Gammaproteobacteria

Last updated

Gammaproteobacteria
Vibrio cholerae.jpg
Vibrio cholerae
Scientific classification OOjs UI icon edit-ltr.svg
Domain: Bacteria
Phylum: Pseudomonadota
Class: Gammaproteobacteria
Garrity et al. 2005
Orders
Synonyms
  • "Chromatiia" Cavalier-Smith 2020

Gammaproteobacteria is a class of bacteria in the phylum Pseudomonadota (synonym Proteobacteria). It contains about 250 genera, which makes it the most genus-rich taxon of the Prokaryotes. [1] Several medically, ecologically, and scientifically important groups of bacteria belong to this class. All members of this class are Gram-negative. It is the most phylogenetically and physiologically diverse class of the Pseudomonadota. [2]

Contents

Members of Gammaproteobacteria live in several terrestrial and marine environments, in which they play various important roles, including in extreme environments such as hydrothermal vents. They can have different shapes, rods, curved rods, cocci, spirilla, and filaments, [3] and include free living bacteria, biofilm formers, commensals and symbionts; [4] some also have the distinctive trait of being bioluminescent. [5] Diverse metabolisms are found in Gammaproteobacteria; there are both aerobic and anaerobic (obligate or facultative) species, chemolithoautotrophics, chemoorganotrophics, photoautotrophs and heterotrophs. [6]

Etymology

The element "gamma" (third letter of the Greek alphabet) indicates that this is Class III in Bergey's Manual of Systematic Bacteriology (Vol. II, page 1). Proteus refers to the Greek sea god who could change his shape. Bacteria (Greek βακτήριον; "rod" "little stick"), in terms of etymological history, refers to Bacillus (rod-shaped bacteria), but in this case is "useful in the interim while the phylogenetic data are being integrated into formal bacterial taxonomy." [7]

Phylogeny

Currently, many different classifications are based on different approaches, such as the National Center for Biotechnology Information, based on genomic, List of Prokaryotic names with Standing in Nomenclature , ARB-Silva Database [8] based on ribosomal RNA, or a multiprotein approach. It is still very difficult to resolve the phylogeny of this bacterial class. [9]

The following molecular phylogeny of Gammaproteobacteria is based on a set of 356 protein families.

Phylogeny of Gammaproteobacteria

Betaproteobacteria

Gammaproteobacteria

Xanthomonadales

Chromatiales

Methylococcus

Beggiatoa

Legionellales

Ruthia ,  Vesicomyosocius ,  Thiomicrospira ,  Dichelobacter ,  Francisella

Moraxellaceae,  Alcanivorax

Saccharophagus

Oceanospirillaceae

Marinobacter

Pseudomonadaceae

Pseudoalteromonadaceae,  Alteromonas ,  Idiomarinaceae

Shewanellaceae

Psychromonadaceae

Aeromonadales

Vibrionales

Pasteurellales

Enterobacterales

Phylogeny of Gammaproteobacteria after [10] Not all orders are monophyletic, consequently families or genera are shown for the Pseudomonadales, Oceanospirillales, and Alteromonadales. In the case of singleton orders, the genus is shown. (In bacterial taxonomy, orders have the suffix -ales, while families have -aceae.)

A number of genera in Gammaproteobacteria have not yet been assigned to an order or family. These include Alkalimonas , Gallaecimonas , Ignatzschineria , Litorivivens , Marinicella , Plasticicumulans , Pseudohongiella , Sedimenticola , Thiohalobacter , Thiohalorhabdus , Thiolapillus , and Wohlfahrtiimonas . [11]

Significance and applications

Gammaproteobacteria, especially the orders Alteromonadales and Vibrionales, are fundamental in marine and coastal ecosystems because they are the major groups involved in nutrient cycling. [12] Despite their fame as pathogens, they find application in a huge number of fields, such as bioremediation and biosynthesis.

Gammaproteobacteria can be used as a microbial fuel cell (MFC) [13] element that applies their ability to dissimilate various metals. [14] The produced energy could be collected as one of the most environmentally friendly and sustainable energy production systems. [15] They are also used as biological methane filters. [16]

Phototrophic purple sulfur bacteria are used in wastewater treatment processes. [17] The ability of some Gammaproteobacteria (e.g. the genus Alcanivorax [18] ) to bioremediate oil is increasingly important for degrading crude oil after oil spills. [19] Some species from the family Chromatiaceae are notable because they may be involved in the production of vitamin B12. [20] Some Gammaproteobacteria are used to synthesize poly-b-hydroxyalkanoate (PHA), [21] which is a polymer that is used in the production of biodegradable plastics. Many Gammaproteobacteria species are able to generate secondary metabolites with antibacterial properties. [22]

