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| Genus: | Beggiatoa Trevisan 1842[1]
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Beggiatoa is a genus of Gammaproteobacteria belonging the order Thiotrichales in the Proteobacteria phylum. This genus was one of the first bacteria discovered by Russian botanist Sergei Winogradsky during his research in Anton de Bary’s laboratory of botany in 1887, he found that Beggiatoa oxidized hydrogen sulfide (H2S) as an energy source, forming intracellular sulfur droplets, Oxygen is the terminal electron acceptor and CO2 is used as carbon source. Winogradsky named it in honor of the Italian medic and botanist Francesco Secondo Beggiato. Winogradsky referred to this form of metabolism as inorgoxidation (oxidation of inorganic compounds). The organisms live in sulfur-rich environments such as soil, hydrothermal water both marine and freshwater, in the deep sea hydrothermal vents and in polluted marine environments.The finding represented the first discovery of lithotrophy.[3][4] Two species of Beggiatoa have been formally described: the type species Beggiatoa alba, and Beggiatoa leptomitoformis, the latter of which was only published in 2017.[5] This colorless and filamentous bacterium, sometimes in association with other sulfur bacteria (for example the genus Thiothrix) can be arranged in biofilm visible at naked eye formed by very long white filamentous mat, the white color is due to the stored sulfur. Species of Beggiatoa have cells up to 200 µ in diameter and they are one of the largest prokaryotes on Earth.[6]
Taxonomy
[edit]Beggiatoa are close relatives of Thioploca.[7]
Morphology and motility
[edit]By the observation of their morphological characteristics, Beggiatoa spp. can be divided into three categories:
- Freshwater strains, characterized by narrow filaments with no vacuoles;
- Narrow marine strains, without vacuoles (filaments' diameter of about 4.4 µm);
- Larger marine strains, with vacoules for nitrate storing (filaments' diameter vary between 5 to 140 µm)
Obviously, this classification is purely ideal so some exceptions can exist. Narrow filaments are usually composed by cylindrical cells which length is about 1.5 to 8 times their thickness; wider filaments instead are disk-shaped with cell lengths from 0.10 to 0.90 times their cell width. In all of the cultured strains the terminal cells of the filaments appear rounded. Although they are Gram-negative bacteria, Beggiatoa show a unusual cell-wall and membrane organization. Sometimes are present further membranes that cover the peptidoglycan layer; the number of this addictional membranes is very variable. Their presence maybe is due to the harsh conditions in which some of these organisms live. Even the intracellular granules can be covered by extra-membranes structure. Beside the sulfur granules, the cells often show the presence of similarly stored granules of polyhydroxybutyrate and polyphosphate. Very common in large marine Beggiatoa are hollow-structured filaments, composed by cells with a narrow cytoplasm surrounding a large central vacuole, exlpoited for nitrate storing. [6][8]
The filaments move by gliding and this movement is likely connected to string-like structures in the outer membrane and trans-peptidoglycan channels. Sometimes the filaments can also breakthrough the formation of necridia cell in the middle of the filament. The motility of the filament is very important for the adaptablity of the bacteria, because it allows to move on more suitable conditions for the cellular metabolism. The main drivers that guide the movement of Beggiatoa filaments are high oxygen and sulfide levels and light exposure, from which the filaments move away. [8]
Cell growth
[edit]Beggiatoa reproducing strategy is fragmentation, the growth of a colony leading to mat development is obtained through alternating filament elongation and breakage. Breakage can happen essentially in the middle of a stretched filament, at the tip of a filament loop or where a tip of a loop was once placed. The presence of sacrificial cells is fundamental as they interrupt the communication between two parts of one filament, in this way each section can change its gliding direction causing the split.
