Abstract
The family Methanopyraceae currently consists of a single genus with a single species: Methanopyrus kandleri. It is a rod-shaped chemolithoautotrophic methanogenic archaeon that grows optimally at 98 °C and grows up to 110 °C and possibly higher under high hydrostatic pressure, making it the most extreme thermophile among the methanogens. No growth is observed below 84 °C. Strains of M. kandleri were isolated from marine hydrothermal vent systems. The organism contains 2,3-di-O-phytanyl-sn-glycerol and 2,3-di-O-geranylgeranyl-sn-glycerol lipids. In 16S rRNA phylogenetic trees, it forms a very deep branch near the root of the Archaea, remote from the other lineages of methanogens. However, in trees based on concatenated alignments of ribosomal proteins or proteins involved in transcription, M. kandleri consistently groups with other methanogens, suggesting that the methanogens are a monophyletic group of Archaea.
Access provided by Autonomous University of Puebla. Download reference work entry PDF
Similar content being viewed by others
Keywords
These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.
Taxonomy
Methanopyraceae Huber and Stetter 2002 (Validation List no. 85, 2002; Effective Publication: Huber and Stetter 2001a, 353)
Me.tha.no.py.ra.ce’ae. N.L. masc. n. Methanopyrus type genus of the family. suff. –aceae, ending to denote a family; N.L. fem. pl. n. Methanopyraceae, the Methanopyrus family. Type genus: Methanopyrus.
The family Methanopyraceae was created in 2001 to harbor a single species of hyperthermophilic hydrogenotrophic methanogenic Archaea, Methanopyrus kandleri. It was first isolated in the early 1990s from submarine hydrothermal vent systems in the Guaymas Basin in the Gulf of California, Mexico, and near Iceland (Kurr et al. 1991). In 16S rRNA-based phylogenetic trees, this species forms a very deep branch near the root of the Archaea, remote from the other lineages of methanogens.
Thus far, the monospecific genus Methanopyrus is the only genus described within the family. Because of the deep branch in the 16S rRNA-based phylogenetic tree, a separate class, the Methanopyri, a separate order, the Methanopyrales, and a separate family, the Methanopyraceae, were created for the classification of M. kandleri (Garrity and Holt 2001; Huber and Stetter 2001a, b).
Phylogenetic Structure of the Family and Its Genera
There are not many prokaryotes for which the phylogenetic position has been disputed so much as in the case of Methanopyrus kandleri. Figure 16.1 presents a 16S rRNA phylogenetic tree that shows its location on a very deep branch near the root of the Archaea, remote from the other lineages of methanogens. A maximum likelihood tree shows a topology similar to that of the neighbor-joining tree illustrated. Early studies suggested that, although more euryarchaeal than crenarchaeal signature features are present in the 16S rRNA, it shows more crenarchaeal signature features than any other known euryarchaeal rRNA (Burggraf et al. 1991).
Based on phylogenetic analyses of its 16S rRNA gene sequence, the M. kandleri lineage was proposed to branch off close to the universal root of life. Analyses of certain other genes strengthened the evidence for a Methanopyrus-proximal root of life. One such study was based on the analysis of transfer RNA and aminoacyl-tRNA synthetase genes. The intraspecies genetic distances between tRNAs cognate for different amino acids, between the initiator and elongator tRNAs for methionine, and between potentially paralogous pairs of aminoacyl-tRNA synthetases were found to be at a minimum within the M. kandleri genome. The findings were presented as evidence for a close genotypic relationship between Methanopyrus and the last universal common ancestor of life (Xue et al. 2005). A comparative study of valine- and isoleucine-tRNA synthetases was made for a number of Methanopyrus isolates from different geographic origins: the Mid-Atlantic Ridge, the Guaymas Basin, and Kolbeinsey Ridge, Iceland, as well as gene fragments cloned from environmental samples. Based on the genetic distance between the sequences, gene fragments recovered from the Central Indian Ridge were considered the most primitive among the sequences studied (Yu et al. 2009). Analysis of the elongation factor 1-α suggested that Methanopyrus may have diverged from the crenarchaeote branch before the eukaryote and the crenarchaeote lineages separated (Rivera and Lake 1996). A study of methyl coenzyme M reductase operon (mcrBDCGA) sequences also supported the placement of M. kandleri on a separate methanogen lineage (Nölling et al. 1996).