Ecology

Gammaproteobacteria are widely distributed and abundant in various ecosystems such as soil, freshwater lakes and rivers, oceans and salt lakes. For example, they constitute about 6–20% (average of 14%) of bacterioplankton in different oceans, [23] and they are distributed world-wide in both deep-sea and coastal sediments. [24] In seawater, bacterial community composition could be shaped by environmental parameters such as phosphorus availability, total organic carbon, salinity, and pH. [25] In soil, higher pH is correlated with higher relative abundance of Alphaproteobacteria , Betaproteobacteria and Gammaproteobacteria. [26] The relative abundance of Betaproteobacteria and Gammaproteobacteria is also positively correlated to the dissolved organic carbon (DOC) concentration, which is a key environmental parameter shaping bacterial community composition. [27] Gammaproteobacteria are also key players in the dark carbon fixation in coastal sediments, which are the largest carbon sink on Earth, and the majority of these bacteria have not been cultured yet. [28] The deep-sea hydrothermal system is one of the most extreme environments on Earth. Almost all vent-endemic animals are strongly associated with the primary production of the endo- and/or episymbiotic chemoautotrophic microorganisms. [29] Analyses of both the symbiotic and free-living microbial communities in the various deep-sea hydrothermal environments have revealed a predominance in biomass of members of the Gammaproteobacteria. [30]

Gammaproteobacteria have a wide diversity, metabolic versatility, and functional redundancy in the hydrothermal sediments, and they are responsible for the important organic carbon turnover and nitrogen and sulfur cycling processes. [31] Anoxic hydrothermal fluids contain several reduced compounds such as H2, CH4, and reduced metal ions in addition to H2S. Chemoautotrophs that oxidize hydrogen sulfide and reduce oxygen potentially sustain the primary production in these unique ecosystems. [32] In the last decades, it has been found that orders belonging to Gammaproteobacteria, like Pseudomonas,  Moraxella , are able to degrade different types of plastics and these microbes might have a key role in plastic biodegradation. [33]

Metabolism

Gammaproteobacteria are metabolically diverse, employing a variety of electron donors for respiration and biosynthesis.

Some groups are nitrite-oxidizers [34] and ammonia oxidizers like the members of Nitrosococcus (with the exception of Nitrosococcus mobilis) and they are also obligate halophilic bacteria. [35]

Others are chemoautotrophic sulfur-oxidizers, like  Thiotrichales , which are found in communities such as filamentous microbial biofilms in the Tor Caldara shallow-water gas vent in the Tyrrhenian Sea . [36] Moreover, thanks to 16S rRNA gene analysis, different sulfide oxidizers in the Gammaporteobacteria class have been detected, and the most important among them are Beggiatoa , Thioploca and Thiomargarita ; besides, large amounts of hydrogen sulfide are produced by sulfate-reducing bacteria in organic-rich coastal sediments. [37]

Marine Gammaproteobacteria include aerobic anoxygenic phototrophic bacteria (AAP) that use bacteriochlorophyll to support the electron transport chain. They are believed to be a widespread and essential community in the oceans. [38]

Methanotrophs, such as the order  Methylococcales, metabolize methane as sole energy source and are very important in the global carbon cycle. They are found in any site with methane sources, like gas reserves, soils, and wastewater. [39]

Purple sulfur bacteria are anoxygenic phototrophs that oxidize sulfur, [40] but potentially also other substrates like iron. [41] They are represented by members of two families, Chromatiaceae (e.g. Allochromatium , Chromatium , Thiodicyton ) and Ectothiorhodospiraceae (e.g. Ectothiorhodospira). [40] A few species within the genus Thermomonas (order Lysobacter) carry out the same metabolism. [42]

Numerous genera are obligate or generalist hydrocarbonclasts. The obligate hydrocarbonoclastic bacteria (OHCB) use hydrocarbons almost exclusively as a carbon source; until now they have been found only in the marine environment. Examples include Alcanivorax , Oleiphilus , Oleispira , Thalassolitus, Cycloclasticus and Neptunomonas, and some species of Polycyclovorans , Algiphilus (order Xanthomonadales ), and Porticoccus hydrocarbonoclasticus (order Cellvibrionales ) that were isolated from phytoplankton. In contrast, aerobic “generalist” hydrocarbon degraders can use either hydrocarbons or nonhydrocarbon substrates as sources of carbon and energy; examples are found in the genera Acinetobacter , Colwellia , Glaciecola , Halomonas , Marinobacter , Marinomonas , Methylomonas , Pseudoalteromonas , Pseudomonas , Rhodanobacter , Shewanella , Stenotrophomonas , and Vibrio . [43]

The most widespread pathway for carbon fixation among Gammaproteobacteria is the Calvin–Benson–Bassham (CBB) cycle, although a minority may use the rTCA cycle. [44] Thioflavicoccus mobilis (a free living species) and "Candidatus Endoriftia persephone" (symbiont of the giant tubeworm Riftia pachyptila ) may use the rTCA cycle in addition to the CBB cycle, and may express these two different pathways simultaneously. [45]

Symbiosis

Symbiosis is a close and a long-term biological interaction between two different biological organisms. A large number of Gammaproteobacteria are able to join in a close endosymbiosis with various species. Evidence for this can be found in a wide variety of ecological niches: on the ground, [46] [47] within plants, [48] or deep on the ocean floor. [49] On the land, it has been reported that Gammaproteobacteria species have been isolated from Robinia pseudoacacia [50] and other plants, [51] [52] while in the deep sea a sulfur-oxidizing gammaproteobacteria was found in a hydrothermal vent chimney; [53] by entering into symbiotic relationships in deep sea areas, sulfur-oxidizing chemolithotrophic microbes receive additional organic hydrocarbons in hydrothermal ecosystems. Some Gammaproteobacteria are symbiotic with geothermic ocean vent-downwelling animals, [54] and in addition, Gammaproteobacteria can have complex relationships with other species that live around thermal springs, [55] for example, with the shrimp Rimicaris exoculata living from hydrothermal vents on the Mid-Atlantic Ridge.

