Nitrososphaera viennensis: Difference between revisions

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==Ecology==
==Ecology==
<I>N. viennensis</I> exists in soil globally<sup>(1)</sup>. The first <I>N. viennensis</I> isolated was from garden soil from the University Center at Althanstrasse in Vienna's 9th District<sup>(3)</sup>.
<I>N. viennensis</I> exists in soil globally<sup>(1)</sup>. The first <I>N. viennensis</I> strain isolated was from garden soil from the University Center at Althanstrasse in Vienna's 9th District<sup>(3)</sup>.


Its optimal temperature is 35°C with an optimum pH of 7.5<sup>(2)</sup>. Generation time of a pure culture with 1mM ammonia and pyruvate was  about ~45h<sup>(2)</sup>. Cell densities reached 5 X 10<sup>7</sup> cells mL<sup>-1(2)</sup>. Growth on cultures with ammonium alone slowed down to ~23d demonstrating it can grow autotrophically exclusively although very slowly<sup>(2)</sup>.
Its optimal temperature is 35°C with an optimum pH of 7.5<sup>(2)</sup>. Generation time of a pure culture with 1mM ammonia and pyruvate was  about ~45h<sup>(2)</sup>. Cell densities reached 5 X 10<sup>7</sup> cells mL<sup>-1(2)</sup>. Growth on cultures with ammonium alone slowed down to ~23d demonstrating it can grow autotrophically exclusively although very slowly<sup>(2)</sup>.


It is able to withstand higher ammonia concentrations than the only other pure isolate from ammonia oxidizing archaea, <I>Nitrosopumilus maritimus</I><sup>(2)</sup>. Growth occurred at 1, 3, 5, and 10 mM initial ammonia concentration<sup>(2)</sup>. Ammonia tolerances were similar to oligotrophic bacterial ammonia oxidizers<sup>(2)</sup>.
It is able to withstand higher ammonia concentrations than other ammonia oxidizing archaea such as <I>Nitrosopumilus maritimus</I> and <I>Nitrososphaera gargensis</I> <sup>(2)</sup>. Growth occurred at concentrations as high as 15 mM, but was inhibited at 20 mM<sup>(2)</sup>. Inhibitory ammonia concentrations for <I>N. maritimus</I> and <I>N. gargensis</I> are 2 to 3 mM. Ammonia tolerances were similar to oligotrophic bacterial ammonia oxidizers<sup>(2)</sup>.


Ammonia oxidizing Archaea such as <I>N. viennensis</I> may contribute to the nitrification of the environment<sup>(2)</sup>. It was previously believed only Bacteria could oxidize ammonia<sup>(2)</sup>. Ammonia oxidation is the first step in denitrification (NH<sub>3</sub> to NO<sub>2-</sub>) <sup>(1)</sup>.  Eventually N<sub>2</sub>O is produced in this process and escapes into the environment <sup>(1)</sup>.  N<sub>2</sub>O has a greenhouse warming potential 310 times higher than CO<sub>2</sub><sup>(1)</sup>.  It is responsible for 5%-7% of the greenhouse effect<sup>(1)</sup>.  It is the third most important greenhouse gas after CO<sub>2</sub> and CH<sub>4</sub><sup>(1)</sup>.  Ammonia oxidizing Bacteria and Archaea are estimated to contribute to ~70% of global N<sub>2</sub>O emissions<sup>(1)</sup>.
Ammonia oxidizing Archaea such as <I>N. viennensis</I> may contribute to the nitrification of the environment<sup>(2)</sup>. It was previously believed only Bacteria could oxidize ammonia<sup>(2)</sup>. Ammonia oxidation is the first step in denitrification (NH<sub>3</sub> to NO<sub>2-</sub>) <sup>(1)</sup>.  Eventually N<sub>2</sub>O is produced in this process and escapes into the environment <sup>(1)</sup>.  N<sub>2</sub>O has a greenhouse warming potential 310 times higher than CO<sub>2</sub><sup>(1)</sup>.  It is responsible for 5%-7% of the greenhouse effect<sup>(1)</sup>.  It is the third most important greenhouse gas after CO<sub>2</sub> and CH<sub>4</sub><sup>(1)</sup>.  Ammonia oxidizing Bacteria and Archaea are estimated to contribute to ~70% of global N<sub>2</sub>O emissions<sup>(1)</sup>.

Revision as of 23:26, 28 April 2013

This student page has not been curated.

