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Fine-Scale Biogeography and the Inference of Ecological Interactions Among Neutrophilic Iron-Oxidizing Zetaproteobacteria as Determined by a Rule-Based Microbial Network
2019
Frontiers in Microbiology
Hydrothermal vents, such as those at Lō'ihi Seamount and the Mariana Arc and back-arc, release iron required to support life from the Earth's crust. In these ecosystems, bacteria and archaea can oxidize the released iron and therefore play an important role in the biogeochemical cycles of essential nutrients. These organisms often form microbial mats, and the primary producers in these communities can support diverse higher trophic levels. One such class of bacteria are the Zetaproteobacteria.
doi:10.3389/fmicb.2019.02389
pmid:31708884
pmcid:PMC6823593
fatcat:ucxkwzi6wjfoxktf3x3ia43i6i