Difference between revisions of "Team:Hong Kong-CUHK/Description"

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<h2>ABCDE (<i><u>A</u>zoto<u>B</u>acter vinelandii</i> in <u>C</u>arbon <u>D</u>ioxide to methane <u>E</u>nergy) </h2>
 
  
<h5>Objective</h5>
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<h1>The Magnetosome </h1>
  
<p>In this project, we aim to utilize modified nitrogenase in <i>Azotobacter vinelandii</i> to convert carbon dioxide (CO<sub>2</sub>) to methane (CH<sub>4</sub>). It is hoped to produce a fuel while fixing carbon.</p>
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<p> Magnetosome is a membrane bounded intracellular structure, something that is actually rare in prokaryotic organisms like bacteria. They are of nano-size ranging from about 35-120 nm. Magnetosomes comprise of a magnetic mineral crystal surrounded by a lipid bilayer membrane about 3–4 nm thick (fig. __). A number of common cytoplasmic membrane fatty acids components can be found in the magnetosome membrane. It is then later highly suspected that magnetosomes are membrane invaginations originating from the cytoplasmic membrane [1].
 +
The magnetosome membrane is highly significant as it creates an isolated environment within the cell which is crucial for mineral crystal nucleation and growth [2]. These membrane-enclosed inorganic crystals consist of either the magnetic minerals magnetite (Fe3O4) or greigite (Fe3S4). The particles usually arrange themselves along the cell axis either in one or multiple chains . Different varieties of crystal morphologies such as cubo-octahedral, elongated hexagonal prismatic, and bullet-shaped morphologies have been discovered [1] </p>.
  
<h5>Background and Significance</h5>
 
  
<p>With the exploitation of carbon-based fossil fuels, we sought for an alternative solution to combat the global energy crisis by utilizing a gas pollutant – CO<sub>2</sub> - through carbon fixation. To maintain current living standard, alternative energy sources are unprecedentedly demanding. We are now engineering a bacteria <i>Azotobacter vinelandii</i> to convert CO<sub>2</sub> into CH<sub>4</sub> inside the bacteria <i>Azotobacter vinelandii</i>. <i>A. vinelandii</i> is a facultative aerobe with an intracellular anaerobic environment which is essential for the reduction reactions.</p>
 
  
<h5>Why CH<sub>4</sub>?</h5>
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<h1>The Magnetotactic Bacteria -- The origin of magnetosome </h1>
<p>CH<sub>4</sub> produced can serve as a fuel, and any CO<sub>2</sub> produced during the process can be returned to the system to CH<sub>4</sub> generation. Comparing to hydrogen (H<sub>2</sub>), a popular alternative energy source because of its "cleanliness" after combustion, storage of CH<sub>4</sub> is cheaper than that of H<sub>2</sub> due to a lower boiling point from the perspective of fuel storage. Thus it requires less energy to liquefy.  Our engineered bacteria would also be able to convert the greenhouse gas CO<sub>2</sub> into CH<sub>4</sub> in closed systems, which eliminates the disadvantage of using CH<sub>4</sub> as a fuel, and being a potent greenhouse gas. Additionally, no change needed to be made on current car engines, which are designed to use of hydrocarbon fuels. </p>
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<p>Magnetosomes are intracellular membrane bounded organelle synthesized by Magnetotactic bacteria. First discovered in 1975 by Richard Blakemore, these magnetotactic bacteria are mobile, aquatic, gram-negative prokaryotes [3] with a myriad of cellular morphologies, including coccoid, rod-shaped, vibrioid, helical or even multi-cellular. They are found in their highest numbers at, or just below, the oxic-anoxic interface in aquatic habitats and exhibit a negative growth response to atmospheric concentrations of oxygen. </p>
  
<h5>Goal to be achieved</h5>
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<p>Magnetosomes form a chain and align themselves along the axis within the bacteria. With the formation of magnetosomes inside them, they are able to align passively to the earth’s magnetic field and hence use  minimum energy to swim along geomagnetic field lines. This behaviour is called magnetotaxis [4] and is beneficial to the survival of the bacteria as it helps them to reach regions of optimal oxygen concentrations without random, unnecessary movements [5]. </p>
<p>From literatures, we found out that the carbon fixation process is not efficient enough, as most energy is wasted in H<sub>2</sub> production. Therefore, we are tackling the fixation efficiency through two approaches: (1) enhancing H<sub>2</sub> recycling to return its energy back to the reaction chain, and; (2) increasing intracellular CO<sub>2</sub> concentration.</p>
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<h2> MNOPQ (<u>M</u>agnetic <u>N</u>anoparticles <u>O</u>n <u>P</u>articular re<u>Q</u>uirement) </h2>
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<h1> Why and What is Azotobacter? </h1>
  
