down dead organic materials, decomposers help in the formation of humus, which improves the fertility and structure of the soil.
Decomposition also plays a role in the carbon cycle. By decomposing organic materials, decomposers release carbon dioxide into the atmosphere, contributing to the greenhouse effect.
Decomposers[edit | edit source]
Decomposers are organisms that break down dead organic materials. They include bacteria, fungi, and other organisms. Decomposers are essential for the process of decomposition as they help in the breakdown of complex organic materials into simpler substances.
See Also[edit | edit source]
References[edit | edit source]
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Contributors: Prab R. Tumpati, MD