High SO (sub 2) flux, sulfur accumulation, and gas fractionation at an erupting submarine volcano

Strombolian-style volcanic activity has persisted for six years at the NW Rota-1 submarine volcano in the southern Mariana Arc, allowing direct observation and sampling of gas-rich fluids produced by actively degassing lavas, and permitting study of the magma-hydrothermal transition zone. Fluids sampled centimeters above erupting lava and percolating through volcaniclastic sediments around an active vent have dissolved sulfite >100 mmol/kg, total dissolved sulfide <30 mu mol/kg, pH as low as 1.05, and dissolved Al and Fe >1 mmol/kg. If NW Rota is representative of submarine arc eruptions, then volcanic vent fluids from seawater-lava interaction on submarine arcs have a significant impact on the global hydrothermal flux of sulfur and Al to the oceans, but a minimal impact on Mg removal. Gas ratios (SO (sub 2) , CO (sub 2) , H (sub 2) , and He) are variable on small spatial and temporal scales, indicative of solubility fractionation and gas scrubbing. Elemental sulfur (S (sub e) ) is abundant in solid and molten form, produced primarily by disproportionation of magmatic SO (sub 2) injected into seawater. S (sub e) accumulates within the porous rock surrounding the lava conduit connecting the magma source to the seafloor. Accumulated S (sub e) can be heated, melted, and pushed upward by rising magma to produce molten S (sub e) flows and lavas saturated with S (sub e) . Molten S (sub e) near the top of the lava conduit may be ejected up into the water column by escaping gases or boiling water. This mechanism of S (sub e) accumulation and refluxing may underlie the relatively widespread occurrence of S (sub e) deposits of many sizes found on submarine arc volcanoes.