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''Chlorobium'' (also known as ''Chlorochromatium'') is a genus of green sulfur bacteria. They are photolithotrophic oxidizers of sulfur and most notably utilise a noncyclic electron transport chain to reduce NAD+. Photosynthesis is achieved using a Type 2 Reaction Centre using bacteriochlorophyll (BChl) ''a'' and in chlorosomes which employ BChl ''c'', ''d'', or ''e''; in addition chlorophyll ''a'' is also present. Hydrogen sulfide is used as an electron source and carbon dioxide its carbon source.〔Prescott, Harley, Klein. (2005). ''Microbiology'' pp. 195, 493, 597, 618-619, 339.〕 ''Chlorobium'' species exhibit a dark green color; in a Winogradsky column, the green layer often observed is composed of ''Chlorobium''. This genus lives in strictly anaerobic conditions below the surface of a body of water, commonly the anaerobic zone of a eutrophic lake.〔 ''Chlorobium aggregatum'' is a species which exists in a symbiotic relationship with a colorless, nonphotosynthetic bacteria. This species looks like a bundle of green bacteria, attached to a central rod-like cell which can move around with a flagellum. The green, outer bacteria use light to oxidize sulfide into sulfate. The inner cell, which is not able to perform photosynthesis, reduces the sulfate into sulfide. These bacteria divide in unison, giving the structure a multicellular appearance which is highly unusual in bacteria.〔Postgate, John: "The Outer Reaches of Life", page 132-134. Cambridge University Press, 1994〕 ''Chlorobium'' species are thought to have played an important part in mass extinction events on Earth. If the oceans turn anoxic (due to the shutdown of ocean circulation) then ''Chlorobium'' would be able to out compete other photosynthetic life. They would produce huge quantities of methane and hydrogen sulfide which would cause global warming and acid rain. This would have huge consequences for other oceanic organisms and also for terrestrial organisms. Evidence for abundant ''Chlorobium'' populations is provided by chemical fossils found in sediments deposited at the Cretaceous mass extinction. The complete ''C. tepidum'' genome, which consists of 2.15 megabases (Mb), was sequenced and published in 2002.〔 〕 It synthesizes chlorophyll ''a'' and bacteriochlorophylls (BChls) ''a'' and ''c'', of which the model organism has been used to elucidate the biosynthesis of BChl ''c''.〔 〕 Several of its carotenoid metabolic pathways (including a novel lycopene cyclase) have similar counterparts in cyanobacteria.〔 〕〔 〕 ==Molecular signatures for ''Chlorobi''== Comparative genomic analysis has led to the identification of 2 conserved signature indels which are uniquely found in members of the phylum ''Chlorobi'' and are thus characteristic of the phylum. The first indel is a 28-amino-acid insertion in DNA polymerase III and the second is a 12 to 14 amino acid insertion in alanyl-tRNA synthetase. These indels are not found in any other bacteria and thus serve as molecular markers for the phylum. In addition to the conserved signature indels, 51 proteins which are uniquely found in members of the phylum ''Chlorobi''. 65 other proteins have been identified which are unique to the ''Chlorobi'' phylum, however these proteins are missing in several ''Chlorobi'' species and are not distributed throughout the phylum with any clear pattern. This means that significant gene loss may have occurred, or the presence of these proteins may be a result of horizontal gene transfer. Of these 65 proteins, 8 are found only in ''Chlorobium luteolum'' and ''Chlorobium phaeovibrioides''. These two species form a strongly supported clade in phylogenetic trees and a close relationship between these species is further supported by the unique sharing of these 8 proteins.〔Gupta, R. S. and Lorenzini, E. (2007). Phylogeny and molecular signatures (conserved proteins and indels) that are specific for the Bacteroidetes and Chlorobi species. BMC Evolutionary Biology. 7:71. doi:10.1186/1471-2148-7-71.〕 抄文引用元・出典: フリー百科事典『 ウィキペディア（Wikipedia）』 ■ウィキペディアで「Chlorobium」の詳細全文を読む スポンサード リンク
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