However, other more comprehensive analyses failed to confirm the special location of Methanopyrus in the universal tree of life. In trees based on concatenated alignments of ribosomal proteins and trees based on gene content, M. kandleri consistently groups with other methanogens (Slesarev et al. 2002). To solve the M. kandleri phylogeny paradox, concatenated datasets of 14 proteins involved in transcription and 53 ribosomal proteins were compared for Methanopyrus and members of the Methanococcales and the Methanobacteriales. Methanopyrus groups with the Methanococcales and the Methanobacteriales in the translation tree, whereas it emerged at the base of the euryarchaeotes in the transcription tree. It was concluded that the unusual placement of M. kandleri in the 16S rRNA tree may be the result of a reconstruction artifact due to the high evolutionary rates of the components of its transcription apparatus (Brochier et al. 2004). Placement of Methanopyrus together with the Methanobacteriales and the Methanosarcinales was therefore proposed (Luo et al. 2009).
Genome Analysis
The genome of the type strain of Methanopyrus kandleri (GenBank accession number AE009439) consists of a single circular chromosome of 1,694,969 base pairs, encoding for 1,692 proteins. The G+C content is 62.1 mol% (values of 59 and 60 mol% were earlier reported based on thermal denaturation and HPLC, respectively). Thirty-nine genes for structural RNAs were identified. The genome contains the same genes implicated in the pathway of the reduction of carbon dioxide to methane as found in the chemolithoautotrophic thermophilic methanogens Methanocaldococcus jannaschii and Methanothermobacter thermautotrophicus, suggesting that archaeal methanogens are monophyletic. Relatively few events of putative lateral gene transfer were identified. Among the unique enzymes present are type 1B DNA topoisomerase V and a two-subunit reverse gyrase. Two-component histidine kinase regulatory systems, which are present, e.g., in Methanothermobacter thermautotrophicus, are lacking. Overall, the regulatory and signaling systems are scaled down in comparison with other Archaea (Slesarev et al. 2002).
The proteins encoded by the genome show a high content of negatively charged amino acids, a possible adaptation to high intracellular ionic content; the enzymes typically require high ionic concentrations for activity and stability (see below). Accordingly, the median isoelectric point of the proteins encoded by the genome is ∼5, close to the values found for the extremely halophilic Archaea of the family Halobacteriaceae.
Phages
No phages attacking Methanopyrus strains have yet been described.
Phenotypic Analyses
Methanopyrus Kurr et al. 1992 (Validation List no. 41, 1992; Effective Publication: Kurr et al. 1991, 245)
Me.tha.no.py’rus. N.L. neut. n. methanum [from French n. méth(yle) and chemical suffix –ane] methane; N.L. pref. methano-, pertaining to methane; Gr. neut. n. pur, fire; N.L. masc. n. Methanopyrus, the “methane fire” (the hyperthermophilic methanogen). The type species, and thus far single species, is Methanopyrus kandleri, with type strain AV19 (= DSM 6324 = JCM 9639 = NBRC 100938).
Methanopyrus kandleri cells are rod-shaped, occurring singly and in chains. Cells are about 0.5 μm in diameter, and their length varies between 2 and 14 μm. Flocs and stringlike aggregates are formed when cultures are shaken. Methanopyrus is an obligately aerobic chemolithoautotroph that obtains its energy from the reduction of CO2 with H2 as the electron donor with the formation of methane. Formate, acetate, methanol, and methylamines are not used for methane formation. Growth is observed between 84 °C and 110 °C with an optimum at 98 °C. Under high hydrostatic pressure some strains may grow up to 122 °C (Takai et al. 2008). Cells grow within a wide range of salt concentrations (0.2–4 % NaCl, optimum 2 % NaCl) at pH values between 5.5 and 7 (optimum pH 6.5) (Table 16.1 ).
