Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/15723
Authors: Liuzzo, Marco* 
Di Muro, Andrea* 
Rizzo, Andrea Luca* 
Grassa, Fausto* 
Coltorti, Massimo* 
Ader, Magali* 
Title: The composition of gas emissions at Petite Terre (Mayotte, Comoros): inference on magmatic fingerprints
Journal: Comptes rendus geoscience 
Series/Report no.: s2/354 (2022)
Issue Date: 2022
DOI: 10.5802/crgeos.148
Keywords: Gas-geochemistry
Hydrothermal system
Biogenic vs abiogenic CO2 & CH4
Stable and noble gas isotopes
Mayotte
Comoros
Abstract: The Comoros archipelago is an active geodynamic region located in theMozambique Channel between East continental Africa andMadagascar. The archipelago results from intra-plate volcanism, the most recent eruptions having occurred on the youngest island of Grande Comore and on the oldest one of Mayotte. Since 2018, the eastern submarine flank of Mayotte has been the site of one of the largest recent eruptive events on Earth in terms of erupted lava volume. On land, the most recent volcanic activity occurred in Holocene on the eastern side of Mayotte, corresponding to the small Petite Terre Island,where twomain and persistent gas seep areas are present (Airport Beach, namely BAS, and Dziani Dzaha intracrateric lake). The large submarine eruption at the feet of Mayotte (50 km offshore; 3.5 km b.s.l.) is associated with deep (mantle level) seismic activity closer to the coast (5–15 km offshore) possibly corresponding to a single and large magmatic plumbing system. Our study aims at characterizing the chemical and isotopic composition of gas seeps on land and assesses their potential link with the magmatic plumbing system feeding the Mayotte volcanic ridge and the recent submarine activity. Data from bubbling gases collected between 2018 and 2021 are discussed and compared with older datasets acquired between 2005 and 2016 from different research teams. The relation between 3He/4He and 13C-CO2 shows a clear magmatic origin for Mayotte bubbling gases, while the variable proportions and isotopic signature of CH4 is related to the occurrence of both biogenic and abiogenic sources of methane. Our new dataset points to a time-decreasing influence of the recent seismo-volcanic activity at Mayotte on the composition of hydrothermal fluids on land, whose equilibriumtemperature steadily decreases since 2018. The increased knowledge on the gas-geochemistry at Mayotte makes the results of this work of potential support for volcanic and environmental monitoring programs
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