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. 2015 Jul 2;16:7. doi: 10.1186/s12932-015-0021-5

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© Knossow et al. 2015

Open AccessThis article is distributed under the terms of the Creative Commons Attribution 4.0 International License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution, and reproduction in any medium, provided you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. 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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Seasonal variations in the depth profiles of the sulfur isotopic composition, δ³⁴S, in sulfate, sulfide, and zero-valent sulfur, as well as of oxygen, δ¹⁸O, in sulfate in Lake Kinneret. Black dashed lines denote the chemocline depth. a Isotopic composition of sulfate during the LK2 sampling, b isotopic composition of sulfate during the LK3 sampling, c isotopic composition of sulfate during the LK4 sampling, d isotopic composition of sulfate during the LK5 sampling, e isotopic composition of sulfate during the LK6 sampling, f isotopic composition of sulfide during the LK2 sampling, g isotopic composition of sulfide during the LK3 sampling, h isotopic composition of sulfide and zero-valent sulfur during the LK4 sampling, i isotopic composition of sulfide and zero-valent sulfur during the LK5 sampling, j isotopic composition of sulfide and zero-valent sulfur during the LK6 sampling. Please notice different depth scale in panels e and j. Error bars are smaller than the symbols.