Desulfosporosinus

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Desulfosporosinus
Scientific classification
Domain:
Phylum:
Class:
Order:
Family:
Genus:
Desulfosporosinus

Stackebrandt et al. 1997 [1] [2]
Type species
Desulfosporosinus orientis
(Adams & Postgate 1959) Stackebrandt et al. 1997
Species

See text.

Desulfosporosinus is a genus of strictly anaerobic, sulfate-reducing bacteria, often found in soil.

The type species D. orientis was isolated in 1959 [3] with the proposed name Desulfovibrio orientis, and was later assigned to the genus Desulfotomaculum. [4] Based on 16S rRNA gene sequence data Desulfotomaculum orientis was reclassified as Desulfosporosinus orientis in 1997. [1]

Species

SpeciesType strainIsolated fromNotesReferences
D. acididuransM1 (DSM 27692)Acidic sedimentmoderately acidophilic [5]
D. acidiphilusSJ4 (DSM 22704)Acid mine drainage sedimentmoderately acidophilic [6]
D. auripigmentiOREX-4 (DSM 13351)Freshwater sediment( [7] ) [8]
D. burensisBSREI1 (DSM 24089)Borehole [9]
D. fructosivorans63.6F (DSM140297)Marine subsurface sediment [10]
D. hippei343 (DSM 8344)Permafrost soil [2]
D. lacusSTP12 (DSM 15449)Freshwater sediment [11]
D. meridieiS10 (DSM 13257)Gasolene-contaminated groundwater [12]
D. nitroreducens59.4B (DSM 140295)Marine subsurface sediment [13]
D. orientisSingapore I (DSM 765)Soil( [3] [4] ) [1]
D. youngiaeJW/YJL-B18 (DSM 17734)Constructed wetland / acid mine drainage sediment [14]

Genomes

Five complete Desulfosporosinus genomes are available, and another two genomes are in the progress of being sequenced.

StrainStatusYearAccession numberReferences
D. acididurans M1Published draft2015 LDZY00000000 [15]
D. acidiphilus SJ4Complete and published2012 CP003639 [16]
D. meridiei S10Complete and published2012 CP003629 [16]
D. orientis Singapore IComplete and published2011 CP003108 [16]
D. sp. OTComplete and published2011 AGAF00000000 [17]
D. youngiae JW/YJL-B18Complete and published2011 CM001441 [16]

Phylogeny

The currently accepted taxonomy is based on the List of Prokaryotic names with Standing in Nomenclature (LPSN) [18] and National Center for Biotechnology Information (NCBI) [19]

16S rRNA based LTP_08_2023 [20] [21] [22] 120 marker proteins based GTDB 08-RS214 [23] [24] [25]
Desulfosporosinus

D. orientis (Adams & Postgate 1959) Stackebrandt et al. 1997

D. metalliduransPanova et al. 2021

D. acididuransSanchez-Andrea et al. 2015

D. acidiphilusAlazard et al. 2012

D. youngiaeLee, Romanek & Wiegel 2009

D. auripigmenticorrig. (Newman et al. 2000) Stackebrandt et al. 2003

D. hippeiVatsurina et al. 2008

D. meridieiRobertson et al. 2001

D. fructosivoransVandieken et al. 2017

D. lacusRamamoorthy et al. 2006

D. burensisMayeux et al. 2013

D. nitroreducensVandieken et al. 2017

Desulfosporosinus

D. acididurans

D. acidiphilus

D. metallidurans

D. fructosivorans

"Ca. D. infrequens" Hausmann et al. 2019

D. orientis

D. youngiae

D. lacus

D. nitroreducens

D. hippei

D. meridiei

See also

Related Research Articles

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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">Campylobacterota</span> Class of bacteria

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References

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