Green sulfur bacteria

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Green sulfur bacteria
Green d winogradsky.jpg
Green sulfur bacteria in a Winogradsky column
Scientific classification
Domain:
Bacteria
Superphylum:
FCB group
(unranked):
Bacteroidota–Chlorobiota group
Phylum:
Chlorobiota

Iino et al. 2021[1]
Class:
"Chlorobia"

Garrity and Holt 2001[2]
Order:
Chlorobiales

Gibbons and Murray 1978 (Approved Lists 1980)[3]
Families and Genera
  • Chlorobiaceae Copeland 1956 (Approved Lists 1980)
    • Gorlenko and Lebedeva 1971 (Approved Lists 1980)
    • Imhoff 2003
    • Chlorobium Nadson 1906 (Approved Lists 1980)
    • Gibson et al. 1985
    • "Chloroplana" Dubinina and Gorlenko 1975
    • "Clathrochloris" Geitler 1925
    • Lauterborn 1913 (Approved Lists 1980)
    • Gorlenko 1970 (Approved Lists 1980)
  • "Candidatus " Liu et al. 2012
    • "Candidatus " Liu et al. 2012
Synonyms
  • Chlorobiota:
    • "Chlorobi" Iino et al. 2010
    • "Chlorobi" Garrity and Holt 2001
    • "Chlorobaeota" Oren et al. 2015
    • "Chlorobiota" Whitman et al. 2018
  • Chlorobiota:
    • "Chlorobia" Whitman et al. 2018
    • Chlorobea Cavalier-Smith 2002
    • "Chlorobiia" Cavalier-Smith 2020
  • Chlorobiales:
    • "Chlorobiales" Garrity and Holt 2001
  • Chlorobiaceae:
    • "Chlorobiaceae" Garrity and Holt 2001

The green sulfur bacteria are a phylum of obligately anaerobic photoautotrophic bacteria.[4]

Green sulfur bacteria are nonmotile (except Chloroherpeton thalassium, which may glide) and capable of anoxygenic photosynthesis.[4][5] In contrast to plants, green sulfur bacteria mainly use sulfide ions as electron donors.[6] They are autotrophs that utilize the reverse tricarboxylic acid cycle to perform carbon fixation.[7] Green sulfur bacteria have been found in depths of up to 145m in the Black Sea, with low light availability.[8]

Characteristics[]

Major photosynthetic pigment: Bacteriochlorophylls a plus c, d, or e

Location of photosynthetic pigment: Chlorosomes and plasma membranes

Photosynthetic electron donor: H2, H2S, S

Sulfur deposition: Outside of the cell

Metabolic type: Photolithoautotrophs[9]

Habitat[]

The Black Sea, an extremely anoxic environment, was found to house a large population of green sulfur bacteria at about 100 m depth. Due to the lack of light available in this region of the sea, most bacteria were photosynthetically inactive. The photosynthetic activity detected in the sulfide chemocline suggests that the bacteria need very little energy for cellular maintenance.[8]

A species of green sulfur bacteria has been found living near a black smoker off the coast of Mexico at a depth of 2,500 m in the Pacific Ocean. At this depth, the bacterium, designated GSB1, lives off the dim glow of the thermal vent since no sunlight can penetrate to that depth.[10]

Green sulfur bacteria has also been found living on coral reef colonies in Taiwan, they make up the majority of a "green layer" on these colonies. They likely play a role in the coral system.[11]

Phylogeny[]

The currently accepted phylogeny is based on 16S rRNA-based LTP release 123 by The All-Species Living Tree Project.[12]

 
 

Ignavibacteriota (outgroup)

 
Chlorobiota
 

Gibson et al. 1985

 
 
 

Gorlenko 1970 emend. Imhoff 2003 (type sp.)

 
 

(Pelsh 1936) Imhoff 2003

 
 
 
 
 

(Gorlenko et al. 1974) Imhoff 2003

 
 

C. tepidum (Wahlund et al. 1996) Imhoff 2003 (type sp.)

 
 

Imhoff 2003

 
 
 
Chlorobium
 

(Schmidle 1901) emend. Imhoff 2003

 
 
 

Pfennig 1968 emend. Imhoff 2003

 
 
 

C. limicola Nadson 1906 emend. Imhoff 2003 (type sp.)

 
 
 

(Szafer 1911) emend. Imhoff 2003

 
 

Pfennig 1968 emend. Imhoff 2003

 
 
 
 
 
 
 
 
 

Metabolism[]

Photosynthesis in the green sulfur bacteria[]

