Geomicrobiology: Difference between revisions
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===Microbial Energetics=== | ===Microbial Energetics=== | ||
Microbial energenetics are driven by Gibbs free-energy yield derived from ATP. ATP is heterotrophically generated by fermentation or respiration. The latter requires terminal electron acceptors (e.g. molecular oxygen, nitrate, sulphate, ferric iron, carbon dioxide, or molecular hydrogen), and produces greater amounts of ATP per unit substrate. Fermentation is less feasible in the presence of either highly oxidised or highly reduced substrate, and may rise toxic products (simple organic acids) that can eventually impede the process. The energy in soil is preserved in both organic and inorganic components enabling the microbial communities to sustain catabolic and anabolic processes. | Microbial energenetics (and all other forms of metabolism) are driven by Gibbs free-energy yield derived from ATP. ATP is heterotrophically generated by fermentation or respiration. The latter requires terminal electron acceptors (e.g. molecular oxygen, nitrate, sulphate, ferric iron, carbon dioxide, or molecular hydrogen), and produces greater amounts of ATP per unit substrate. Fermentation is less feasible in the presence of either highly oxidised or highly reduced substrate, and may rise toxic products (simple organic acids) that can eventually impede the process. The energy in soil is preserved in both organic and inorganic components enabling the microbial communities to sustain catabolic and anabolic processes. | ||
==Geobiology method== | ==Geobiology method== | ||
Revision as of 06:35, 9 March 2008
Introduction
Welcome to the world of GEOMICROBIOLOGY! In a nutshell, geomicrobiology includes microbes that "eat rocks". A more precise definition is "a subset of the scientific discipline microbiology. The field of geomicrobiology concerns the role of microbe and microbial processes in geological and geochemical processes. The field is especially important when dealing with microorganisms in aquifers and public drinking water supplies." (wikipedia)
This page will discuss a broad introduction to what geomicrobiological processes are all about, key microorganisms found in geomicrobiology, examples of such microbes, and current research in this field.
Enjoy!
Process - key points
Describe the process, using as many sections/subsections as you require. Look at the list of other topics. Which involve processes similar to yours? Create links where relevant.
Geobiology habitats
place
soil---aggregate pore
water--deep sea
Hydrothermo vent
condition
Temperature extreme---polar
PH-Low or High PH env.
Atmosphere-
Microbial Energetics
Microbial energenetics (and all other forms of metabolism) are driven by Gibbs free-energy yield derived from ATP. ATP is heterotrophically generated by fermentation or respiration. The latter requires terminal electron acceptors (e.g. molecular oxygen, nitrate, sulphate, ferric iron, carbon dioxide, or molecular hydrogen), and produces greater amounts of ATP per unit substrate. Fermentation is less feasible in the presence of either highly oxidised or highly reduced substrate, and may rise toxic products (simple organic acids) that can eventually impede the process. The energy in soil is preserved in both organic and inorganic components enabling the microbial communities to sustain catabolic and anabolic processes.
Geobiology method
We need to measure redox potential, PH, temperature and available electron donor and acceptor. Microbe foam a consortium so we need pure isolate method. Phase contrast, DIC, Epiflorsentce FISH MPN
Key Microorganisms within Geomicrobiology
Geomicrobiology included organisms that are concidered extremophiles. Extremophiles are microorganisms that live in areas considered too hostile for most. An example of an extremophile is anerobic sulfate reducing bacteria, which are know to live in hyper-saline lagoons in Brazil and Australia. It is believed these bacteria may be responsible for the formation of dolmite
Examples of Microorganisms
An example of extemophile organism is: anaerobic sulfate-reducing bacteria
Sulfate-reducing bacteria (SRB) comprise of several groups of bacteria that use sulfate as an oxidizing agent, reducing it to sulfide. Most sulfate-reducing bacteria can also use other oxidized sulfur compounds such as sulfite and thiosulfate, or elemental sulfur. This type of metabolism is called dissimilatory, since sulfur is not incorporated - assimilated - into any organic compounds. Sulfate-reducing bacteria have been considered as a possible way to deal with acid mine waters that are produced by other bacteria.
Another interested description of SRB is found at http://www.glossary.oilfield.slb.com/Display.cfm?Term=sulfate-reducing%20bacteria.
Acidithiobacillus is a genus of proteobacteria. The members of this genus used to belong to Thiobacillus, before they were reclassified in the year 2000. Members of this genus can be fined in pyrite deposits, metabolizing iron and sulfur and producing sulfuric acid. Example: Acidithiobacillus thiooxidans consumes sulfur and produces sulfuric acid. This bacterium in conjunction with others of the same genus is currently used in a mining technique called bioleaching whereby metals are extracted from their ores through oxidation. The bacteria are used as catalysts.
Hydrogenophilaceae also belongs to the Proteobacteria, and it is believed to be made of two genera. They are thermophilic bacterium growing in temperatures close to 50 °C. They obtain their energy from hydrogen oxidation. Example: Thiobacillus genus; includes only species from beta proteobacteria. This bacterium is used as a pest control in potato fields to control scabs.
Bacillus sp. strain SG-1 and Pseudomonas putida are common soil and freshwater Mn(II)-oxidizing bacterium. Mn(II)-oxidizing bacteria are a diverse group found in almost all environments. These bacteria are up to 5 orders of magnitude faster than abiotic reactions in the production of Mn oxides which have an amorphous structure with a high surface area. Mn(II) oxides are the only known oxidants of Cr(III) in the environment. The mechanism of Mn(II) oxidation by these bacteria is not clear, although recent outcomes from studies with Bacillus sp. strain SG-1 have shown that a Mn(III) is an intermediate in the final oxidation of Mn(II) through enzymatic activity. For more information on this group of bacterium look at the reference from Karen et al., 2007
The Epsilon-proteobacteria have recently been recognized as globally ubiquitous in marine and terrestrial ecosystems. They play a major role in biogeochemical and geological processes and have been isolated from sulfur rich terrestrial and marine environments, some of which are considered extreme habitats. Most representatives are only known through the 16S rRNA gene sequence despite current effort to develop culture techniques. For more information of this bacterium look at the reference from Campbell et al., 2006.
Current Research and Links
There is a very intresting site hosted by the Geomicrobiology & Environmental Microbiology Studies at Louisiana State University http://www.geol.lsu.edu/aengel/index.htm This site is filled with current research photos and informative discussions concerning the topic.
References
Murray, K. J., Tebo, B. M. 2007. Cr(III) Is Indirectly Oxidized by the Mn(II)-Oxidizing Bacterium Bacillus sp. Strain SG-1 Environ. Sci. Technol. 41: 528-533
Campbell, B.J., Engel, A.S., Porter, M.L., and Takai, K. (2006) The versatile Epsilonproteobacteria: Key players in sulphidic habitats. Nature Reviews Microbiology. 4: 458-468.
Edited by student of Kate Scow
