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Jiangsi Liu

Researcher at China University of Geosciences (Wuhan)

Publications -  15
Citations -  684

Jiangsi Liu is an academic researcher from China University of Geosciences (Wuhan). The author has contributed to research in topics: Carboniferous & Late Devonian extinction. The author has an hindex of 10, co-authored 15 publications receiving 357 citations. Previous affiliations of Jiangsi Liu include University of Cincinnati & Xiamen University.

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A re-assessment of elemental proxies for paleoredox analysis

TL;DR: In this paper, the authors evaluated 21 elemental proxies, including six proxies based on the C-S-Fe-P system (TOC, S, TOC/S, DOPT, Fe/Al, Corg/P), nine proxy based on trace-metal enrichment factors (CoEF, CrEF, CuEF, MoEF, NiEF, PbEF, UEF, VEF, ZnEF), and six additional proxies from Jones and Manning (1994) (U/Th, Uauth, V/Cr, Ni/Co, Ni
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Sedimentary host phases of mercury (Hg) and implications for use of Hg as a volcanic proxy

TL;DR: In this article, the authors investigate the relationship between Hg concentrations and their relationship to TOC, TS, and Al in four modern marine settings (Black Sea, Japan Sea, Saanich Inlet, and Peru Margin) and six ancient marine formations (from Lower Cambrian to Lower Jurassic).
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The TICE event: Perturbation of carbon–nitrogen cycles during the mid-Tournaisian (Early Carboniferous) greenhouse–icehouse transition

TL;DR: The mid-Tournaisian carbon isotope excursion (TICE) as discussed by the authors was probably triggered by an increase in organic carbon burial rates linked to changes in global ocean circulation.
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Beyond redox: Control of trace-metal enrichment in anoxic marine facies by watermass chemistry and sedimentation rate

TL;DR: In this article, a diffusion-reaction model was used to evaluate the effects of variations in watermass chemistry and sedimentation rate on authigenic trace-metal enrichment in modern Black Sea sediments and North American Devonian-Carboniferous boundary (DCB) black shales.
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Local overprints on the global carbonate δ13C signal in Devonian–Carboniferous boundary successions of South China

TL;DR: In this article, an integrated study of the litho-, bio-, and chemostratigraphy of the Devonian-Carboniferous boundary at four sections (Qilinzhai, Malanbian, Gedongguan and Long'an) in South China was undertaken in order to better understand paleoenvironmental changes and controls on δ 13 C carb variation during the Hangenberg Crisis.