Pulsated Global Hydrogen and Methane Flux at Mid-Ocean Ridges Driven by Pangea Breakup - INSU - Institut national des sciences de l'Univers Access content directly
Journal Articles Geochemistry, Geophysics, Geosystems Year : 2020

Pulsated Global Hydrogen and Methane Flux at Mid-Ocean Ridges Driven by Pangea Breakup

Abstract

Molecular hydrogen production occurs through the serpentinization of mantle peridotite exhumed at mid-ocean ridges. Hydrogen is considered essential to sustain microbial life in the subsurface; however, estimates of hydrogen flux through geological time are unknown. Here we present a model of the primary, abiotic production of molecular hydrogen from the serpentinization of oceanic lithosphere using full-plate tectonic reconstructions for the last 200 Ma. We find significant variability in hydrogen fluxes (1-70 • 1016 mol/Ma or 0.2-14.1 • 105 Mt/a), which are a function of the sensitivity of evolving ocean basins to spreading rates and can be correlated with the opening of key ocean basins during the breakup of Pangea. We suggest that the primary driver of this hydrogen flux is the continental reconfiguration during Pangea breakup, as this produces ocean basins more conducive to exhuming and exposing mantle peridotite at slow and ultraslow spreading ridges. Consequently, present-day flux estimates are ~7 • 1017 mol/Ma (1.4 • 106 Mt/a), driven primarily by the slow and ultraslow spreading ridges in the Atlantic, Indian, and Arctic oceans. As methane has also been sampled alongside hydrogen at hydrothermal vents, we estimate the methane flux using methane-to-hydrogen ratios from present-day hydrothermal vent fluids. These ratios suggest that methane flux ranges between 10 and 100% of the total hydrogen flux, although as the release of methane from these systems is still poorly understood, we suggest a lower estimate, equivalent to around 7-12 • 1016 mol/Ma (1.1-1.9 • 107 Mt/Ma) of methane.
Fichier principal
Vignette du fichier
Geochem Geophys Geosyst - 2020 - Merdith - Pulsated Global Hydrogen and Methane Flux at Mid%u2010Ocean Ridges Driven by Pangea.pdf (16.73 Mo) Télécharger le fichier
Origin : Publisher files allowed on an open archive

Dates and versions

insu-03710132 , version 1 (30-06-2022)

Licence

Copyright

Identifiers

Cite

Andrew S. Merdith, Pablo García. del Real, Isabelle Daniel, Muriel Andreani, Nicky M. Wright, et al.. Pulsated Global Hydrogen and Methane Flux at Mid-Ocean Ridges Driven by Pangea Breakup. Geochemistry, Geophysics, Geosystems, 2020, 21, ⟨10.1029/2019GC008869⟩. ⟨insu-03710132⟩
35 View
40 Download

Altmetric

Share

Gmail Facebook X LinkedIn More