Little to no active faulting likely at Europa’s seafloor today

Many of the outer Solar System's icy satellites feature known or suspected subsurface oceans, at least some of which are likely situated atop rocky interiors. Water-rock interactions at and beneath these seafloors might support active chemoautotrophic habitats, with subseafloor fluid flow facilitated by active faulting and hydrothermal systems. Absent such phenomena, however, any attainment of chemical equilibrium between the seafloor and ocean might limit the availability of chemical energy for life. Here, we characterise the stress state of the seafloor of Jupiter's moon Europa, and thus the prospect for fracturing and associated sub-seafloor fluid flow there. We consider stresses from tidal forcing, global contraction, mantle convection, and serpentinisation. We find that none of these mechanisms is likely able to drive slip along even weak, pre-existing fractures in the present. Ocean water-rock reactions taking place today are therefore probably restricted to fluid flow through only the upper few hundred metres of the seafloor. Any processes able to sustain habitable conditions at the Europan seafloor today must therefore be independent of ongoing tectonic activity.

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Publication Details

Journal
Nature Communications
Published
2026-01-06
DOI
https://doi.org/10.1038/s41467-025-67151-3
Primary Topic
Astro and Planetary Science
Type
article
Field-Weighted Citation Impact
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article

Little to no active faulting likely at Europa’s seafloor today

D. Hemingway, Kelsey Crane, A. P. Green, Bradford J. Foley et al.
Nature Communications
Astro and Planetary Science
article

Little to no active faulting likely at Europa’s seafloor today

D. Hemingway, Kelsey Crane, A. P. Green, Bradford J. Foley, Christopher R. German, M. P. Panning, P. V. Regensburger, S. Vance, C. M. Elder, Christian Klimczak, Jeffrey Catalano, Barbara Sherwood Lollar, N. G. Randolph‐Flagg, Mohit Melwani Daswani, P. D. Byrne, Douglas A. Wiens, Philip Skemer, Henry Dawson
article en

Abstract

Many of the outer Solar System's icy satellites feature known or suspected subsurface oceans, at least some of which are likely situated atop rocky interiors. Water-rock interactions at and beneath these seafloors might support active chemoautotrophic habitats, with subseafloor fluid flow facilitated by active faulting and hydrothermal systems. Absent such phenomena, however, any attainment of chemical equilibrium between the seafloor and ocean might limit the availability of chemical energy for life. Here, we characterise the stress state of the seafloor of Jupiter's moon Europa, and thus the prospect for fracturing and associated sub-seafloor fluid flow there. We consider stresses from tidal forcing, global contraction, mantle convection, and serpentinisation. We find that none of these mechanisms is likely able to drive slip along even weak, pre-existing fractures in the present. Ocean water-rock reactions taking place today are therefore probably restricted to fluid flow through only the upper few hundred metres of the seafloor. Any processes able to sustain habitable conditions at the Europan seafloor today must therefore be independent of ongoing tectonic activity.

Nature CommunicationsVol. 17(1)
James S. McDonnell Foundation (US), Pennsylvania State University (US), Jet Propulsion Laboratory (US), University of Kentucky (US), University of Georgia (US), University of Oregon (US), University of Toronto (CA), Washington University in St. Louis (US), Serco (United Kingdom) (GB), Woods Hole Oceanographic Institution (US), Virginia Tech (US), The University of Texas at Austin (US)
Life below water
Openalex Percentile: Top 92%
Astro and Planetary Science
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