The average filament length achieved through this process is also result of gene-environment interactions as, for instance, the growth and position of the filament is function of vertical gradients of oxygen and sulfide. Therefore it is proposed that good environmental conditions will paradoxically cause cell death in order to enhance filament breakage thus reproduction. [9]
Metabolism
[edit]Beggiatoa group is mainly composed by chemolithotrophic, sulfide-oxidizing bacteria. However, the range of possible metabolic pathways is very diversified, varying from the heterotrophy to the chemolithoautotrophy. Because of this huge variability the diverse bacteria of this genus can differ greatly from each other.[8]
Carbon metabolism
[edit]In Beggiatoa group are present both autotrophic and heterotrophic metabolisms. Autotrophic Beggiatoa carry out the CO2 fixation through the Calvin cycle and the employment of the RuBisCO enzyme. The latter shows different regulation levels in obligated and facultative autotrophs. For instance, in the obligately autotrophic strain MS-81-1c RuBisCO cannot be repressed, while in the facultatively autotrophic strain MS-81-6 it is tightly regulated to switch from autotrophic to heterotrophic growth and vice-versa. Beside the autotrophic strains, most of the freshwater Beggiatoa strains are heterotrophic, requiring organic substrates for growth. Specifically, many of them can be considered mixotrophs, because they grow heterotrophically, oxidizing organic compounds, but they can also use sulfide or other reduced sulfur compounds as electron donors. By this strategy, the organic carbon skeletons are saved for the purpose of increasing biomass and the CO2 autotrophic fixation is not required. Mixotrophy has been suspected to be the trophic modality for many freshwater strains, but it has only been found in one marine strain of Beggiatoa, MS-81-6.[8][6]
Nitrogen metabolism
[edit]Beggiatoa group show substantial versatility in utilizing nitrogen compounds. Nitrogen can be a source for growth or, in the case of nitrate, it can be an electron acceptor for anaerobic respiration. Heterotrophic freshwater Beggiatoa spp. assimilate nitrogen for growth. Nitrogen sources include nitrate, nitrite, ammonia, amino acids, urea, aspartate, asparagine, alanine and thiourea, depending on the capability of specific strains.
Autotrophic vacuolated Beggiatoa are able to store nitrate in their vacuoles 20.000 times the concentration of the surrounding sea water, and use it as terminal electron acceptor in anoxic conditions. This process, called Dissimilatory Nitrate Reduction to Ammonium (DNRA), reduces nitrate to ammonium. The capability of using nitrate as electron acceptor allows the colonization of anoxic environments, such as microbial mats and sediments.
Several species are able to fix nitrogen using nitrogenase enzyme. [6][8]
Sulfur metabolism
[edit]One of the defining features of the genus Beggiatoa is the production of intracellular inclusions of sulfur resulting from the oxidation of reduced sulfur sources (e.g. hydrogen sulfide). In autotrophic Beggiatoa, sulfide is a source of energy and electrons for carbon fixation and growth. The oxidation of sulfide can be aerobic or anaerobic, in fact it can be coupled with the reduction of oxygen or with the reduction of nitrate. Sulfur produced by the oxidation of sulfide is stored into internal globules and can be used when the concentration of sulfide decreases. Thus, the temporarily storing of elemental sulfur increase the adaptability of an organism and its tolerance to changes in the concentrations of sulfide and oxygen. [6][8]
Sulfide oxidation: 2H2S O2 → 2S 2H2O
There are some cases of chemoorganotrophy, too. For instance, the strain Beggiatoa sp. 35Flor usually do an aerobic respiration coupled with the oxidation of sulfide, but in anoxic condition a different type of respiration is activated. The energy is gained chemoorganotrophically from oxidation of PHA (polyhydroxyalkanoates), organic compounds previously synthesized through CO2 fixation during chemolithotrophic growth on oxygen and sulfide. In this case electron acceptor is the sulfur stored into the cell, so the final product is hydrogen sulfide. [10]
Hydrogen metabolism
[edit]The strain Beggiatoa sp. 35Flor is able to use hydrogen as alternative electron donor to sulfide. This oxidation process can provide energy for maintenance and assimilatory purposes and is helpful to reduce stored sulfur when it becomes excessive, but it can’t provide growth to the strain. [11]
Phosphorus metabolism
[edit]Beggiatoa’s metabolism include the use of phosphorus in the polyphosphate form. The regulation of this metabolism relies on the environmental conditions. Oxygenated surroundings cause an accumulation of phosphate, while anoxia (coupled with an increasing concentration of sulfide) produces a breakdown of polyphosphate and its subsequent release from the cells. The released phosphate can then be deposited as phosphorite minerals in the sediments or stay dissolved in the water. [8]
