Marcel Regelous
Tellurium in Late Permian-Early Triassic Sediments as a Proxy for Siberian Flood Basalt Volcanism
Regelous, Marcel; Regelous, Anette; Grasby, Stephen E.; Bond, David P.G.; Haase, Karsten M.; Gleißner, Stefan; Wignall, Paul B.
Authors
Anette Regelous
Stephen E. Grasby
David Bond D.Bond@hull.ac.uk
Palaeoenvironmental Scientist and Schools Liason Officer
Karsten M. Haase
Stefan Gleißner
Paul B. Wignall
Abstract
We measured the concentrations of trace elements in Late Permian to Early Triassic sediments from Spitsbergen. High mercury concentrations in sediments from the level of the Permo-Triassic Mass Extinction (PTME) at this location were previously attributed to the emplacement of the Siberian Traps Large Igneous Province and used to link the timing of volcanism with the record of environmental change and extinction in these sediments. We investigated the use of the moderately to highly volatile, siderophile elements Ni, Zn, Cd, Sb, Te, Re, and Tl as proxies for the intensity of Siberian volcanism. These trace elements, like Hg, have high concentrations in volcanic gas compared to crustal rocks. Tellurium is highly enriched at the PTME, and Te/Th ratios increase by a factor of ∼20 across the PTME, similar to the variation in Hg/total organic carbon (TOC) in the same samples. Te/Th and Hg/TOC values imply that Siberian volcanism initiated at the onset of the PTME, coincident with the start of the δ13Corganic excursion and abrupt warming. Based on Te and Hg, most Siberian volcanism occurred between the two phases of the PTME boundary (a period of less than 100 ky), but also continued into the Early Triassic. The duration of Siberian volcanism inferred from Te/Th and Hg/TOC is shorter than that indicated by recent high-precision U-Pb ages of Siberian intrusive and extrusive rocks. Te concentrations and Te/Th ratios in sediments represent a useful new proxy for volcanism, which can be used to link the marine sedimentary record with large volcanic events on land.
Citation
Regelous, M., Regelous, A., Grasby, S. E., Bond, D. P., Haase, K. M., Gleißner, S., & Wignall, P. B. (2020). Tellurium in Late Permian-Early Triassic Sediments as a Proxy for Siberian Flood Basalt Volcanism. Geochemistry, geophysics, geosystems G³, 21(11), Article e2020GC009064. https://doi.org/10.1029/2020GC009064
Journal Article Type | Article |
---|---|
Acceptance Date | Oct 21, 2020 |
Online Publication Date | Oct 31, 2020 |
Publication Date | Nov 1, 2020 |
Deposit Date | Mar 24, 2022 |
Publicly Available Date | Mar 28, 2022 |
Journal | Geochemistry, Geophysics, Geosystems |
Electronic ISSN | 1525-2027 |
Publisher | American Geophysical Union |
Peer Reviewed | Peer Reviewed |
Volume | 21 |
Issue | 11 |
Article Number | e2020GC009064 |
DOI | https://doi.org/10.1029/2020GC009064 |
Public URL | https://hull-repository.worktribe.com/output/3667517 |
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Copyright Statement
© 2020. The Authors. This is an open access article under the terms of the Creative Commons Attribution-NonCommercial License, which permits use, distribution and reproduction in any medium, provided the original work is properly cited and is not used for commercial purposes
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