The green sulfur bacteria use a Type I reaction center for photosynthesis. Type I reaction centers are the bacterial homologue of photosystem I (PSI) in plants and cyanobacteria. The GSB reaction centers contain bacteriochlorophyll a and are known as P840 reaction centers due to the excitation wavelength of 840 nm that powers the flow of electrons. In green sulfur bacteria the reaction center is associated with a large antena complex called the chlorosome that captures and funnels light energy to the reaction center. The chlorosomes have a peak absorption in the far red region of the spectrum between 720-750 nm because they contain bacteriocholorophyll c, d and e.[13] A protein complex called the Fenna-Matthews-Olson complex (FMO) is physically located between the chlorosomes and the P840 RC. The FMO complex helps efficiently transfer the energy absorbed by the antena to the reaction center.

PSI and Type I reaction centers are able to reduce ferredoxin (Fd), a strong reductant that can be used to fix CO
2 and reduce NADPH. Once the reaction center (RC) has given an electron to Fd it becomes an oxidizing agent (P840+) with a reduction potential of around +300 mV. While this is not positive enough to strip electrons from water to synthesize O
2 (E
0 = +820 mV), it can accept electrons from other sources like H
2S, thiosulphate or Fe2+
 ions.[14] This transport of electrons from donors like H
2S to the acceptor Fd is called linear electron flow or linear electron transport. The oxidation of sulfide ions leads to the production of sulfur as a waste product that accumulates as globules on the extracellular side of the membrane. These globules of sulfur give green sulfur bacteria their name. When sulfide is depleted, the sulfur globules are consumed and further oxidized to sulfate. However, the pathway of sulfur oxidation is not well-understood.[6]

Instead of passing the electrons onto Fd, the Fe-S clusters in the P840 reaction center can transfer the electrons to menaquinone (MQ:MQH
2) which returns the electrons to the P840+ via an electron transport chain (ETC). On the way back to the RC the electrons from MQH2 pass through a cytochrome bc1 complex (similar to the complex III of mitochondria) that pumps H+
 ions across the membrane. The electrochemical potential of the protons across the membrane is used to synthesize ATP by the FoF1 ATP synthase. This cyclic electron transport is responsible for converting light energy into cellular energy in the form of ATP.

Carbon fixation of green sulfur bacteria[]

Green sulfur bacteria are photoautotrophs: they not only get energy from light, they can grow using carbon dioxide as their sole source of carbon. They fix carbon dioxide using the reverse tricarboxylic acid cycle (rTCA) cycle[7] where energy is consumed to reduce carbon dioxide in order to synthesize pyruvate and acetate. These molecules are used as the raw materials to synthesize all the building blocks a cell needs to generate macromolecules. The rTCA cycle is highly energy efficient enabling the bacteria to grow under low light conditions.[15] However it has several oxygen sensitive enzymes that limits it's efficiency in aerobic conditions.[15]

The reactions of reversal of the oxidative tricarboxylic acid cycle are catalyzed by four enzymes:[7]

  1. pyruvate:ferredoxin (Fd) oxidoreductase:
    acetyl-CoA + CO2 + 2Fdred + 2H+ ⇌ pyruvate + CoA + 2Fdox
  2. ATP citrate lyase:
    ACL, acetyl-CoA + oxaloacetate + ADP + Pi ⇌ citrate + CoA + ATP
  3. α-keto-glutarate:ferredoxin oxidoreductase:
    succinyl-CoA + CO2 + 2Fdred + 2H+ ⇌ α-ketoglutarate + CoA + 2Fdox
  4. fumarare reductase
    succinate + acceptor ⇌ fumarate + reduced acceptor

Mixotrophy in green sulfur bacteria[]

Green sulfur bacteria are obligate photoautotrophs: they cannot grow in the absence of light even if they are provided with organic matter.[7][14] However they exhibit a form of mixotrophy where they can consume simple organic compounds in the presence of light and CO2.[7]

Nitrogen fixation[]

The majority of green sulfur bacteria are diazotrophs: they can reduce nitrogen to ammonia which is then used to synthesize amino acids.[16]

References[]

