Ferroplasma | |
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Ferroplasma acidiphilum | |
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Genus: | Ferroplasma Golyshina et al. 2000 |
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Ferroplasma acidiphila Golyshina et al. 2000 | |
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Ferroplasma is a genus of Archaea that belong to the family Ferroplasmaceae. Members of the Ferroplasma are typically acidophillic, pleomorphic, irregularly shaped cocci. [1] [2]
The archaean family Ferroplasmaceae was first described in the early 2000s. [3] To date very few species of Ferroplasma have been isolated and characterized. Isolated species include Ferroplasma acidiphilum, Ferroplasma acidarmanus, and Ferroplasma thermophilum. [1] [4] A fourth isolate Ferroplasma cupricumulans was later determined to belong to a separate genus. [5] [6] All known Ferroplasma sp. are iron-oxidizers.
Ferroplasma cells are pleomorphic and lack a cell-wall. [2] All known members of the genera are acidophiles that thrive in environments where pH ranges from 0.0 to 2.0. [1] [2] They are also mesophilic to moderately thermophilic with optimal temperatures ranging from 35-55 °C. [3]
Tetraether-based lipids are an important part of the Ferroplasma cellular membrane and allow cells to maintain a pH gradient. A study of F.acidarmanus found that cytoplasmic pH was maintained ~5.6 while the environmental pH ranged from ~0-1.2. [7] Variations in the tetraether lipids of the family Ferroplasmaceae are used for chemotaxonomic identification at the genus and species level because many members possess identical 16S rRNA sequences. [3]
Members of the genus Ferroplasma are chemomixotrophs that can oxidize ferrous iron to acquire energy, but despite evidence of carbon fixation, lab cultures often require an organic carbon source such as yeast extract for growth. [1] [3] In the absence of iron, some lab-grown strains have been capable of chemoorganotrophic growth. [1]
Iron is the fourth most abundant mineral in Earth's crust. As iron-oxidizers Ferroplasma sp. participate in the biogeochemical of iron. Ferroplasma sp. are often identified at acid mine drainage (AMD) sites. [3] When ferrous iron (Fe2+) is oxidized to ferric iron (Fe3+) at mine sites, Fe3+ spontaneously reacts with water and iron-sulfur compounds like pyrite to produce sulfate and hydrogen ions. [8] During this reaction ferrous iron, which can be utilized by Ferroplasma, is also regenerated leading to a "propagation cycle" where pH is lowered. The reaction can be described by the following equation:
Ferroplasma species are often present at AMD sites where they participate in this cycle through the biotic oxidation of ferrous iron. [8]
Ferroplasma sp. may have important applications for bioleaching metals. Microbial bioleaching occurs naturally in the highly acidic environments that are home to Ferroplasma sp. Harnessing the power of bioleaching to recover metal from low quality ores and waste material is energetically advantageous compared to smelting and purifying. [9] [10] It also produces fewer toxic byproducts. Studies have shown that the inclusion of Ferroplasma thermophilum along with the bacteria Acidithiobacillus caldus and Leptospirillum ferriphilum can bioaugment the leaching process of chalcopyrite and increase the rate at which copper is recovered. [11]
Ferroplasma acidiphilum has been shown to grow as a chemomixotroph and to grow synergistically with the acidophilic bacteria Leptospirillum ferriphilum. [12] The strain Ferroplasma acidiphilum YT is a facultative anaerobe with all the required genes for arginine fermentation. [13] Although it is unclear whether Ferroplasma acidiphilum YT uses its arginine fermentation pathway, the pathway itself is an ancient metabolism that traces back to the last universal common ancestor (LUCA) of the three domains of life. [13] [14]
Ferroplasma acidarmanus Fer1 was isolated from mine samples collected at Iron Mountain, California. [15] Iron Mountain (CA) is a former mine that is known for its acid mine drainage (AMD) and heavy metal contamination. In addition to being acidophilic, F. acidarmanus Fer1 is highly resistant to both copper and arsenic. [15] [16]
In 2006 Ferroplasma cupricumulans was isolated from leachate solution collected from the Myanmar Ivanhoe Copper company (MICCL) mining site in Myanmar. [5] It was noted to be the first slightly thermophilic member of the genus Ferroplasma. However, in 2009 a new genus of acidophilic, thermophilic archaea, Acidiplasma, was identified. It was proposed that, based on 16S rRNA similarity and DNA-DNA hybridization, be transferred to the genus Acidiplasma and renamed Acidiplasma cupricumulans. [6]
In 2008, Zhou, et al. described the isolation of the organism Ferroplasma thermophilum L1T from a chalcopyrite column reactor that was inoculated with acid mine drainage (AMD) from the Daye copper mine in China’s Hubei province. [4] In aerobic conditions with low concentrations of yeast extract F. thermophilum grows by oxidizing ferrous iron. [4] However, in anaerobic conditions F. thermophilum reduces ferric iron and sulfate. [4] This makes F. thermophilum ecologically important for iron and sulfur cycling at pyrite-rich mine sites.
