Evidence map›Paper›PMID 36316329›Full record

ArticleNature communications2022

Volcanically hosted venting with indications of ultramafic influence at Aurora hydrothermal field on Gakkel Ridge.

Christopher R German, Eoghan P Reeves, Andreas Türke, Alexander Diehl, Elmar Albers, Wolfgang Bach, Autun Purser, Sofia P Ramalho, Stefano Suman, Christian Mertens and 5 more

Abstract read
In one paragraph

Article in Nature communications, 2022. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 11 papers.

0numbers the graph read from it
0cells of the map it votes in
11citing 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

11 citing papers in PubMed.

  1. Review
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  3. Enigmatic HScientific reports · 2025
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  5. Review
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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

15 authors.

Christopher R GermanWoods Hole Oceanographic Institution, Woods Hole, USA. cgerman@whoi.edu.ORCID 0000-0002-3417-6413
Eoghan P ReevesDepartment of Earth Science & Centre for Deep Sea Research, University of Bergen, Bergen, Norway.ORCID 0000-0003-0146-0714
Andreas TürkeDepartment of Earth Science & Centre for Deep Sea Research, University of Bergen, Bergen, Norway.ORCID 0000-0001-8827-2032
Alexander DiehlMARUM-Center for Marine Environmental Sciences, University of Bremen, Bremen, Germany.ORCID 0000-0001-8875-8796
Elmar AlbersFaculty of Geosciences, University of Bremen, Bremen, Germany.ORCID 0000-0002-0874-5926
Wolfgang BachMARUM-Center for Marine Environmental Sciences, University of Bremen, Bremen, Germany.ORCID 0000-0002-3099-7142
Autun PurserAlfred Wegener Institute Helmholtz Centre for Polar & Marine Research, Bremerhaven, Germany.ORCID 0000-0001-5427-0151
Sofia P RamalhoCentre for Environmental & Marine Studies (CESAM), Department of Biology, University of Aveiro, Aveiro, Portugal.ORCID 0000-0001-8714-4696
Stefano SumanWoods Hole Oceanographic Institution, Woods Hole, USA.
Christian MertensMARUM-Center for Marine Environmental Sciences, University of Bremen, Bremen, Germany.ORCID 0000-0002-7602-4194
Maren WalterMARUM-Center for Marine Environmental Sciences, University of Bremen, Bremen, Germany.ORCID 0000-0001-5108-2278
Eva Ramirez-LlodraNorwegian Institute for Water Research (NIVA), Oslo, Norway.
Vera SchlindweinMARUM-Center for Marine Environmental Sciences, University of Bremen, Bremen, Germany.ORCID 0000-0001-5570-2753
Stefan BünzCentre for Arctic Gas Hydrate, Environment and Climate (CAGE), University of Tromso-The Arctic University of Norway, Tromsø, Norway.ORCID 0000-0002-9215-7325
Antje BoetiusMARUM-Center for Marine Environmental Sciences, University of Bremen, Bremen, Germany.ORCID 0000-0003-2117-4176

Funding

No grant is acknowledged in the PubMed record.

6 · The paper itself

Abstract

The Aurora hydrothermal system, Arctic Ocean, hosts active submarine venting within an extensive field of relict mineral deposits. Here we show the site is associated with a neovolcanic mound located within the Gakkel Ridge rift-valley floor, but deep-tow camera and sidescan surveys reveal the site to be ≥100 m across-unusually large for a volcanically hosted vent on a slow-spreading ridge and more comparable to tectonically hosted systems that require large time-integrated heat-fluxes to form. The hydrothermal plume emanating from Aurora exhibits much higher dissolved CH

Indexed as

Hydrothermal VentsSeawaterArctic RegionsGeologyHot Temperature

Identifiers

PMID36316329
PMCPMC9622739

What OpenQuestion holds

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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.