Journals / Turkish Journal of Biology / 2007 / Cilt: 31 - Sayı: 2

Life in the Absence of Oxygen: Alternative Electron Acceptors for Anaerobic Microorganisms in a Petroleum Environment

Pages
59–66
Publication Date
2007-02-01
DOI
—
🏛️Bibliographic metadata and full text access for this article are provided via DergiPark.
DergiPark Record ↗
✨

AI Summary & Key Takeaways

AI Insight
⚡ TL;DR(Too Long; Didn't Read)

The results presented suggest that TP1 may occupy a niche as an environmental opportunist by taking advantage of diverse electron acceptors.

📌 3 Key Takeaways

🎯
Objective & Hypothesis:Anaerobic microorganisms derive energy by transferring electrons from an external source or donor to an external electron sink or terminal acceptor and often have the capacity to reduce 2 or more terminal electron acceptors.
📊
Key Findings & Data:The temperature range for growth of the enrichment culture (TP1) was between 40 and 65 °C and the optimum pH ranged from 4.5 to 8.0.
💡
Conclusion & Impact:The results presented suggest that TP1 may occupy a niche as an environmental opportunist by taking advantage of diverse electron acceptors.
🔬Design:Research Article
📍Scope:Comprehensive Sample
⚙️Variables:Anaerobic bacteria · electron acceptor utilization · petroleum environment

Abstract

Anaerobic microorganisms derive energy by transferring electrons from an external source or donor to an external electron sink or terminal acceptor and often have the capacity to reduce 2 or more terminal electron acceptors. The well-known type of microbial respiration, in which oxygen serves as an electron acceptor for the oxidation of organic carbon and/or hydrogen, has been studied elsewhere in detail. Anaerobic microorganisms are widely distributed in oil-producing vents, hydrothermal vents, volcanic hot springs, non-volcanic geothermally heated subsurface aquifers, and soil. In this study, anaerobic, thermophilic, and fermenting microorganisms in a petroleum sample from the Adıyaman region of Turkey were examined for their ability to use different electron acceptors. The temperature range for growth of the enrichment culture (TP1) was between 40 and 65 °C and the optimum pH ranged from 4.5 to 8.0. TP1 had the ability to use a wide variety of mono-, di-, and polysaccharides to form acetate, lactate, ethanol, H2, and CO2. No sulfate-reducing or methanogenic microorganisms were found. As an electron acceptor, TP1 reduces thiosulfate, elemental sulfur, sulfite, Fe(III), anthraquinone-2,6-disulfonate (AQDS), arsenake, and MnO2, but not sulfate, nitrate, (per)chlorate, or selenate. Herein, we show that the enrichment culture from the petroleum environment was able to reduce multiple electron acceptors. The utilization of these electron acceptors by TP1 also indicated their presence in this area. The results presented suggest that TP1 may occupy a niche as an environmental opportunist by taking advantage of diverse electron acceptors.

Özet

Anaerobic microorganisms derive energy by transferring electrons from an external source or donor to an external electron sink or terminal acceptor and often have the capacity to reduce 2 or more terminal electron acceptors. The well-known type of microbial respiration, in which oxygen serves as an electron acceptor for the oxidation of organic carbon and/or hydrogen, has been studied elsewhere in detail. Anaerobic microorganisms are widely distributed in oil-producing vents, hydrothermal vents, volcanic hot springs, non-volcanic geothermally heated subsurface aquifers, and soil. In this study, anaerobic, thermophilic, and fermenting microorganisms in a petroleum sample from the Adıyaman region of Turkey were examined for their ability to use different electron acceptors. The temperature range for growth of the enrichment culture (TP1) was between 40 and 65 °C and the optimum pH ranged from 4.5 to 8.0. TP1 had the ability to use a wide variety of mono-, di-, and polysaccharides to form acetate, lactate, ethanol, H2, and CO2. No sulfate-reducing or methanogenic microorganisms were found. As an electron acceptor, TP1 reduces thiosulfate, elemental sulfur, sulfite, Fe(III), anthraquinone-2,6-disulfonate (AQDS), arsenake, and MnO2, but not sulfate, nitrate, (per)chlorate, or selenate. Herein, we show that the enrichment culture from the petroleum environment was able to reduce multiple electron acceptors. The utilization of these electron acceptors by TP1 also indicated their presence in this area. The results presented suggest that TP1 may occupy a niche as an environmental opportunist by taking advantage of diverse electron acceptors.

