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dc.contributor.authorFortney, Nathaniel W.
dc.contributor.authorHe, Shaomei
dc.contributor.authorKulkarni, Ajinkya
dc.contributor.authorHolz, Charlotte
dc.contributor.authorBoyd, Eric S.
dc.contributor.authorRoden, Eric E.
dc.date.accessioned2018-10-03T20:29:13Z
dc.date.available2018-10-03T20:29:13Z
dc.date.issued2018-06
dc.identifier.citationFortney, Nathaniel W. , Shaomei He, Ajinkya Kulkarni, Michael W. Friedrich, Charlotte Holz, Eric S. Boyd, and Eric E. Roden. "Stable isotope probing of microbial iron reduction in Chocolate Pots hot spring, Yellowstone National Park." Applied and Environmental Microbiology 84, issue 11 (June 2018). DOI:10.1128/AEM.02894-17.en_US
dc.identifier.issn0099-2240
dc.identifier.urihttps://scholarworks.montana.edu/xmlui/handle/1/14886
dc.description.abstractChocolate Pots hot springs (CP) is a circumneutral pH, Fe-rich geothermal feature located in Yellowstone National Park. Previous Fe(III)-reducing enrichment culture studies with CP sediments identified close relatives of known dissimilatory Fe(III)-reducing bacterial (FeRB) taxa, including Geobacter and Melioribacter However, the abundance and activity of such organisms in the native microbial community is unknown. Here we used stable isotope probing experiments combined with 16S rRNA gene amplicon and shotgun metagenomic sequencing to gain an understanding of the in situ Fe(III)-reducing microbial community at CP. Fe-Si oxide precipitates collected near the hot spring vent were incubated with unlabeled and 13C-labeled acetate to target active FeRB. We searched reconstructed genomes for homologs of genes involved in known extracellular electron transfer (EET) systems to identify taxa involved in Fe redox transformations. Known FeRB taxa containing putative EET systems (Geobacter, Ignavibacteria) increased in abundance under acetate-amended conditions, whereas genomes related to Ignavibacterium, and Thermodesulfovibrio that contained putative EET systems were recovered from no electron donor incubations. Our results suggest FeRB play an active role in Fe redox cycling within Fe-Si oxide-rich deposits located at the hot spring vent.IMPORTANCE The identification of past near-surface hydrothermal environments on Mars emphasizes the importance of using modern Earth environments such as CP to gain insight into potential Fe-based microbial life on other rocky worlds, as well as ancient Fe-rich Earth ecosystems. By combining stable carbon isotope probing techniques and DNA sequencing technology, we gained insight into pathways of microbial Fe redox cycling at CP. The results suggest that microbial Fe(III) oxide reduction is prominent in situ, with important implications for generation of geochemical and stable Fe isotopic signatures of microbial Fe redox metabolism within Fe-rich circumneutral-pH thermal spring environments on Earth and Mars.en_US
dc.language.isoenen_US
dc.rightsThis Item is protected by copyright and/or related rights. You are free to use this Item in any way that is permitted by the copyright and related rights legislation that applies to your use. For other uses you need to obtain permission from the rights-holder(s).en_US
dc.rights.urihttp://rightsstatements.org/vocab/InC/1.0/en_US
dc.titleStable isotope probing of microbial iron reduction in Chocolate Pots hot spring, Yellowstone National Parken_US
dc.typeArticleen_US
mus.citation.issue11en_US
mus.citation.journaltitleApplied and Environmental Microbiologyen_US
mus.citation.volume84en_US
mus.identifier.categoryLife Sciences & Earth Sciencesen_US
mus.identifier.doi10.1128/AEM.02894-17en_US
mus.relation.collegeCollege of Letters & Scienceen_US
mus.relation.departmentMicrobiology & Immunology.en_US
mus.relation.universityMontana State University - Bozemanen_US
mus.data.thumbpage3en_US


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