Halobacterium volcanii

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Halobacteria volcanii
Scientific classification
Phylum: euryarchaeota Genus: haloferax Species: h. volcanii
Binomial name
halobacterium volcanii

Also known as Haloferax volcanii

Description and Significance

Haloferax volcanii is an archaeon that can survive in environments of extreme salt concentrations. Halobacteria are located throughout the world in salt ponds and lakes, and may exist in the form of dormant or living cells, biopolymers in rocks, salt crystals, or as evaporates in desert regions.⁷ Haloferax volcanii in particular resides largely and predominantly in the bottom sediment of the Dead Sea, and are distinct from other organisms in their class in a few ways.²

H. volcanii are presumed to have been among the first living organisms on Earth when environmental conditions were much harsher than they are now. Though this is still highly debated, such a notion would correlate with the suggestion that H. volcanii may be present on and able to withstand the harsh conditions of Mars.⁷ Along with their ability to withstand harsh conditions is H. volcanii’s extensive ability for DNA repair. H. volcanii are also the first kind of archaeon to show horizontal gene transfer involving phage-mediated transduction, assimilation of naked DNA and conjugation, demonstrating importance and implications of surface proteins.⁶

Genome structure

Only one strain of Haloferax volcanii (Haloferax volcanii DS2) has a mapped genome. DS2 contains 4.01 million base pairs with approximately 4209 predicted genes. The most recent genome sequence draft was performed in April of 2007 by the Institute for Genomic Research. DS2 is found to have one chromosome and four plasmids. The chromosome has 2847757 base pairs and is 66.64% GC. Plasmid pHV4 has 635786 base pairs and is 61.67% GC. pHV 3 is 437906 base pairs and is 65.56% GC. pHV2 is 6359 base pairs and is 56.06% GC. Lastly, plasmid pHV1 is 85092 base pairs and is 55.5% GC.⁴

Cell structure and metabolism

There are two distinct properties in which Haloferax volcanii differ from other halobacteria. First, the cells of H. volcanii are disc shaped and cupped when grown under optimum conditions (highly saline, and a temperature of 42 degrees Celsius, although they can grow at 37 degrees Celsius). Secondly, optimum requirements for NaCl are 1.7 to 2.5M which is twice the range value that is normally seen for other halobacteria. Their tolerance for MgCl₂ is also much higher than other halobacteria.²

In general, Haloferax volcanii are gram positive, irregularly shaped rods, discs, or cups. They contain no endospores, are usually motile, and are at the minimum moderately halophilic. They are facultative anaerobes, meaning that they prefer to be in oxygenic environments but can survive in the lack of oxygen and always in aquatic environments and are chemoorganotrophs which means that in addition to using oxygen for respiration, they need carbon as their energy source.⁵ Cellular potassium ions help H. volcanii cells to survive lysis in high salt concentrations, while their pigments serve as a shield against ultraviolet light and also as a way to increase temperature by absorbing sunlight.⁷ Their highly negatively charged surfaces (due to a negatively charged amino terminus of amino acids) makes them more soluble and flexible at extreme salt concentrations.⁶

All archea have chaperonins that are similar to type II chaperonins found in eukaryotic organisms. Most archea also contain several heat shock proteins (Hsp), and those that do not usually contain the genes that encode for them. H. volcanii were used to determine that only one of these three genes are required for the organism to grow, though each does allow for functional specialization when present.⁹

H. volcanii are also the species of halobacteria and microorganisms that have helped to establish the importance of surface proteins. Seen under a resolution of 2nm, it has been determined that H. volcanii have dome-shaped, morphological complexes with pores at their apex which open into a funnel in the direction of the cell membrane. These complexes (cell envelopes) are also capable of establishing lateral connectivity, also important to the cell’s structure.³

Spatial organization and overall structure depicting functional dome shape of cell envelope of H. voclanii.

Ecology

Haloferax volcanii have many features that allow them to interact in a unique way with their environment. As suggested by their preponderance at the bottom of the Dead Sea where other organisms cannot survive, they have adapted to living in extreme environmental conditions. Among these is their ability to lie dormant for long periods of time in the event that environmental conditions are too unfavorable; once the conditions have moderated some, they return to their free-living state.⁷ The ability to lie dormant, specialized Hsp’s, and unparalleled DNA repair mechanisms give H. volcanii the ability to experience life and environments unattainable by almost all other microorganisms. Research has demonstrated that when the DNA of H. volcanii has been completely fragmented via exposure to extreme radiation not tolerated by any other microbe, H. volcanii reassembles completely and functionally in a matter of hours. This archaeon has also survived lethal amounts of UV exposure, extreme dryness, and a simulated vacuum (like that of outer space). It has further been determined that extreme salt concentrations lead to the same DNA mutations that radiation does. In this regard, H. volcanii already has available DNA repair mechanisms when exposed to radiation.⁸ Their extremophilic nature has lead scientists to experiment and believe that H. volcanii would be able to withstand environmental conditions on Mars that are so harsh no other organism tested has yet been able to survive.

