Desulfobacterales

Desulfobacterales are an order of sulfate-reducing bacteria within the phylum Thermodesulfobacteria.<ref>Template:Cite journal</ref> The bacteria 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.<ref>Template:Citation</ref><ref>Template:Cite journal</ref> They 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.<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref><ref>Template:Cite journal</ref>

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.<ref name=":0">Template:Cite journal</ref> 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.<ref name=":0" />

Nitrogen cycling

Nitrogen cycle pathways in mangrove ecosystems.

Human activity, such as increased fertilizer use, has caused nitrogen pollution in inland and coastal waters. An influx of nitrogen inputs into aquatic ecosystems can cause negative effects such as eutrophication, resulting in anoxic conditions.<ref>Template:Cite journal</ref> Desulfobacterales are important in nitrogen pollution mitigation in coastal mangrove ecosystems through nitrate reduction.<ref name=":1">Template:Cite journal</ref> Nitrate is reduced by Desulfobacterales species via dissimilatory nitrate reduction genes. Dissimilatory nitrate reduction accounts for roughly 75.7–85.9% of nitrate reduction in mangrove ecosystems.<ref name=":1" /> 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.<ref name=":1" />

Phylogeny

The currently accepted taxonomy is based on the List of Prokaryotic names with Standing in Nomenclature (LPSN)<ref name=LPSN>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> and National Center for Biotechnology Information (NCBI)<ref name=NCBI>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref>

16S rRNA based LTP_10_2024<ref>{{#invoke:citation/CS1|citation	CitationClass=web }}</ref><ref>{{#invoke:citation/CS1|citation	CitationClass=web }}</ref><ref>{{#invoke:citation/CS1|citation	CitationClass=web }}</ref>	120 marker proteins based GTDB 09-RS220<ref name="about">{{#invoke:citation/CS1|citation	CitationClass=web }}</ref><ref name="tree">{{#invoke:citation/CS1|citation	CitationClass=web }}</ref><ref name="taxon_history">{{#invoke:citation/CS1|citation	CitationClass=web }}</ref>