Oxidation state of Mayotte magmatic series: insights from Fe and S K-edge XANES spectroscopy
Abstract
Following the 2018-2020 Fani Maoré submarine eruption near Mayotte Island, Indian Ocean, multiple oceanographic expeditions provide unprecedented access to fresh alkaline volcanic glasses spanning basanite to phonolite compositions from the East-Mayotte Volcanic Chain (EMVC). We applied Fe and S K-edge X-ray Absorption Near-Edge Spectroscopy (XANES) to determine iron and sulfur oxidation states in 13 glass samples, providing the first comprehensive redox characterization of this submarine volcanic system. Fe 3+ /Fe TOT ratios range from 0.19 to 0.51, while S 6+ /S TOT ratios span 0.02-0.17, with more evolved compositions that tend to show higher oxidation states. Beam damage monitoring revealed significant photo-oxidation effects on sulfur measurements, requiring analysis of initial spectra only. Comparison of redox estimates from multiple independent oxybarometers based on the Fe 3+ /Fe TOT and S 6+ /S TOT as well as the olivine-spinel-a melt SiO 2 reveals systematic discrepancies between Fe-based and S-based estimates, likely due to Fe-Ti nanolite contamination along X-ray beam paths. Integration of S 6+ /S TOT measurements with the olivine-spinel-a melt SiO 2 oxybarometer indicates ΔFMQ = +0.3 ± 0.2 for basanite to tephriphonolite magmas, suggesting slightly more oxidized conditions than previously estimated for EMVC. These results provide essential constraints for thermodynamic modeling of alkaline submarine volcanism and highlight the importance of multi-proxy approaches in determining magmatic redox conditions. The oxidation state is consistent with other regional volcanic systems in the SW Indian Ocean, supporting a moderately oxidized mantle source beneath the Comoros archipelago.
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BibTeX
@article{losq2026oxidation,
title = {{Oxidation state of Mayotte magmatic series: insights from Fe and S K-edge XANES spectroscopy}},
author = {Charles Le Losq and Roberto Moretti and Etienne Médard and Carole Berthod and Federica Schiavi and Nicolas Trcera and Elodie Lebas},
journal = {Volcanica},
year = {2026},
month = oct,
doi = {10.30909/vol/mldi7329},
url = {https://uca.hal.science/hal-05775168v1},
note = {CC BY 4.0},
}
RIS
TY - JOUR
TI - Oxidation state of Mayotte magmatic series: insights from Fe and S K-edge XANES spectroscopy
AU - Charles Le Losq
AU - Roberto Moretti
AU - Etienne Médard
AU - Carole Berthod
AU - Federica Schiavi
AU - Nicolas Trcera
AU - Elodie Lebas
PY - 2026
DA - 2026/10/02
JO - Volcanica
DO - 10.30909/vol/mldi7329
UR - https://uca.hal.science/hal-05775168v1
AB - Following the 2018-2020 Fani Maoré submarine eruption near Mayotte Island, Indian Ocean, multiple oceanographic expeditions provide unprecedented access to fresh alkaline volcanic glasses spanning basanite to phonolite compositions from the East-Mayotte Volcanic Chain (EMVC). We applied Fe and S K-edge X-ray Absorption Near-Edge Spectroscopy (XANES) to determine iron and sulfur oxidation states in 13 glass samples, providing the first comprehensive redox characterization of this submarine volcanic system. Fe 3+ /Fe TOT ratios range from 0.19 to 0.51, while S 6+ /S TOT ratios span 0.02-0.17, with more evolved compositions that tend to show higher oxidation states. Beam damage monitoring revealed significant photo-oxidation effects on sulfur measurements, requiring analysis of initial spectra only. Comparison of redox estimates from multiple independent oxybarometers based on the Fe 3+ /Fe TOT and S 6+ /S TOT as well as the olivine-spinel-a melt SiO 2 reveals systematic discrepancies between Fe-based and S-based estimates, likely due to Fe-Ti nanolite contamination along X-ray beam paths. Integration of S 6+ /S TOT measurements with the olivine-spinel-a melt SiO 2 oxybarometer indicates ΔFMQ = +0.3 ± 0.2 for basanite to tephriphonolite magmas, suggesting slightly more oxidized conditions than previously estimated for EMVC. These results provide essential constraints for thermodynamic modeling of alkaline submarine volcanism and highlight the importance of multi-proxy approaches in determining magmatic redox conditions. The oxidation state is consistent with other regional volcanic systems in the SW Indian Ocean, supporting a moderately oxidized mantle source beneath the Comoros archipelago.
SN - 2610-3540
ER -