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تيرصنتسولا تعهاجلا ةايحلا مولع نسق/مولعلا تيلك تيحابصلا تساردلا/تيرهجولا ءايحلاا عرف/ تثلاثلا تلحرولا Lec (5): Extreme Environments There are two definitions of extreme Environments ,The first characterizes an environments as extreme if the environmental conditions are at one or two extreme ( high or low).these environmental conditions can include pH, temperature , salinity ,pressure and nutrients . The second definition refers to Environments in which conditions select for extremely low microbial diversity. Extremophile: The organisms that have successfully adapted to environments where it is difficult or impossible for other organisms to survive.Extreme environments are important to environmental microbiologists because there is much speculation that such environments harbor unique microorganisms with activities that are not only of scientific interest but also that have commercial potential. Microbial communities in extreme environments have adapted to amazing levels of stress. These adaptations are of interest for development of remediation approaches for some contaminated sites including acid mine drainage sites and radioactive waste sites. They also are of interest for applications of novel enzymes adapted to temperature or pH extremes. Finally, they are of interest for understanding evolutionary history and possible impacts of future climate change. Types of extreme environments Extremophiles have been selected over time for characteristic that allow them to grow and multiply in a variety of extreme environments,will describe some of environments and the physiological adaptions use by extremophiles to compete or survive in their particular niche. يجرعلاا نشاه نظاك . د.أ : ةداولا ذاتسأ يركسعلا يلع ءارفع .د.م 1 1. Low Temperature Environments The McMurdo Dry Valleys in Antarctica represent one of the driest and coldest ecosystems known. The average mean annual surface air temperature is -27.6°C and the average surface soil temperature is -26.1°C. This ecosystem has the only permanently ice-covered lakes on Earth, varying in ice-cover thickness from 3 to 5 m .Researchers studying the site found a diverse community of phototrophic purple bacteria , sulfur chemoautotrophs, and heterotrophic sulfate-reducers. For example, cell numbers of sulfur-oxidizing bacteria were found to peak at 200 cells per ml at a depth of 9.5 m , this is where both dissolved oxygen and sulfide coexist in the water column. Three sulfur-oxidizers were cultured from lake water samples, all most closely related to Thiobacillus thioparus .Sulfate-reducing bacteria were also found In addition a methane gradient begins at a depth of 12 m .This gradient implies the presence of a methane cycle and the presence of both methanogenic and methanotrophic microorganisms . cold-adapted microorganisms: Their ability to survive and grow in the cold requires specialized adaptations For example, these microorganisms synthesize cold-adapted enzymes which have had to evolve specific structural features that make them highly flexible in comparison to their warm temperature equivalents .This flexibility, particularly around the active site of the enzyme (the site where the enzyme interacts with its substrate) means that the enzyme can operate efficiently at low temperatures. This also means that at high temperatures the enzyme becomes unstable. In fact, it is these two properties of coldactive enzymes that makes them suitable for biotechnological application: their high activity at low temperature and their low stability at elevated temperatures. Low temperature enzymes that have been examined or used in industry include α- amylase ,cellulase , β- galactosidase ,lipase proteases , xylanase . 2. Desiccation and UV Stress The deserts of the world represent both hot and semi- cold and hyperarid environments where extreme conditions severely limit primary productivity and thus the diversity of life. Factors limiting microbial life in the arid deserts include water availability, temperature, and the intensity of UV radiation. Arid 2 deserts are characterized by mean annual rainfall levels of 25–200 mm while hyperarid deserts have mean annual rainfall of < 25 mm. Water availability in a desert is determined not only by mean annual rainfall, but also by the combined effects of precipitation (P) and potential evapotranspiration (PET). Hyperarid areas are defined as those with a P/PET ratio less than 0.05 Due to the lack of available moisture, plants are sparse or completely absent, creating soil conditions with extremely low soil organic carbon and nitrogen levels, further limiting the potential diversity of microbial life. commonly studied feature in arid environments is the lithic microbial communities, those that inhabit rock surfaces and subsurface rock pores. These communities are dominated by photoautotrophic nitrogen-fixing cyanobacteria and are capable of colonizing a diverse group of minerals including, granite, gypsum, halite, , quartz, and sandstone. These communities have been found in a range of hot and cold deserts. These hypolithic (inhabit rock surfaces) and endolithic (inhabit pore spaces within the rocks) communities are believed to exploit the protection offered by rock surfaces that scatter UV radiation and presumably trap limited water supplies. The dominant photoautotroph found in the majority of these communities is the desiccation and radiation tolerant cyanobacterium Chroococcidiopsis . Adaptation to desiccation is unique among the extremes experienced by bacteria induce survival strategies for the cells rather than the ability to function under extreme conditions. The survival strategies identified include the following: ● The ability to protect and repair DNA exposed to UV radiation ● Maintenance of protein stability in the dehydrated state ● Maintenance of membrane integrity The primary adaptative mechanism of the cyanobacteria is the production of an extracellular polysaccharide (EPS) sheath. This sheath regulates the uptake and loss of water, serves as a matrix for immobilization of cellular components produced by the cell in response to desiccation, and may protect cell walls during shrinking and swelling . 3 3- Air-Water Interface The air –water interface is a unique habitat that is often considered an extreme environment for many reasons, including high levels of solar radiation accumulation of toxic substances(e.g. heavy metals,pesticides). Large temperature pH salinity fluctuations competition The air–water interface, also referred to as the neuston, contains higher concentrations of organisms than other layers of the water column ,most reports suggest that the numbers may be higher but the ratio of metabolic activity to total counts is lower in the neuston than in the planktonic habitat. The neuston accumulates nutrients and especially attracts nonpolar organic and inorganic molecules, in addition to the nutrients accumulation the neuston tends to accumulate toxins .Among these toxins are nonpolar organic molecules,including pesticides such as DDT and petroleum hydrocarbons,as well as metals such as Cd,Cu,Mn,Hg,Pb,Se and Cr .The microorganisms that inhabit the neuston have developed unique metabolic,genetic and functional strategies that allow them to survive the extreme environments.These strategies include Use of pathways that catabolize toxic compounds and provide resistance to metals that accumulate at the interface. Some microbes have developed efficient DNA repair mechanisms to combat DNA damage caused by exposure to ultraviolet radiation. 4- High Temperature There are many examples of environments with extreme temperature. Environments with high temperature (>70 oC) include terrestrial and submarine hot springs, some of which can reach temperature of 100 oC and hydrothermal vents, which can reach temperature in excess of 300 oC. Such high temperature are inhospitable for most forms of life except for certain bacteria and archaebacteria. Genera commonly found in these environments include Thermus, Methanobacterium, Sulfolobus, Pyrodictium, and Pyrococcus. temperatures of up to 100°C. 4
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