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. 2014 Aug 12;15:12. doi: 10.1186/s12932-014-0012-y

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Copyright © 2014 Gilhooly et al.; licensee Chem Central

This is an Open Access article distributed under the terms of the Creative Commons Attribution License (http://creativecommons.org/licenses/by/2.0), which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly credited. The Creative Commons Public Domain Dedication waiver (http://creativecommons.org/publicdomain/zero/1.0/) applies to the data made available in this article, unless otherwise stated.

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Temperature and δ³⁴S of hydrothermal sulfide from deep-sea hydrothermal vents (DSHV’s; open symbols) and Milos pore waters (solid symbols). Estimates calculated for sulfide in equilibrium (red line) with seawater sulfate (δ³⁴S_SO4 = 21.2‰). The Milos regression intersects the equilibrium model at 311.4°C and δ³⁴S_H2S = 1.7‰.