Cells divide by septum formation and stain Gram-positive (Huber et al. 1989). Cells are very rigid, and in the electron microscope they show a two-layered cell wall. The inner layer is composed of pseudomurein which contains ornithine in addition to lysine as diamino acid and lacks N-acetylglucosamine. It consists of l-glutamic acid, l-alanine acid, l-lysine acid, l-ornithine acid, N-acetylgalactosamine acid, and talosaminuronic acid. The pseudomurein layer is surrounded by an outer layer which is sensitive to treatment with sodium dodecyl sulfate and probably consists of protein (Kurr et al. 1991). According to Kurr et al. (1991), the thickness of each layer is about 20 nm, but Huber and Stetter (2001c) gave a total width of ∼10–15 nm for the combined layers.
M. kandleri was reported to be motile by means of polar tufts of flagella (Huber et al. 1989; Kurr et al. 1991). However, no genes for archaellin/flagellin were annotated in the genome (Slesarev et al. 2002). A search of the genome sequence yielded two putative pili operons, but no signs for the presence of genes for archaella were found (Sonja-Verena Albers, Max Planck Institute for Terrestrial Microbiology, Marburg, personal communication).
The core lipids of Methanopyrus are 2,3-di-O-phytanyl-sn-glycerol and the unsaturated 2,3-di-O-geranylgeranyl-sn-glycerol (Hafenbradl et al. 1993). The presence of the latter unsaturated terpenoid lipid is considered to be a primitive feature. During the biosynthesis of polar lipids, the fully unsaturated pre-diethers (2,3-di-O-geranylgeranyl-sn-glycerol as core lipid) are linked stepwise with polar groups and finally reduced to saturated membrane lipids (Hafenbradl et al. 1996). Thus, hydrocarbon chains with one to four double bonds can be detected (Nishihara et al. 2002). Sprott et al. (1997) also reported the presence of minor amounts of caldarchaeol tetraether lipids and hydroxyarchaeols. Nonpolar lipids account for about 50 % by weight of the total lipids, with a high proportion of 2,3-di-O-geranylgeranyl-sn-glycerol, 2,3-di-O-phytanyl-sn-glycerol, and geranylgeraniol. Two-dimensional thin layer chromatography of the polar lipids shows mostly glycolipids and minor amounts of aminophospholipids, phosphoglycolipids, and other phospholipids. Purification yielded three diglycosyl lipids, one triglycosyl lipid, and six lipids with five glycosyl groups. The glycosyl moieties contain glucose, galactose, and mannose (Hafenbradl et al. 1996). A more detailed study of the polar lipids showed an even greater variety of archaeol glycolipids with one to six hexose units composed primarily of mannose, with in addition glucose, galactose, and N-acetylglucosamine (Sprott et al. 1997). A choline-containing phospholipid is also present (Nishihara et al. 2002).
As polyamines M. kandleri contains spermidine, spermine, and agmatine. Long and branched polyamines are lacking (Hamana et al. 1999). Its tRNAs contain an exceptionally large number (31) of modified nucleosides. Many have a 2′-O-methyl group. The novel modified nucleoside N 6-acetyladenosine was characterized from M. kandleri tRNA (Sauerwald et al. 2005).
Elemental sulfur is reduced to H2S, which causes the cells to lyse (Huber and Stetter 2001c; Kurr et al. 1991).