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<p>Though magnetotactic bacteria is the origin of magnetosomes, these bacteria are described by scientists as a group of fastidious prokaryotic bacteria -- meaning that they are difficult to cultivate owing to their unusual growth requirements. Their micro-aerophilic nature require elaborate growth techniques, and they are difficult to grow on the surface of agar plates, which would make the screening for mutants a problem [6]. </p>
  
 +
<p>The lack of effective methods of DNA transfer in these microorganisms is a challenge too. Luckily, the situation is improving due to better technologies recently and some of the genes from M. magnetotacticum have been confirmed functionally expressed in E. coli. This shows that the transcriptional and translational elements of the two microorganisms are compatible. With such good news, a number of previous igem teams including kyoto: 2014, OCU-China: 2013, Washington: 2011 and UNIK_Copenhagen: 2013 have been working with transferring the magnetosome related genes to e.coli. Some exciting results the formation of magnetosome membrane in e.coli (by the kyoto team) has been reported by previous teams, however, never the whole magnetosome.
 +
We have been wondering why magnetosomes seems so hard to be formed in e.coli. And then, we come up with a hypothesis -- the formation of magnetosome requires a micro-aerobic or anaerobic environment as the magnetotatic bacteria are all living micro-aerobically. </p>
  
<h5>Objective</h5>
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<p>Therefore, we chose a new bacteria to work on our magnetosome project -- the Azotobacter vinelandii.  
 
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Azotobacter vinelandii is gram-negative diazotroph. It is a soil bacterium related to the Pseudomonas genus that fixes nitrogen under aerobic conditions while having enzymatic mechanisms protecting its oxygen-sensitive nitrogenase from oxygen damage. This findings shows that A. vinelandii is an excellent host for the production and characterization of oxygen-sensitive proteins or organelles as in our case [7]. </p>
<p>We aim to produce magnetic nanoparticles to meet certain requirements. <i>Azotobacter vinelandii</i> is also used in this project because it provides an intracellular anaerobic condition that is essential for the production processes. </p>
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<h5>Background and Significance</h5>
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<p>Magnetosome is an organelle with magnetic iron crystal (magnetite) encapsulated by lipid bilayer which is originated from bacteria such as <i>Magnetospirillum gryphiswaldense</i>. It serves as a navigational device in magnetotactic bacteria by interacting with the Earth magnetic field. Magnetic beads formed could be applied in various aspects.
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Biomolecules, such as enzymes and antibodies, can be expressed on the magnetosome so that they can be easily controlled by magnet for specific purposes. </p>
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<p>Unfortunately, most of the magnetotactic bacteria require microaerobic conditions for magnetosome biogenesis, which is hard to maintain with normal lab equipment. We are transferring essential genes for magnetosome formation into <i>A. vinelandii</i>, a facultative aerobe with an intracellular anaerobic environment, in hope of producing magnetic beads with functional biomolecules under aerobic conditions with greater yield. We are also modifying the transmembrane protein presented on magnetosome membrane by fusing with biomolecules. Reactions could be more accelerated as magnetites generated from magnetosome provides a greater surface area-to-volume ratio than that of artificial magnetic beads. </p>
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<h5>Applications</h5>
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<p>One of the applications is to use engineered magnetites to capture heavy metal ion in water. Heavy metal is one of the major components in marine pollution. Different kinds of heavy metal ions, such as Pb, Cu and Ni, are found in marine system. By expressing different heavy metal binding proteins onto magnetic beads, heavy metal ions could be captured and be easily removed by magnet. It is better than the previous methods, in terms of operating cost, efficiency and eco-friendliness.
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<p>We are also adding antibodies on magnetosome for immunoprecipitation. Due to the smaller size of magnetosome than traditional magnetic beads, magnetosome with antibodies could have a higher binding efficiency. Also, the antibodies containing magnetic beads can be massively produced in bacteria.</p>
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<p>With the biggest advantage of using azotobacter is that it is an aerobic bacteria with an intracellular anaerobic condition, we can grow it easily in normal conditions in lab without expensive equipments like fermenter, while fulfilling the growing criteria for the magnetosome.  Besides, most parts in registry are functionable in Azotobacter and Azotobacter is of safety level group 1 too.  One more important thing is that it can do homologous recombination by itself which is a critical process we need in our project. </p>
  
