Immiscible sulfi
de liquids in basaltic magmas play an important role in trace metal transport and the sulfur budget of volcanic eruptions. However, sulfi
des are transient phases, whose origin and fate are poorly constrained. We address these issues by analyzing sulfi
de destabilization products preserved in lavas from La Réunion Island. Iron oxi
de globules and coatings, typically 20–80 μm in size, were found to occur in vesicles of differentiated lavas from Piton
des Neiges, and recent pumice samples from Piton
de la Fournaise. Field and mineralogical evi
dence indicates that the iron oxi
des are syn-eruptive phases not resulting from hydrothermal processes. Samples were first studied by Scanning Electron Microscopy. The globules were separated, whereas the smaller spherules and coatings were concentrated by magnetic sorting and acid leaching, and samples were processed through wet chemistry. The Fe oxi
de phases comprise 49–74 wt.% Fe, 26–40 wt.% O, and up to 6 wt.% Cu, 811 ppm Ni, 140 ppm Bi, and 8.5 ppm Pb. Compared to the host lava, Cu, Ni, and Bi are enriched by a factor of 10
1–10
3. Systematic Pb isotope disequilibrium (between 500 ppm and 2.9% for
206Pb/
204Pb) exists between Fe oxi
des and host rocks, with Fe oxi
des generally displaying less radiogenic ratios. Unradiogenic Pb is a typical signature of sulfi
de, which tends to concentrate Pb, but not its parent elements U and Th. Thus, both the chemical and isotopic compositions of the vesicle-hosted Fe oxi
des suggest that they are more or less direct products of the
destabilization of immiscible sulfi
de liquids. Although Pb dominantly partitions into the gas phase during sulfi
de breakdown, the original Pb isotope signature of sulfi
de is preserved in the residual oxi
de. The composition estimated for the parent sulfi
des (
206Pb/
204Pb = 18.20–18.77,
207Pb/
204Pb = 15.575, and
208Pb/
204Pb = 38.2–38.8) preclu
des a genetic link with the La Réunion plume, and suggests a lithospheric or crustal origin.
It is estimated that magma ascent velocities at Piton de la Fournaise are high enough to counterbalance the settling velocities of millimeter-size sulfides. Despite their high density, sulfide liquids are thus transferred upward during eruptions and their destabilization contributes to SO2 emanations. Assimilation of foreign sulfides from the lithosphere can explain why SO2 emissions sometimes (e.g., during the April 2007 eruption) exceed those predicted from the S content of melt inclusions.