Rhodothermus marinus: Difference between revisions
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''Rhodothermus. marinus'' was first isolated from submarine alkaline freshwater hot springs in Isafjardardjup, Iceland in 1988 and from other geothermal sites in Iceland including coastal springs from a borehole effluent in Oxarfjordur, Iceland, from borehole effluents from a powerplant at the Blue Lagoon, and from a salt factory in Reykjanes, Iceland. As well, it has been isolated from similar habitats in geothermal environments at various regions around the world, including Praia de Ribeira Quenta, Ferraria, Sa˜o Miguel in the Azores, Portugal, Stufe di Nerone near Naples, Italy, and on Monserrat island in the Carribean Sea. It should be noted that the populations of '' | ''Rhodothermus. marinus'' was first isolated from submarine alkaline freshwater hot springs in Isafjardardjup, Iceland in 1988 and from other geothermal sites in Iceland including coastal springs from a borehole effluent in Oxarfjordur, Iceland, from borehole effluents from a powerplant at the Blue Lagoon, and from a salt factory in Reykjanes, Iceland. As well, it has been isolated from similar habitats in geothermal environments at various regions around the world, including Praia de Ribeira Quenta, Ferraria, Sa˜o Miguel in the Azores, Portugal, Stufe di Nerone near Naples, Italy, and on Monserrat island in the Carribean Sea. It should be noted that the populations of ''Rhodothermus marinus'' in these geographic locations are genetically distinct. High genetic diversity and low horizontal gene transfer indicate the populations at these geographically distinct sites are evolving independently and indicate that genetic drift and geographic isolation is an important mechanism in species divergence (Petursdottir ''et al''). | ||
''Rhodothermus. marinus'' is a heterotrophic obligate aerobe that is thermophilic and slightly although strictly halophilic. The growth of this organism is dependent on a multitude of factors including temperature, salt and oxygen concentration, and the availability of organic material. Growth occurs at a temperature range of 54-77 degrees Celsius with optimal growth occurring at 65 degrees Celsius. '' | ''Rhodothermus. marinus'' is a heterotrophic obligate aerobe that is thermophilic and slightly although strictly halophilic. The growth of this organism is dependent on a multitude of factors including temperature, salt and oxygen concentration, and the availability of organic material. Growth occurs at a temperature range of 54-77 degrees Celsius with optimal growth occurring at 65 degrees Celsius. ''Rhodotherms marinus'' has also been characterized at growing at NaCl concentrations optimally at 2% and not above 6%. This species only utilizes a single carbon source, with slight differences in carbon sources between strains. The physiology of this microbe dictates a narrow niche for it to occupy. ''Rhodothermus marinus'' can only grow close to the openings of hot springs where oxygen is readily available and close to the surface of the water where the temperatures are warm. Not much is known about any symbiotic relationships that ''Rhodothermus marinus'' might hold. Hopefully future ecological studies can shed light on such relationships. | ||
[[Image:Blue-lagoon-iceland-geothermal-spring.jpg||300px|thumb|right|The Blue Lagoon Geothermal Spa Close to Reykjavik, Iceland. From: [http://www.icelandviking.com/tourism/relaxation-holidays-iceland/]]] | [[Image:Blue-lagoon-iceland-geothermal-spring.jpg||300px|thumb|right|The Blue Lagoon Geothermal Spa Close to Reykjavik, Iceland. From: [http://www.icelandviking.com/tourism/relaxation-holidays-iceland/]]] | ||
The genome of ''Rhodothermus. marinus'' was found in a study by Canfield et al. that studied the cryptic sulfur cycle in oxygen-minimum zone (OMZ) waters off the Chilean coast. This biogeochemical cycling was dubbed cryptic because evidence of this cycling in the environment is hidden. Usually the reduction of sulfate through respiration of specialized microbes generates sulfide. As sulfate dissipates sulfide accumulates, indicating microbial sulfate reduction. In this case, the accumulation of sulfide is mediated by sulfide oxidizing bacteria instead of reducing bacteria. Because sulfide is so efficiently re-oxidized, it does not accumulate in the water column. This is important as it prevents