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Sulfur cycle, circulation of sulfur in various forms through nature. Sulfur occurs in all living matter as a component of certain amino acids. It is abundant in the soil in proteins and, through a series of microbial transformations, ends up as sulfates usable by plants.
The sulfur cycle is a biogeochemical cycle consisting of various processes that together enable the movement of sulfur through different reservoirs like the atmosphere, biosphere, and lithosphere. Sulfur is an important mineral in living organisms that is found in biomolecules like proteins.
Description of the sulfur cycle and how does it work, also learn the steps along with its importance and human impacts explained using examples and simple diagram.
The important sulfur cycle is a biogeochemical cycle in which the sulfur moves between rocks, waterways and living systems.
The Sulfur Cycle. Sulfur is an essential element for the macromolecules of living things. As a part of the amino acid cysteine, it is involved in the formation of disulfide bonds within proteins, which help to determine their 3-D folding patterns and, hence, their functions.
Sulfur enters the ocean via runoff from land, from atmospheric fallout, and from underwater geothermal vents. Some ecosystems rely on chemoautotrophs using sulfur as a biological energy source. This sulfur then supports marine ecosystems in the form of sulfates.
The sulfur cycle describes the movement of sulfur through the geosphere and biosphere. Sulfur is released from rocks through weathering, and then assimilated by microbes and plants. It is then passed up the food chain and assimilated by plants and animals, and released when they decompose.