| Aerophobota | |
|---|---|
| Scientific classification | |
| Domain: | |
| Phylum: | "Aerophobota" corrig. Rinke et al., 2013 |
| Class | |
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| Synonyms | |
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Aerophobota is a candidate bacterial phylum within the domain Bacteria. This phylum is found mainly in deep-sea, hydrocarbon-rich sediments, especially those associated with methane hydrates. Aerophobota is notable for its likely involvement in organic carbon and methane cycling in anoxic, deep ocean sediment environments. [1]
The classification is based on genomic and metagenomic data without cultured isolates, and the name is not yet validly published under formal bacterial nomenclature. [1] [2] [3]
Aerophobetes are abundant in hydrate-containing, silty sediment layers beneath the ocean floor and thrive in anoxic (oxygen-free) conditions. [4] Genetic analyses suggest they ferment organic matter, producing hydrogen and acetate, which can then be used by syntrophic methanogenic archaea to generate methane. [5] These metabolic interactions indicate Aerophobota's likely contribution to methane formation and carbon cycling in deep-sea ecosystems. [6] [7]
Research into Aerophobota and its functional roles is of interest because methane is a potent greenhouse gas. [8] Understanding these microbes could inform strategies for mitigating methane emissions from seafloor hydrates. [9]