Cultivation
[edit]Selective Enrichments
[edit]The most successful enrichments for Beggiatoa spp. have been made using a shallow pan or aquarium in which it has been added few centimeters of sand, different amount of CaSO4 and K2HPO4, a source of complex organic polymers such as seaweed, several centimeters of sulfide-rich marine mud and seawater. The enrichment must contain the proper sulfide-oxygen interface that can be possible only if air is introduced, for example, by a slow steady flow of freshly aerated seawater. Another type of enrichment associated with Beggiatoa spp. is based on the use of extracted dried grass or hay in a mineral medium because the complex polymers such as cellulose residues in the material provide sulfate reduction. This also provides the hydrogen sulfide necessary to enrich for Beggiatoa.[6]
Pure Culture Isolation
[edit]There are three different possible techniques to obtain isolated Beggiatoa strains in pure culture:
- Isolation on agar plates
- Isolation using liquid media
- Isolation and cultivation in gradient media
Isolation on agar plates
[edit]The procedure that allows to obtain isolated heterotrophic strain requires an agar plate containing dilute organic substrate such as small amount of peptone. Then, it’s necessary to collect tufts of Beggiatoa filaments from the environment, to wash them using sterile washing solution and to place them on the agar plate. In this way there will be some growing filaments moving away from the centrale inoculum that can be used as inoculum for a new agar plate. For the isolation of marine Beggiatoa strains (that show autotrophic growth), since they are obligate microaereophiles it’s essential to provide micro-oxic conditions and to use particular agar plates made by filtered seawater supplemented with sodium sulfide and sodium acetate. On the contrary, for the freshwater strains isolation it’s necessary to perform under oxic conditions (air atmosphere) using a variety of media containing a low concentration of single organic compound such as acetate, Na2S or thiosulfate.[6]
Isolation using liquid media
[edit]Liquid media are often used for enrichment, MPN enumeration and bulk cultivation of Beggiatoa. In order to have a successful cultivation of heterotrophic or mixotrophic freshwater Beggiatoa, liquid media has to contain little amounts of carbon substrate, either soil extracts or acetate. The type species and strain (Beggiatoa alba str. B18LD) and related strains are generally grown in media that include a salt base, acetate as carbon source, and variable yeast extract and sulfide additions [(Mezzino et al., 1984; Schmidt et al., 1986).]. Some marine autotrophic Beggiatoa strains are also been cultured on defined liquid mineral medium with thiosulfate, CO2, micro-oxic conditions under aeration with 0.25% O2 (v/v) in the gas phase.[6]
Isolation and cultivation in gradient media
[edit]Autotrophic strains coming from a single filament isolation on agar can easily be maintained and propagated in sulfide gradient tubes in which sulfide-rich agar plugs are overlaid with sulfide-free soft agar. Tubs are loosely closed in order to permit the exchange of headspace gasses with the atmosphere. As result, two opposite layers are formed, one that contains sulfide while the other one oxygen: this allows the growth of a well-defined Beggiatoa layer at the sulfide-oxygen interface. The gradient medium construction requires different amounts of J3 medium (made by agar and NaHCO3) supplemented with neutralized Na2S placed in a screw-capped tube. Here, the sulfur source is provided by the flux of sulfide. Another ‘’ layer ‘’ is made by NaHCO3 without sulfide or thiosulfate: all of the sulfide will be below the interface between the sulfidic agar plug and the sulfide-free overlay agar while there will be another layer in the top of the tube that represents the oxygen reservoir. It begins to form a gradient shape due to the reaction between sulfide and oxygen: as results, the filaments rapidly proliferate at the sulfide-oxygen interface, forming a marked layer or “plate,” of 1 mm but it’s also possible to appreciate that these bacteria can track the interface and slowly descend owing to the gradual depletion of the sulfide reservoir.[6]
Ecology
[edit]Filaments have been observed to form dense mats on sediments in estuarine, shelf, seep, and deep-sea hydrothermal vent environments. They appear as a whitish layer and since they are present and flourish in marine environments which have been subject to pollution, they can be considered as an indicator species.
