Lithogeochemical and sulfide trace-element systematics across the Permian–Triassic boundary, Perth Basin, Western Australia: constraints on the shallow marine environment during the end-Permian mass extinction
Author:
Affiliation:
1. CODES, Centre for Ore Deposit and Earth Sciences, University of Tasmania, Hobart, Australia
2. Western Australian Organic and Isotope Geochemistry Centre, School of Earth and Planetary Science, Curtin University, Perth, Australia
Funder
Australian Research Council Discovery
Publisher
Informa UK Limited
Subject
General Earth and Planetary Sciences,Earth and Planetary Sciences (miscellaneous)
Link
https://www.tandfonline.com/doi/pdf/10.1080/08120099.2023.2200476
Reference77 articles.
1. Spatial variation in sediment fluxes, redox conditions, and productivity in the Permian–Triassic Panthalassic Ocean
2. Permian-Triassic of the Tethys: Carbon isotope studies
3. Sedimentary Fe–Mn oxyhydroxides as paleoceanographic archives and the role of aeolian flux in regulating oceanic dissolved REE
4. Belousov, I., Danyushevsky, L., Olin, P., Gilbert, S., Thompson, J. (2014). New calibration standard for LA-ICPMS analysis of sulphides. AGU, 2014 Fall Meeting. https://agu.confex.com/agu/fm14/webprogram/Paper19453.html.
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1. End-Permian marine ecosystem collapse was a direct consequence of deforestation: Evidence from the Kockatea Shale of the Perth Basin, Western Australia;Evolving Earth;2023-12
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