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Books on the topic 'Iron bacteria'

Author: Grafiati
Published: 4 June 2021
Last updated: 27 July 2024

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1

Crosa, Jorge H., Alexandra R. Mey, and Shelley M. Payne, eds. Iron Transport in Bacteria. Washington, DC, USA: ASM Press, 2004. http://dx.doi.org/10.1128/9781555816544.

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2

MacLean, Martin. Autotrophy in iron-oxidizing, acidophilic bacteria. [s.l.]: typescript, 1993.

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3

Hampshire), Conference on Iron Biominerals (1989 University of New. Iron biominerals. New York: Plenum Press, 1991.

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4

Lazurenko, V. I. Geologicheskai͡a︡ dei͡a︡telʹnostʹ zhelezobakteriĭ. Kiev: Nauk. dumka, 1989.

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5

Barr, David William. Comparison of iron oxidation by acidophilic bacteria. [s.l.]: typescript, 1989.

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6

Marsh, Rowena Margaret. Thermophilic acidophilic bacteria: Iron, sulphur and mineral oxidation. [s.l.]: typescript, 1985.

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7

Geological Survey (U.S.), ed. Sites in the Virginia-Washington, D.C.-Maryland metro area to observe or collect bacteria that precipitate iron and manganese oxides. [Reston, Va.?: U.S. Dept. of the Interior, U.S. Geological Survey, 1998.

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8

Geological Survey (U.S.), ed. Sites in the Virginia-Washington, D.C.-Maryland metro area to observe or collect bacteria that precipitate iron and manganese oxides. [Reston, Va.?: U.S. Dept. of the Interior, U.S. Geological Survey, 1998.

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9

Geological Survey (U.S.), ed. Sites in the Virginia-Washington, D.C.-Maryland metro area to observe or collect bacteria that precipitate iron and manganese oxides. [Reston, Va.?: U.S. Dept. of the Interior, U.S. Geological Survey, 1998.

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10

Geological Survey (U.S.), ed. Sites in the Virginia-Washington, D.C.-Maryland metro area to observe or collect bacteria that precipitate iron and manganese oxides. [Reston, Va.?: U.S. Dept. of the Interior, U.S. Geological Survey, 1998.

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11

Geological Survey (U.S.), ed. Sites in the Virginia-Washington, D.C.-Maryland metro area to observe or collect bacteria that precipitate iron and manganese oxides. [Reston, Va.?: U.S. Dept. of the Interior, U.S. Geological Survey, 1998.

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12

Geological Survey (U.S.), ed. Sites in the Virginia-Washington, D.C.-Maryland metro area to observe or collect bacteria that precipitate iron and manganese oxides. [Reston, Va.?: U.S. Dept. of the Interior, U.S. Geological Survey, 1998.

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13

Geological Survey (U.S.), ed. Red slime, black coats, and oily films: The iron and manganese cycles at Huntley Meadows Wetland, Fairfax County, VA : field trip guidebook for Geological Society of Washington. [Reston, Va.?: U.S. Geological Survey, 1996.

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14

Geological Survey (U.S.), ed. Sites in the Virginia-Washington, D.C.-Maryland metro area to observe or collect bacteria that precipitate iron and manganese oxides. [Reston, Va.?: U.S. Dept. of the Interior, U.S. Geological Survey, 1998.

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15

Cox, Simon Peter. Iron oxidation and mineral oxidation by moderately thermophilic bacteria. [s.l.]: typescript, 1992.

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16

Clark, Darren Alan. The study of acidophilic, moderately thermophilic iron-oxidizing bacteria. [s.l.]: typescript, 1995.

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17

Hackett, Glen. Iron bacteria occurrence: Problems and control methods in water wells. Worthington, OH: National Water Well Association, 1985.

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18

J, Bullen J., and Griffiths E. 1940-, eds. Iron and infection: Molecular, physiological and clinical aspects. 2nd ed. Chichester: John Wiley, 1999.

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19

Donovan, Joseph J. Iron in Montana's groundwater: How to recognized and manage the problem. Bozeman, MT: Montana Water Resources Center, 1986.

