Figure 12From: Sulfur and oxygen isotope insights into sulfur cycling in shallow-sea hydrothermal vents, Milos, Greeceδ18O SO4 and δ34S SO4 of pore water in the hydrothermal sites Twinkie (+), Rocky Point (●), and Spiegelei (▲), relative to the Brine pool (×), background sediments (◇), and seawater (■). The inset illustrates the potential mixing trajectory between seawater sulfate (sw) and secondary sulfate (ss).Back to article page