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Patterns of (trace) metals and microorganisms in the Rainbow hydrothermal vent plume at the Mid-Atlantic Ridge

Hydrothermal vent fields found at mid-ocean ridges emit hydrothermal fluids that disperse as neutrally buoyant plumes. From these fluids seafloor massive sulfides (SMS) deposits are formed, which are being explored as possible new mining sites for (trace) metals and rare earth elements (REEs). It ha...

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Bibliographic Details
Published in:Biogeosciences 2020-05, Vol.17 (9), p.2499-2519
Main Authors: Haalboom, Sabine, Price, David M, Mienis, Furu, van Bleijswijk, Judith D. L, de Stigter, Henko C, Witte, Harry J, Reichart, Gert-Jan, Duineveld, Gerard C. A
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Language:English
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Summary:Hydrothermal vent fields found at mid-ocean ridges emit hydrothermal fluids that disperse as neutrally buoyant plumes. From these fluids seafloor massive sulfides (SMS) deposits are formed, which are being explored as possible new mining sites for (trace) metals and rare earth elements (REEs). It has been suggested that during mining activities large amounts of suspended matter will appear in the water column due to excavation processes and discharge of mining waste from the surface vessel. Understanding how hydrothermal plumes can be characterised by means of geochemistry and microbiology as they spread away from their source and how they affect their surrounding environment may help in characterising the behaviour of the dilute distal part of chemically enriched mining plumes.
ISSN:1726-4189
1726-4170
1726-4189
DOI:10.5194/bg-17-2499-2020