Evidence map›Paper›PMID 31628335›Full record

ArticleNature communications2019

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, Mats E Åström

Open access · goldAbstract read
In one paragraph

Article in Nature communications, 2019. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 5 papers.

0numbers the graph read from it
0cells of the map it votes in
5citing papers in PubMed
4.5field-weighted citation impact, top 5% of its field
1 · What the graph read from it

What it found

Each row is one number read from the abstract, on the scale the paper reported it, with its interval. Left of the dashed line favours the treatment, right favours the comparator. Under each row is the sentence it came from. New to these charts? A ten-minute tutorial.

The abstract states no effect estimate the extractor could read, or names no intervention and outcome on the map, so this paper lights no cell and moves no belief. It is still indexed, cited and linked below.

2 · The registry

The trial behind it

Trials whose registry record cites this paper, or whose number appears in the abstract. A trial that started after this paper was published is citing it as background, not reporting it.

Neither the registry nor the abstract names a trial number. If this is a trial report, that itself is worth knowing.

3 · Its place in the literature

Who cites it

5 citing papers in PubMed, 52 citations in OpenAlex.

  1. Article
  2. Article
  3. Article
  4. Thermochronologic perspectives on the deep-time evolution of the deep biosphere.Proceedings of the National Academy of Sciences of the United States of America · 2021
    Article
  5. Article
4 · The record

Corrections and comments

PubMed lists nothing against this paper. Absence here is not a guarantee, only a check that was made.

5 · Who and what money

Authors and funding

9 authors at 7 institutions in 5 countries.

Henrik DrakeLinnæus University, Department of Biology and Environmental Science, 39182, Kalmar, Sweden. henrik.drake@lnu.se.ORCID http://orcid.org/0000-0001-7230-6509
Nick M W RobertsGeochronology and Tracers Facility, British Geological Survey, Nottingham, NG12 5GG, UK.ORCID http://orcid.org/0000-0001-8272-5432
Christine HeimDepartment of Geobiology, Geoscience Centre Göttingen of the Georg-August University, Goldschmidtstr. 3, 37077, Göttingen, Germany.ORCID http://orcid.org/0000-0003-4716-9316
Martin J WhitehouseSwedish Museum of Natural History, P.O. Box 50 007, 10405, Stockholm, Sweden.ORCID http://orcid.org/0000-0003-2227-577X
Sandra SiljeströmBioscience and Materials/Chemistry and Materials, RISE Research Institutes of Sweden, Box 5607, 114 86, Stockholm, Sweden.
Ellen KooijmanSwedish Museum of Natural History, P.O. Box 50 007, 10405, Stockholm, Sweden.
Curt BromanDepartment of Geological Sciences, Stockholm University, 106 91, Stockholm, Sweden.
Magnus IvarssonSwedish Museum of Natural History, P.O. Box 50 007, 10405, Stockholm, Sweden.
Mats E ÅströmLinnæus University, Department of Biology and Environmental Science, 39182, Kalmar, Sweden.
Linnaeus University · SESwedish Museum of Natural History · SEBritish Geological Survey · GBRISE Research Institutes of Sweden · SEStockholm University · SEUniversity of Göttingen · DEUniversity of Southern Denmark · DK

Funding

No grant is acknowledged in the PubMed record.

6 · The paper itself

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.

Identifiers

PMID31628335
PMCPMC6802084
OpenAlexW2980438757

What OpenQuestion holds

Textmetadata
LicenceCC BY
Read underepoch 390

Registered trials

None linked

Read under generation 80e0d062 · epoch 390. Bibliography from PubMed, PubMed Central and OpenAlex; grants from NIH RePORTER; trial links from ClinicalTrials.gov; estimates, votes and beliefs from the OpenQuestion graph.