Large CO2 seeps and hydrate field on the seafloor offshore Mayotte Island

Gas hydrates modulate methane and carbon dioxide benthic fluxes into the ocean and usually occur embedded in the sediment. Here we use acoustic surveys alongside optical and geochemical observations from remotely operated vehicles to show that CO2 hydrate mounds are forming directly on the seafloor atop a large liquid CO2 vent field offshore Mayotte Island. The venting, which initiated following volcanic activity in 2018, deleteriously impacts surrounding coral communities due to local acidification. Carbon dioxide hydrates on the seafloor are sustained by the venting of liquid CO2 associated with volcanic activity near Mayotte Island, according to observations from remotely operated vehicles and geochemical analyses.

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Publication Details

Journal
Nature Geoscience
Published
2026-06-12
DOI
https://doi.org/10.1038/s41561-026-02004-2
Primary Topic
Methane Hydrates and Related Phenomena
Type
article
Field-Weighted Citation Impact
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article

Large CO2 seeps and hydrate field on the seafloor offshore Mayotte Island

Manon Mastin, Christophe Rabouille, Valérie Chavagnac, Andrea Luca Rizzo et al.
Nature Geoscience
Methane Hydrates and Related Phenomena
article

Large CO2 seeps and hydrate field on the seafloor offshore Mayotte Island

Manon Mastin, Christophe Rabouille, Valérie Chavagnac, Andrea Luca Rizzo, Emmanuel Rinnert, Vivien Guyader, Nathalie Feuillet, Morgan Tardivel, Carla Scalabrin, Olivier Rouxel, T. Giunta, Olivia Fandiño, Marjolaine Matabos, N. Feuillet, Cécile Cathalot, S. L. Walker, V. Puzenat, B. Bombled, H. Ondreas, J. P. Donval, M. Manoux, G. Page, J. P. Dumoulin, E. Prado, on behalf of the GEOFLAMME scientific cruise party, A. S. Alix
article en

Abstract

Gas hydrates modulate methane and carbon dioxide benthic fluxes into the ocean and usually occur embedded in the sediment. Here we use acoustic surveys alongside optical and geochemical observations from remotely operated vehicles to show that CO2 hydrate mounds are forming directly on the seafloor atop a large liquid CO2 vent field offshore Mayotte Island. The venting, which initiated following volcanic activity in 2018, deleteriously impacts surrounding coral communities due to local acidification. Carbon dioxide hydrates on the seafloor are sustained by the venting of liquid CO2 associated with volcanic activity near Mayotte Island, according to observations from remotely operated vehicles and geochemical analyses.

Nature Geoscience
Centre National de la Recherche Scientifique (FR), Université Toulouse III - Paul Sabatier (FR), Institut de physique du globe de Paris (FR), Ifremer (FR), Université de Bretagne Occidentale (FR), Université de Versailles Saint-Quentin-en-Yvelines (FR), Université Paris Cité (FR), Commissariat à l'Énergie Atomique et aux Énergies Alternatives (FR), Université Paris-Saclay (FR), NOAA Pacific Marine Environmental Laboratory (US), Istituto Nazionale di Geofisica e Vulcanologia (IT), Laboratoire des Sciences du Climat et de l'Environnement (FR), Observatoire Midi-Pyrénées (FR), CEA Paris-Saclay (FR), Laboratoire de Mesure du Carbone 14 (FR), Institut de Recherche pour le Développement (FR), University of Milano-Bicocca (IT)
Life below water
Openalex Percentile: Top 10%
Methane Hydrates and Related Phenomena
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