Evidence map›Paper›PMID 30682803›Full record

ArticleLife (Basel, Switzerland)2019

Origin of Life's Building Blocks in Carbon- and Nitrogen-Rich Surface Hydrothermal Vents.

Paul B Rimmer, Oliver Shorttle

Open access · goldAbstract read
In one paragraph

Article in Life (Basel, Switzerland), 2019. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 34 papers.

0numbers the graph read from it
0cells of the map it votes in
34citing papers in PubMed
6.0field-weighted citation impact, top 4% 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

34 citing papers in PubMed, 89 citations in OpenAlex.

  1. Highly diverse diazotrophs drive high NFundamental research · 2026
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  7. Exploring the influence of atmospheric COApplied and environmental microbiology · 2024
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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

2 authors at 2 institutions in 1 country.

Paul B RimmerDepartment of Earth Sciences, University of Cambridge, Downing Street, Cambridge CB2 3EQ, UK. pbr27@cam.ac.uk.ORCID 0000-0002-7180-081X
Oliver ShorttleDepartment of Earth Sciences, University of Cambridge, Downing Street, Cambridge CB2 3EQ, UK. os258@cam.ac.uk.ORCID 0000-0002-8713-1446
MRC Laboratory of Molecular Biology · GBUniversity of Cambridge · GB

Funding

Medical Research Council MC_UP_A024_1009Simons Foundation SCOL awards 599634
6 · The paper itself

Abstract

There are two dominant and contrasting classes of origin of life scenarios: those predicting that life emerged in submarine hydrothermal systems, where chemical disequilibrium can provide an energy source for nascent life; and those predicting that life emerged within subaerial environments, where UV catalysis of reactions may occur to form the building blocks of life. Here, we describe a prebiotically plausible environment that draws on the strengths of both scenarios: surface hydrothermal vents. We show how key feedstock molecules for prebiotic chemistry can be produced in abundance in shallow and surficial hydrothermal systems. We calculate the chemistry of volcanic gases feeding these vents over a range of pressures and basalt C/N/O contents. If ultra-reducing carbon-rich nitrogen-rich gases interact with subsurface water at a volcanic vent they result in 10 - 3 ⁻ 1 M concentrations of diacetylene (C₄H₂), acetylene (C₂H₂), cyanoacetylene (HC₃N), hydrogen cyanide (HCN), bisulfite (likely in the form of salts containing HSO₃

Indexed as

hydrothermal ventsorigin of lifevolcanism on the early earth

Identifiers

PMID30682803
PMCPMC6463091
OpenAlexW2913129161

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.