Nostoc muscorum: Difference between revisions

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==Classification==
==Classification==


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==Description and Significance==
==Description and Significance==
Describe the appearance, habitat, etc. of the organism, and why you think it is important.
 
<i>Nostoc muscorum</i> is a free-living microorganism which inhabits both terrestrial and freshwater aquatic environments (Cameron, 1960) (Blumwald & Tel-Or, 1982). <i>N. muscorum</i> cells are filamentous, gram-negative green-brown colored algal cells which can form spores under desiccation conditions (Allison et al., 1937). As cyanobacteria, these organisms are phototrophic, performing photosynthesis in their environments and also fixing atmospheric nitrogen (Blumwald & Tel-Or, 1982).
 
The ideal environment for <i>Nostoc muscorum</i> is one with pH in the range of 7.0 to 8.5. These organisms cannot tolerate a pH lower than 5.7 (Allison et al., 1937). <i>N. muscorum</i> grows best when light intensity is less than that of direct sunlight, but can continue to grow and fix nitrogen for months in the presence of glucose and absence of sunlight. (Allison et al., 1937)
 
<i>Nostoc muscorum</i> are important for the nutrient cycling of carbon and nitrogen within the soil ecosystems in which they are found. Inoculation with this species has been shown to increase soil C content by 50-63% and N content by 111-120% as compared with uninoculated soil. (Rogers and Burns, 1993) The process of fixing atmospheric nitrogen contributes plant-available nitrogen to the soil, improving plant growth (Rogers and Burns, 1993).
 
Soils inoculated with <i>N. muscorum</i> also show an increase in soil aggregate resistance to degradation during wetting and physical disruption. (Rogers and Burns, 1993) This soil stability contribution can help prevent soil erosion, contributing to a higher success of seedling emergence in soils containing <i>N. muscorum</i> compared to those without it (Rogers and Burns, 1993) (Cameron, 1960). The aggregate-forming contributions of the microorganism also helps prevent desertification or the erosion of desert soils, where it is often present as part of cyanobacterial algal crusts (Cameron, 1960).
 
Current research with <i>Nostoc muscorum</i> involves manipulating the cells’ formation of poly (3-hydroxybutyrate) (PHB) and poly(3-hydroxybutyrate-co-3-hydroxyvalerate) [P(3HB-co-3HV)] co-polymer as potential materials to use in bioplastics for general and medical applications (Bhati and Mallick, 2012). <i>Nostoc muscorum</i> has the potential to be used in industrial settings which produce CO2 waste by using this waste as fuel under propionate- or valerate-supplemented conditions to form the above polymers for thermoplastic formation (Bhati and Mallick, 2012).  


==Genome Structure==
==Genome Structure==

Revision as of 15:09, 14 April 2012

Classification

Domain; Bacteria Phylum; Cyanobacteria Class; Cyanophyceae Order; Nostocales family; Nostocaceae Genus: Nostoc

Species

NCBI: Taxonomy

Genus species

Description and Significance

Nostoc muscorum is a free-living microorganism which inhabits both terrestrial and freshwater aquatic environments (Cameron, 1960) (Blumwald & Tel-Or, 1982). N. muscorum cells are filamentous, gram-negative green-brown colored algal cells which can form spores under desiccation conditions (Allison et al., 1937). As cyanobacteria, these organisms are phototrophic, performing photosynthesis in their environments and also fixing atmospheric nitrogen (Blumwald & Tel-Or, 1982).

The ideal environment for Nostoc muscorum is one with pH in the range of 7.0 to 8.5. These organisms cannot tolerate a pH lower than 5.7 (Allison et al., 1937). N. muscorum grows best when light intensity is less than that of direct sunlight, but can continue to grow and fix nitrogen for months in the presence of glucose and absence of sunlight. (Allison et al., 1937)

Nostoc muscorum are important for the nutrient cycling of carbon and nitrogen within the soil ecosystems in which they are found. Inoculation with this species has been shown to increase soil C content by 50-63% and N content by 111-120% as compared with uninoculated soil. (Rogers and Burns, 1993) The process of fixing atmospheric nitrogen contributes plant-available nitrogen to the soil, improving plant growth (Rogers and Burns, 1993).

Soils inoculated with N. muscorum also show an increase in soil aggregate resistance to degradation during wetting and physical disruption. (Rogers and Burns, 1993) This soil stability contribution can help prevent soil erosion, contributing to a higher success of seedling emergence in soils containing N. muscorum compared to those without it (Rogers and Burns, 1993) (Cameron, 1960). The aggregate-forming contributions of the microorganism also helps prevent desertification or the erosion of desert soils, where it is often present as part of cyanobacterial algal crusts (Cameron, 1960).

Current research with Nostoc muscorum involves manipulating the cells’ formation of poly (3-hydroxybutyrate) (PHB) and poly(3-hydroxybutyrate-co-3-hydroxyvalerate) [P(3HB-co-3HV)] co-polymer as potential materials to use in bioplastics for general and medical applications (Bhati and Mallick, 2012). Nostoc muscorum has the potential to be used in industrial settings which produce CO2 waste by using this waste as fuel under propionate- or valerate-supplemented conditions to form the above polymers for thermoplastic formation (Bhati and Mallick, 2012).

Genome Structure

Describe the size and content of the genome. How many chromosomes? Circular or linear? Other interesting features? What is known about its sequence?


Cell Structure, Metabolism and Life Cycle

Interesting features of cell structure; how it gains energy; what important molecules it produces.


Ecology and Pathogenesis

Habitat; symbiosis; biogeochemical significance; contributions to environment.
If relevant, how does this organism cause disease? Human, animal, plant hosts? Virulence factors, as well as patient symptoms.

References

[Sample reference] Takai, K., Sugai, A., Itoh, T., and Horikoshi, K. "Palaeococcus ferrophilus gen. nov., sp. nov., a barophilic, hyperthermophilic archaeon from a deep-sea hydrothermal vent chimney". International Journal of Systematic and Evolutionary Microbiology. 2000. Volume 50. p. 489-500.

Author

Page authored by _____, student of Prof. Jay Lennon at Michigan State University.

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