sulfide toxicity. Nitrate is plays an important role in this process, too. Sulfide oxidation is limited by nitrate reducing in these OMZ waters, preventing sulfide toxicity seen in waters where marine sediments are rich in degradable biomass. This biomass fuels sulfate reduction, drastically increases sulfide production and overwhelms the nitrate pool. Nitrogen cycling is a complex process, and certain factors which may have an influence on this study such as microbial cycling of ammonia in the oxycline, microbial anaerobic ammonia oxidation, and novel mechanisms that microbes employ to cope with sulfide limitation, were neglected. To elucidate this further, Canfield et al. calls for long term seasonal studies. | |||
Canfield et al. | |||
''Rhodothermus. marinus'' is important to the environment because it decomposes organic matter, releasing carbon, nitrogen, phosphorus, sulfur and other important nutrients back into the environment. It is also biotechnologically important as it has many thermostable enzymes that are used in research. | ''Rhodothermus. marinus'' is important to the environment because it decomposes organic matter, releasing carbon, nitrogen, phosphorus, sulfur and other important nutrients back into the environment. It is also biotechnologically important as it has many thermostable enzymes that are used in research. | ||
Revision as of 19:56, 23 April 2012
Classification
Domain: Bacteria; Phylum: Bacteroidetes; Class: Bacteriodetes (Chlorobi group); Order: Incertae sedis; Family: Rhodothermaceae; Genus: Rhodothermus
Description and Significance
Rhodothermus. marinus form reddish-coloured, low convex colonies, 3-4 mm in diameter and with an entire edge. The bacteria also has Gram negative rods about 0.5 µm in diameter and 2-2.5 µm long.
Rhodothermus. marinus can be found in several similar but distantly located geothermal habitats. Many have large fluctuations in environmental conditions. Temperatures higher than 65 ̊C allow for optimum activity and growth. Shallow water hot springs of Iceland have been a place for studying samples of R. marinus. Rhodothermus. marinus has also been found in other regions of the world including Portugal, Italy and Monserrat Island in the Caribbean Sea.
Most thermophiles that have been studied in the past have been found in deep-sea hydrothermal vents in the Pacific Ocean. The study of R. marinus found in shallow-water hot springs in comparison to similar thermophiles found deep in the ocean can bring more understanding to these organisms’ ability to survive in extreme environments.
Genome Structure
Complete genome sequencing of Rhodothermus marinus (strain R-10=DSM4252=ATCC43812) is a part of the Genomic Encyclopedia of Bacteria and Archaea project. This is the first time to obtain the complete genome sequence of the genus Rhodothermus, and the second sequence from members of the family Rhodothermaceae. The whole genome (3,386,737 bp) includes one main circular chromosome and one circular plasmid. The GC content is 64.3%, and the DNA coding region is about 92.5%. The length of the plasmid is 125 kbp. There are 2,914 protein-coding and 48 RNA genes among the total 2,962 predicted genes. Only 71.6% (2,122) genes were identified with a putative function. However, the other genes are designated as hypothetical proteins. Moreover, there were 51 pseudogenes identified. The genome project is deposited in the Genomes Online Database, and the complete genome sequence in Genebank (Nolan et al).
Cell Structure, Metabolism and Life Cycle
Rhodothermus marinus cells are rod shaped and are 0.5 µm in diameter and 2-2.5 µm long. They are convex, reddish in color, and contain a slime capsule. They are aerobic and halophilic. They require a high concentration of sodium chloride to grow. The cells are catalase positive and oxidase negative (Nolan et al). According to Batista et al, R. marinus has a complex I structure, which consists of fourteen subunits. Seven are hydrophilic proteins located in the peripheral arm, the other 7 hydrophobic proteins in the membrane arm. There were many protein and peptide separation strategies. The combination of all of the methodologies allowed the identification of complex I canonical subunits, there was also a possible novel subunit, a PCD (pterin-4[alpha]-carbinolamine dehydratase). PCD possibly plays a regulatory role, though further research needs to be conducted.
