Assembly and Succession of Iron Oxide Microbial Mat Communities in Acidic Geothermal Springs

dc.contributor.authorBeam, Jacob P.
dc.contributor.authorBernstein, Hans C.
dc.contributor.authorJay, Zackary J.
dc.contributor.authorKozubal, Mark A.
dc.contributor.authorJennings, Ryan deM.
dc.contributor.authorTringe, Susannah G.
dc.contributor.authorInskeep, William P.
dc.date.accessioned2016-08-01T18:35:02Z
dc.date.available2016-08-01T18:35:02Z
dc.date.issued2016-02
dc.description.abstractBiomineralized 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.en_US
dc.description.sponsorship(subcontract 112443); (CSP 787081 and 787701); (DGE 0654336); No. DE-AC02-05CH11231; (YELL-SCI-5068)en_US
dc.identifier.citationBeam, Jacob P. , Hans C. Bernstein, Zackary J. Jay, Mark A. Kozubal, Ryan M. de Jennings, Susannah G. Tringe, and William P. Inskeep. "Assembly and Succession of Iron Oxide Microbial Mat Communities in Acidic Geothermal Springs." Frontiers in Microbiology 7 (February 2016). DOI: 10.3389/fmicb.2016.00025.en_US
dc.identifier.issn1664-302X
dc.identifier.urihttps://scholarworks.montana.edu/handle/1/9953
dc.rightsCC BY 4.0en_US
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/legalcodeen_US
dc.titleAssembly and Succession of Iron Oxide Microbial Mat Communities in Acidic Geothermal Springsen_US
dc.typeArticleen_US
mus.citation.journaltitleFrontiers in Microbiologyen_US
mus.citation.volume7en_US
mus.contributor.orcidBernstein, Hans C.|0000-0003-2913-7708en_US
mus.data.thumbpage3en_US
mus.identifier.categoryChemical & Material Sciencesen_US
mus.identifier.categoryEngineering & Computer Scienceen_US
mus.identifier.categoryLife Sciences & Earth Sciencesen_US
mus.identifier.doi10.3389/fmicb.2016.00025en_US
mus.relation.collegeCollege of Agricultureen_US
mus.relation.collegeCollege of Letters & Scienceen_US
mus.relation.departmentCenter for Biofilm Engineering.en_US
mus.relation.departmentChemical & Biological Engineering.en_US
mus.relation.departmentLand Resources & Environmental Sciences.en_US
mus.relation.researchgroupCenter for Biofilm Engineering.en_US
mus.relation.researchgroupThermal Biology Institute.en_US
mus.relation.universityMontana State University - Bozemanen_US

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