Skip to main content
Figure 11 | Geochemical Transactions

Figure 11

From: Sulfur and oxygen isotope insights into sulfur cycling in shallow-sea hydrothermal vents, Milos, Greece

Figure 11

Relationship between pore water δ34S SO4 and temperature. (a) δ34SSO4 decreases with increasing temperature across the hydrothermal sites Twinkie (+), Rocky Point (), and Spiegelei (▲), relative to the Brine pool (×), background sediments (), and surface seawater sulfate (sw; ■). (b) A mass balance model suggests an increasing fraction of secondary sulfate (f SS ) in sites with elevated temperatures.

Back to article page
\