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Sweetman et al., 2024

Evidence of dark oxygen production at the abyssal seafloor

Sweetman, A. K., Smith, A. J., de Jonge, D. S. W., Hahn, T., Schroedl, P., Silverstein, M., Andrade, C., Edwards, R. L., Lough, A. J. M., Woulds, C., Homoky, W. B., Koschinsky, A., Fuchs, S., Kuhn, T., Geiger, F., Marlow, J. J.
DOI10.1038/s41561-024-01480-8
Year2024
JournalNature Geoscience
Volume17
Number8
Pages737-739
Typearticle in journal
OpenAccess
LitsentsCC BY 4.0
LanguageEnglish
Id51893

Abstract

Deep-seafloor organisms consume oxygen, which can be measured by in situ benthic chamber experiments. Here we report such experiments at the polymetallic nodule-covered abyssal seafloor in the Pacific Ocean in which oxygen increased over two days to more than three times the background concentration, which from ex situ incubations we attribute to the polymetallic nodules. Given high voltage potentials (up to 0.95 V) on nodule surfaces, we hypothesize that seawater electrolysis may contribute to this dark oxygen production.

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