Abstract
Two microbial processes are involved in the sulfur cycle of the earth’s biosphere: anoxic dissimilatory sulfur oxidation by phototrophic bacteria and dissimilatory sulfate reduction by sulfate-reducing bacteria. In the presence of oxygen at chemoclines and redoxclines dissimilatory sulfur oxidation by chemolithotrophic bacteria (Thiobacillus, Beggiatoa, and others) occurs. In addition, dissimilatory sulfur reducing bacteria participate in the sulfur cycle. The processes of sulfur assimilation and of microbial liberation of sulfur compounds by decomposition of organic materials are of secondary geomicrobiological importance. Although functioning in opposite directions, the enzymatic equipment of the bacteria involved in dissimilatory sulfur transformations shows a surprising degree of uniformity. Possible phylogenetic relationships between the bacteria involved are discussed on the basis of recent findings in the field of chemotaxomony.
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© 1982 Dr. S. Bernhard, Dahlem Konferenzen, Berlin
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Trüper, H.G. (1982). Microbial Processes in the Sulfur Cycle Through Time. In: Holland, H.D., Schidlowski, M. (eds) Mineral Deposits and the Evolution of the Biosphere. Dahlem Workshop Report, vol 3. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-68463-0_2
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