Isolation, Enrichment, and Maintenance Procedures
All extant Methanopyrus isolates were obtained from enrichment cultures based on mineral media in the presence of 1.5 % NaCl (e.g., 10 ml portions in 120 ml serum bottles) incubated at 100 °C under an atmosphere of H2-CO2 (4:1, 300 kPa) (Huber et al. 1989; Huber and Stetter 2001c; Kurr et al. 1991). Elemental sulfur should not be added: reduction of sulfur to H2S leads to rapid lysis of Methanopyrus cells. Colonies can be isolated on medium solidified with Gelrite® gellan gum following 1 week of incubation at 98 °C under H2/CO2 in stainless steel anaerobic jars. Colonies appear after about 7 days.
Methanopyrus can survive under anaerobic conditions for long periods at low temperatures. Isolation was still possible from hydrothermal vent samples that had been stored anaerobically for 7 months at 4 °C (Kurr et al. 1991). For long-term storage cells can be suspended in liquid nitrogen in the presence of 5 % dimethyl sulfoxide (Huber and Stetter 2001c).
Physiological and Biochemical Features
Methanopyrus kandleri is a hyperthermophile that shows optimal growth at 98 °C. The doubling time under optimal conditions is 50 min. At 110 °C, near the maximum temperature enabling growth, a doubling time of 8 h is still possible (Huber et al. 1989). M. kandleri strain 116, isolated from the Kairei hydrothermal field on the Central Indian Ridge, can proliferate at 116 °C when incubated at a pressure of 0.4 MPa and even at 122 °C at 20 MPa pressure (Takai et al. 2008). This is still the highest temperature at which cell growth and multiplication has been documented to date.
The only mechanism for energy generation is the reduction of carbon dioxide to methane with hydrogen as the electron donor. None of the other substrates used by many other methanogenic archaea (acetate, formate, methanol, methylated amines) supports growth of Methanopyrus (Huber and Stetter 2001c). The enzymatic machinery involved in methanogenesis by M. kandleri is no different from that of the other autotrophic methanogens. All enzymes necessary for the operation of the pathway have been found by their activities in cell extracts (Rospert et al. 1991; Shima and Thauer 2001), and their genes were identified in the genome sequence (Slesarev et al. 2002). In the fluorescence microscope cells show the characteristic blue fluorescence due to the deazaflavin cofactor F420 (Huber et al. 1989; Kurr et al. 1991). Based on the genome sequence, the metabolic network of M. kandleri could be reconstructed (Chen et al. 2013).
A special feature of many enzymes of Methanopyrus, beyond their thermophilicity, is their marked requirement for high ionic concentrations for optimal activity. Concentrations >1 M of lyotropic salts such as K2HPO4/KH2PO4 or (NH4)2SO4 are generally needed for optimal activity. NaCl, KCl, and NH4Cl are not effective. Moreover, in the presence of 1.5 M salts, thermostability of the enzymes is dramatically increased. Enzymes showing this behavior include the N-formylmethanofuran:tetrahydromethanopterin formyltransferase and the methenyltetrahydromethanopterin cyclohydrolase (Breitung et al. 1992; Shima and Thauer 2001; Shima et al. 1998).
Inside the cells the high concentration of the osmotic solute cyclic 2,3-diphosphoglycerate (Martins et al. 1997) (estimated at ∼1.1 M; Kurr et al. 1992) is responsible for the activation and stabilization of the thermophilic enzymes. At the concentrations present in the cell, the enzymes are highly active and thermostable (Shima et al. 1998).
Ecology
Cultures of M. kandleri have been obtained from different submarine hydrothermal vent systems worldwide: the Guaymas Basin in the Gulf of California, the Mid-Atlantic Ridge, the Kairei Field in the Central Indian Ridge, and shallow marine hydrothermal system of the Kolbeinsey Ridge, Iceland. However, no positive enrichments were obtained from samples from the near-shore hydrothermal field at Vulcano, Italy, in spite of the fact that the in situ water temperatures (98–103 °C) were in the range optimal for the growth of Methanopyrus (Huber and Stetter 2001c; Kurr et al. 1991; Takai et al. 2008).