R. marinus is in a group of bacteria that are important degraders of organic matter under aerobic conditions. This bacteria contains all three main groups of enzymes: endocellulase, exocellulase, and beta-glucosidase. Endocellulase and exocellulase degrade cellulose to oligosaccharides and cellobiose. Cellobiose is hydrolyzed to glucose monomers by beta-glucosidase. (Hreggvidsson et al). Most strains use several common sugars, such as glucose, galactose, lactose, maltose, raffinose, and sucrose. R. marinus JCM 9785 utilizes several amino acids while other strains are only reported to use aspartate, glutamate, asparagine, and glutamine.
Not much is known about the life cycle of R. marinus, further research needs to be conducted.
Ecology
Habitat
Rhodothermus. marinus was first isolated from submarine alkaline freshwater hot springs in Isafjardardjup, Iceland in 1988 and from other geothermal sites in Iceland including coastal springs from a borehole effluent in Oxarfjordur, Iceland, from borehole effluents from a powerplant at the Blue Lagoon, and from a salt factory in Reykjanes, Iceland. As well, it has been isolated from similar habitats in geothermal environments at various regions around the world, including Praia de Ribeira Quenta, Ferraria, Sa˜o Miguel in the Azores, Portugal, Stufe di Nerone near Naples, Italy, and on Monserrat island in the Carribean Sea. It should be noted that the populations of Rhodothermus marinus in these geographic locations are genetically distinct. High genetic diversity and low horizontal gene transfer indicate the populations at these geographically distinct sites are evolving independently and indicate that genetic drift and geographic isolation is an important mechanism in species divergence (Petursdottir et al).
Rhodothermus. marinus is a heterotrophic obligate aerobe that is thermophilic and slightly although strictly halophilic. The growth of this organism is dependent on a multitude of factors including temperature, salt and oxygen concentration, and the availability of organic material. Growth occurs at a temperature range of 54-77 degrees Celsius with optimal growth occurring at 65 degrees Celsius. Rhodotherms marinus has also been characterized at growing at NaCl concentrations optimally at 2% and not above 6%. This species only utilizes a single carbon source, with slight differences in carbon sources between strains. The physiology of this microbe dictates a narrow niche for it to occupy. Rhodothermus marinus can only grow close to the openings of hot springs where oxygen is readily available and close to the surface of the water where the temperatures are warm. Not much is known about any symbiotic relationships that Rhodothermus marinus might hold. Hopefully future ecological studies can shed light on such relationships.
The genome of Rhodothermus. marinus was found in a study by Canfield et al. that studied the cryptic sulfur cycle in oxygen-minimum zone (OMZ) waters off the Chilean coast. This biogeochemical cycling was dubbed cryptic because evidence of this cycling in the environment is hidden. Usually the reduction of sulfate through respiration of specialized microbes generates sulfide. As sulfate dissipates sulfide accumulates, indicating microbial sulfate reduction. In this case, the accumulation of sulfide is mediated by sulfide oxidizing bacteria instead of reducing bacteria. Because sulfide is so efficiently re-oxidized, it does not accumulate in the water column. This is important as it prevents sulfide toxicity. Nitrate is plays an important role in this process, too. Sulfide oxidation is limited by nitrate reducing in these OMZ waters, preventing sulfide toxicity seen in waters where marine sediments are rich in degradable biomass. This biomass fuels sulfate reduction, drastically increases sulfide production and overwhelms the nitrate pool. Nitrogen cycling is a complex process, and certain factors which may have an influence on this study such as microbial cycling of ammonia in the oxycline, microbial anaerobic ammonia oxidation, and novel mechanisms that microbes employ to cope with sulfide limitation, were neglected. To elucidate this further, Canfield et al. calls for long term seasonal studies.
Rhodothermus. marinus is important to the environment because it decomposes organic matter, releasing carbon, nitrogen, phosphorus, sulfur and other important nutrients back into the environment. It is also biotechnologically important as it has many thermostable enzymes that are used in research.
References
Author
Page authored by Cassandra Martin, Michelle Meng, Lauren Masek, and Robert Marks, students of Prof. Jay Lennon at Michigan State University.
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