Regelous M, Regelous A, Grasby SE, Bond DP, Haase K, Gleißner S, Wignall PB (2020)
Publication Type: Journal article
Publication year: 2020
Book Volume: 21
Article Number: e2020GC009064
Journal Issue: 11
DOI: 10.1029/2020GC009064
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 δ13C
APA:
Regelous, M., Regelous, A., Grasby, S.E., Bond, D.P., Haase, K., Gleißner, S., & Wignall, P.B. (2020). Tellurium in Late Permian-Early Triassic Sediments as a Proxy for Siberian Flood Basalt Volcanism. Geochemistry Geophysics Geosystems, 21(11). https://doi.org/10.1029/2020GC009064
MLA:
Regelous, Marcel, et al. "Tellurium in Late Permian-Early Triassic Sediments as a Proxy for Siberian Flood Basalt Volcanism." Geochemistry Geophysics Geosystems 21.11 (2020).
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