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Nat Commun. 2016 Oct 14;7:12770. doi: 10.1038/ncomms12770.

Reconstructing a hydrogen-driven microbial metabolic network in Opalinus Clay rock.

Author information

1
Ecole Polytechnique Fédérale de Lausanne, Environmental Microbiology Laboratory, Station 6, Lausanne CH-1015, Switzerland.
2
Oak Ridge National Laboratory, Chemical Sciences Division, Oak Ridge, Tennessee 37831, USA.
3
Bioinformatics Infrastructure for Life Sciences (BILS), Stockholm 171 65, Sweden.
4
KTH Royal Institute of Technology, Science for Life Laboratory, School of Biotechnology, Division of Gene Technology, Stockholm 171 65, Sweden.
5
Nagra, Wettingen CH-5430, Switzerland.

Abstract

The Opalinus Clay formation will host geological nuclear waste repositories in Switzerland. It is expected that gas pressure will build-up due to hydrogen production from steel corrosion, jeopardizing the integrity of the engineered barriers. In an in situ experiment located in the Mont Terri Underground Rock Laboratory, we demonstrate that hydrogen is consumed by microorganisms, fuelling a microbial community. Metagenomic binning and metaproteomic analysis of this deep subsurface community reveals a carbon cycle driven by autotrophic hydrogen oxidizers belonging to novel genera. Necromass is then processed by fermenters, followed by complete oxidation to carbon dioxide by heterotrophic sulfate-reducing bacteria, which closes the cycle. This microbial metabolic web can be integrated in the design of geological repositories to reduce pressure build-up. This study shows that Opalinus Clay harbours the potential for chemolithoautotrophic-based system, and provides a model of microbial carbon cycle in deep subsurface environments where hydrogen and sulfate are present.

PMID:
27739431
PMCID:
PMC5067608
DOI:
10.1038/ncomms12770
[Indexed for MEDLINE]
Free PMC Article

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