The remarkable longevity of submarine plumes: Implications for the hydrothermal input of iron to the deep-ocean

Carazzo, G. and Jellinek, A. M. and Turchyn, A. V. (2013) The remarkable longevity of submarine plumes: Implications for the hydrothermal input of iron to the deep-ocean. Earth and Planetary Science Letters, 382. pp. 66-76. ISSN 0012-821X DOI 10.1016/j.epsl.2013.09.008

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Official URL: http://www.sciencedirect.com/science/article/pii/S...

Abstract

The longevity of submarine plumes generated at sea-floor hydrothermal systems constrains the hydrothermal input of chemical species into the deep-ocean. Decades of observations of episodic “event plumes” suggest that a key process governing the dynamics of an hydrothermal cloud spreading out laterally from a buoyant rising plume is the production of internal layering. Here, we use analog experiments on turbulent, hot particle-laden plumes and clouds to show that this layering occurs where particle diffusive convection driven by the differential diffusion of heat and small mineral precipitates gives rise to a large scale double diffusive instability. Where hydrothermal clouds are enriched in fine minerals, this “particle diffusive convection” can extend the longevity of an event plume to 2 yr after its emplacement. The very long residence time imposed by diffusive convective effects enables complete dissolution of fine sulfide and sulfate minerals. We develop a new theoretical model that includes both sedimentation and dissolution processes to quantify the potential amount of iron produced by the dissolution of iron-sulfide minerals settling through the cloud by diffusive convection. A key prediction is that the concentration of dissolved iron in hydrothermal clouds can reach up to 19±3 nM19±3 nM, which represents about 5% of the global hydrothermal discharge. If these results are representative of all hydrothermal vent fields, hydrothermal systems could provide 75% of the global budget of dissolved iron in the deep-ocean. Regionally, this flux is expected to scale in magnitude with mid-ocean ridge heat flow, consistent with observations and global ocean models.

Item Type: Article
Uncontrolled Keywords: 2013AREP; IA67;
Subjects: 01 - Climate Change and Earth-Ocean Atmosphere Systems
Divisions: 01 - Climate Change and Earth-Ocean Atmosphere Systems
Journal or Publication Title: Earth and Planetary Science Letters
Volume: 382
Page Range: pp. 66-76
Identification Number: 10.1016/j.epsl.2013.09.008
Depositing User: Sarah Humbert
Date Deposited: 11 Apr 2014 15:40
Last Modified: 15 Apr 2014 20:19
URI: http://eprints.esc.cam.ac.uk/id/eprint/3013

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