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dc.contributor.authorCousins, Claire R.
dc.contributor.authorFogel, Marilyn
dc.contributor.authorBowden, Roxane
dc.contributor.authorCrawford, Ian
dc.contributor.authorBoyce, Adrian
dc.contributor.authorCockell, Charles
dc.contributor.authorGunn, Matthew
dc.identifier.citationCousins , C R , Fogel , M , Bowden , R , Crawford , I , Boyce , A , Cockell , C & Gunn , M 2018 , ' Biogeochemical probing of microbial communities in a basalt-hosted hot spring at Kverkfjöll volcano, Iceland ' , Geobiology , vol. 16 , no. 5 , pp. 507-521 .
dc.identifier.otherPURE: 253289654
dc.identifier.otherPURE UUID: 3d16ad7b-9b86-4b7e-a816-b6bf112cc209
dc.identifier.othercrossref: 10.1111/gbi.12291
dc.identifier.otherScopus: 85052496419
dc.identifier.otherORCID: /0000-0002-3954-8079/work/60196580
dc.identifier.otherWOS: 000441436700004
dc.descriptionThis work was funded by a The Leverhulme Trust Research Project Grant to I. Crawford (F/07 112/AA). C. Cousins is funded by a Royal Society of Edinburgh Research Fellowship. Stable isotope analyses at the Carnegie Institution of Washington, USA, were funded by a grant from the W. M. Keck Foundation (2007-6-29) and through the NASA Astrobiology grant (NNH082ZDA0002C) to M. Fogel.en
dc.description.abstractWe investigated bacterial and archaeal communities along an ice‐fed surficial hot spring at Kverkfjöll volcano—a partially ice‐covered basaltic volcano at Vatnajökull glacier, Iceland, using biomolecular (16S rRNA, apsA, mcrA, amoA, nifH genes) and stable isotope techniques. The hot spring environment is characterized by high temperatures and low dissolved oxygen concentrations at the source (68°C and <1 mg/L (±0.1%)) changing to lower temperatures and higher dissolved oxygen downstream (34.7°C and 5.9 mg/L), with sulfate the dominant anion (225 mg/L at the source). Sediments are comprised of detrital basalt, low‐temperature alteration phases and pyrite, with <0.4 wt. % total organic carbon (TOC). 16S rRNA gene profiles reveal that organisms affiliated with Hydrogenobaculum (54%–87% bacterial population) and Thermoproteales (35%–63% archaeal population) dominate the micro‐oxic hot spring source, while sulfur‐oxidizing archaea (Sulfolobales, 57%–82%), and putative sulfur‐oxidizing and heterotrophic bacterial groups dominate oxic downstream environments. The δ13Corg (‰ V‐PDB) values for sediment TOC and microbial biomass range from −9.4‰ at the spring's source decreasing to −12.6‰ downstream. A reverse effect isotope fractionation of ~3‰ between sediment sulfide (δ34S ~0‰) and dissolved water sulfate (δ34S +3.2‰), and δ18O values of ~ −5.3‰ suggest pyrite forms abiogenically from volcanic sulfide, followed by abiogenic and microbial oxidation. These environments represent an unexplored surficial geothermal environment analogous to transient volcanogenic habitats during putative “snowball Earth” scenarios and volcano–ice geothermal environments on Mars.
dc.rights© 2018 John Wiley & Sons Ltd. This work has been made available online in accordance with the publisher’s policies. This is the author created, accepted version manuscript following peer review and may differ slightly from the final published version. The final published version of this work is available at
dc.subjectQE Geologyen
dc.subjectQH301 Biologyen
dc.subjectQD Chemistryen
dc.titleBiogeochemical probing of microbial communities in a basalt-hosted hot spring at Kverkfjöll volcano, Icelanden
dc.typeJournal articleen
dc.contributor.institutionUniversity of St Andrews.School of Earth & Environmental Sciencesen
dc.contributor.institutionUniversity of St Andrews.St Andrews Centre for Exoplanet Scienceen
dc.description.statusPeer revieweden

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