Evidence map›Paper›PMID 37935706›Full record

ArticleNature communications2023

Near-surface magma flow instability drives cyclic lava fountaining at Fagradalsfjall, Iceland.

Samuel Scott, Melissa Pfeffer, Clive Oppenheimer, Enikö Bali, Oliver D Lamb, Talfan Barnie, Andrew W Woods, Rikey Kjartansdóttir, Andri Stefánsson

Open access · goldAbstract read
In one paragraph

Article in Nature communications, 2023. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 1 paper.

0numbers the graph read from it
0cells of the map it votes in
1citing papers in PubMed
5.3field-weighted citation impact, top 3% 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

1 citing paper in PubMed, 19 citations in OpenAlex.

  1. 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 4 institutions in 4 countries.

Samuel ScottInstitute of Earth Sciences, University of Iceland, Sturlugata 7, Reykjavík, 102, Iceland. samuels@hi.is.ORCID http://orcid.org/0000-0001-7608-7358
Melissa PfefferIcelandic Meteorological Office, Bústaðavegur 7-9, Reykjavík, 105, Iceland.ORCID http://orcid.org/0000-0002-1689-1739
Clive OppenheimerDepartment of Geography, University of Cambridge, Downing Place, Cambridge, CB2 3EN, UK.
Enikö BaliInstitute of Earth Sciences, University of Iceland, Sturlugata 7, Reykjavík, 102, Iceland.ORCID http://orcid.org/0000-0001-7289-6393
Oliver D LambDepartment of Earth, Marine and Environmental Sciences, University of North Carolina at Chapel Hill, 104 South Road, Chapel Hill, NC, 27599-3315, USA.
Talfan BarnieIcelandic Meteorological Office, Bústaðavegur 7-9, Reykjavík, 105, Iceland.
Andrew W WoodsBP Institute, University of Cambridge, Cambridge, CB3 0EZ, UK.
Rikey KjartansdóttirInstitute of Earth Sciences, University of Iceland, Sturlugata 7, Reykjavík, 102, Iceland.
Andri StefánssonInstitute of Earth Sciences, University of Iceland, Sturlugata 7, Reykjavík, 102, Iceland.
University of Iceland · ISIcelandic Meteorological Office · ISUniversity of Cambridge · GBUniversity of North Carolina at Chapel Hill · US

Funding

No grant is acknowledged in the PubMed record.

6 · The paper itself

Abstract

Lava fountains are a common manifestation of basaltic volcanism. While magma degassing plays a clear key role in their generation, the controls on their duration and intermittency are only partially understood, not least due to the challenges of measuring the most abundant gases, H

Identifiers

PMID37935706
PMCPMC10630439
OpenAlexW4388446675

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.