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Modern water/rock reactions in Oman hyperalkaline peridotite aquifers and implications for microbial habitability



Details

  • Journal Title:
    Geochimica et Cosmochimica Acta
  • Personal Author:
  • NOAA Program & Office:
  • Description:
    The Samail ophiolite in Oman is undergoing modern hydration and carbonation of peridotite and may host a deep subsurface biosphere. Previous investigations of hyperalkaline fluids in Oman have focused on fluids released at surface seeps, which quickly lose their reducing character and precipitate carbonates upon contact with the O2/CO2-rich atmosphere. In this work, geochemical analysis of rocks and fluids from the subsurface provides new insights into the operative reactions in serpentinizing aquifers. Serpentinite rock and hyperalkaline fluids (pH > 10), which exhibit millimolar concentrations of Ca2+, H2 and CH4, as well as variable sulfate and nitrate, were accessed from wells situated in mantle peridotite near Ibra and studied to investigate their aqueous geochemistry, gas concentrations, isotopic signatures, mineralogy, Fe speciation and microbial community composition.
  • Source:
    Geochimica et Cosmochimica Acta, 179, 217-241
  • DOI:
  • ISSN:
    0016-7037
  • Format:
  • Publisher:
  • Document Type:
  • Rights Information:
    Accepted Manuscript
  • Rights Statement:
    The NOAA IR provides access to this content under the authority of the government's retained license to distribute publications and data resulting from federal funding. While users may legally access this content, the copyright owners retain rights that govern the reproduction, redistribution, and re-use of this work. The user is solely responsible for complying with applicable copyright law.
  • Compliance:
    Library
  • Main Document Checksum:
    urn:sha-512:77a08513848835c263a155f792461902bed4cd2f9b94e8b8a9aabe8a0316e945956bdfaf4d12f84070dc083fcb2e6ccd3d461eb3a2aa629e24bb2b6965c61058
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    Filetype[PDF - 2.13 MB ]
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