Bioleaching is the extraction or liberation of metals from their ores through the use of living organisms. Bioleaching is one of several applications within biohydrometallurgy and several methods are used to treat ores or concentrates containing copper, zinc, lead, arsenic, antimony, nickel, molybdenum, gold, silver, and cobalt.
Acidithiobacillus is a genus of the Acidithiobacillia in the phylum "Pseudomonadota". This genus includes ten species of acidophilic microorganisms capable of sulfur and/or iron oxidation: Acidithiobacillus albertensis, Acidithiobacillus caldus, Acidithiobacillus cuprithermicus, Acidithiobacillus ferrianus, Acidithiobacillus ferridurans, Acidithiobacillus ferriphilus, Acidithiobacillus ferrivorans, Acidithiobacillus ferrooxidans, Acidithiobacillus sulfuriphilus, and Acidithiobacillus thiooxidans.A. ferooxidans is the most widely studied of the genus, but A. caldus and A. thiooxidans are also significant in research. Like all "Pseudomonadota", Acidithiobacillus spp. are Gram-negative and non-spore forming. They also play a significant role in the generation of acid mine drainage; a major global environmental challenge within the mining industry. Some species of Acidithiobacillus are utilized in bioleaching and biomining. A portion of the genes that support the survival of these bacteria in acidic environments are presumed to have been obtained by horizontal gene transfer.
In taxonomy, Picrophilus is an archaean genus of the family Picrophilaceae.
Geoglobus is a hyperthermophilic member of the Archaeoglobaceae within the Euryarchaeota. It consists of two species, the first, G. ahangari, isolated from the Guaymas Basin hydrothermal system located deep within the Gulf of California. As a hyperthermophile, it grows best at a temperature of 88 °C and cannot grow at temperatures below 65 °C or above 90 °C. It possess an S-layer cell wall and a single flagellum. G. ahangari is an anaerobe, using poorly soluble ferric iron (Fe3+) as a terminal electron acceptor. It can grow either autotrophically using hydrogen gas (H2) or heterotrophically using a large number of organic compounds, including several types of fatty acids, as energy sources. G. ahangari was the first archaeon isolated capable of using hydrogen gas coupled to iron reduction as an energy source and the first anaerobe isolated capable of using long-chain fatty acids as an energy source.
Biomining refers to any process that uses living organisms to extract metals from ores and other solid materials. Typically these processes involve prokaryotes, however fungi and plants may also be used. Biomining is one of several applications within biohydrometallurgy with applications in ore refinement, precious metal recovery, and bioremediation. The largest application currently being used is the treatment of mining waste containing iron, copper, zinc, and gold allowing for salvation of any discarded minerals. It may also be useful in maximizing the yields of increasingly low grade ore deposits. Biomining has been proposed as a relatively environmentally friendly alternative and/or supplementation to traditional mining. Current methods of biomining are modified leach mining processes. These aptly named bioleaching processes most commonly includes the inoculation of extracted rock with bacteria and acidic solution, with the leachate salvaged and processed for the metals of value. Biomining has many applications outside of metal recovery, most notably is bioremediation which has already been used to clean up coastlines after oil spills. There are also many promising future applications, like space biomining, fungal bioleaching and biomining with hybrid biomaterials.
In taxonomy, the Ferroplasmaceae are a family of the Thermoplasmatales.
Iron Mountain Mine, also known as the Richmond Mine at Iron Mountain, is a mine near Redding in Northern California, US. Geologically classified as a "massive sulfide ore deposit", the site was mined for iron, silver, gold, copper, zinc, quartz, and pyrite intermittently from the 1860s until 1963. The mine is the source of extremely acidic mine drainage which also contains large amounts of zinc, copper, and cadmium. One of America's most toxic waste sites, it has been listed as a federal Superfund site since 1983.
In taxonomy, Thermococcus is a genus of thermophilic Archaea in the family the Thermococcaceae.
The outflow of acidic liquids and other pollutants from mines is often catalysed by acid-loving microorganisms; these are the acidophiles in acid mine drainage.
