ArticleProceedings of the National Academy of Sciences of the United States of America2022
Volume and rate of volcanic CO
Article in Proceedings of the National Academy of Sciences of the United States of America, 2022. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 4 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
4 citing papers in PubMed.
- Limited long-term cooling effects of Pangaean flood basalt weathering.Nature communications · 2025Article
- Gut Fungi in Alzheimer's Disease: Mechanisms, Biomarkers and Therapeutic Potential.Aging and disease · 2025Review
- Radioisotopic chronology of Ocean Anoxic Event 1a: Framework for analysis of driving mechanisms.Science advances · 2024Article
- Article
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Authors and funding
8 authors.
Funding
Abstract
The emplacement of large igneous provinces (LIPs) has been linked to catastrophic mass extinctions in Earth's history, but some LIPs are only associated with less severe oceanic anoxic events, and others have negligible environmental effects. Although it is widely accepted that massive magma outpouring can affect the environment through volatile degassing, it remains debated what controls the severity of environmental crises. Here, we demonstrate that the second-most-voluminous Phanerozoic LIP, the Kerguelen LIP, may have contributed to the early Aptian oceanic anoxic event 1a, a global event previously believed to have been caused by the Ontong Java LIP. Geochronological data show that the earliest eruptions of the Kerguelen LIP preceded the onset of oceanic anoxic event 1a by at least ∼5 million years. Analyses of CO
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