Figure 13From: Sulfur and oxygen isotope insights into sulfur cycling in shallow-sea hydrothermal vents, Milos, Greeceδ34S SO4 values exhibit an inverse relationship with chloride concentrations. A conservative mixing model demonstrates elevated contributions of high-Cl fluid in Rocky Point (●), Spiegelei (▲), and the Brine pool (×), relative to Twinkie (+), background sediments (◇), and surface seawater (■).Back to article page