Desulfobacterales

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Desulfobacterales
Stromatolites next to a volcanic lake, found to harbor abundant Desulfobacterales
Scientific classification
Domain:
Phylum:
Class:
Waite et al. 2020
Order:
Desulfobacterales

Kuever, Rainey & Widdel 2006
Families

See text

Desulfobacterales are an order of sulfate-reducing bacteria within the phylum Thermodesulfobacteria.[1] The order contains three families; Desulfobacteraceae, Desulfobulbaceae, and Nitrospinaceae.[2] The bacterium in this order are strict anaerobic respirators, using sulfate or nitrate as the terminal electron acceptor instead of oxygen. Desulfobacterales can degrade ethanol, molecular hydrogen, organic acids, and small hydrocarbons.[3][4] The bacterium of this order have a wide ecological range and play important environmental roles in symbiotic relationships and nutrient cycling.

Habitat

Desulfobacterales are found globally and often in extreme environments, such as deep-sea hydrothermal vents, hot springs, marine sediment, and solfataric fields, an area of volcanic venting that gives off sulfurous gases.[5][6]

Symbiotic relationships

Sulfate-reduction by Desulfobacteraceae and Desulfobulbaceae in coastal marine sediments plays an important role in molecular hydrogen cycling through a close relationship with fermenting microorganisms.[7] Fermenting microbes break down organic materials on the seafloor and produce molecular oxygen and organic acids. Molecular hydrogen is an essential electron donor used by Desulfobacterales; they use the molecular hydrogen produced by fermentation to drive sulfate reduction. This feedback loop maintains molecular hydrogen at an energetically favorable level for fermenting respiration and provides ample molecular hydrogen for sulfate reduction.[7]

Nitrogen cycling

Nitrogen cycle pathways in mangrove ecosystems.

Human activity, such as increased fertilizer use, has caused

Dissimilatory nitrate reduction accounts for roughly 75.7–85.9% of nitrate reduction in mangrove ecosystems.[9] Dissimilatory nitrate reduction is important because nitrate is reduced to ammonium, which can then be taken up by other microorganisms and plants in the system.[9]

Phylogeny

The currently accepted taxonomy is based on the List of Prokaryotic names with Standing in Nomenclature (LPSN)[10] and National Center for Biotechnology Information (NCBI)[11]

16S rRNA based
LTP_08_2023[12][13][14]
120 marker proteins based GTDB 08-RS214[15][16][17]

Desulfonema ishimotoei

Desulfatibacillaceae

Desulforegulaceae

Desulfofabaceae Galushko & Kuever 2021

Desulfatibacillaceae
Waite et al. 2020

"Magnetomoraceae" Waite et al. 2020

Desulfatirhabdiaceae
Waite et al. 2020

"Desulfaltiaceae" Pallen, Rodriguez-R & Alikhan 2022

"Desulfatibiaceae" Pallen, Rodriguez-R & Alikhan 2022

Desulfosarcinaceae Waite et al. 2020

Desulfosudaceae Galushko & Kuever 2021

Desulfosalsimonadaceae Galushko & Kuever 2021

Desulfolunaceae
Waite et al. 2020

Desulforegulaceae
Waite et al. 2020

Desulfobacteraceae Kuever, Rainey & Widdel 2006

See also

References

  1. S2CID 226257730.{{cite journal}}: CS1 maint: numeric names: authors list (link
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  2. ^ "ITIS - Report: Desulfobacterales". www.itis.gov. Retrieved 2022-10-02.
  3. , retrieved 2022-11-06
  4. .
  5. ^ "solfatara | geology". www.britannica.com. Retrieved 2022-11-06.
  6. PMID 21856405
    .
  7. ^ .
  8. .
  9. ^ .
  10. ^ A.C. Parte; et al. "Desulfobacterales". List of Prokaryotic names with Standing in Nomenclature (LPSN). Retrieved 2023-09-09.
  11. ^ Sayers; et al. "Desulfobacterales". National Center for Biotechnology Information (NCBI) taxonomy database. Retrieved 2023-09-09.
  12. ^ "The LTP". Retrieved 20 November 2023.
  13. ^ "LTP_all tree in newick format". Retrieved 20 November 2023.
  14. ^ "LTP_08_2023 Release Notes" (PDF). Retrieved 20 November 2023.
  15. ^ "GTDB release 08-RS214". Genome Taxonomy Database. Retrieved 10 May 2023.
  16. ^ "bac120_r214.sp_label". Genome Taxonomy Database. Retrieved 10 May 2023.
  17. ^ "Taxon History". Genome Taxonomy Database. Retrieved 10 May 2023.