Regarding the endosymbionts, most of them lack many of their family characteristics due to significant genome reduction. [56] [57]

Pathogens

Gammaproteobacteria include several medically and scientifically important groups of bacteria, such as the families Enterobacteriaceae , Vibrionaceae , and Pseudomonadaceae . A number of human pathogens belong to this class, including Yersinia pestis , Vibrio cholerae , Pseudomonas aeruginosa , Escherichia coli , and some species of Salmonella . The class also contains plant pathogens such as Xanthomonas axonopodis pv. citri (citrus canker), Pseudomonas syringae pv. actinidiae (kiwifruit Psa outbreak), and Xylella fastidiosa. In the marine environment, several species from this class can infect different marine organisms, such as species in the genus Vibrio which affect fish, shrimp, corals or oysters, [58] and species of Salmonella which affect grey seals (Halichoerus grypus). [59] [60]

See also

Related Research Articles

<span class="mw-page-title-main">Chemosynthesis</span> Biological process building organic matter using inorganic compounds as the energy source

In biochemistry, chemosynthesis is the biological conversion of one or more carbon-containing molecules and nutrients into organic matter using the oxidation of inorganic compounds or ferrous ions as a source of energy, rather than sunlight, as in photosynthesis. Chemoautotrophs, organisms that obtain carbon from carbon dioxide through chemosynthesis, are phylogenetically diverse. Groups that include conspicuous or biogeochemically important taxa include the sulfur-oxidizing Gammaproteobacteria, the Campylobacterota, the Aquificota, the methanogenic archaea, and the neutrophilic iron-oxidizing bacteria.

<i>Riftia</i> Giant tube worm (species of annelid)

Riftia pachyptila, commonly known as the giant tube worm and less commonly known as the giant beardworm, is a marine invertebrate in the phylum Annelida related to tube worms commonly found in the intertidal and pelagic zones. R. pachyptila lives on the floor of the Pacific Ocean near hydrothermal vents. The vents provide a natural ambient temperature in their environment ranging from 2 to 30 °C, and this organism can tolerate extremely high hydrogen sulfide levels. These worms can reach a length of 3 m, and their tubular bodies have a diameter of 4 cm (1.6 in).

<span class="mw-page-title-main">Sulfur-reducing bacteria</span> Microorganisms able to reduce elemental sulfur to hydrogen sulfide

Sulfur-reducing bacteria are microorganisms able to reduce elemental sulfur (S0) to hydrogen sulfide (H2S). These microbes use inorganic sulfur compounds as electron acceptors to sustain several activities such as respiration, conserving energy and growth, in absence of oxygen. The final product of these processes, sulfide, has a considerable influence on the chemistry of the environment and, in addition, is used as electron donor for a large variety of microbial metabolisms. Several types of bacteria and many non-methanogenic archaea can reduce sulfur. Microbial sulfur reduction was already shown in early studies, which highlighted the first proof of S0 reduction in a vibrioid bacterium from mud, with sulfur as electron acceptor and H
2
as electron donor. The first pure cultured species of sulfur-reducing bacteria, Desulfuromonas acetoxidans, was discovered in 1976 and described by Pfennig Norbert and Biebel Hanno as an anaerobic sulfur-reducing and acetate-oxidizing bacterium, not able to reduce sulfate. Only few taxa are true sulfur-reducing bacteria, using sulfur reduction as the only or main catabolic reaction. Normally, they couple this reaction with the oxidation of acetate, succinate or other organic compounds. In general, sulfate-reducing bacteria are able to use both sulfate and elemental sulfur as electron acceptors. Thanks to its abundancy and thermodynamic stability, sulfate is the most studied electron acceptor for anaerobic respiration that involves sulfur compounds. Elemental sulfur, however, is very abundant and important, especially in deep-sea hydrothermal vents, hot springs and other extreme environments, making its isolation more difficult. Some bacteria – such as Proteus, Campylobacter, Pseudomonas and Salmonella – have the ability to reduce sulfur, but can also use oxygen and other terminal electron acceptors.

<span class="mw-page-title-main">Iron-oxidizing bacteria</span> Bacteria deriving energy from dissolved iron

Iron-oxidizing bacteria are chemotrophic bacteria that derive energy by oxidizing dissolved iron. They are known to grow and proliferate in waters containing iron concentrations as low as 0.1 mg/L. However, at least 0.3 ppm of dissolved oxygen is needed to carry out the oxidation.

<i>Beggiatoa</i> Genus of bacteria

Beggiatoa is a genus of Gammaproteobacteria belonging to the order Thiotrichales, in the Pseudomonadota phylum. These bacteria form colorless filaments composed of cells that can be up to 200 µm in diameter, and are one of the largest prokaryotes on Earth. Beggiatoa are chemolithotrophic sulfur-oxidizers, using reduced sulfur species as an energy source. They live in sulfur-rich environments such as soil, both marine and freshwater, in the deep sea hydrothermal vents, and in polluted marine environments. In association with other sulfur bacteria, e.g. Thiothrix, they can form biofilms that are visible to the naked eye as mats of long white filaments; the white color is due to sulfur globules stored inside the cells.