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20

Chakraborty, Ranjan, Volkmar Braun, Klaus Hantke, and Pierre Cornelis, eds. Iron Uptake in Bacteria with Emphasis on E. coli and Pseudomonas. Dordrecht: Springer Netherlands, 2013. http://dx.doi.org/10.1007/978-94-007-6088-2.

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21

Guay, Roger. Development of a modified MPN procedure to enumerate iron oxidizing bacteria: Final report. Ottawa, Ont: Canada Centre for Mineral and Energy Technology = Centre canadien de la technologie des minéraux et de l'énergie, 1993.

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22

Pollett, Haemi. Effects of iron on the generation of hydrogen sulfide in a mixed culture containing sulfate-reducing bacteria (SRB) and methane-producing bacteria (MPB). Ottawa: National Library of Canada, 2003.

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23

Yates, Jacqueline Marie. Influence of iron on bacterial infections in leukaemia. Birmingham: Aston University. Department of Pharmaceutical Sciences, 1992.

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24

J, Bullen J., and Griffiths E. 1940-, eds. Iron and infection: Molecular, physiological, and clinical aspects. Chichester: Wiley, 1987.

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25

Cornelis, Pierre, and Simon C. Andrews. Iron uptake and homeostasis in microorganisms. Norfolk, UK: Caister Academic Press, 2010.

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26

Tateo, Yamanaka, ed. The Electron transfer system in an acidophilic iron-oxidizing bacterium. Tokyo: Academic Press, 1991.

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27

Iron transport in bacteria. Washington, DC: ASM Press, 2005.

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28

Mey, Alexandra R., Shelley M. Payne, and Jorge H. Crosa. Iron Transport in Bacteria. Wiley & Sons, Limited, John, 2014.

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29

Ellis, David B. Microbiology of the Iron - Depositing Bacteria. Wexford College Press, 2003.

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30

(Editor), R. Blakemore, and R. Frankel (Editor), eds. Iron Biominerals. Springer, 1991.

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31

Frankel, R., and R. Blakemore. Iron Biominerals. Springer London, Limited, 2013.

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32

Iron Biominerals. Springer, 2012.

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33

Ellis, David B. Iron Bacteria - Organisms And Their Identification - Illustrated. Merchant Books, 2006.

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34

Red slime, black coats, and oily films: The iron and manganese cycles at Huntley Meadows Wetland, Fairfax County, VA : field trip guidebook for Geological Society of Washington. [Reston, Va.?: U.S. Geological Survey, 1996.

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35

Red slime, black coats, and oily films: The iron and manganese cycles at Huntley Meadows Wetland, Fairfax County, VA : field trip guidebook for Geological Society of Washington. [Reston, Va.?: U.S. Geological Survey, 1996.

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36

Sites in the Virginia-Washington, D.C.-Maryland metro area to observe or collect bacteria that precipitate iron and manganese oxides. [Reston, Va.?: U.S. Dept. of the Interior, U.S. Geological Survey, 1998.

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37

Hackett, Glen. Iron Bacteria Occurrence: Problems and Control Methods in Water Wells. Natl Water Well Assn, 1986.

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38

Braun, Volkmar, Ranjan Chakraborty, and Klaus Hantke. Iron Uptake in Bacteria with Emphasis on E. coli and Pseudomonas. Springer, 2013.

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39

(Editor), D. J. Bullen, and E. Griffiths (Editor), eds. Iron and Infection: Molecular, Physiological and Clinical Aspects. 2nd ed. Wiley, 1999.

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40

Taiping yang zhong bu shui--yan xi tong zhong wei sheng wu huo dong ji qi cheng kuang zuo yong ("Taiping yang zhong bu duo jin shu jie he zong he yan jiu"). Xin hua shu dian zong dian ke ji fa xing suo jing xiao, 1994.

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41

(Editor), Jorge H. Crosa, Alexandra R. Mey (Editor), and Shelley M. Payne (Editor), eds. Iron Transport In Bacteria: Molecular Genetics, Biochemistry, And Role In Pathogenicity And Ecology. ASM Press, 2004.

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42

Iron Uptake in Bacteria with Emphasis on E. coli and Pseudomonas. Springer, 2013.

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43

Braun, Volkmar, Pierre Cornelis, Ranjan Chakraborty, and Klaus Hantke. Iron Uptake in Bacteria with Emphasis on E. Coli and Pseudomonas. Springer London, Limited, 2013.