Acidiplasma is a genus in the phylum Euryarchaeota (Archaea).
Nitrososphaera is a mesophilic genus of ammonia-oxidizing Crenarchaeota. The first Nitrososphaera organism was discovered in garden soils at the University of Vienna leading to the categorization of a new genus, family, order and class of Archaea. This genus is contains three distinct species: N. viennensis, Ca. N. gargensis, and Ca N. evergladensis. Nitrososphaera are chemolithoautotrophs and have important biogeochemical roles as nitrifying organisms.
Ferroplasma acidiphilum is an acidophilic, autotrophic, ferrous iron-oxidizing, cell wall-lacking, mesophilic member of the Ferroplasmaceae. F. acidophilum is a mesophile with a temperature optimum of approximately 35 °C, growing optimally at a pH of 1.7. F. acidophilum is generally found in acidic mine tailings, primarily those containing pyrite (FeS2). It is especially abundant in cases of severe acid mine drainage, where other organisms such as Acidithiobacillus and Leptospirillum lower the pH of the environment to the extent that F. acidophilum is allowed to flourish.
Leptospirillum ferriphilum is an iron-oxidising bacterium able to exist in environments of high acidity, high iron concentrations, and moderate to moderately high temperatures. It is one of the species responsible for the generation of acid mine drainage and the principal microbe used in industrial biohydrometallurgy processes to extract metals.
Sulfolobus metallicus is a coccoid shaped thermophilic archaeon. It is a strict chemolithoautotroph gaining energy by oxidation of sulphur and sulphidic ores into sulfuric acid. Its type strain is Kra 23. It has many uses that take advantage of its ability to grow on metal media under acidic and hot environments.
Acidithiobacillus caldus formerly belonged to the genus Thiobacillus prior to 2000, when it was reclassified along with a number of other bacterial species into one of three new genera that better categorize sulfur-oxidizing acidophiles. As a member of the Gammaproteobacteria class of Pseudomonadota, A. caldus may be identified as a Gram-negative bacterium that is frequently found in pairs. Considered to be one of the most common microbes involved in biomining, it is capable of oxidizing reduced inorganic sulfur compounds (RISCs) that form during the breakdown of sulfide minerals. The meaning of the prefix acidi- in the name Acidithiobacillus comes from the Latin word acidus, signifying that members of this genus love a sour, acidic environment. Thio is derived from the Greek word thios and describes the use of sulfur as an energy source, and bacillus describes the shape of these microorganisms, which are small rods. The species name, caldus, is derived from the Latin word for warm or hot, denoting this species' love of a warm environment.
Picrophilus torridus is a species of Archaea described in 1996. Picrophilus torridus was found in soil near a hot spring in Hokkaido, Japan. The pH of the soil was less than 0.5. P. torridus also has one of the smallest genomes found among organisms that are free-living and are non-parasitic and a high coding density, meaning that the majority of its genes are coding regions and provide instructions for building proteins. The current research suggests the two hostile conditions favored by P. torridus have exerted selective pressure towards having a small and compact genome, which is less likely to be damaged by the harsh environment.
Sulfolobus tokodaii is a thermophilic archaeon. It is acidophilic and obligately aerobic. The type strain is 7. Its genome has been sequenced.
Metallosphaera sedula is a species of Metallosphaera that is originally isolated from a volcanic field in Italy. Metallosphaera sedula can be roughly translated into “metal mobilizing sphere” with the word “sedulus” meaning busy, describing its efficiency in mobilizing metals. M. sedula is a highly thermoacidophilic Archaean that is unusually tolerant of heavy metals.
Ferrimicrobium acidiphilum is an extremely acidophilic and iron-oxidizing bacterium from the genus Ferrimicrobium which has been isolated from mine water from the Cae Coch sulfur mine in North Wales in England.
Acidithrix ferrooxidans is a heterotrophic, acidophilic and Gram-positive bacterium from the genus Acidithrix. The type strain of this species, A. ferrooxidans Py-F3, was isolated from an acidic stream draining from a copper mine in Wales. This species grows in a variety of acidic environments such as streams, mines or geothermal sites. Mine lakes with a redoxcline support growth with ferrous iron as the electron donor. "A. ferrooxidans" grows rapidly in macroscopic streamer, producing greater cell densities than other streamer-forming microbes. Use in a bioreactors to remediate mine waste has been proposed due to cell densities and rapid oxidation of ferrous iron oxidation in acidic mine drainage. Exopolysaccharide production during metal substrate metabolism, such as iron oxidation helps to prevent cell encrustation by minerals.