Article,

Olivine-Respiring Bacteria Isolated from the Rock-Ice Interface in a Lava-Tube Cave, a Mars Analog Environment

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Astrobiology, (January 2012)
DOI: 10.1089/ast.2011.0639

Abstract

<p>The boundary between ice and basalt on Earth is an analogue for some near-surface environments of Mars. We investigated neutrophilic iron-oxidizing microorganisms from the basalt-ice interface in a lava tube from the Oregon Cascades with perennial ice. One of the isolates (<em>Pseudomonas</em> sp. HerB) can use ferrous iron Fe(II) from the igneous mineral olivine as an electron donor and O<sub>2</sub> as an electron acceptor. The optimum growth temperature is \~12–14°C, but growth also occurs at 5°C. Bicarbonate is a facultative source of carbon. Growth of <em>Pseudomonas</em>sp. HerB as a chemolithotrophic iron oxidizer with olivine as the source of energy is favored in low O<sub>2</sub> conditions (<em>e.g</em>.<em>,</em> 1.6\% O<sub>2</sub>). Most likely, microbial oxidation of olivine near pH 7 requires low O<sub>2</sub> to offset the abiotic oxidation of iron. The metabolic capabilities of this bacterium would allow it to live in near-surface, icy, volcanic environments of Mars in the present or recent geological past and make this type of physiology a prime candidate in the search for life on Mars. Key Words: Extremophiles—Mars—Olivine—Iron-oxidizing bacteria—Redox. Astrobiology 12, 9–18.</p>

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