Timing and origin of natural gas accumulation in the Siljan impact structure, Sweden
Henrik Drake (),
Nick M. W. Roberts,
Christine Heim,
Martin J. Whitehouse,
Sandra Siljeström,
Ellen Kooijman,
Curt Broman,
Magnus Ivarsson and
Mats E. Åström
Additional contact information
Henrik Drake: Department of Biology and Environmental Science
Nick M. W. Roberts: British Geological Survey
Christine Heim: Geoscience Centre Göttingen of the Georg-August University
Martin J. Whitehouse: Swedish Museum of Natural History
Sandra Siljeström: RISE Research Institutes of Sweden
Ellen Kooijman: Swedish Museum of Natural History
Curt Broman: Stockholm University
Magnus Ivarsson: Swedish Museum of Natural History
Mats E. Åström: Department of Biology and Environmental Science
Nature Communications, 2019, vol. 10, issue 1, 1-14
Abstract:
Abstract Fractured rocks of impact craters may be suitable hosts for deep microbial communities on Earth and potentially other terrestrial planets, yet direct evidence remains elusive. Here, we present a study of the largest crater of Europe, the Devonian Siljan structure, showing that impact structures can be important unexplored hosts for long-term deep microbial activity. Secondary carbonate minerals dated to 80 ± 5 to 22 ± 3 million years, and thus postdating the impact by more than 300 million years, have isotopic signatures revealing both microbial methanogenesis and anaerobic oxidation of methane in the bedrock. Hydrocarbons mobilized from matured shale source rocks were utilized by subsurface microorganisms, leading to accumulation of microbial methane mixed with a thermogenic and possibly a minor abiotic gas fraction beneath a sedimentary cap rock at the crater rim. These new insights into crater hosted gas accumulation and microbial activity have implications for understanding the astrobiological consequences of impacts.
Date: 2019
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Persistent link: https://EconPapers.repec.org/RePEc:nat:natcom:v:10:y:2019:i:1:d:10.1038_s41467-019-12728-y
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DOI: 10.1038/s41467-019-12728-y
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