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Thermophile
Organism that thrives at relatively high temperatures
Organism that thrives at relatively high temperatures
A thermophile is a type of extremophile that thrives at relatively high temperatures, between 41 and. Many thermophiles are archaea, though some of them are bacteria and fungi. Thermophilic bacteria are suggested to have been among the earliest bacteria.
Thermophiles are found in geothermally heated regions of the Earth, such as hot springs like those in Yellowstone National Park and deep sea hydrothermal vents, as well as decaying plant matter, such as peat bogs and compost. They can live at high temperatures, whereas other bacteria or archaea would be damaged and sometimes killed if exposed to the same temperatures.
The enzymes in thermophiles function at high temperatures. Some of these enzymes are used in molecular biology, for example the Taq polymerase used in PCR. "Thermophile" is derived from "heat", and "love".
Comparative surveys suggest that thermophile diversity is principally driven by pH, not temperature.
Classification
Thermophiles can be classified in various ways. One classification sorts these organisms according to their optimal growth temperatures:
- Simple thermophiles: 50–64 C
- Extreme thermophiles 65–79 C
- Hyperthermophiles 80 C and beyond, but not below 50 C
In a related classification, thermophiles are sorted as follows:
- Facultative thermophiles (also called moderate thermophiles) can thrive at high temperatures, but also at lower temperatures (below 50 C), whereas
- Obligate thermophiles (also called extreme thermophiles) require such high temperatures for growth.
- Hyperthermophiles are particularly extreme thermophiles for which the optimal temperatures are above 80 C.
60 C.]]
Many hyperthermophilic Archaea require elemental sulfur for growth. Some are anaerobes that use the sulfur instead of oxygen as an electron acceptor during anaerobic cellular respiration. Some are lithotrophs that oxidize sulphur to create sulfuric acid as an energy source, thus requiring the microorganism to be adapted to very low pH (i.e., it is an acidophile as well as thermophile). These organisms are inhabitants of hot, sulfur-rich environments usually associated with volcanism, such as hot springs, geysers, and fumaroles. In these places, especially in Yellowstone National Park, zonation of microorganisms according to their temperature optima occurs. These organisms are often colored, due to the presence of photosynthetic pigments.
Thermophile versus mesophile
Thermophiles can be discriminated from mesophiles from genomic features. For example, the GC-content levels in the coding regions of some signature genes were consistently identified as correlated with the temperature range condition when the association analysis was applied to mesophilic and thermophilic organisms regardless of their phylogeny, oxygen requirement, salinity, or habitat conditions.
Fungal thermophiles
Fungi are the only group of organisms in the Eukaryota domain that can survive at temperature ranges of 50–60 °C. Thermophilic fungi have been reported from a number of habitats, with most of them belonging to the fungal order Sordariales. Thermophilic fungi have great biotechnological potential due to their ability to produce industrial-relevant thermostable enzymes, in particular for the degradation of plant biomass.
Gene transfer and genetic exchange
Sulfolobus solfataricus and Sulfolobus acidocaldarius are hyperthermophilic Archaea. When these organisms are exposed to the DNA damaging agents UV irradiation, bleomycin or mitomycin C, species-specific cellular aggregation is induced. In S. acidocaldarius, UV-induced cellular aggregation mediates chromosomal marker exchange with high frequency. and Ajon et al.
In science
Thermus aquaticus is historically important. Its discovery pushed forward the maximum temperature in which it was believed any organism could grow, and its heat-resistant DNA polymerase enabled it to develop an efficient way to multiply DNA quickly without the enzyme being denatured, a key step in the amelioration of PCR tests.
References
References
- Madigan MT. (2006). "Brock Biology of Microorganisms". Pearson.
- Takai T. (2008). "Cell proliferation at 122°C and isotopically heavy CH4 production by a hyperthermophilic methanogen under high-pressure cultivation". PNAS.
- Horiike T. (January 2009). "Phylogenetic construction of 17 bacterial phyla by new method and carefully selected orthologs". Gene.
- (March 2001). "Hyperthermophilic Enzymes: Sources, Uses, and Molecular Mechanisms for Thermostability". Microbiology and Molecular Biology Reviews.
- Power, J.F., Carere, C.R., Lee, C.K., Wakerley, G.L., Evans, D.W., Button, M., White, D., Climo, M.D., Hinze, A.M., Morgan, X.C. and McDonald, I.R., 2018. Microbial biogeography of 925 geothermal springs in New Zealand. Nature communications, 9(1), p.2876.
- Stetter, K.. (2006). "History of discovery of the first hyperthermophiles". Extremophiles.
- Zheng H. (December 2010). "Gene-centric association analysis for the correlation between the guanine-cytosine content levels and temperature range conditions of prokaryotic species". BMC Bioinformatics.
- (1993-09-01). "Thermophilic fungi: An assessment of their potential for growth in soil". Journal of Biosciences.
- (2021). "Thermophilic fungi: Diversity, physiology, genetics, and applications". Elsevier.
- (December 2015). "Thermophilic growth and enzymatic thermostability are polyphyletic traits within Chaetomiaceae". Fungal Biology.
- Fröls S. (November 2008). "UV-inducible cellular aggregation of the hyperthermophilic archaeon Sulfolobus solfataricus is mediated by pili formation". Mol. Microbiol..
- (November 2011). "UV-inducible DNA exchange in hyperthermophilic archaea mediated by type IV pili". Mol. Microbiol..
- Fröls S. (February 2009). "Reactions to UV damage in the model archaeon Sulfolobus solfataricus". Biochem. Soc. Trans..
- Barr, Camille. "Thermus Aquaticus". Montana Natural History Center.
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