<span class="mw-page-title-main">Campylobacterota</span> Class of bacteria

Campylobacterota are a phylum of Gram-negative bacteria. Only a few genera have been characterized, including the curved to spirilloid Wolinella, Helicobacter, and Campylobacter. Until the 2021 revision of bacterial taxonomy by the ICSP, the entire phylum was classified within the Proteobacteria as the Epsilonproteobacteria.

Thiothrix is a genus of filamentous sulfur-oxidizing bacteria, related to the genera Beggiatoa and Thioploca. They are usually Gram-negative and rod-shaped. They form ensheathed multicellular filaments that are attached at the base, and form gonidia at their free end. The apical gonidia have gliding motility. Rosettes of the filaments are not always formed but are typical. Sulfur is deposited in invaginations within the cell membrane.

Sulfur is metabolized by all organisms, from bacteria and archaea to plants and animals. Sulfur can have an oxidation state from -2 to +6 and is reduced or oxidized by a diverse range of organisms. The element is present in proteins, sulfate esters of polysaccharides, steroids, phenols, and sulfur-containing coenzymes.

The genus Methylophaga consists of halophilic methylotrophic members of the Gammaproteobacteria, all of which were isolated from marine or otherwise low water activity environments, such as the surface of marble or hypersaline lakes. The cells are rod-shaped. and are motile by a single polar flagellum.

<span class="mw-page-title-main">Bacterial phyla</span> Phyla or divisions of the domain Bacteria

Bacterial phyla constitute the major lineages of the domain Bacteria. While the exact definition of a bacterial phylum is debated, a popular definition is that a bacterial phylum is a monophyletic lineage of bacteria whose 16S rRNA genes share a pairwise sequence identity of ~75% or less with those of the members of other bacterial phyla.

<span class="mw-page-title-main">Zetaproteobacteria</span> Class of bacteria

The class Zetaproteobacteria is the sixth and most recently described class of the Pseudomonadota. Zetaproteobacteria can also refer to the group of organisms assigned to this class. The Zetaproteobacteria were originally represented by a single described species, Mariprofundus ferrooxydans, which is an iron-oxidizing neutrophilic chemolithoautotroph originally isolated from Kamaʻehuakanaloa Seamount in 1996 (post-eruption). Molecular cloning techniques focusing on the small subunit ribosomal RNA gene have also been used to identify a more diverse majority of the Zetaproteobacteria that have as yet been unculturable.

Solemya velum, the Atlantic awning clam, is a species of marine bivalve mollusc in the family Solemyidae, the awning clams. This species is found along the eastern coast of North America, from Nova Scotia to Florida and inhabits subtidal sediments with high organic matter (OM) content and low Oxygen, such as salt ponds, salt marshes, and sewage outfalls.

<i>Olavius algarvensis</i> Species of annelid worm

Olavius algarvensis is a species of gutless oligochaete worm in the family Tubificidae which depends on symbiotic bacteria for its nutrition.

Sulfurimonas is a bacterial genus within the class of Campylobacterota, known for reducing nitrate, oxidizing both sulfur and hydrogen, and containing Group IV hydrogenases. This genus consists of four species: Sulfurimonas autorophica, Sulfurimonas denitrificans, Sulfurimonas gotlandica, and Sulfurimonas paralvinellae. The genus' name is derived from "sulfur" in Latin and "monas" from Greek, together meaning a “sulfur-oxidizing rod”. The size of the bacteria varies between about 1.5-2.5 μm in length and 0.5-1.0 μm in width. Members of the genus Sulfurimonas are found in a variety of different environments which include deep sea-vents, marine sediments, and terrestrial habitats. Their ability to survive in extreme conditions is attributed to multiple copies of one enzyme. Phylogenetic analysis suggests that members of the genus Sulfurimonas have limited dispersal ability and its speciation was affected by geographical isolation rather than hydrothermal composition. Deep ocean currents affect the dispersal of Sulfurimonas spp., influencing its speciation. As shown in the MLSA report of deep-sea hydrothermal vents Campylobacterota, Sulfurimonas has a higher dispersal capability compared with deep sea hydrothermal vent thermophiles, indicating allopatric speciation.

<span class="mw-page-title-main">Marine microbial symbiosis</span>

Microbial symbiosis in marine animals was not discovered until 1981. In the time following, symbiotic relationships between marine invertebrates and chemoautotrophic bacteria have been found in a variety of ecosystems, ranging from shallow coastal waters to deep-sea hydrothermal vents. Symbiosis is a way for marine organisms to find creative ways to survive in a very dynamic environment. They are different in relation to how dependent the organisms are on each other or how they are associated. It is also considered a selective force behind evolution in some scientific aspects. The symbiotic relationships of organisms has the ability to change behavior, morphology and metabolic pathways. With increased recognition and research, new terminology also arises, such as holobiont, which the relationship between a host and its symbionts as one grouping. Many scientists will look at the hologenome, which is the combined genetic information of the host and its symbionts. These terms are more commonly used to describe microbial symbionts.

<span class="mw-page-title-main">Microbial oxidation of sulfur</span>

Microbial oxidation of sulfur is the oxidation of sulfur by microorganisms to build their structural components. The oxidation of inorganic compounds is the strategy primarily used by chemolithotrophic microorganisms to obtain energy to survive, grow and reproduce. Some inorganic forms of reduced sulfur, mainly sulfide (H2S/HS) and elemental sulfur (S0), can be oxidized by chemolithotrophic sulfur-oxidizing prokaryotes, usually coupled to the reduction of oxygen (O2) or nitrate (NO3). Anaerobic sulfur oxidizers include photolithoautotrophs that obtain their energy from sunlight, hydrogen from sulfide, and carbon from carbon dioxide (CO2).