Beggiatoa and other related filamentous bacteria can cause settling problems in sewage treatment plants, industrial waste lagoons in canning, paper pulping, brewing, milling, causing the phenomenon called "bulking". Beggiatoa are also able to detoxify hydrogen sulfide in soil.
Habitat
[edit]The incredible number of adaptations and metabolisms of this genus of bacteria are conseguences of the extraordinary environmental variability they can live in, so Beggiatoa it’s almost benthic. It can be found in marine (Beggiatoa sp. MS-81-6 and MS-81-1c) or freshwater (Beggiatoa alba) environments and they only need sulfide or thiosulfide as electron donor and an oxidizer. They can usually be found in habitats that have high levels of hydrogen sulfide, these environments include cold seeps, sulfur springs, sewage contaminated water, mud layers of lakes, and near deep hydrothermal vents. Beggiatoa can also be found in the rhizosphere of swamp plants[12],[7] in soil and in marine sediments, in the mangrove lagoon too.[13] The freshwater species have tipical habitat in sulfur springs, ditches, puddles, wetlands, lake sediments and in rice fields where it can grow associated with the rice plants’ roots. The Beggiatoa that live in marine water can be found in region where their source of energy (sulfide or thiosulfide) can be found, this can be extracted from both inorganic or organic source, in general energy source must be coupled with a general low oxygen content. [6]
Vacuolated Beggiatoa can be very common in coastal upwelling regions (for example Peru and Chile coasts),deep sea hydrothermal vents and cold vents; in these environments the floc mats (hair-like breast) can grow up and cover large areas and reach the height of 30 cm. In deep sea hydrothermal vents and cold-seeps Beggiatoa can grow in filaments that can be up to 200 micrometres in diameter, which makes these ones the largest prokaryotes currently known. Vacuolated Beggiatoa can be found also in hypoxic seafloor where the filaments can live inside the sediments at the depth of few cm (from 2 to 4 cm), in same cases the Beggiatoa bacterial filaments can be the most abundant part of the microbial biomass in the sediments. [8]
Beggiatoa can also be found in salt marshes, saline, and geothermally active underwater caves. Some studies on these environments have been carried out in the underwater caves of dolomitized limestone which contain hydrothermal sulphidic springs in Capo Palinuro, Salerno, (Italy) in which the distribution of microbial biofilm is associated with the flow of hydrothermal fluid from sources whose activity is intermittent and started during low tide; mats found in the caves were composed of filaments resembling in most part Beggiatoa, Thiothrix and Flexibacter, this Beggiatoa-like filaments were morphologically close to those found attached to rocks and the byssus of the mussels from Lucky Strike Hydrothermal vents on the Mid-Atlantic Ridge.[14]This genus of Gammaprotobacteria is also common in localizated area of anaerobic decomposition as whale carcass on the deep ocean floor. [6]
Interactions with other organisms
[edit]Frequently, microorganisms of the genus Beggiatoa can form complex microbial mats, where they live in association with many other filamentous bacteria, such as cyanobacteria. The latter usually occupy the surface layer of the mat and during the day they produce a great amount of oxygen, derived from the photosynthetic activity. Conversely, Beggiatoa grow along an oxic/anoxic (oxygen/sulfide) interface, beneath the phototrophs. Sometimes Beggiatoa mats are enriched by the presence of diatoms and green euglenoids too.[6] [15]