  
 
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Revision as of 18:55, 16 September 2015

The Magnetosome

Magnetosome is a membrane bounded intracellular structure, something that is actually rare in prokaryotic organisms like bacteria. They are of nano-size ranging from about 35-120 nm. Magnetosomes comprise of a magnetic mineral crystal surrounded by a lipid bilayer membrane about 3–4 nm thick (fig. __). A number of common cytoplasmic membrane fatty acids components can be found in the magnetosome membrane. It is then later highly suspected that magnetosomes are membrane invaginations originating from the cytoplasmic membrane [1]. The magnetosome membrane is highly significant as it creates an isolated environment within the cell which is crucial for mineral crystal nucleation and growth [2]. These membrane-enclosed inorganic crystals consist of either the magnetic minerals magnetite (Fe3O4) or greigite (Fe3S4). The particles usually arrange themselves along the cell axis either in one or multiple chains . Different varieties of crystal morphologies such as cubo-octahedral, elongated hexagonal prismatic, and bullet-shaped morphologies have been discovered [1]

.

The Magnetotactic Bacteria -- The origin of magnetosome

Magnetosomes are intracellular membrane bounded organelle synthesized by Magnetotactic bacteria. First discovered in 1975 by Richard Blakemore, these magnetotactic bacteria are mobile, aquatic, gram-negative prokaryotes [3] with a myriad of cellular morphologies, including coccoid, rod-shaped, vibrioid, helical or even multi-cellular. They are found in their highest numbers at, or just below, the oxic-anoxic interface in aquatic habitats and exhibit a negative growth response to atmospheric concentrations of oxygen.

Magnetosomes form a chain and align themselves along the axis within the bacteria. With the formation of magnetosomes inside them, they are able to align passively to the earth’s magnetic field and hence use minimum energy to swim along geomagnetic field lines. This behaviour is called magnetotaxis [4] and is beneficial to the survival of the bacteria as it helps them to reach regions of optimal oxygen concentrations without random, unnecessary movements [5].

Why and What is Azotobacter?

Though magnetotactic bacteria is the origin of magnetosomes, these bacteria are described by scientists as a group of fastidious prokaryotic bacteria -- meaning that they are difficult to cultivate owing to their unusual growth requirements. Their micro-aerophilic nature require elaborate growth techniques, and they are difficult to grow on the surface of agar plates, which would make the screening for mutants a problem [6].

The lack of effective methods of DNA transfer in these microorganisms is a challenge too. Luckily, the situation is improving due to better technologies recently and some of the genes from M. magnetotacticum have been confirmed functionally expressed in E. coli. This shows that the transcriptional and translational elements of the two microorganisms are compatible. With such good news, a number of previous igem teams including kyoto: 2014, OCU-China: 2013, Washington: 2011 and UNIK_Copenhagen: 2013 have been working with transferring the magnetosome related genes to e.coli. Some exciting results the formation of magnetosome membrane in e.coli (by the kyoto team) has been reported by previous teams, however, never the whole magnetosome. We have been wondering why magnetosomes seems so hard to be formed in e.coli. And then, we come up with a hypothesis -- the formation of magnetosome requires a micro-aerobic or anaerobic environment as the magnetotatic bacteria are all living micro-aerobically.

Therefore, we chose a new bacteria to work on our magnetosome project -- the Azotobacter vinelandii. Azotobacter vinelandii is gram-negative diazotroph. It is a soil bacterium related to the Pseudomonas genus that fixes nitrogen under aerobic conditions while having enzymatic mechanisms protecting its oxygen-sensitive nitrogenase from oxygen damage. This findings shows that A. vinelandii is an excellent host for the production and characterization of oxygen-sensitive proteins or organelles as in our case [7].

With the biggest advantage of using azotobacter is that it is an aerobic bacteria with an intracellular anaerobic condition, we can grow it easily in normal conditions in lab without expensive equipments like fermenter, while fulfilling the growing criteria for the magnetosome. Besides, most parts in registry are functionable in Azotobacter and Azotobacter is of safety level group 1 too. One more important thing is that it can do homologous recombination by itself which is a critical process we need in our project.