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Science 20 October 1995: Vol. 270. no. 5235, pp. 450 - 455 DOI: 10.1126/science.270.5235.450
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Reports
Lithoautotrophic Microbial Ecosystems in Deep Basalt Aquifers
Todd O. Stevens (1)
and
James P. McKinley
Bacterial communities were detected in deep crystalline rock
aquifers within the Columbia River Basalt Group (CRB). CRB ground
waters contained up to 60 µM dissolved H and autotrophic
microorganisms outnumbered heterotrophs. Stable carbon isotope
measurements implied that autotrophic methanogenesis dominated this
ecosystem and was coupled to the depletion of dissolved inorganic
carbon. In laboratory experiments, H , a potential energy
source for bacteria, was produced by reactions between crushed basalt
and anaerobic water. Microcosms containing only crushed basalt and
ground water supported microbial growth. These results suggest that the
CRB contains a lithoautotrophic microbial ecosystem that is independent
of photosynthetic primary production.
Pacific Northwest Laboratory, Post Office Box 999, Richland, WA
99352, USA. E-mail: to_stevens{at}pnl.gov or jp_mckinley{at}pnl.gov
(1) To whom correspondence should be addressed.
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