Mercury anomalies across the end Permian mass extinction in South China from shallow and deep water depositional environments

Xiangdong Wang, Peter A. Cawood, He Zhao, Laishi Zhao, Stephen E. Grasby, Zhong Qiang Chen, Paul B. Wignall, Zhengyi Lv, Chen Han

Research output: Contribution to journalArticleResearchpeer-review

Abstract

Life on Earth suffered its greatest bio-crisis since multicellular organisms rose 600 million years ago during the end-Permian mass extinction. Coincidence of the mass extinction with flood basalt eruptions in Siberia is well established, but the exact causal connection between the eruptions and extinction processes in South China is uncertain due to their wide spatial separation and the absence of direct geochemical evidence linking the two. The concentration and stable isotope analysis of mercury provides a way to test these links as its concentration is thought to be tied to igneous activity. Mercury/total organic carbon ratios from three Permian–Triassic boundary sections with a well-resolved extinction record in South China show elevated values (up to 900 ppb/wt.% relative to a background of <100 ppb/wt.%) that exactly coincides with the end-Permian mass extinction horizon. This enrichment does not show any correlation with redox and sedimentation rate variations during that time. Hg isotope mass-independent fractionation (Δ 199 Hg), with sustained positive values, indicate a predominant atmospheric-derived signature of volcanic Hg in deep-shelf settings of the Daxiakou and Shangsi sections. In contrast, the nearshore environment of the Meishan section displays a negative Δ 199 Hg signature, interpreted to be related to terrestrial Hg sources. Such temporal differences in Δ 199 Hg values shed new light on Hg geochemical behavior in marine settings, and also on the kill mechanisms associated with volcanism that were responsible for biotic mortality at the end of the Permian.

Original languageEnglish
Pages (from-to)159-167
Number of pages9
JournalEarth and Planetary Science Letters
Volume496
DOIs
Publication statusPublished - 15 Aug 2018

Keywords

  • bio-crisis
  • Hg isotopes
  • Meishan GSSP
  • Permian–Triassic boundary
  • Siberian Traps
  • South China

Cite this

Wang, Xiangdong ; Cawood, Peter A. ; Zhao, He ; Zhao, Laishi ; Grasby, Stephen E. ; Chen, Zhong Qiang ; Wignall, Paul B. ; Lv, Zhengyi ; Han, Chen. / Mercury anomalies across the end Permian mass extinction in South China from shallow and deep water depositional environments. In: Earth and Planetary Science Letters. 2018 ; Vol. 496. pp. 159-167.
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abstract = "Life on Earth suffered its greatest bio-crisis since multicellular organisms rose 600 million years ago during the end-Permian mass extinction. Coincidence of the mass extinction with flood basalt eruptions in Siberia is well established, but the exact causal connection between the eruptions and extinction processes in South China is uncertain due to their wide spatial separation and the absence of direct geochemical evidence linking the two. The concentration and stable isotope analysis of mercury provides a way to test these links as its concentration is thought to be tied to igneous activity. Mercury/total organic carbon ratios from three Permian–Triassic boundary sections with a well-resolved extinction record in South China show elevated values (up to 900 ppb/wt.{\%} relative to a background of <100 ppb/wt.{\%}) that exactly coincides with the end-Permian mass extinction horizon. This enrichment does not show any correlation with redox and sedimentation rate variations during that time. Hg isotope mass-independent fractionation (Δ 199 Hg), with sustained positive values, indicate a predominant atmospheric-derived signature of volcanic Hg in deep-shelf settings of the Daxiakou and Shangsi sections. In contrast, the nearshore environment of the Meishan section displays a negative Δ 199 Hg signature, interpreted to be related to terrestrial Hg sources. Such temporal differences in Δ 199 Hg values shed new light on Hg geochemical behavior in marine settings, and also on the kill mechanisms associated with volcanism that were responsible for biotic mortality at the end of the Permian.",
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Mercury anomalies across the end Permian mass extinction in South China from shallow and deep water depositional environments. / Wang, Xiangdong; Cawood, Peter A.; Zhao, He; Zhao, Laishi; Grasby, Stephen E.; Chen, Zhong Qiang; Wignall, Paul B.; Lv, Zhengyi; Han, Chen.

In: Earth and Planetary Science Letters, Vol. 496, 15.08.2018, p. 159-167.

Research output: Contribution to journalArticleResearchpeer-review

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AU - Cawood, Peter A.

AU - Zhao, He

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AU - Chen, Zhong Qiang

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