Marine methane paradox: Enigmatic production of methane in oxygenated waters
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REFERENCES
[1] Repeta, D., Ferrón, S., Sosa, O., et al. (2016). Marine methane paradox explained by bacterial degradation of dissolved organic matter. Nat Geosci 9(12): 884−887. DOI: 10.1038/ngeo2837. [2] Mao, S., Zhang, H., Zhuang, G., et al. (2022). Aerobic oxidation of methane significantly reduces global diffusive methane emissions from shallow marine waters. Nat Commun 13(1): 7309. DOI: 10.1038/s41467-022-35082-y. [3] Klintzsch, T., Geisinger, H., Wieland, A., et al. (2023). Stable carbon isotope signature of methane released from phytoplankton. Geophys Res Lett 50(12): e2023GL103317. DOI: 10.1029/2023GL103317. [4] Wang, Q., Alowaifeer, A., Kerner, P., et al. (2021). Aerobic bacterial methane synthesis. Proc Natl Acad Sci USA 118(27): e2019229118. DOI: 10.1073/pnas.2019229118. [5] Ernst, L., Steinfeld, B., Barayeu, U., et al. (2022). Methane formation driven by reactive oxygen species across all living organisms. Nature 603(7901): 482−487. DOI: 10.1038/s41586-022-04511-9. -
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Mao S.-H., Wang J.-Y., Joye S., et al., (2024). Marine methane paradox: Enigmatic production of methane in oxygenated waters. The Innovation Geoscience 2(2): 100071. https://doi.org/10.59717/j.xinn-geo.2024.100071
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Mao S.-H., Wang J.-Y., Joye S., et al., (2024). Marine methane paradox: Enigmatic production of methane in oxygenated waters. The Innovation Geoscience 2(2): 100071. https://doi.org/10.59717/j.xinn-geo.2024.100071
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Figure 1.
Sources of methane and pathways for methane production in oxygenated seawater