Sequences of 16S rRNA genes with a high similarity to M. kandleri were recovered from 16S rRNA gene clone libraries from samples of sulfide structures from the hydrothermal vents on the East Pacific Rise (13°N) (Nercessian et al. 2003) and from the deep-sea hydrothermal systems of the Kairei Field in the Central Indian Ridge (Takai et al. 2004). However, the Iheya North site in the Okinawa Trough off Japan did not yield such sequences (Takai et al. 2004).
To increase the sensitivity of detection of the presence of Methanopyrus in environmental samples, a protocol for the PCR amplification of its isoleucyl-tRNA synthetase gene was optimized following testing of different primer combinations, polymerase enzymes, and target DNA length (Yu 2010).
Pathogenicity, Clinical Relevance
As expected for a hyperthermophile that does not grow at temperatures below 84 °C, Methanopyrus is not known to be associated with humans, animals, or plants.
Application
No applications for Methanopyrus are currently known.
References
Breitung J, Börner G, Scholz S, Linder D, Stetter KO, Thauer RK (1992) Salt dependence, kinetic properties and catalytic mechanism of N-formylmethanofuran: tetrahydromethanopterin formyltransferase from the extreme thermophile Methanopyrus kandleri. Eur J Biochem 210:971–981
Brochier C, Forterre P, Gribaldo S (2004) Archaeal phylogeny based on proteins of the transcription and translation machineries: tackling the Methanopyrus kandleri paradox. Genome Biol 5:R17
Burggraf S, Stetter KO, Rouviere P, Woese CR (1991) Methanopyrus kandleri: an archaeal methanogen unrelated to all other known methanogens. Syst Appl Microbiol 14:346–351
Chen J, Ding Y, Xu W (2013) Comparative analysis of metabolic networks in mesophilic and thermophilic archaea methanogens based on modularity. J Biol Syst 21:1350015
Garrity GM, Holt JG (2001) Class VII. Methanopyri class. nov. In: Boone DR, Castenholz RW, Garrity GM (eds) Bergey’s manual of systematic bacteriology, vol 1, 2nd edn, The Archaea and the deeply branching and phototrophic Bacteria. Springer, New York, p 353
Hafenbradl D, Keller M, Thiericke R, Stetter KO (1993) A novel unsaturated archaeal ether core lipid from the hyperthermophile Methanopyrus kandleri. Syst Appl Microbiol 16:165–169
Hafenbradl D, Keller M, Stetter KO (1996) Lipid analysis of Methanopyrus kandleri. FEMS Microbiol Lett 136:199–202
Hamana K, Hamana H, Shinozawa T, Niitsu M, Samejima K, Itoh T (1999) Polyamines of the thermophilic eubacteria belonging to the genera Aquifex, Thermodesulfobacterium, Thermus and Meiothermus, and the thermophilic archaebacteria Sulfurisphaera, Sulfophobococcus, Stetteria, Thermocladium, Pyrococcus, Thermococcus, Methanopyrus and Methanothermus. Microbios 97:117–130
Huber R, Stetter KO (2001a) Order I. Methanopyrales ord. nov. In: Boone DR, Castenholz RW, Garrity GM (eds) Bergey’s manual of systematic bacteriology, vol 1, 2nd edn, The Archaea and the deeply branching and phototrophic Bacteria. Springer, New York, p 353
Huber R, Stetter KO (2001b) Family I. Methanopyraceae fam. nov. In: Boone DR, Castenholz RW, Garrity GM (eds) Bergey’s manual of systematic bacteriology, vol 1, 2nd edn, The Archaea and the deeply branching and phototrophic Bacteria. Springer, New York, p 353