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44

Winkelmann, Gunther. Handbook of Microbial Iron Chelates (1991). Taylor & Francis Group, 2017.

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45

Handbook of Microbial Iron Chelates (1991). Taylor & Francis Group, 2017.

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46

Winkelmann, Gunther. Handbook of Microbial Iron Chelates (1991). Taylor & Francis Group, 2017.

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47

Kirchman, David L. Introduction to geomicrobiology. Oxford University Press, 2018. http://dx.doi.org/10.1093/oso/9780198789406.003.0013.

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Geomicrobiology, the marriage of geology and microbiology, is about the impact of microbes on Earth materials in terrestrial systems and sediments. Many geomicrobiological processes occur over long timescales. Even the slow growth and low activity of microbes, however, have big effects when added up over millennia. After reviewing the basics of bacteria–surface interactions, the chapter moves on to discussing biomineralization, which is the microbially mediated formation of solid minerals from soluble ions. The role of microbes can vary from merely providing passive surfaces for mineral formation, to active control of the entire precipitation process. The formation of carbonate-containing minerals by coccolithophorids and other marine organisms is especially important because of the role of these minerals in the carbon cycle. Iron minerals can be formed by chemolithoautotrophic bacteria, which gain a small amount of energy from iron oxidation. Similarly, manganese-rich minerals are formed during manganese oxidation, although how this reaction benefits microbes is unclear. These minerals and others give geologists and geomicrobiologists clues about early life on Earth. In addition to forming minerals, microbes help to dissolve them, a process called weathering. Microbes contribute to weathering and mineral dissolution through several mechanisms: production of protons (acidity) or hydroxides that dissolve minerals; production of ligands that chelate metals in minerals thereby breaking up the solid phase; and direct reduction of mineral-bound metals to more soluble forms. The chapter ends with some comments about the role of microbes in degrading oil and other fossil fuels.
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48

Zughaier, Susu M., and Pierre Cornelis, eds. The Role of Iron in Bacterial Pathogenesis. Frontiers Media SA, 2018. http://dx.doi.org/10.3389/978-2-88945-662-8.

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49

Kang, Sun Ki. Iron oxidation by Thiobacillus ferrooxidans. 1989.

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50

Kirchman, David L. Processes in anoxic environments. Oxford University Press, 2018. http://dx.doi.org/10.1093/oso/9780198789406.003.0011.

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During organic material degradation in oxic environments, electrons from organic material, the electron donor, are transferred to oxygen, the electron acceptor, during aerobic respiration. Other compounds, such as nitrate, iron, sulfate, and carbon dioxide, take the place of oxygen during anaerobic respiration in anoxic environments. The order in which these compounds are used by bacteria and archaea (only a few eukaryotes are capable of anaerobic respiration) is set by thermodynamics. However, concentrations and chemical state also determine the relative importance of electron acceptors in organic carbon oxidation. Oxygen is most important in the biosphere, while sulfate dominates in marine systems, and carbon dioxide in environments with low sulfate concentrations. Nitrate respiration is important in the nitrogen cycle but not in organic material degradation because of low nitrate concentrations. Organic material is degraded and oxidized by a complex consortium of organisms, the anaerobic food chain, in which the by-products from physiological types of organisms becomes the starting material of another. The consortium consists of biopolymer hydrolysis, fermentation, hydrogen gas production, and the reduction of either sulfate or carbon dioxide. The by-product of sulfate reduction, sulfide and other reduced sulfur compounds, is oxidized back eventually to sulfate by either non-phototrophic, chemolithotrophic organisms or by phototrophic microbes. The by-product of another main form of anaerobic respiration, carbon dioxide reduction, is methane, which is produced only by specific archaea. Methane is degraded aerobically by bacteria and anaerobically by some archaea, sometimes in a consortium with sulfate-reducing bacteria. Cultivation-independent approaches focusing on 16S rRNA genes and a methane-related gene (mcrA) have been instrumental in understanding these consortia because the microbes remain uncultivated to date. The chapter ends with some discussion about the few eukaryotes able to reproduce without oxygen. In addition to their ecological roles, anaerobic protists provide clues about the evolution of primitive eukaryotes.
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