  1. ^ Oren A, Garrity GM (2021). "Valid publication of the names of forty-two phyla of prokaryotes". Int J Syst Evol Microbiol. 71 (10): 5056. doi:10.1099/ijsem.0.005056. PMID 34694987.
  2. ^ Garrity GM, Holt JG. (2001). "Phylum BXI. Chlorobi phy. nov.". In Boone DR, Castenholz RW, Garrity GM. (eds.). Bergey's Manual of Systematic Bacteriology. Vol. 1 (The Archaea and the deeply branching and phototrophic Bacteria) (2nd ed.). New York, NY: Springer–Verlag. pp. 601–623.
  3. ^ Gibbons NE, Murray RGE. (1978). "Proposals Concerning the Higher Taxa of Bacteria". International Journal of Systematic Bacteriology. 28: 1–6. doi:10.1099/00207713-28-1-1.
  4. ^ a b Bryant DA, Frigaard NU (November 2006). "Prokaryotic photosynthesis and phototrophy illuminated". Trends in Microbiology. 14 (11): 488–96. doi:10.1016/j.tim.2006.09.001. PMID 16997562.
  5. ^ Green BR (2003). Light-Harvesting Antennas in Photosynthesis. p. 8. ISBN 0792363353.
  6. ^ a b Sakurai H, Ogawa T, Shiga M, Inoue K (June 2010). "Inorganic sulfur oxidizing system in green sulfur bacteria". Photosynthesis Research. 104 (2–3): 163–76. doi:10.1007/s11120-010-9531-2. PMID 20143161. S2CID 1091791.
  7. ^ a b c d e Tang KH, Blankenship RE (November 2010). "Both forward and reverse TCA cycles operate in green sulfur bacteria". The Journal of Biological Chemistry. 285 (46): 35848–54. doi:10.1074/jbc.M110.157834. PMC 2975208. PMID 20650900.
  8. ^ a b Marschall E, Jogler M, Hessge U, Overmann J (May 2010). "Large-scale distribution and activity patterns of an extremely low-light-adapted population of green sulfur bacteria in the Black Sea". Environmental Microbiology. 12 (5): 1348–62. doi:10.1111/j.1462-2920.2010.02178.x. PMID 20236170.
  9. ^ Pranav kumar, Usha mina (2014). Life science fundamental and practice part I.
  10. ^ Beatty JT, Overmann J, Lince MT, Manske AK, Lang AS, Blankenship RE, Van Dover CL, Martinson TA, Plumley FG (June 2005). "An obligately photosynthetic bacterial anaerobe from a deep-sea hydrothermal vent". Proceedings of the National Academy of Sciences of the United States of America. 102 (26): 9306–10. Bibcode:2005PNAS..102.9306B. doi:10.1073/pnas.0503674102. PMC 1166624. PMID 15967984.
  11. ^ Yang, Shan-Hua; Lee, Sonny T. M.; Huang, Chang-Rung; Tseng, Ching-Hung; Chiang, Pei-Wen; Chen, Chung-Pin; Chen, Hsing-Ju; Tang, Sen-Lin (2016-02-26). "Prevalence of potential nitrogen-fixing, green sulfur bacteria in the skeleton of reef-building coral Isopora palifera". Limnology and Oceanography. 61 (3): 1078–1086. doi:10.1002/lno.10277. ISSN 0024-3590.
  12. ^ See the All-Species Living Tree Project [1]. Data extracted from the "16S rRNA-based LTP release 123 (full tree)" (PDF). Silva Comprehensive Ribosomal RNA Database. Retrieved 2016-03-20.
  13. ^ Hauska G, Schoedl T, Remigy H, Tsiotis G (October 2001). "The reaction center of green sulfur bacteria(1)". Biochimica et Biophysica Acta. 1507 (1–3): 260–77. doi:10.1016/S0005-2728(01)00200-6. PMID 11687219.
  14. ^ a b Ligrone, Roberto (2019). "Moving to the Light: The Evolution of Photosynthesis". In Roberto Ligrone (ed.). Biological Innovations that Built the World: A Four-billion-year Journey through Life and Earth History. Cham: Springer International Publishing. pp. 99–127. doi:10.1007/978-3-030-16057-9_4. ISBN 978-3-030-16057-9. Retrieved 2021-01-29.
  15. ^ a b Bar-Even, Arren; Noor, Elad; Milo, Ron (2012). "A survey of carbon fixation pathways through a quantitative lens". Journal of Experimental Botany. 63 (6): 2325–2342. doi:10.1093/jxb/err417. ISSN 1460-2431. PMID 22200662.
  16. ^ Madigan, Michael T. (1995). "Microbiology of Nitrogen Fixation by Anoxygenic Photosynthetic Bacteria". In Robert E. Blankenship; Michael T. Madigan; Carl E. Bauer (eds.). Anoxygenic Photosynthetic Bacteria. Advances in Photosynthesis and Respiration. Vol. 2. Dordrecht: Springer Netherlands. pp. 915–928. doi:10.1007/0-306-47954-0_42. ISBN 978-0-306-47954-0.

See Also[]

External links[]

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