As the microbial mats can reach 3 cm in width, they can represent a source of food for many grazers. This trophic connection has been observed in mangrove systems, where Beggiatoa cover part of marine sediments. It has been observed that these bacteria give an important contribution to meiofauna’s diet, in particular rotifers, polychaetes, nematodes and some groups of platyhelminthes, aschelminths and gnathostomulids.[16] A remarkable relationship has been found between nematodes and Beggiatoa. In fact nematodes seem to favor development of Beggiatoa mats, through the increasing of oxygen penetration and nutrient diffusion into the mat.[17]
Role in biogeochemical cycles
[edit]Large species of white sulfur bacteria in the family Beggiatoaceae are able to accumulate and transport NO3-, taken from shallow coastal sediments which is fundamental in metabolism and accumulate it in filaments. The reduction of NO3- to ammonium implies the oxidation of H2S: this reduction leads to the formation of suboxic zones characterized by positive redox potential and only trace concentrations of free H2S. So, in marine environment the presence of these species is important because they have an important role in regulation of the amount of H2S and NO3- :
- On one hand, the regulation of free H2 S concentration in marine sediments is fundamental because sulfide-depleted surface sediments are essential for survival of benthic infauna in fact sulfide is highly toxic to bottom fauna and other organisms living in the sediment;
- On the other hand, NO3- reduction is important for control of eutrophication in nitrogen-limited coastal waters. [18]
Beggiatoa can also accumulate phosphorus as polyphosphate and subsequently releases phosphate in anoxic conditions. This might increase the availability of phosphorus to primary producers if the phosphate is released from the sediment to the water column. Some studies about the phosphorus cycling and the release of phosphorus linked to Beggiatoa has been realized in Baltic Sea. These studies showed that the reduction of sulfide by these bacteria may decrease the rate of iron sulfide formation in the sediments, and thus increase the phosphorus retention capability of the sediment. [8]
References
[edit]- ^ Trevisan, V. 1842. Prospetto della Flora Euganea. Coi Tipi Del Seminario, Padova, pp. 1-68.
- ^ Parte, A.C. "Beggiatoa". LPSN.
- ^ Ljungdahl LG (2003). Biochemistry and physiology of anaerobic bacteria. Springer. p. 17. ISBN 978-0-387-95592-6.
- ^ Mukhopadhyaya PN, Deb C, Lahiri C, Roy P (Aug 2000). "A soxA gene, encoding a diheme cytochrome c, and a sox locus, essential for sulfur oxidation in a new sulfur lithotrophic bacterium". J Bacteriol. 182 (15): 4278–87. doi:10.1128/JB.182.15.4278-4287.2000. PMC 101942. PMID 10894738.
- ^ Parte, A.C. "Beggiatoa". LPSN. Retrieved 2017-10-18.
- ^ a b c d e f g h i j k l Teske, Andreas; Nelson, Douglas C. (2006), Dworkin, Martin; Falkow, Stanley; Rosenberg, Eugene; Schleifer, Karl-Heinz (eds.), "The Genera Beggiatoa and Thioploca", The Prokaryotes, Springer New York, pp. 784–810, doi:10.1007/0-387-30746-x_27., ISBN 978-0-387-25496-8, retrieved 2020-11-18
{{citation}}: Check|doi=value (help) - ^ a b Ahmad A, Barry JP, Nelson DC (Jan 1999). "Phylogenetic affinity of a wide, vacuolate, nitrate-accumulating Beggiatoa sp. from Monterey Canyon, California, with Thioploca spp". Appl Environ Microbiol. 65 (1): 270–7. PMC 91012. PMID 9872789.
- ^ a b c d e f g h i Ruuskanen, Matti (2014). "The genus Beggiatoa and its effects on the nutrient cycles of the Baltic Sea". doi:10.13140/RG.2.1.4814.6329.