Pathology

H. volcanii has no known pathogenic traits to any other microorganisms, animals, plants or humans.⁵

Application to Biotechnology

There is much to be gained from the understanding of Haloferax volcanii’s thriving in environmental conditions that are sometimes not tolerated by similar phylogenetic microorganisms. Gaining insight into the means by which H. volcanii has such unique environmental adaptive abilities can help in understanding the biological pathways of other, related organisms, that have yet to be understood. Once this understanding had been reached, much more is to be gained about the world we live in.

In addition, if scientists can discern the method by which H. volcanii achieves such immaculate and immediate DNA repair in response to mutagenic factors, then possible discoveries and associations can potentially be made in the human medical sector where mutagenic agents are a leading cause of many chronic ailments, including many cancers.

Current Research

H. volcanii is a particularly applicable microbe to the field of biotechnology. One reason is that their ability to withstand such extreme conditions and the locations in which they are found (which as mentioned, has also lead scientists to believe they are one of the oldest existing microorganisms), may guide researchers to further understanding of primitive life on Earth and thus more information on the path to modern day life. Many researchers are currently working with this proposal.⁵

In another area, because of their believed ability to protect astronauts against one of the biggest threats they face—space radiation—that has many long-lasting effects, NASA is currently researching H. volcanii’s mechanisms and abilities to perform such unseen yet greatly beneficial tasks.⁸

The third area of current research that ties the two other areas together is that of H. volcanii’s ability to tolerate ‘Martian conditions’. To date, H. volcanii has been able to survive in simulated Martian conditions. Some physiological changes have been noted, though the reason for why is unclear and is being studied further in order to gain a more complete understanding of the archaeon.⁷

The ability of H. volcanii to remain dormant in order to withstand extreme environmental conditions leads researchers to believe that it may exist in crystallized rock from vaporized salt lake beds on Mars.

References

[1] Haloferax volcanii. (n.d.). Retrieved April 20, 2009, from NCBI Web site:

    http://www.ncbi.nlm.nih.gov/Taxonomy/Browser/wwwtax.cgi?lvl=0&id=2246

[2] Mullakhanbhai, M. F., & Larsen, H. (1975, August 28). Halobacterium volcanii spec. nov., a dead sea halobacterium with a moderate salt requirement. Archives of Microbiology, 104(3), 207-214. Abstract retrieved April 20, 2009, from http://www.ncbi.nlm.nih.gov/1190944?dopt=Abstract

[3] Kessel, M., Wildhaber, I., Cohen, S., & Baumeister, W. (1988, May). Three-dimensional structure of the regular surface glycoprotein layer of halobacterium volcanii from the dead sea. The EMBO Journal, 7(5), 1549-1554. Retrieved April 21, 2009, from Department of Membrane and Ultrastructure Research, Hadassah Medical School, The Hebrew University Web site: http://www.pubmedcentral.nih.gov/articlefinder.fcgi?artid=458407

[4] About the haloferax volcanii april 2007. (2007, April). Haloferax volcanii (Haloferax volcanii DS2)

    Genome Browser Gateway. Retrieved April 22, 2009, from The University of California Web site: http://archaea.ucsc.edu/cgi-bin/hgGateway?db=halovolc1

[5] Haloferax volcanii DS2. (n.d.). Halophilic organism isolated from dead sea. Retrieved April 22,

    2009, from http://ncbi.nlm.nigh.gov/sites/enterez?db=genomeprj&cmd=search&term=Haloferax%20volcanii

[6] Mevarech, M. (n.d.). The mechanism of the natural genetic exchange system of haloferax volcanii. Retrieved April 20, 2009, from Tel Aviv University Web site: http://www.tau.ac.ll/lifesci/departments/biotech/members/mevarech/mevarech/html

[7] Chu, H., Sheng, W., Gan, D. C., & Kuznetz, L. (n.d.). Exobiology: The survival ability of halophiles

    under martian conditions. Retrieved April 20, 2009, from University of California at Berkeley 
    Web site: http://www.lpi.usra.edu/publications/reports/CB-1152/berkeley-1.pdf

[8] Barry, P. L. (2004, September 10). Secrets of a salty survivor: A microbe that grows in the dead sea is teaching scientists about the art of dna repair. Retrieved April 11, 2009, from NASA Web site: http://science.nasa.gov/headlines/y2004/10sep_radmicrobe.htm

[9] Large, A. T., Goldberg, M. D., & Lund, P. A. (2009, February). Chaperones and protein folding in the archaea. Biochemical society transactions, 37(Part 1), 46-51. Abstract retrieved April 21, 2009, from School of Biosciences, University of Birmingham Web site: http://www.ncbi.nlm.nih.gov/pubmed/19143600?ordinalpos=9&itool=EnterezSystem2.PEnterez.Pubmed.Pubmed_ResultsPanel.Pubmed_DefaultReportPanel.Pubmed_RVDocsum