Pedomicrobium
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| Pedomicrobium | |
|---|---|
| Scientific classification | |
| Domain: | Bacteria |
| Kingdom: | Pseudomonadati |
| Phylum: | Pseudomonadota |
| Class: | Alphaproteobacteria |
| Order: | Hyphomicrobiales |
| Family: | Hyphomicrobiaceae |
| Genus: | Pedomicrobium Aristovskaya 1961[1] |
| Type species | |
| Pedomicrobium ferrugineum[1] | |
| Species | |
Pedomicrobium is a ubiquitous bacterium dominant in biofilms of man-made aquatic environments such as water distribution systems and bioreactors. Due to their abilities to oxidise manganese (Mn), they are found to be the main culprits of Mn related “dirty water” (Sly et al., 1988a).
Taxonomy
Based on 16S rRNA sequence analysis, Pedomicrobium is a bacterium that belongs to the family Hyphomicrobiaceae, within the order of Hyphomicrobiales under the class of Alphaproteobacteria, in the phylum Pseudomonadota (Garrity et al., 2001). There are twenty genera in the family Hyphomicrobiaceae (Williams et al., 1990), of which Pedomicrobium is most closely related to Hyphomicrobium and Filomicrobium (Stahl et al., 1992).
The genus Pedomicrobium consists of four species, with Mn oxidizing and accumulating species represented by Pedomicrobium manganicum and Pedomicrobium americanum, whilst the species Pedomicrobium ferrugineum oxidizes iron but not Mn (Cox and Sly, 1997).
Ecology
Pedomicrobium are budding hyphal bacteria found in both terrestrial and aquatic environments (Sly et al., 1988a). The dimorphic mode of reproduction results in a non-motile form, which has the ability to adhere strongly to surfaces and form biofilm (Sly et al., 1988b). The attached cells take advantage of the nutrients and soluble manganous ions attracted to the solid–liquid interface, which are continually replenished by the water flow (Sly et al., 1988a). Mn oxidising bacteria in biofilms have been shown to greatly enhance the rate of Mn oxidation (Sly et al., 1988b).