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Assembly and Succession of Iron Oxide Microbial Mat Communities in Acidic Geothermal Springs
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...
Autores principales: | , , , , , , |
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Formato: | Online Artículo Texto |
Lenguaje: | English |
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Frontiers Media S.A.
2016
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Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4753309/ https://www.ncbi.nlm.nih.gov/pubmed/26913020 http://dx.doi.org/10.3389/fmicb.2016.00025 |
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author | Beam, Jacob P. Bernstein, Hans C. Jay, Zackary J. Kozubal, Mark A. Jennings, Ryan deM. Tringe, Susannah G. Inskeep, William P. |
author_facet | Beam, Jacob P. Bernstein, Hans C. Jay, Zackary J. Kozubal, Mark A. Jennings, Ryan deM. Tringe, Susannah G. Inskeep, William P. |
author_sort | Beam, Jacob P. |
collection | PubMed |
description | 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 O(2) into the Fe(III)-oxide mat. The formation of microterracettes also implicated O(2) 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. |
format | Online Article Text |
id | pubmed-4753309 |
institution | National Center for Biotechnology Information |
language | English |
publishDate | 2016 |
publisher | Frontiers Media S.A. |
record_format | MEDLINE/PubMed |
spelling | pubmed-47533092016-02-24 Assembly and Succession of Iron Oxide Microbial Mat Communities in Acidic Geothermal Springs Beam, Jacob P. Bernstein, Hans C. Jay, Zackary J. Kozubal, Mark A. Jennings, Ryan deM. Tringe, Susannah G. Inskeep, William P. Front Microbiol Microbiology 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 O(2) into the Fe(III)-oxide mat. The formation of microterracettes also implicated O(2) 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. Frontiers Media S.A. 2016-02-15 /pmc/articles/PMC4753309/ /pubmed/26913020 http://dx.doi.org/10.3389/fmicb.2016.00025 Text en Copyright © 2016 Beam, Bernstein, Jay, Kozubal, Jennings, Tringe and Inskeep. http://creativecommons.org/licenses/by/4.0/ This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY). The use, distribution or reproduction in other forums is permitted, provided the original author(s) or licensor are credited and that the original publication in this journal is cited, in accordance with accepted academic practice. No use, distribution or reproduction is permitted which does not comply with these terms. |
spellingShingle | Microbiology Beam, Jacob P. Bernstein, Hans C. Jay, Zackary J. Kozubal, Mark A. Jennings, Ryan deM. Tringe, Susannah G. Inskeep, William P. Assembly and Succession of Iron Oxide Microbial Mat Communities in Acidic Geothermal Springs |
title | Assembly and Succession of Iron Oxide Microbial Mat Communities in Acidic Geothermal Springs |
title_full | Assembly and Succession of Iron Oxide Microbial Mat Communities in Acidic Geothermal Springs |
title_fullStr | Assembly and Succession of Iron Oxide Microbial Mat Communities in Acidic Geothermal Springs |
title_full_unstemmed | Assembly and Succession of Iron Oxide Microbial Mat Communities in Acidic Geothermal Springs |
title_short | Assembly and Succession of Iron Oxide Microbial Mat Communities in Acidic Geothermal Springs |
title_sort | assembly and succession of iron oxide microbial mat communities in acidic geothermal springs |
topic | Microbiology |
url | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4753309/ https://www.ncbi.nlm.nih.gov/pubmed/26913020 http://dx.doi.org/10.3389/fmicb.2016.00025 |
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