ArticleProceedings of the National Academy of Sciences of the United States of America2021
Reconciling early Deccan Traps CO
Article in Proceedings of the National Academy of Sciences of the United States of America, 2021. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 8 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.
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Who cites it
8 citing papers in PubMed, 61 citations in OpenAlex.
- Massive release of predominantly magmatic carbon drove an Early Jurassic hyperthermal.Nature communications · 2026Article
- Terrestrial evidence for volcanogenic sulfate-driven cooling event ~30 kyr before the Cretaceous-Paleogene mass extinction.Science advances · 2024Article
- Recurring volcanic winters during the latest Cretaceous: Sulfur and fluorine budgets of Deccan Traps lavas.Science advances · 2023Article
- Reply to Henehan and Witts: Continental flood basalts drive extinctions after the mid-Mesozoic.Proceedings of the National Academy of Sciences of the United States of America · 2023Article
- Low dinosaur biodiversity in central China 2 million years prior to the end-Cretaceous mass extinction.Proceedings of the National Academy of Sciences of the United States of America · 2022Article
- Continental flood basalts drive Phanerozoic extinctions.Proceedings of the National Academy of Sciences of the United States of America · 2022Article
- Volume and rate of volcanic COProceedings of the National Academy of Sciences of the United States of America · 2022Article
- The History of Water in Martian Magmas From Thorium Maps.Geophysical research letters · 2022Article
Corrections and comments
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Authors and funding
6 authors at 5 institutions in 2 countries.
Funding
No grant is acknowledged in the PubMed record.
Abstract
A 2 to 4 °C warming episode, known as the Latest Maastrichtian warming event (LMWE), preceded the Cretaceous-Paleogene boundary (KPB) mass extinction at 66.05 ± 0.08 Ma and has been linked with the onset of voluminous Deccan Traps volcanism. Here, we use direct measurements of melt-inclusion CO
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Registered trials
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