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. 2017 Jul 13;7:5304. doi: 10.1038/s41598-017-05524-5

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© The Author(s) 2017

Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as 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 images or other third party material in this article are included in the article’s Creative Commons license, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons license and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/.

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Geochemical plots for Wangjiawan (A) and Dingjiapo (B) sections across the Ordovician-Silurian boundary. Plots show variation of δ¹³C_org for Wangjiawan and Hg, TOC, Hg/TOC, Hg/Mo, δ²⁰²Hg and Δ¹⁹⁹Hg for Wangjiawan and Dingjiapo. Graptolitic zone is from Chen et al.³⁵ and δ¹³C_org data are from Yan et al.⁴⁰. Abbreviation: Fm. = Formation, Kyc. = Kuanyinchiao.