By Geoffrey Michael Gadd
ISBN-10: 0521845793
ISBN-13: 9780521845793
Fungi play vital roles within the biking of parts within the biosphere yet are usually overlooked inside microbiological and geochemical examine spheres. Symbiotic mycorrhizal fungi are liable for significant changes and redistribution of inorganic food, whereas free-living fungi have significant roles within the decomposition of natural fabrics, together with xenobiotics. Fungi also are significant biodeterioration brokers of stone, wooden, plaster, cement and different development fabrics, and are vital elements of rock-inhabiting microbial groups. the purpose of this publication is to advertise extra figuring out of the most important roles that free-living and symbiotic fungi (in mycorrhizas and lichens) play within the biogeochemical biking of components, the chemical and organic mechanisms which are concerned, and their environmental and biotechnological value. the place applicable, relationships with micro organism also are mentioned to spotlight the dynamic interactions which can exist among those significant microbial teams and their built-in functionality in different forms of habitat.
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Oremland, R. , Newman, D. , Kail, B. W. & Stolz, J. F. (2002b). Bacterial respiration of arsenate and its significance in the environment. In Environmental Chemistry of Arsenic, ed. W. T. Frankenberger. New York: Marcel Dekker, pp. 273–95. Oremland, R. , Stolz, J. F. & Hollibaugh, J. T. (2004). The microbial arsenic cycle in Mono Lake, California. FEMS Microbiology Ecology, 48, 15–27. Orphan, V. , Ussler, W. III et al. (2001). Comparative analysis of methane oxidizing Archaea and sulfate-reducing bacteria in anoxic marine sediments.
Et al. (2002a). Anaerobic oxidation of arsenite in Mono Lake water by a facultative arsenite oxidizing chemoautotroph, strain MLHE-1. Applied and Environmental Microbiology, 68, 4795–802. Oremland, R. , Newman, D. , Kail, B. W. & Stolz, J. F. (2002b). Bacterial respiration of arsenate and its significance in the environment. In Environmental Chemistry of Arsenic, ed. W. T. Frankenberger. New York: Marcel Dekker, pp. 273–95. Oremland, R. , Stolz, J. F. & Hollibaugh, J. T. (2004). The microbial arsenic cycle in Mono Lake, California.
7) Digenite, Cu9S5, containing Cu(I) and Cu(II), appears to be an intermediate in this process (Fox, 1967; Nielsen & Beck, 1972). 8) summarizes the subsequent steps in the oxidation: CuS þ 2O2 ! 8) In indirect attack, planktonic At. ferrooxidans forms ferric iron in the bulk phase by oxidizing dissolved ferrous iron. The resultant ferric iron 18 H. L. Ehrlich then acts as a chemical oxidant that attacks the chalcocite, forming Cu2þ, So and Fe2þ as end-products. A form of cupric sulphide, CuS, appears also to be an intermediate in this chemical oxidation (Sullivan, 1930).
Fungi in Biogeochemical Cycles (British Mycological Society Symposia) by Geoffrey Michael Gadd
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