How Large Igneous Provinces affect global climate, sometimes cause mass extinctions, and represent natural markers in the geological record

2017/03/15 by Richard E. Ernst, Nasrrddine Youbi · 8 citations
Earth and Planetary Sciences · #Geological and Geochemical Analysis #Geology and Paleoclimatology Research #Paleontology and Stratigraphy of Fossils

paper · doi:10.1016/j.palaeo.2017.03.014

openalex publication_date 2017/03/15 · crossref created 2017/03/15 · crossref issued 2017/07/01 · crossref published 2017/07/01 · crossref published-print 2017/07/01 · crossref deposited 2022/06/16 · openalex created_date 2025/10/10 · crossref indexed 2026/07/24 · openalex updated_date 2026/08/01

Citations

• Phanerozoic Overview of Mass Extinction
• Geochemistry of oceanic anoxic events
• Mass Extinctions in the Marine Fossil Record
• A Chronology of Paleozoic Sea-Level Changes
• U-Pb geochronology of the Deccan Traps and relation to the end-Cretaceous mass extinction
• Global record of 1600–700Ma Large Igneous Provinces (LIPs): Implications for the reconstruction of the proposed Nuna (Columbia) and Rodinia supercontinents
• Terrestrial-marine teleconnections in the Devonian: links between the evolution of land plants, weathering processes, and marine anoxic events
• Extensive 200-Million-Year-Old Continental Flood Basalts of the Central Atlantic Magmatic Province
• On the ages of flood basalt events
• Assembly, configuration, and break-up history of Rodinia: A synthesis
• Volatile fluxes during flood basalt eruptions and potential effects on the global environment: A Deccan perspective
• Fluctuations in Precambrian atmospheric oxygenation recorded by chromium isotopes
• Determination of rapid Deccan eruptions across the Cretaceous‐Tertiary boundary using paleomagnetic secular variation: 2. Constraints from analysis of eight new sections and synthesis for a 3500‐m‐thick composite section
• Large igneous provinces and mass extinctions
• End Ordovician extinctions: A coincidence of causes
• Severe selenium depletion in the Phanerozoic oceans as a factor in three global mass extinction events
• A negative feedback mechanism for the long‐term stabilization of Earth's surface temperature
• PHANEROZOIC BIODIVERSITY MASS EXTINCTIONS
• Paleozoic large igneous provinces of Northern Eurasia: Correlation with mass extinction events
• Extraterrestrial Cause for the Cretaceous-Tertiary Extinction
• Contemporaneous massive subaerial volcanism and late cretaceous Oceanic Anoxic Event 2
• The oxygenation of the atmosphere and oceans
• Triggering of the largest Deccan eruptions by the Chicxulub impact
• Massive release of hydrogen sulfide to the surface ocean and atmosphere during intervals of oceanic anoxia
• The Chicxulub Asteroid Impact and Mass Extinction at the Cretaceous-Paleogene Boundary
• Zircon U-Pb Geochronology Links the End-Triassic Extinction with the Central Atlantic Magmatic Province
• State shift in Deccan volcanism at the Cretaceous-Paleogene boundary, possibly induced by impact
• Latest Permian mercury anomalies
• Large igneous provinces and silicic large igneous provinces: Progress in our understanding over the last 25 years
• End-Cretaceous extinction in Antarctica linked to both Deccan volcanism and meteorite impact via climate change

Cited by

• Climate and biotic evolution during the Permian-Triassic transition in the temperate Northern Hemisphere, Kuznetsk Basin, Siberia, Russia
• The influence of Late Ordovician volcanism on the marine environment based on high-resolution mercury data from South China
• Limitation of fixed nitrogen and deepening of the carbonate-compensation depth through the Hirnantian at Dob's Linn, Scotland
• Seawater sources of Hg enrichment in Ordovician-Silurian boundary strata, South China
• Ordovician-Silurian volcanism in northern Iran: Implications for a new Large Igneous Province (LIP) and a robust candidate for the Late Ordovician mass extinction
• Arc-continent collisions in the tropics set Earth’s climate state
• Pannotia: To be or not to be?
• Extinction event [wikipedia]