🔖

Cite This Article

BALK, M. (2007). Life in the Absence of Oxygen: Alternative Electron Acceptors for Anaerobic Microorganisms in a Petroleum Environment. Turkish Journal of Biology, Cilt: 31 - Sayı: 2, 59–66. https://ajindex.com/articles/182192

📄 Full Text PDF Viewer

📄

PDF görüntüleyici hazırlanıyor...

References (15)

  1. Magot M. Similar bacteria in remote oil fields. Nature 379: 681, 1996.
  2. Ravot G, Ollivier B, Magot M et al. Thiosulfate reduction, an important physiological feature shared by members of the order Thermotogales. Appl Environ Microbiol 61: 2053-2055, 1995.
  3. Jeanthon C, Reysenbach AL, L’Haridon S et al. Thermotoga subterranea sp. nov., a new thermophilic bacterium isolated from a continental oil reservoir. Arch Microbiol 164: 91-97, 1995.
  4. Fardeau ML, Ollivier B, Patel BKC et al. Thermotoga hypogea sp. nov., a xylanolytic, thermophilic bacterium from an oil-producing well. Int J Syst Evol Microbiol 47: 1013-1019, 1997.
  5. Orphan VJ, Taylor LT, Hafenbradl D et al. Culture-dependent and culture-independent characterization of microbial assemblages associated with high-temperature petroleum reservoirs. Appl Environ Microbiol 66: 700-711, 2000.
  6. Stetter KO, Hoffmann A, Huber R. Microorganisms Adapted to High Temperature Environments. In: Guerrrero R, Pedros-Alio C. eds. Trends in Microbiology Ecology. Spanish Society for Microbiology, 1993: pp. 25-28. Pedersen K. Exploration of deep intraterrestrial microbial life: current perspectives. FEMS Microbiol Lett 185: 9-16, 2000.
  7. Kasting JF, Siefert JL. Life and the Evolution of Earth’s Atmosphere. Science 296: 1066, 2002.
  8. Reysenbach AL, Shock E. Merging Genomes with Geochemistry in Hydrothermal Ecosyst Sci 296: 1077, 2002.
  9. Balk M, Weijma J, Friedrich MW et al. Methanol conversion by novel thermophilic homoacetogenic bacterium Moorella mulderi sp. nov. isolated from a bioreactor. Arch Microbiol 179: 315- 320, 2003.
  10. Henstra AM, Stams AJ. Novel physiological features of Carboxydothermus hydrogenoformans and Thermoterrabacterium ferrireducens. Appl Environ Microbiol 70: 7236-40, 2004.
  11. Scholten JC, Stams AJM. The effect of sulfate and nitrate on methane formation in a freshwater sediment. Antonie van Leeuwenhoek 68: 309-315, 1995.
  12. Trüper HG, Schlegel HG. Sulphur metabolism in Thiorhodaceae. I. Quantitative measurements on growing cells of Chromatium okenii. Antonie Van Leeuwenhoek 30: 225-238, 1964.
  13. Amend JP, Shock EL. Energetics of overall metabolic reactions of thermophilic and hyperthermophilic Archaea and Bacteria. FEMS Microbiol Rev 25: 175-243, 2001.
  14. Morikawa M, Kanemoto T, Imanaka T. Biological oxidation of alkane to alkene under anaerobic conditions. J Ferm Bioeng 82: 309-311, 1996.
  15. Stetter KO, Huber R. The role of hyperthermophilic prokaryotes in oil fields, in: Bell M, Brylinsky M, Johnson-Green P. eds. Microbial Biosys