<span class="mw-page-title-main">Hydrothermal vent microbial communities</span> Undersea unicellular organisms

The hydrothermal vent microbial community includes all unicellular organisms that live and reproduce in a chemically distinct area around hydrothermal vents. These include organisms in the microbial mat, free floating cells, or bacteria in an endosymbiotic relationship with animals. Chemolithoautotrophic bacteria derive nutrients and energy from the geological activity at Hydrothermal vents to fix carbon into organic forms. Viruses are also a part of the hydrothermal vent microbial community and their influence on the microbial ecology in these ecosystems is a burgeoning field of research.

<span class="mw-page-title-main">Marine microbiome</span>

All animals on Earth form associations with microorganisms, including protists, bacteria, archaea, fungi, and viruses. In the ocean, animal–microbial relationships were historically explored in single host–symbiont systems. However, new explorations into the diversity of marine microorganisms associating with diverse marine animal hosts is moving the field into studies that address interactions between the animal host and a more multi-member microbiome. The potential for microbiomes to influence the health, physiology, behavior, and ecology of marine animals could alter current understandings of how marine animals adapt to change, and especially the growing climate-related and anthropogenic-induced changes already impacting the ocean environment.

<span class="mw-page-title-main">Marine prokaryotes</span> Marine bacteria and marine archaea

Marine prokaryotes are marine bacteria and marine archaea. They are defined by their habitat as prokaryotes that live in marine environments, that is, in the saltwater of seas or oceans or the brackish water of coastal estuaries. All cellular life forms can be divided into prokaryotes and eukaryotes. Eukaryotes are organisms whose cells have a nucleus enclosed within membranes, whereas prokaryotes are the organisms that do not have a nucleus enclosed within a membrane. The three-domain system of classifying life adds another division: the prokaryotes are divided into two domains of life, the microscopic bacteria and the microscopic archaea, while everything else, the eukaryotes, become the third domain.

Ann Patricia Wood is a retired British biochemist and bacteriologist who specialized in the ecology, taxonomy and physiology of sulfur-oxidizing chemolithoautotrophic bacteria and how methylotrophic bacteria play a role in the degradation of odour causing compounds in the human mouth, vagina and skin. The bacterial genus Annwoodia was named to honor her contributions to microbial research in 2017.

