Evidence that deep-sea black carbon comes from hydrothermal vents
In the eastern South Pacific Ocean, excess DBC concentrations increase closer to the equator, and are correlated with helium-3 isotopes from hydrothermal vents. Hydrothermal vents are the primary source of excess DBC. Credit: Youhei Yamashita, Yutaro Mori, Hiroshi Ogawa, Science Advances (2023). DOI: 10.1126/sciadv.ade3807
Hydrothermal vents have been identified as a previously undiscovered source of dissolved black carbon in…