Evidence map›Paper›PMID 40465709›Full record

ArticleScience advances2025

Subduction-like process in Europa's ice shell triggered by enhanced eccentricity periods.

Martin Kihoulou, Gaël Choblet, Gabriel Tobie, Klára Kalousová, Ondřej Čadek

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Article in Science advances, 2025. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 2 papers.

0numbers the graph read from it
0cells of the map it votes in
2citing 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

2 citing papers in PubMed.

  1. 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

5 authors.

Martin KihoulouNantes Université, Univ Angers, Le Mans Université, CNRS, Laboratoire de Planétologie et Géosciences, LPG UMR 6112, 44000 Nantes, France.ORCID 0000-0003-4935-4400
Gaël ChobletNantes Université, Univ Angers, Le Mans Université, CNRS, Laboratoire de Planétologie et Géosciences, LPG UMR 6112, 44000 Nantes, France.ORCID 0000-0002-0220-9233
Gabriel TobieNantes Université, Univ Angers, Le Mans Université, CNRS, Laboratoire de Planétologie et Géosciences, LPG UMR 6112, 44000 Nantes, France.ORCID 0000-0002-4494-0294
Klára KalousováDepartment of Geophysics, Charles University, Faculty of Mathematics and Physics, V Holešovičkách 2, Praha 8, 180 00, Czech Republic.ORCID 0000-0002-1602-8142
Ondřej ČadekDepartment of Geophysics, Charles University, Faculty of Mathematics and Physics, V Holešovičkách 2, Praha 8, 180 00, Czech Republic.ORCID 0000-0001-8331-3093

Funding

No grant is acknowledged in the PubMed record.

6 · The paper itself

Abstract

Jupiter's icy moon Europa has a liquid water ocean beneath the ice shell and a geologically young surface, both related to extensive tidal processes. Interlaced by tectonic faults, the surface records convergent motions that induced crustal disappearance in some areas. Subduction has been advocated as an explanation; however, its driving mechanism still remains unexplained. We perform numerical simulations to test under what conditions may lateral compression initiate subduction in Europa's ice shell. We demonstrate that subduction-like recycling can occur only for shells of thickness [Formula: see text]10 kilometers, transporting the surface ice into the subsurface ocean. We further show that compression large enough to initiate subduction-like behavior in a thin shell is achieved during brief periods of enhanced eccentricity, implying increased hydrothermal activity at the seafloor. Together with the subduction-like transport of surface oxidants, such conjunction should favor chemical disequilibria in the ocean, increasing its astrobiological potential.

Identifiers

PMID40465709
PMCPMC12136034

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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.