References

  1. Garrity GM, Bell JA, Lilburn TG. (2005). Class III. Gammaproteobacteria class. nov. In: Brenner DJ, Krieg NR, Staley JT, Garrity GM (eds) Bergey's Manual of Systematic Bacteriology 2nd edn, vol. 2 Springer: New York, p 1
  2. T. Gutierrez – 2019 - Institute of Mechanical, Process and Energy Engineering, School of Engineering and Physical Sciences, Heriot-Watt University, Edinburgh, UK
  3. Schulz HN, Brinkhoff T, Ferdelman TG, Mariné MH, Teske A, Jorgensen BB (April 1999). "Dense populations of a giant sulfur bacterium in Namibian shelf sediments". Science. 284 (5413): 493–5. Bibcode:1999Sci...284..493S. doi:10.1126/science.284.5413.493. PMID   10205058.
  4. Williams KP, Gillespie JJ, Sobral BW, Nordberg EK, Snyder EE, Shallom JM, Dickerman AW (May 2010). "Phylogeny of gammaproteobacteria". Journal of Bacteriology. 192 (9): 2305–14. doi:10.1128/JB.01480-09. PMC   2863478 . PMID   20207755.
  5. Munn CB (2019-11-26). Marine Microbiology: Ecology & Applications. CRC Press. ISBN   978-0-429-59236-2.
  6. "Proteobacteria | Microbiology".
  7. Stackebrandt, E.; Murray, R. G. E.; Truper, H. G. (1988). "Proteobacteria classis nov., a Name for the Phylogenetic Taxon That Includes the "Purple Bacteria and Their Relatives"". International Journal of Systematic Bacteriology. 38 (3): 321–325. doi: 10.1099/00207713-38-3-321 . ISSN   0020-7713.
  8. "Silva". www.arb-silva.de. Retrieved 2020-11-22.
  9. Williams KP, Gillespie JJ, Sobral BW, Nordberg EK, Snyder EE, Shallom JM, Dickerman AW (May 2010). "Phylogeny of gammaproteobacteria". Journal of Bacteriology. 192 (9): 2305–14. doi:10.1128/JB.01480-09. PMC   2863478 . PMID   20207755.
  10. Williams KP, Gillespie JJ, Sobral BW, Nordberg EK, Snyder EE, Shallom JM, Dickerman AW (May 2010). "Phylogeny of gammaproteobacteria". Journal of Bacteriology. 192 (9): 2305–14. doi:10.1128/JB.01480-09. PMC   2863478 . PMID   20207755.
  11. "Classification of domains and phyla - Hierarchical classification of prokaryotes (bacteria) - Gammaproteobacteria". List of Prokaryotic Names with Standing in Nomenclature. Retrieved 13 January 2017.
  12. Evans FF, Egan S, Kjelleberg S (May 2008). "Ecology of type II secretion in marine gammaproteobacteria". Environmental Microbiology. 10 (5): 1101–7. doi: 10.1111/j.1462-2920.2007.01545.x . PMID   18218035.
  13. Qian F, Morse DE (February 2011). "Miniaturizing microbial fuel cells". Trends in Biotechnology. 29 (2): 62–9. doi:10.1016/j.tibtech.2010.10.003. PMID   21075467.
  14. Gorby YA, Yanina S, McLean JS, Rosso KM, Moyles D, Dohnalkova A, et al. (July 2006). "Electrically conductive bacterial nanowires produced by Shewanella oneidensis strain MR-1 and other microorganisms". Proceedings of the National Academy of Sciences of the United States of America. 103 (30): 11358–63. Bibcode:2006PNAS..10311358G. doi: 10.1073/pnas.0604517103 . PMC   1544091 . PMID   16849424.
  15. Hau HH, Gralnick JA (September 2007). "Ecology and biotechnology of the genus Shewanella". Annual Review of Microbiology. 61 (1): 237–58. doi:10.1146/annurev.micro.61.080706.093257. PMID   18035608.
  16. Rosenberg E, DeLong EF, Lory EF, Stackebrandt E, Erko T, Thompson F, eds. (2014). The Prokaryotes: Gammaproteobacteria (4th ed.). Berlin Heidelberg: Springer-Verlag. p. 434. ISBN   978-3-642-38921-4.
  17. Kobayashi M, Michiharu T, Tchan YT (1973-08-01). "Treatment of industrial waste solutions and production of useful by-products using a photosynthetic bacterial method". Water Research. 7 (8): 1219–1224. doi:10.1016/0043-1354(73)90075-4. ISSN   0043-1354.
  18. Harayama S, Kishira H, Kasai Y, Shutsubo K (August 1999). "Petroleum biodegradation in marine environments". Journal of Molecular Microbiology and Biotechnology. 1 (1): 63–70. PMID   10941786.
  19. Kasai Y, Kishira H, Syutsubo K, Harayama S (April 2001). "Molecular detection of marine bacterial populations on beaches contaminated by the Nakhodka tanker oil-spill accident". Environmental Microbiology. 3 (4): 246–55. doi:10.1046/j.1462-2920.2001.00185.x. PMID   11359510.
  20. Koppenhagen VB, Schlingmann G, Schaer W, Dresow. Moo-young M, Vezina C, Singh K (eds.). "Extracellular metabolites from phototrophic bacteria as possible intermediates in the biosynthesis of vitamin B12". Fermentation Products. Pergamon: 247–252. ISBN   978-0-08-025385-5.
  21. de la Haba RR, Sánchez-Porro C, Márquez MC, Ventosa A (April 2010). "Taxonomic study of the genus Salinicola: transfer of Halomonas salaria and Chromohalobacter salarius to the genus Salinicola as Salinicola salarius comb. nov. and Salinicola halophilus nom. nov., respectively". International Journal of Systematic and Evolutionary Microbiology. 60 (Pt 4): 963–971. doi:10.1099/ijs.0.014480-0. PMID   19661506.
  22. "Marine bacteria associated with marine macroorganisms: The potential antimicrobial resources - AMiner". www.aminer.org. Retrieved 2020-11-20.
