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Aerobic ecosystem

In aerobic ecosystems, iron is mostly present as the insoluble Fe(III). Cells must synthesize, excrete and re-import iron-specific chelators, siderophores, for a sufficient supply with iron under these conditions (Braun et al. 1998). In contrast, under anaerobic conditions iron is mainly present as Fe(II). Similar to Mn(II), Fe(II) can be imported into the cell by a variety of uptake systems. [Pg.266]

Gopper, when present in aerobic ecosystems as Gu(II), is reduced by most microbial cells to Gu(I), which is the predominant form in the cytoplasm. This easy one-electron redox reaction makes copper very useful as cofactor for the reaction with radicalic compounds such as molecular oxygen. The last enzyme complex of the respiratory chain in mitochondria and in many fully aerobic bacteria is that of cytochrome c oxidase. This contains two copper centers one for uptake of electrons from cytochrome c (Cu A center) the other (Cu B center) for the reduction of molecular oxygen to water using these electrons. This reaction generates a proton-motive force that may be used for the synthesis of ATP (Iwata et al. 1995, Michel et al. 1998, Ostermeier and Michel 1997). [Pg.268]

There is not so much competition between organisms following these developments as there is specialisation since new secondary energy and chemical sources are best employed in different compartments, here largely different isolated cells, chemotypes. (Use was made of debris by cells from other organisms.) Separation of anaerobes, plant- and animallike aerobes, including different chemotypes, where their coexistence and cooperativity is more notable than competition, was an essential evolutionary step towards a cyclic state of the whole ecosystem. [Pg.271]

If cells of eukaryotes are much slower to reproduce and adapt, why did they evolve at all and so successfully Why did they continue to evolve yet their predecessor prokaryotes also evolved (as aerobes) and both they and early and late eukaryotes are also extant in considerable numbers today Clearly a large number of types of organisms, chemotypes, co-exist. Why We shall provide answers to these questions in terms of the different efficiencies of different chemotypes within the ecosystem, including mutual chemical dependences. [Pg.286]

Kurek E (2002) Microbial mobilization of metals from soil minerals under aerobic conditions. In Huang PM, Bollag J-M, Senesi N (eds) Interactions between soil particles and microorganisms. Impact on the terrestrial ecosystem, vol 8, IUPAC series on analytical and physical chemistry of environmental systems. Wiley, Chichester, UK, pp 189-225... [Pg.33]

Biodegradation aerobic t,/2 = 14616-33600 h, based on mineralization half-life in fresh water and estuarine ecosystems (Heitkamp 1988 quoted, Howard et al. 1991) ... [Pg.822]

Aerobic and anaerobic metabolism in an aqnatic bacterial ecosystem... [Pg.7]

Figure 1.3 Aerobic and anaerobic metaboiism in an aquatic bacterial ecosystem. Figure 1.3 Aerobic and anaerobic metaboiism in an aquatic bacterial ecosystem.
The human GI tract consists of a highly complex ecosystem of aerobic and anaerobic microorganisms [77]. Although the gastric microflora is predominantly aerobic and its bacterial concentration is around 103 colony-forming units (CFU)/mL, the large bowel environment is anaerobic in nature with a typical bacterial concentration of 1011 CFU/mL... [Pg.12]

Data on exposure and environmental fate are needed, not to determine toxicity, but to provide information that may be useful in the prediction of possible exposure in the event that the chemical is toxic. These tests are primarily useful for chemicals released into the environment such as pesticides, and they include the rate of breakdown under aerobic and anaerobic conditions in soils of various types, the rates of leaching into surface water from soils of various types, and the rate of movement toward groundwater. The effects of physical factors on degradation through photolysis and hydrolysis studies and the identification of the product formed can indicate the rate of loss of the hazardous chemical or the possible formation of hazardous degradation products. Tests for accumulation in plants and animals and movement within the ecosystem are considered in Section 21.7. [Pg.358]


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See also in sourсe #XX -- [ Pg.266 ]




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