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- W4320032744 abstract "Deep-sea hydrothermal vents are a possible source of thermogenic dissolved black carbon (DBC), which is a component of recalcitrant dissolved organic carbon, but little is known about the distribution of hydrothermal DBC in the deep ocean. Here, we show basin-scale distributions of DBC along two transects in the eastern Pacific Ocean, which are located outside the jet-like hydrothermal plumes from the East Pacific Rise. The DBC concentration in the deep waters did not show a strong linear relationship with apparent oxygen utilization (AOU), as previously observed in the central and western Pacific Ocean. Deviations in DBC concentration from the DBC-AOU relationship observed in the central and western Pacific Ocean were quantified. The deviation was linearly correlated with excess 3He, a tracer for hydrothermal input, indicating that a fraction of the DBC in the deep ocean is transported long distances from hydrothermal systems." @default.
- W4320032744 created "2023-02-12" @default.
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- W4320032744 date "2023-02-10" @default.
- W4320032744 modified "2023-10-18" @default.
- W4320032744 title "Hydrothermal-derived black carbon as a source of recalcitrant dissolved organic carbon in the ocean" @default.
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- W4320032744 doi "https://doi.org/10.1126/sciadv.ade3807" @default.
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