Huber R, Stetter KO (2001c) Genus I. Methanopyrus Kurr, Huber, König, Jannasch, Fricke, Trincone, Kristjansson and Stetter 1992, 327VP (Effective publication: Kurr, Huber, König, Jannasch, Fricke, Trincone, Kristjansson and Stetter 1991, 245). In: Boone DR, Castenholz RW, Garrity GM (eds) Bergey’s manual of systematic bacteriology, vol 1, 2nd edn, The Archaea and the deeply branching and phototrophic Bacteria. Springer, New York, pp 353–355
Huber R, Kurr M, Jannasch HW, Stetter KO (1989) A novel group of abyssal methanogenic archaebacteria (Methanopyrus) growing at 110 °C. Nature 342:833–834
Kurr M, Huber R, König H, Jannasch HW, Fricke H, Trincone A, Kristjansson JK, Stetter KO (1991) Methanopyrus kandleri, gen. and sp. nov. represents a novel group of hyperthermophilic methanogens, growing at 110 °C. Arch Microbiol 156:239–247
Luo H, Sun Z, Arndt W, Shi J, Friedman R, Tang J (2009) Gene order phylogeny and the evolution of methanogens. PLoS One 4:e6069
Martins LO, Huber R, Huber H, Stetter KO, Da Costa MS, Santos H (1997) Organic solutes in hyperthermophilic Archaea. Appl Environ Microbiol 63:896–902
Nercessian O, Reysenbach A-L, Prieur D, Jeanthon C (2003) Archaeal diversity associated with in situ samplers deployed on hydrothermal vents on the East Pacific Rise (13°N). Environ Microbiol 5:492–502
Nishihara M, Morii H, Matsuno K, Ohga M, Stetter KO, Koga Y (2002) Structural analysis by reductive cleavage with LiAlH4 of an allyl ether choline-phospholipid, archaetidylcholine, from the hyperthermophilic methanoarchaeon Methanopyrus kandleri. Archaea 1:123–131
Nölling J, Elfner A, Palmer JR, Steigerwald VJ, Pihl TD, Lake JA, Reeve JN (1996) Phylogeny of Methanopyrus kandleri based on methyl coenzyme M reductase operons. Int J Syst Bacteriol 46:1170–1173
Oren A (2014a) Family Methanothermaceae. In: Rosenberg E, DeLong EF, Thompson F, Lory S, Stackebrandt E (eds) The prokaryotes, 4th edn, A handbook on the biology of bacteria: ecophysiology and biochemistry. Springer, New York
Oren A (2014b) Family Methanocaldococcaceae. In: Rosenberg E, DeLong EF, Thompson F, Lory S, Stackebrandt E (eds) The prokaryotes, 4th edn, A handbook on the biology of bacteria: ecophysiology and biochemistry. Springer, New York
Oren A (2014c) Family Methermicoccaceae. In: Rosenberg E, DeLong EF, Thompson F, Lory S, Stackebrandt E (eds) The prokaryotes, 4th edn, A handbook on the biology of bacteria: ecophysiology and biochemistry. Springer, New York
Rivera MC, Lake JA (1996) The phylogeny of Methanopyrus kandleri. Int J Syst Bacteriol 46:348–351
Rospert S, Breitung J, Ma K, Schwörer B, Zirngibl C, Thauer RK, Linder D, Huber R, Stetter KO (1991) Methyl-coenzyme M reductase and other enzymes involved in methanogenesis from CO2 and H2 in the extreme thermophile Methanopyrus kandleri. Arch Microbiol 156:49–55
Sauerwald A, Sitaramaiah D, McCloskey JA, Söll D, Crain PF (2005) N 6-Acetyladenosine: a new modified nucleoside from Methanopyrus kandleri tRNA. FEBS Lett 579:2807–2810
Shima S, Thauer RK (2001) Tetrahydromethanopterin-specific enzymes from Methanopyrus kandleri. In: Adams MWW, Kelly RM (eds) Hyperthermophilic enzymes B, vol 331, Methods in enzymology. Academic, San Diego, pp 317–353
