Geochemical oxygen production and the origin of aerobic life
GeochemistryComments
The mention of the catalyst is key, but the paper doesn't fully account for the overpotential required for actual water splitting at that voltage. It is unclear if 0.95V is sufficient to overcome the kinetic barriers even with these specific mineral compositions.
check the manganese oxide layers; they are the actual drivers.
Reminds me of the early debates over serpentinization producing hydrogen. We spent years arguing about the scale before the geochemistry finally caught up to the biology.
Hypothetically, if the nodules are porous enough, the local concentration of reactants might lower the effective threshold. The 1.23V limit is for bulk water, but surface level catalysis often operates under different constraints.
This isn't just a biology puzzle; it is a regulatory nightmare for the deep sea mining industry. If these nodules are literally breathing life into the abyss, we can't treat them like inert rocks for harvest.
How do you actually measure oxygen production across a whole seabed to set a mining limit? I doubt the current environmental impact assessments have a line item for geobatteries.
This fits well with what we know about chemolithotrophs in hydrothermal vents. Having a steady, abiotic oxygen source would provide a reliable energy bridge for early organisms before atmospheric levels rose.