ArticleFrontiers in microbiology2016
Assembly and Succession of Iron Oxide Microbial Mat Communities in Acidic Geothermal Springs.
Article in Frontiers in microbiology, 2016. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 11 papers.
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11 citing papers in PubMed, 29 citations in OpenAlex.
- Microbial succession and assembly shaped by sulfur, spatial partitioning, and water flow in a volcanic acidic river of northern Patagonia.The ISME journal · 2026Article
- Bacterial community structure in geothermal springs on the northern edge of Qinghai-Tibet plateau.Frontiers in microbiology · 2022Article
- Metaproteogenomic Profiling of Chemosynthetic Microbial Biofilms Reveals Metabolic Flexibility During Colonization of a Shallow-Water Gas Vent.Frontiers in microbiology · 2021Article
- A review of the mechanisms of mineral-based metabolism in early Earth analog rock-hosted hydrothermal ecosystems.World journal of microbiology & biotechnology · 2019Review
- Multiscale analysis of autotroph-heterotroph interactions in a high-temperature microbial community.PLoS computational biology · 2018Article
- Mechanisms of Mineral Substrate Acquisition in a Thermoacidophile.Applied and environmental microbiology · 2018Article
- Marsarchaeota are an aerobic archaeal lineage abundant in geothermal iron oxide microbial mats.Nature microbiology · 2018Article
- Ecological Succession of Sulfur-OxidizingFrontiers in microbiology · 2018Article
- Genomic Comparison of Two Family-Level Groups of the Uncultivated NAG1 Archaeal Lineage from Chemically and Geographically Disparate Hot Springs.Frontiers in microbiology · 2017Article
- Integration of Metagenomic and Stable Carbon Isotope Evidence Reveals the Extent and Mechanisms of Carbon Dioxide Fixation in High-Temperature Microbial Communities.Frontiers in microbiology · 2017Article
- Stoichiometric modelling of assimilatory and dissimilatory biomass utilisation in a microbial community.Environmental microbiology · 2016Article
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Authors and funding
7 authors at 2 institutions in 1 country.
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No grant is acknowledged in the PubMed record.
Abstract
Biomineralized ferric oxide microbial mats are ubiquitous features on Earth, are common in hot springs of Yellowstone National Park (YNP, WY, USA), and form due to direct interaction between microbial and physicochemical processes. The overall goal of this study was to determine the contribution of different community members to the assembly and succession of acidic high-temperature Fe(III)-oxide mat ecosystems. Spatial and temporal changes in Fe(III)-oxide accretion and the abundance of relevant community members were monitored over 70 days using sterile glass microscope slides incubated in the outflow channels of two acidic geothermal springs (pH = 3-3.5; temperature = 68-75°C) in YNP. Hydrogenobaculum spp. were the most abundant taxon identified during early successional stages (4-40 days), and have been shown to oxidize arsenite, sulfide, and hydrogen coupled to oxygen reduction. Iron-oxidizing populations of Metallosphaera yellowstonensis were detected within 4 days, and reached steady-state levels within 14-30 days, corresponding to visible Fe(III)-oxide accretion. Heterotrophic archaea colonized near 30 days, and emerged as the dominant functional guild after 70 days and in mature Fe(III)-oxide mats (1-2 cm thick). First-order rate constants of Fe(III)-oxide accretion ranged from 0.046 to 0.05 day(-1), and in situ microelectrode measurements showed that the oxidation of Fe(II) is limited by the diffusion of O2 into the Fe(III)-oxide mat. The formation of microterracettes also implicated O2 as a major variable controlling microbial growth and subsequent mat morphology. The assembly and succession of Fe(III)-oxide mat communities follows a repeatable pattern of colonization by lithoautotrophic organisms, and the subsequent growth of diverse organoheterotrophs. The unique geochemical signatures and micromorphology of extant biomineralized Fe(III)-oxide mats are also useful for understanding other Fe(II)-oxidizing systems.
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