ArticlePhilosophical transactions. Series A, Mathematical, physical, and engineering sciences2016
Hydrothermal impacts on trace element and isotope ocean biogeochemistry.
Article in Philosophical transactions. Series A, Mathematical, physical, and engineering sciences, 2016. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 11 papers.
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Who cites it
11 citing papers in PubMed.
- Setting the geological scene for the origin of life and continuing open questions about its emergence.Frontiers in astronomy and space sciences · 2023Article
- Impact of high Fe-concentrations on microbial community structure and dissolved organics in hydrothermal plumes: an experimental study.Scientific reports · 2022Article
- Niche differentiation of sulfur-oxidizing bacteria (SUP05) in submarine hydrothermal plumes.The ISME journal · 2022Article
- Fe-catalyzed sulfide oxidation in hydrothermal plumes is a source of reactive oxygen species to the ocean.Proceedings of the National Academy of Sciences of the United States of America · 2021Article
- High mercury accumulation in deep-ocean hadal sediments.Scientific reports · 2021Article
- New clues on the Atlantic eels spawning behavior and area: the Mid-Atlantic Ridge hypothesis.Scientific reports · 2020Article
- The interplay between regeneration and scavenging fluxes drives ocean iron cycling.Nature communications · 2019Article
- The microbiomes of deep-sea hydrothermal vents: distributed globally, shaped locally.Nature reviews. Microbiology · 2019Review
- Iron from a submarine source impacts the productive layer of the Western Tropical South Pacific (WTSP).Scientific reports · 2018Article
- Could It Be Snowing Microbes on Enceladus? Assessing Conditions in Its Plume and Implications for Future Missions.Astrobiology · 2017Article
- Quantifying He fluxes from the mantle using multi-tracer data assimilation.Philosophical transactions. Series A, Mathematical, physical, and engineering sciences · 2016Article
Corrections and comments
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Authors and funding
12 authors.
Funding
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Abstract
Hydrothermal activity occurs in all ocean basins, releasing high concentrations of key trace elements and isotopes (TEIs) into the oceans. Importantly, the calculated rate of entrainment of the entire ocean volume through turbulently mixing buoyant hydrothermal plumes is so vigorous as to be comparable to that of deep-ocean thermohaline circulation. Consequently, biogeochemical processes active within deep-ocean hydrothermal plumes have long been known to have the
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