ArticleScience advances2021
Felsic volcanism as a factor driving the end-Permian mass extinction.
Article in Science advances, 2021. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 12 papers.
What it found
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The abstract states no effect estimate the extractor could read, or names no intervention and outcome on the map, so this paper lights no cell and moves no belief. It is still indexed, cited and linked below.
The trial behind it
Trials whose registry record cites this paper, or whose number appears in the abstract. A trial that started after this paper was published is citing it as background, not reporting it.
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Who cites it
12 citing papers in PubMed.
- A ∼0.5 Myr perturbation of carbon and mercury cycles during the Middle Triassic biotic radiation.Science advances · 2026Article
- Regional postdeforestation weathering feedback drove diachronous C-S cycle perturbations during the end-Permian crisis.Proceedings of the National Academy of Sciences of the United States of America · 2025Article
- Global cooling drove diversification and warming caused extinction among Carboniferous-Permian fusuline foraminifera.Science advances · 2025Article
- Article
- Respiratory protein-driven selectivity during the Permian-Triassic mass extinction.Innovation (Cambridge (Mass.)) · 2024Article
- The terrestrial end-Permian mass extinction in the paleotropics postdates the marine extinction.Science advances · 2024Article
- The great catastrophe: causes of the Permo-Triassic marine mass extinction.National science review · 2024Review
- Centennial scale sequences of environmental deterioration preceded the end-Permian mass extinction.Nature communications · 2023Article
- Aquatic quillworts,Ecology and evolution · 2023Review
- Volcanic COScience advances · 2023Article
- Dying in the Sun: Direct evidence for elevated UV-B radiation at the end-Permian mass extinction.Science advances · 2023Article
- High temperature methane emissions from Large Igneous Provinces as contributors to late Permian mass extinctions.Nature communications · 2022Article
Corrections and comments
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Authors and funding
26 authors.
Funding
No grant is acknowledged in the PubMed record.
Abstract
The Siberian Traps large igneous province (STLIP) is commonly invoked as the primary driver of global environmental changes that triggered the end-Permian mass extinction (EPME). Here, we explore the contributions of coeval felsic volcanism to end-Permian environmental changes. We report evidence of extreme Cu enrichment in the EPME interval in South China. The enrichment is associated with an increase in the light Cu isotope, melt inclusions rich in copper and sulfides, and Hg concentration spikes. The Cu and Hg elemental and isotopic signatures can be linked to S-rich vapor produced by felsic volcanism. We use these previously unknown geochemical data to estimate volcanic SO
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