Geomicrobiology: Difference between revisions
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'''Geomicrobiology''' is a science that combines [[geology]] and [[microbiology]], and studies the interaction of [[Microorganism|microscopic organisms]] with their inorganic environment, such as in [[sedimentary rock]]s. The field is especially important when dealing with microorganisms in [[aquifer]]s and public drinking water supplies. | '''Geomicrobiology''' is a science that combines [[geology]] and [[microbiology]], and studies the interaction of [[Microorganism|microscopic organisms]] with their inorganic environment, such as in [[sedimentary rock]]s. The field is especially important when dealing with microorganisms in [[aquifer]]s and public drinking water supplies. | ||
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An application of geomicrobiology is [[bioleaching]], the use of microbes to extract metals from [[mining|mine]] waste. | An application of geomicrobiology is [[bioleaching]], the use of microbes to extract metals from [[mining|mine]] waste. | ||
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Latest revision as of 08:27, 30 October 2024
Geomicrobiology is a science that combines geology and microbiology, and studies the interaction of microscopic organisms with their inorganic environment, such as in sedimentary rocks. The field is especially important when dealing with microorganisms in aquifers and public drinking water supplies.
Another field of study in geomicrobiology is the study of extremophile organisms, the microorganisms that thrive in environments normally considered hostile. Such environments may include extremely hot (hot springs or mid-ocean ridge black smoker) environments, extremely saline environments, or even space environments such as Martian soil or comets.
Recent observations and research in hyper-saline lagoon environments in Brazil and Australia have shown that anaerobic sulfate-reducing bacteria may be directly involved in the formation of dolomite. This suggests the alteration and replacement of limestone sediments by dolomitization in ancient rocks was possibly aided by ancestors to these anaerobic bacteria.
Some bacteria use metal ions as their energy source. They convert (or chemically reduce) the dissolved metal ions from one electrical state to another. This reduction releases energy for the bacteria's use, and, as a side product, serves to concentrate the metals into what ultimately become ore deposits. Certain iron, uranium and even gold ores are thought to have formed as the result of microbe action.
Microbial life has been found at great depths in sedimentary and other rocks, several kilometers below the surface. The energy sources for growth of these microbes includes hydrogen gas generated in the interior of the planet, and it is estimated the biomass of these sub-surface microbial communities may equal the weght of all ocean and land plants. [1]
Microbes are being studied and used to degrade organic and even nuclear waste pollution (see Deinococcus radiodurans) and assist in environmental cleanup.
An application of geomicrobiology is bioleaching, the use of microbes to extract metals from mine waste.
Attribution
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References
- ↑ Exploration of deep intraterrestrial microbial life: current perspectives. Pedersen K. (2000). FEMS Microbiol Lett. Apr 1;185(1):9-16.