Evidence map›Paper›PMID 30824745›Full record

ArticleScientific reports2019

New ecosystems in the deep subsurface follow the flow of water driven by geological activity.

G Borgonie, C Magnabosco, A García-Moyano, B Linage-Alvarez, A O Ojo, L B Freese, C Van Jaarsveld, C Van Rooyen, O Kuloyo, E D Cason and 6 more

Abstract read
In one paragraph

Article in Scientific reports, 2019. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 6 papers.

0numbers the graph read from it
0cells of the map it votes in
6citing papers in PubMed
–field-weighted citation impact
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

6 citing papers in PubMed.

  1. Review
  2. Nature communications · 2022
    Article
  3. Geological activity shapes the microbiome in deep-subsurface aquifers by advection.Proceedings of the National Academy of Sciences of the United States of America · 2022
    Article
  4. Article
  5. Article
  6. 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

16 authors.

G BorgonieExtreme Life Isyensya (ELI), PB 65, 9050, Gentbrugge, Belgium. gaebor@eli-deeplife.be.ORCID 0000-0003-1196-8159
C MagnaboscoFlatiron Institute Center for Computational Biology, Simons Foundation, 162 5th Ave., New York, 10010, USA.
A García-MoyanoCentre for Applied Biotechnology, Uni Research AS Thormøhlensgate 55, N-5008, Bergen, Norway.ORCID 0000-0003-1997-8589
B Linage-AlvarezDepartment of Microbial, Biochemical and Food Biotechnology, Swot Street, 9300, Bloemfontein, Republic of South Africa.
A O OjoDepartment of Microbial, Biochemical and Food Biotechnology, Swot Street, 9300, Bloemfontein, Republic of South Africa.
L B FreeseAngloGold Ashanti Kopanang Mine, Private Bag X5010, Vaal Reef, North West, 2621, Republic of South Africa.
C Van JaarsveldNortham Platinum Ltd., Zondereinde Division, Farm Zondereinde 384KQ, District Thabazimbi, Limpopo Province, Republic of South Africa.
C Van RooyenDepartment of Microbial, Biochemical and Food Biotechnology, Swot Street, 9300, Bloemfontein, Republic of South Africa.
O KuloyoDepartment of Geoscience, University of Calgary, 2500 University Drive Northwest Calgary, Alberta, Canada, T2N 1N4.
E D CasonDepartment of Microbial, Biochemical and Food Biotechnology, Swot Street, 9300, Bloemfontein, Republic of South Africa.
J VermeulenDepartment of Microbial, Biochemical and Food Biotechnology, Swot Street, 9300, Bloemfontein, Republic of South Africa.
C PienaarAngloGold Ashanti Kopanang Mine, Private Bag X5010, Vaal Reef, North West, 2621, Republic of South Africa.
E Van HeerdenBiosaense,Walter Sisulu 5, Bloemfontein, 9031, South Africa.
B Sherwood LollarDepartment of Earth Sciences, University of Toronto, 22 Russell Street, Toronto, Ontario, Canada, M5S 3B1.
T C OnstottDepartment of Geosciences, Princeton University, B79 Guyot Hall, Princeton, 08544, New Jersey, USA.
S O C MundleGreat Lakes Institute for Environmental Research, University of Windsor, 401 Sunset Ave., Windsor, ON, Canada, N9B 3P4. smundle@uwindsor.ca.ORCID 0000-0001-5976-9656

Funding

No grant is acknowledged in the PubMed record.

6 · The paper itself

Abstract

Eukarya have been discovered in the deep subsurface at several locations in South Africa, but how organisms reach the subsurface remains unknown. We studied river-subsurface fissure water systems and identified Eukarya from a river that are genetically identical for 18S rDNA. To further confirm that these are identical species one metazoan species recovered from the overlying river interbred successfully with specimen recovered from an underlying mine at -1.4 km. In situ seismic simulation experiments were carried out and show seismic activity to be a major force increasing the hydraulic conductivity in faults allowing organisms to create ecosystems in the deep subsurface. As seismic activity is a non-selective force we recovered specimen of algae and Insecta that defy any obvious other explanation at a depth of -3.4 km. Our results show there is a steady flow of surface organisms to the deep subsurface where some survive and adapt and others perish. As seismic activity is also present on other planets and moons in our solar system the mechanism elucidated here may be relevant for future search and selection of landing sites in planetary exploration.

Identifiers

PMID30824745
PMCPMC6397172

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Registered trials

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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.