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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.
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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
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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 .
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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.
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