  23. Broszat M, Nacke H, Blasi R, Siebe C, Huebner J, Daniel R, Grohmann E. 2014. Wastewater irrigation increases the abundance of potentially harmful Gammaproteobacteria in soils in Mezquital Valley, Mexico. Appl Environ Microbiol.
  24. Bienhold C, Zinger L, Boetius A, Ramette A (2016-01-27). "Diversity and Biogeography of Bathyal and Abyssal Seafloor Bacteria". PLOS ONE. 11 (1): e0148016. Bibcode:2016PLoSO..1148016B. doi: 10.1371/journal.pone.0148016 . PMC   4731391 . PMID   26814838.
  25. Jiang H, Dong H, Ji S, Ye Y, Wu N (2007-09-26). "Microbial Diversity in the Deep Marine Sediments from the Qiongdongnan Basin in South China Sea". Geomicrobiology Journal. 24 (6): 505–517. doi:10.1080/01490450701572473. S2CID   130552094.
  26. Rousk J, Bååth E, Brookes PC, Lauber CL, Lozupone C, Caporaso JG, Knight R, Fierer N (October 2010). "Soil bacterial and fungal communities across a pH gradient in an arable soil". The ISME Journal. 4 (10): 1340–51. doi: 10.1038/ismej.2010.58 . PMID   20445636. S2CID   205156612.
  27. Li D, Sharp JO, Saikaly PE, Ali S, Alidina M, Alarawi MS, Keller S, Hoppe-Jones C, Drewes JE (October 2012). "Dissolved organic carbon influences microbial community composition and diversity in managed aquifer recharge systems". Applied and Environmental Microbiology. 78 (19): 6819–28. Bibcode:2012ApEnM..78.6819L. doi:10.1128/AEM.01223-12. PMC   3457517 . PMID   22798375.
  28. Hedges JI, Keil RG (April 1995). "Sedimentary organic matter preservation: an assessment and speculative synthesis". Marine Chemistry. 49 (2–3): 81–115. doi:10.1016/0304-4203(95)00008-F.
  29. Jeanthon C (February 2000). "Molecular ecology of hydrothermal vent microbial communities". Antonie van Leeuwenhoek. 77 (2): 117–33. doi:10.1023/a:1002463825025. PMID   10768471. S2CID   24324674.
  30. Stewart FJ, Newton IL, Cavanaugh CM (September 2005). "Chemosynthetic endosymbioses: adaptations to oxic-anoxic interfaces". Trends in Microbiology. 13 (9): 439–48. doi:10.1016/j.tim.2005.07.007. PMID   16054816.
  31. Baker BJ, Lazar CS, Teske AP, Dick GJ (2015). "Genomic resolution of linkages in carbon, nitrogen, and sulfur cycling among widespread estuary sediment bacteria". Microbiome. 3: 14. doi: 10.1186/s40168-015-0077-6 . PMC   4411801 . PMID   25922666.
  32. Jannasch,H.W.,andMottl,M.J. (1985). Geomicrobiologyofdeep- sea hydrothermalvents. Science 229, 717–725
  33. soixanteseize (2015-01-06). "Explore to understand, share to bring about change". Fondation Tara Océan. Retrieved 2020-11-22.
  34. Han S, Li X, Luo X, Wen S, Chen W, Huang Q (2018). "Nitrite-Oxidizing Bacteria Community Composition and Diversity Are Influenced by Fertilizer Regimes, but Are Independent of the Soil Aggregate in Acidic Subtropical Red Soil". Frontiers in Microbiology. 9: 885. doi: 10.3389/fmicb.2018.00885 . PMC   5951965 . PMID   29867799.
  35. Cesar Mota, Jennifer Ridenoure, Jiayang Cheng, Francis L. de los Reyes, High levels of nitrifying bacteria in intermittently aerated reactors treating high ammonia wastewater. FEMS Microbiology Ecology, Volume 54, Issue 3, November 2005, pp. 391–400
  36. Patwardhan S, Foustoukos DI, Giovannelli D, Yücel M, Vetriani C (2018). "Gammaproteobacteria During Colonization of a Shallow-Water Gas Vent". Frontiers in Microbiology. 9: 2970. doi: 10.3389/fmicb.2018.02970 . PMC   6291522 . PMID   30574130.
  37. Sabine Lenk, Julia Arnds, Katrice Zerjatke, Niculina Musat, Rudolf Amann and Marc Mußmann* Max Planck Institute for Marine Microbiology, Celsiusstraße 1, 28359 Bremen, Germany. Novel groups of Gammaproteobacteria catalyse sulfur oxidation and carbon fixation in a coastal, intertidal sediment. (2011)
  38. Cho JC, Stapels MD, Morris RM, Vergin KL, Schwalbach MS, Givan SA, et al. (June 2007). "Polyphyletic photosynthetic reaction centre genes in oligotrophic marine Gammaproteobacteria". Environmental Microbiology. 9 (6): 1456–63. doi:10.1111/j.1462-2920.2007.01264.x. PMID   17504483.
  39. Orata FD, Meier-Kolthoff JP, Sauvageau D, Stein LY (2018). "Methylococcales) Calls for the Reclassification of Members at the Genus and Species Levels". Frontiers in Microbiology. 9: 3162. doi: 10.3389/fmicb.2018.03162 . PMC   6315193 . PMID   30631317.
  40. 1 2 Michael T. Madigan; Deborah O. Jung (2009). An Overview of Purple Bacteria: Systematics, Physiology, and Habitats. pp. 1–15. doi:10.1007/978-1-4020-8815-5_1. ISBN   978-1-4020-8814-8. Wikidata   Q124526524.{{cite book}}: |journal= ignored (help)
  41. Bryce C, Blackwell N, Schmidt C, Otte J, Huang YM, Kleindienst S, et al. (October 2018). "Microbial anaerobic Fe(II) oxidation - Ecology, mechanisms and environmental implications". Environmental Microbiology. 20 (10): 3462–3483. doi: 10.1111/1462-2920.14328 . PMID   30058270. S2CID   51865641.
  42. Sabrina Hedrich,Michael Schlomann and D. Barrie Johnson. The iron-oxidizing proteobacteria. School of Biological Sciences, College of Natural Sciences, Bangor University, Deiniol Road, Bangor LL57 2UW, UK 2 Interdisciplinary Ecological Center, TU Bergakademie Freiberg, Leipziger Strasse 29, 09599 Freiberg, Germany. (2011)