A Microbial Biorealm page on the genus Nitrososphaera viennensis

Classification

Higher order taxa

Archaea; Thaumarchaeota; Nitrososphaerales; Nitrososphaeraceae

Species

Nitrososphaera viennensis

Nitrososphaera viennensis From: ScienceDaily

NCBI: Taxonomy

Description and significance

N. viennensis is a slightly irregular, spherically shaped ammonia oxidizing archaeon with a cell diameter of approximately 0.5-0.8 μm(2). It was the first cultivated terrestrial archaeal ammonia oxidizer(2).

Genome structure

The sequence divergence of N. viennensis's 16s rRNA gene from its closest relative, N. gargensis, is 3%(2).

Ammonia oxidizing Bacteria aerobically oxidize ammonia using ammonia monooxygenase (amoA) to catalyze the initial oxidation of NH3(1). Ammonia oxidizing archaea have amo-like genes that may contribute to their ammonia oxidation(1).

The urease gene cluster was located in one strain of N. viennensis, EN76(2). The cluster consisted of the encoding subunits ureA, ureB, and ureC and the accessory proteins ureE, ureF, ureG, and ureD(2).

NCBI: Genome

Metabolism

N. viennensis used urea or ammonia as an energy source in laboratory conditions(2). It is able to grow chemolithoautotrohically with inorganic compounds as an electron donor, but displayed higher growth rates when grown with bacteria or with the addition of pyruvate(2). It is currently unknown whether it is capable of heterotrophic or mixotrophic growth(2). The addition of vitamins, amino acids, and sugars had only a marginal effect on growth(2). Acetylene is a possible growth inhibitor(2).

The electron transfer process is not fully understood yet in ammonia oxidizing archaea(1). The amount of ATP per mole of NH3 is unknown since it varies depending on growth stage and other factors(1). Lack of cytochrome c proteins and many copper-containing proteins suggest a different electron transport mechanism than ammonia oxidizing bacteria, which is iron-heme-dependent(1).

Ecology

N. viennensis exists in soil globally(1). The first N. viennensis strain isolated was from garden soil from the University Center at Althanstrasse in Vienna's 9th District(3).

Its optimal temperature is 35°C with an optimum pH of 7.5(2). Generation time of a pure culture with 1mM ammonia and pyruvate was about ~45h(2). Cell densities reached 5 X 107 cells mL-1(2). Growth on cultures with ammonium alone slowed down to ~23d demonstrating it can grow autotrophically exclusively although very slowly(2).

It is able to withstand higher ammonia concentrations than other ammonia oxidizing archaea such as Nitrosopumilus maritimus and Nitrososphaera gargensis (2). Growth occurred at concentrations as high as 15 mM, but was inhibited at 20 mM(2). Inhibitory ammonia concentrations for N. maritimus and N. gargensis are 2 to 3 mM. Ammonia tolerances were similar to oligotrophic bacterial ammonia oxidizers(2).

Ammonia oxidizing Archaea such as N. viennensis may contribute to the nitrification of the environment(2). It was previously believed only Bacteria could oxidize ammonia(2). Ammonia oxidation is the first step in denitrification (NH3 to NO2-) (1). Eventually N2O is produced in this process and escapes into the environment (1). N2O has a greenhouse warming potential 310 times higher than CO2(1). It is responsible for 5%-7% of the greenhouse effect(1). It is the third most important greenhouse gas after CO2 and CH4(1). Ammonia oxidizing Bacteria and Archaea are estimated to contribute to ~70% of global N2O emissions(1).

References

1. Hatzenpichler, Roland (2012) Diversity, Physiology, and Niche Differentiation of Ammonia-Oxidizing Archaea, Applied and Environmental Microbiology 2012 Nov: 78(21): 7501-10. doi: 10.1128/AEM.01960-12.

2. Tourna, Maria, M. Stieglmeier, A. Spang, M. Könneke, A. Schintlmeister, T. Urich, M. Engel, M. Schloter, M. Wagner, A. Richter, and C. Schleper (2011) Nitrososphaera viennensis, an ammonia oxidizing archaeon from soil, PNAS 2011 ; doi:10.1073/pnas.1013488108

3. University of Vienna (2011) Novel microorganism 'Nitrososphaera viennensis' isolated. ScienceDaily, 2011 April 28. Retrieved April 28, 2013, from http://www.sciencedaily.com/releases/2011/04/110425153556.htm

Edited by Shanna Lovelace of Dr. Lisa R. Moore, University of Southern Maine, Department of Biological Sciences, http://www.usm.maine.edu/bio