{{cite journal}}: Cite journal requires|journal=(help) - ^ Kamp, Anja; Røy, Hans; Schulz-Vogt, Heide N. (2008-10). "Video-supported Analysis of Beggiatoa Filament Growth, Breakage, and Movement". Microbial Ecology. 56 (3): 484–491. doi:10.1007/s00248-008-9367-x. ISSN 0095-3628. PMC 2755761. PMID 18335158.
{{cite journal}}: Check date values in:|date=(help)CS1 maint: PMC format (link) - ^ Schwedt, Anne; Kreutzmann, Anne-Christin; Polerecky, Lubos; Schulz-Vogt, Heide N. (2012). "Sulfur Respiration in a Marine Chemolithoautotrophic Beggiatoa Strain". Frontiers in Microbiology. 2. doi:10.3389/fmicb.2011.00276. ISSN 1664-302X. PMC 3253548. PMID 22291687.
{{cite journal}}: CS1 maint: PMC format (link) CS1 maint: unflagged free DOI (link) - ^ Kreutzmann, Anne-Christin; Schulz-Vogt, Heide N. (2016-04-15). Löffler, F. E. (ed.). "Oxidation of Molecular Hydrogen by a Chemolithoautotrophic Beggiatoa Strain". Applied and Environmental Microbiology. 82 (8): 2527–2536. doi:10.1128/AEM.03818-15. ISSN 0099-2240.
- ^ Michael Dudley. "Beggiatoa". Archived 2009-02-07 at the Wayback Machine
- ^ Jean, Maïtena R. N.; Gonzalez-Rizzo, Silvina; Gauffre-Autelin, Pauline; Lengger, Sabine K.; Schouten, Stefan; Gros, Olivier (2015-02-17). Kellogg, Christina A. (ed.). "Two New Beggiatoa Species Inhabiting Marine Mangrove Sediments in the Caribbean". PLOS ONE. 10 (2): e0117832. doi:10.1371/journal.pone.0117832. ISSN 1932-6203. PMC 4331518. PMID 25689402.
{{cite journal}}: CS1 maint: PMC format (link) CS1 maint: unflagged free DOI (link) - ^ Mattison, R.G.; Abbiati, M.; Dando, P.R.; Fitzsimons, M.F.; Pratt, S.M.; Southward, A.J.; Southward, E.C. (1998-01-01). "Chemoautotrophic Microbial Mats in Submarine Caves with Hydrothermal Sulphidic Springs at Cape Palinuro, Italy". Microbial Ecology. 35 (1): 58–71. doi:10.1007/s002489950060. ISSN 1432-184X.
- ^ Fenchel, T; Bernard, C (1995). "Mats of colourless sulphur bacteria. I. Major microbial processes". Marine Ecology Progress Series. 128: 161–170. doi:10.3354/meps128161. ISSN 0171-8630.
- ^ Pascal, PY; Dubois, S; Boschker, HTS; Gros, O (2014-12-03). "Trophic role of large benthic sulfur bacteria in mangrove sediment". Marine Ecology Progress Series. 516: 127–138. doi:10.3354/meps11035. ISSN 0171-8630.
- ^ Salvadó, Humbert; Palomo, Alejandro; Mas, Meritxell; Puigagut, Jaume; Gracia, Mª del Pilar (2004-05). "Dynamics of nematodes in a high organic loading rotating biological contactors". Water Research. 38 (10): 2571–2578. doi:10.1016/j.watres.2004.03.007. ISSN 0043-1354.
{{cite journal}}: Check date values in:|date=(help) - ^ Sayama, Mikio; Risgaard-Petersen, Nils; Nielsen, Lars Peter; Fossing, Henrik; Christensen, Peter Bondo (2005-11-01). "Impact of Bacterial NO3− Transport on Sediment Biogeochemistry". Applied and Environmental Microbiology. 71 (11): 7575–7577. doi:10.1128/AEM.71.11.7575-7577.2005. ISSN 0099-2240. PMC 1287653. PMID 16269807.
{{cite journal}}: CS1 maint: PMC format (link)