  43. Terry J. McGenity, Taxonomy, Genomics and Ecophysiology of Hydrocarbon-Degrading Microbes, 2019 143-152; 181-189; 191-205.
  44. Markert S, Arndt C, Felbeck H, Becher D, Sievert SM, Hügler M, et al. (January 2007). "Physiological proteomics of the uncultured endosymbiont of Riftia pachyptila". Science. 315 (5809): 247–50. Bibcode:2007Sci...315..247M. doi:10.1126/science.1132913. hdl: 1912/1514 . PMID   17218528. S2CID   45745396.
  45. Rubin-Blum M, Dubilier N, Kleiner M (January 2019). "Genetic Evidence for Two Carbon Fixation Pathways (the Calvin-Benson-Bassham Cycle and the Reverse Tricarboxylic Acid Cycle) in Symbiotic and Free-Living Bacteria". mSphere. 4 (1). doi:10.1128/mSphere.00394-18. PMC   6315080 . PMID   30602523.
  46. Karamipour N, Fathipour Y, Mehrabadi M (September 2016). "Gammaproteobacteria as essential primary symbionts in the striped shield bug, Graphosoma Lineatum (Hemiptera: Pentatomidae)". Scientific Reports. 6 (1): 33168. Bibcode:2016NatSR...633168K. doi:10.1038/srep33168. PMC   5016839 . PMID   27609055.
  47. Kikuchi Y, Hosokawa T, Nikoh N, Fukatsu T (February 2012). "Gut symbiotic bacteria in the cabbage bugs Eurydema rugosa and Eurydema dominulus (Heteroptera: Pentatomidae)". Applied Entomology and Zoology. 47 (1): 1–8. doi:10.1007/s13355-011-0081-7. S2CID   14943700.
  48. Tannenbaum I, Kaur J, Mann R, Sawbridge T, Rodoni B, Spangenberg G (August 2020). "Profiling the Lolium perenne microbiome: from seed to seed". Phytobiomes Journal. 4 (3): 281–9. doi: 10.1094/PBIOMES-03-20-0026-R .
  49. Breusing C, Schultz DT, Sudek S, Worden AZ, Young CR (September 2020). "High‐contiguity genome assembly of the chemosynthetic gammaproteobacterial endosymbiont of the cold seep tubeworm Lamellibrachia barhami". Molecular Ecology Resources. 20 (5): 1432–44. doi:10.1111/1755-0998.13220. PMC   7540712 .
  50. Shiraishi A, Matsushita N, Hougetsu T (August 2010). "Nodulation in black locust by the Gammaproteobacteria Pseudomonas sp. and the Betaproteobacteria Burkholderia sp". Systematic and Applied Microbiology. 33 (5): 269–74. doi:10.1016/j.syapm.2010.04.005. PMID   20542651.
  51. Ghosh PK, De TK, Maiti TK (2015-04-01). "Ascorbic acid production in root, nodule and Enterobacter spp. (Gammaproteobacteria) isolated from root nodule of the legume Abrus precatorius L.". Biocatalysis and Agricultural Biotechnology. 4 (2): 127–134. doi:10.1016/j.bcab.2014.11.006.
  52. Benhizia Y, Benhizia H, Benguedouar A, Muresu R, Giacomini A, Squartini A (August 2004). "Gamma proteobacteria can nodulate legumes of the genus Hedysarum". Systematic and Applied Microbiology. 27 (4): 462–8. doi:10.1078/0723202041438527. PMID   15368852.
  53. Nunoura T, Takaki Y, Kazama H, Kakuta J, Shimamura S, Makita H, et al. (2014-08-18). "Physiological and genomic features of a novel sulfur-oxidizing gammaproteobacterium belonging to a previously uncultivated symbiotic lineage isolated from a hydrothermal vent". PLOS ONE. 9 (8): e104959. Bibcode:2014PLoSO...9j4959N. doi: 10.1371/journal.pone.0104959 . PMC   4136832 . PMID   25133584.
  54. Holt JR (6 February 2013). "Description of the Phylum Gammaproteobacteria". Susquehanna University - Systematic Biology Course Website. Retrieved 17 April 2018.
  55. Petersen JM, Ramette A, Lott C, Cambon-Bonavita MA, Zbinden M, Dubilier N (August 2010). "Dual symbiosis of the vent shrimp Rimicaris exoculata with filamentous gamma- and epsilonproteobacteria at four Mid-Atlantic Ridge hydrothermal vent fields". Environmental Microbiology. 12 (8): 2204–18. doi: 10.1111/j.1462-2920.2009.02129.x . hdl: 21.11116/0000-0001-CADC-4 . PMID   21966914.
  56. Shigenobu S, Watanabe H, Hattori M, Sakaki Y, Ishikawa H (September 2000). "Genome sequence of the endocellular bacterial symbiont of aphids Buchnera sp. APS". Nature. 407 (6800): 81–6. Bibcode:2000Natur.407...81S. doi: 10.1038/35024074 . PMID   10993077. S2CID   4405072.
  57. Burke GR, Moran NA (2011). "Massive genomic decay in Serratia symbiotica, a recently evolved symbiont of aphids". Genome Biology and Evolution. 3: 195–208. doi:10.1093/gbe/evr002. PMC   3056288 . PMID   21266540.
  58. Evans FF, Egan S, Kjelleberg S (May 2008). "Ecology of type II secretion in marine gammaproteobacteria". Environmental Microbiology. 10 (5): 1101–7. doi: 10.1111/j.1462-2920.2007.01545.x . PMID   18218035.
  59. Baily JL, Foster G, Brown D, Davison NJ, Coia JE, Watson E, et al. (March 2016). "Salmonella infection in grey seals (Halichoerus grypus), a marine mammal sentinel species: pathogenicity and molecular typing of Salmonella strains compared with human and livestock isolates". Environmental Microbiology. 18 (3): 1078–87. doi:10.1111/1462-2920.13219. PMID   26768299.
  60. Daniels NA, MacKinnon L, Bishop R, Altekruse S, Ray B, Hammond RM, Thompson S, Wilson S, Bean NH, Griffin PM, Slutsker L (May 2000). "Vibrio parahaemolyticus infections in the United States, 1973-1998". The Journal of Infectious Diseases. 181 (5): 1661–6. doi: 10.1086/315459 . PMID   10823766.