Evidence map›Paper›PMID 28614348›Full record

ArticlePloS one2017

Organic compounds in fluid inclusions of Archean quartz-Analogues of prebiotic chemistry on early Earth.

Ulrich Schreiber, Christian Mayer, Oliver J Schmitz, Pia Rosendahl, Amela Bronja, Markus Greule, Frank Keppler, Ines Mulder, Tobias Sattler, Heinz F Schöler

Open access · goldAbstract read
In one paragraph

Article in PloS one, 2017. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 10 papers.

0numbers the graph read from it
0cells of the map it votes in
10citing papers in PubMed
2.2field-weighted citation impact, top 13% 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

10 citing papers in PubMed, 34 citations in OpenAlex.

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  8. Water is a preservative of microbes.Microbial biotechnology · 2022
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  10. Molecular Evolution in a Peptide-Vesicle System.Life (Basel, Switzerland) · 2018
    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

10 authors at 2 institutions in 1 country.

Ulrich SchreiberDepartment of Geology, University Duisburg-Essen, Universitaetsstr. 5, Essen, Germany.
Christian MayerFaculty of Chemistry, CeNIDE, University Duisburg-Essen, Universitaetsstr. 5, Essen, Germany.
Oliver J SchmitzFaculty of Chemistry, Applied Analytical Chemistry, University Duisburg-Essen, Universitaetsstr. 5, Essen, Germany.
Pia RosendahlFaculty of Chemistry, Applied Analytical Chemistry, University Duisburg-Essen, Universitaetsstr. 5, Essen, Germany.
Amela BronjaFaculty of Chemistry, Applied Analytical Chemistry, University Duisburg-Essen, Universitaetsstr. 5, Essen, Germany.
Markus GreuleInstitute of Earth Sciences, Ruprecht Karls University Heidelberg, Im Neuenheimer Feld 234-236, Heidelberg, Germany.
Frank KepplerInstitute of Earth Sciences, Ruprecht Karls University Heidelberg, Im Neuenheimer Feld 234-236, Heidelberg, Germany.
Ines MulderInstitute of Earth Sciences, Ruprecht Karls University Heidelberg, Im Neuenheimer Feld 234-236, Heidelberg, Germany.
Tobias SattlerInstitute of Earth Sciences, Ruprecht Karls University Heidelberg, Im Neuenheimer Feld 234-236, Heidelberg, Germany.
Heinz F SchölerInstitute of Earth Sciences, Ruprecht Karls University Heidelberg, Im Neuenheimer Feld 234-236, Heidelberg, Germany.
Heidelberg University · DEUniversity of Duisburg-Essen · DE

Funding

No grant is acknowledged in the PubMed record.

6 · The paper itself

Abstract

The origin of life is still an unsolved mystery in science. Hypothetically, prebiotic chemistry and the formation of protocells may have evolved in the hydrothermal environment of tectonic fault zones in the upper continental crust, an environment where sensitive molecules are protected against degradation induced e.g. by UV radiation. The composition of fluid inclusions in minerals such as quartz crystals which have grown in this environment during the Archean period might provide important information about the first organic molecules formed by hydrothermal synthesis. Here we present evidence for organic compounds which were preserved in fluid inclusions of Archean quartz minerals from Western Australia. We found a variety of organic compounds such as alkanes, halocarbons, alcohols and aldehydes which unambiguously show that simple and even more complex prebiotic organic molecules have been formed by hydrothermal processes. Stable-isotope analysis confirms that the methane found in the inclusions has most likely been formed from abiotic sources by hydrothermal chemistry. Obviously, the liquid phase in the continental Archean crust provided an interesting choice of functional organic molecules. We conclude that organic substances such as these could have made an important contribution to prebiotic chemistry which might eventually have led to the formation of living cells.

Indexed as

Earth, PlanetHumansMethaneOrigin of LifePrebioticsQuartzWaterWestern AustraliaMethanePrebioticsQuartzWater

Identifiers

PMID28614348
PMCPMC5470662
OpenAlexW2889658722

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.