Long-Term Sustainability of a High-Energy, Low-Diversity Crustal Biome

Author:

Lin Li-Hung12345,Wang Pei-Ling12345,Rumble Douglas12345,Lippmann-Pipke Johanna12345,Boice Erik12345,Pratt Lisa M.12345,Lollar Barbara Sherwood12345,Brodie Eoin L.12345,Hazen Terry C.12345,Andersen Gary L.12345,DeSantis Todd Z.12345,Moser Duane P.12345,Kershaw Dave12345,Onstott T. C.12345

Affiliation:

1. Department of Geosciences, Princeton University, Princeton, NJ, USA.

2. Department of Geosciences, National Taiwan University, Taipei, Taiwan.

3. Institute of Oceanography, National Taiwan University, Taipei, Taiwan.

4. Geophysical Laboratory, Carnegie Institution of Washington, Washington, DC, USA.

5. GeoForschungsZentrum Potsdam, Telegrafenberg, Potsdam, Germany.

Abstract

Geochemical, microbiological, and molecular analyses of alkaline saline groundwater at 2.8 kilometers depth in Archaean metabasalt revealed a microbial biome dominated by a single phylotype affiliated with thermophilic sulfate reducers belonging to Firmicutes . These sulfate reducers were sustained by geologically produced sulfate and hydrogen at concentrations sufficient to maintain activities for millions of years with no apparent reliance on photosynthetically derived substrates.

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

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