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Ecological succession among iron-oxidizing bacteria
Emily J Fleming1, Ivona Cetinić2, Clara S Chan3
1Bigelow Laboratory for Ocean Sciences, East Boothbay, ME, USA.
The ISME Journal
|November 15, 2013
Summary
Species dominance in iron-oxidizing bacterial communities is clarified. Gallionellales thrive in low-carbon, steep redoxcline waters, while Leptothrix ochracea prefers high-carbon, gentle redoxcline environments.
Area of Science:
- Microbiology
- Environmental Science
- Ecology
Background:
- Factors controlling neutrophilic iron-oxidizing bacterial (FeOB) dominance are poorly understood despite extensive research.
- Ecological succession and niche differentiation are key concepts in microbial community dynamics.
Purpose of the Study:
- To investigate the ecological factors driving species dominance in freshwater wetland FeOB communities.
- To elucidate the niche separation between stalk-forming Gallionellales and sheath-forming Leptothrix ochracea.
Main Methods:
- Combined microscopy (light, scanning electron) with cultivation-independent molecular methods (FISH, SSU rRNA gene pyrosequencing).
- Quantified Fe-oxyhydroxide morphotypes and FeOB abundance.
- Analyzed physicochemical parameters of iron mats using redundancy analysis.
Main Results:
- Documented a clear ecological succession: Gallionellales dominated in early spring, transitioning to Leptothrix ochracea for the rest of the year.
- Species-specific FISH probes and SSU rRNA sequencing confirmed the Gallionellales to L. ochracea transition.
- Redundancy analysis revealed distinct environmental niches: Gallionellales favor low organic carbon and steep redoxclines; L. ochracea prefers high organic carbon, high Fe/Mn, and gentle redoxclines.
Conclusions:
- Ecological niches for stalk-forming Gallionellales and sheath-forming L. ochracea are defined by organic carbon levels and redoxcline steepness.
- A significant, previously underappreciated relationship exists between FeOB and organic carbon in aquatic ecosystems.
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