Shima S, Hérault DA, Berkessel A, Thauer RK (1998) Activation and thermostabilization effects of cyclic 2,3-diphosphoglycerate on enzymes from the hyperthermophilic Methanopyrus kandleri. Arch Microbiol 170:469–472
Slesarev AI, Mezhevaya KV, Makarova KS, Polushin NN, Shcherbinina OV, Shakhova VV, Belova GI, Aravind L, Natale DA, Rogozin IB, Tatusov RL, Wolf YI, Stetter KO, Malykh AG, Koonin EV, Kozyavkin SA (2002) The complete genome of hyperthermophile Methanopyrus kandleri AV19 and monophyly of archaeal methanogens. Proc Natl Acad Sci USA 99:4644–4649
Sprott GD, Agnew BJ, Patel GB (1997) Structural features of ether lipids in the archaeobacterial thermophiles Pyrococcus furiosus, Methanopyrus kandleri, Methanothermus fervidus, and Sulfolobus acidocaldarius. Can J Microbiol 43:467–476
Stamatakis A (2006) RAxML-VI-HPC: maximum likelihood-based phylogenetic analyses with thousands of taxa and mixed models. Bioinformatics 22:2688–2690
Takai K, Oida H, Suzuki Y, Hirayama H, Nakagawa S, Nunoura T, Inagaki F, Nealson KH, Horikoshi K (2004) Spatial distribution of marine Crenarchaeota group I in the vicinity of deep-sea hydrothermal systems. Appl Environ Microbiol 70:2404–2413
Takai K, Nakamura K, Toki T, Tsunogai U, Miyazaki M, Miyazaki J, Hirayama H, Nakagawa S, Nunoura T, Horikoshi K (2008) Cell proliferation at 122 °C and isotopically heavy CH4 production by a hyperthermophilic methanogen under high-pressure cultivation. Proc Natl Acad Sci USA 105:10949–10954
Whitman WB, Bowen TL, Boone DR (2006) The methanogenic bacteria. In: Dworkin M, Falkow S, Rosenberg E, Schleifer K-H, Stackebrandt E (eds) The prokaryotes, vol 3, A handbook on the biology of bacteria: ecophysiology and biochemistry. Springer, New York, pp 165–207
Xue H, Ng S-K, Tong K-L, Wong JT-F (2005) Congruence for evidence for a Methanopyrus-proximal root of life based on transfer RNA and aminoacyl-tRNA synthetase genes. Gene 360:120–130
Yarza P, Ludwig W, Euzéby J, Amann R, Schleifer KH, Glöckner FO, Rosselló-Móra R (2010) Update of the All-Species Living Tree project based on 16S and 23S rRNA sequence analyses. Syst Appl Microbiol 33:291–299
Yu Z (2010) Optimization of PCR amplification for sensitive capture of Methanopyrus isoleucyl-tRNA synthetase gene in environmental samples. Ann Microbiol 60:757–762
Yu Z, Takai K, Slesarev A, Xue H, Wong JT-F (2009) Search for primitive Methanopyrus based on genetic distance between Val- and Ile-tRNA synthetases. J Mol Evol 69:386–394
Author information
Authors and Affiliations
Corresponding author
Editor information
Editors and Affiliations
Rights and permissions
Copyright information
© 2014 Springer-Verlag Berlin Heidelberg
About this entry
Cite this entry
Oren, A. (2014). The Family Methanopyraceae . In: Rosenberg, E., DeLong, E.F., Lory, S., Stackebrandt, E., Thompson, F. (eds) The Prokaryotes. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-38954-2_328
Download citation
DOI: https://doi.org/10.1007/978-3-642-38954-2_328
Published:
Publisher Name: Springer, Berlin, Heidelberg
Print ISBN: 978-3-642-38953-5
Online ISBN: 978-3-642-38954-2
eBook Packages: Biomedical and Life SciencesReference Module Biomedical and Life Sciences