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Geochemical fluxes of gases and elements from hydrothermal vents

The overall total mass flux from the world s deep-sea hydrothermal vents is estimated to be on the same order of magnitude as estimates of the flux from the Amazon river, or about 2% of global river discharge (Elderfield Schultz, 1996 Scott, 1997). Hydrothermal vents can have globally significant mass fluxes that are especially important for their effect on the budgets of elements [Pg.243]

Compositional data and river fluxes from Kadko etal. (1994) with modifications based on Edmond etal. (1995) and Scott (1997). Hydrothermal fluxes were calculated assuming a fluid flux of 3.70 x 1013 kg y-1 (Mottl, 2002). Value of magnesium flux from the oceans to the crust is from Mottl (2002). [Pg.244]

Not all elements dissolved in hydrothermal fluids end up in the ocean. For example, Fe and Mn are generally deposited as sulphides or oxides in chimneys [Pg.244]


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