Sulfur is found in all living organisms as a constituent of some proteins, vitamins, and hormones. Like carbon and nitrogen, sulfur cycles between the atmosphere, lithosphere, and hydrosphere; but, unlike these two other elements, it has major reservoirs in both the atmosphere and the lithosphere. As is true in the nitrogen cycle, the activities of microorganisms are crucial in the global cycling of this nutrient.
The process begins with geochemical and meteorologic processes such as the weathering of rock. When sulfur is released from the rock and comes in contact with air, it is converted into sulfate (SO4), which is taken up by plants and microorganisms and converted into organic forms. Animals acquire these organic forms of sulfur from their foods. When organisms die and decompose, some of the sulfur enters the tissues of microorganisms and some is released again as sulfate. There is, however, a continual loss of sulfur from terrestrial ecosystems as some of it drains into lakes and streams and eventually into the ocean as runoff. Additional sulfur enters the ocean through fallout from the atmosphere.
Once in the ocean, some of the sulfur cycles through marine communities as it moves through food chains, some reenters the atmosphere, and some is lost to the ocean depths as it combines with iron to form ferrous sulfide (FeS), which is responsible for the black colour of marine sediments. Sulfur reenters the atmosphere naturally in three major ways: sea spray releases large amounts of the element from the ocean into the atmosphere; anaerobic respiration by sulfate-reducing bacteria causes the release of hydrogen sulfide (H2S) gas especially from marshes, tidal flats, and similar environments in which anaerobic microorganisms thrive; and volcanic activity releases additional but much smaller amounts of sulfur gas into the atmosphere.
Since the Industrial Revolution, human activities have contributed significantly to the movement of sulfur from the lithosphere to the atmosphere as the burning of fossil fuels and the processing of metals have occasioned large emissions of sulfur dioxide. Oxides of sulfur and nitrogen contribute to the acid rain that is common downwind from these industrial activities (see acid rain).
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Estimated-number-of-known-living-speciesFigure 1: Estimated number of known living species. The majority of species are still …[Credits : Encyclopædia Britannica, Inc.]
Transfer-of-energy-through-an-ecosystemFigure 2: Transfer of energy through an ecosystem. At each trophic level only a small proportion of …[Credits : Encyclopædia Britannica, Inc.]
General-paths-of-energy-flow-and-nutrient-cycling-in-theFigure 3: General paths of energy flow and nutrient cycling in the biosphere.[Credits : Encyclopædia Britannica, Inc.]
Atmospheric-carbon-dioxide-concentration-remained-fairly-constant-over-the-pastFigure 4: Atmospheric carbon dioxide concentration remained fairly constant over the past thousand …[Credits : From W.M. Post, F. Chavez, P.J. Mulholland, J. Pastor, T.H. Peng, K. Prentice, and T. Webb III, “Climatic Feedbacks in the Global Carbon Cycle,” in David A. Dunnette and Robert J. O’Brien (eds.), The Science of Global Change: The Impact of Human Activities on the Environment, American Chemical Society Symposium Series 483, 1992]
The-nitrogen-cycleThe nitrogen cycle.[Credits : Encyclopædia Britannica, Inc.]
The-roots-of-an-Austrian-winter-pea-plant-with-nodulesFigure 6: (Right) The roots of an Austrian winter pea plant (Pisum sativum) with nodules …[Credits : (Left) Encyclopædia Britannica, Inc.; (right) photograph, © John Kaprielian, The National Audubon Society Collection/Photo Researchers]
Energy-exchange-between-a-terrestrial-reptile-and-the-environmentFigure 7: Energy exchange between a terrestrial reptile and the environment.[Credits : Encyclopædia Britannica, Inc.]
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