Phanerozoic Overview of Mass Extinction
1986/01/01 by J. John Sepkoski, J. J. Sepkoski · 16 citations
Earth and Planetary Sciences · #Marine Biology and Ecology Research #Paleontology and Evolutionary Biology #Paleontology and Stratigraphy of Fossils
paper · doi:10.1007/978-3-642-70831-2_15
crossref issued 1986/01/01 · crossref published 1986/01/01 · crossref published-print 1986/01/01 · openalex publication_date 1986/01/01 · crossref created 2011/11/02 · crossref deposited 2020/01/30 · openalex created_date 2025/10/10 · openalex updated_date 2026/08/04 · crossref indexed 2026/08/04
Citations
Cited by
- How Large Igneous Provinces affect global climate, sometimes cause mass extinctions, and represent natural markers in the geological record
- Periodicity in extinction and the problem of catastrophism in the history of life
- Secular increase in nutrient levels through the Phanerozoic; implications for productivity, biomass, and diversity of the marine biosphere
- Terrestrial-marine teleconnections in the Devonian: links between the evolution of land plants, weathering processes, and marine anoxic events
- PHANEROZOIC BIODIVERSITY MASS EXTINCTIONS
- Estimates of the magnitudes of major marine mass extinctions in earth history
- Cyclic and secular variation in microfossil biomineralization: clues to the biogeochemical evolution of Phanerozoic oceans
- Rarity in mass extinctions and the future of ecosystems
- High-resolution dynamics of Early Jurassic marine extinctions: the case of Pliensbachian–Toarcian ammonites (Cephalopoda)
- The stratigraphy of mass extinction
- Morphological Diversity In The Evolutionary Radiation Of Paleozoic and Post-Paleozoic Crinoids
- Climate and biotic evolution during the Permian-Triassic transition in the temperate Northern Hemisphere, Kuznetsk Basin, Siberia, Russia
- Changing fluvial environments across the Permian-Triassic boundary in the Karoo Basin, South Africa and possible causes of tetrapod extinctions
- Contrasting the ecological and taxonomic consequences of extinction
- Mass extinction of the marine biota at the Ordovician-Silurian transition due to environmental changes
- Extinction event [wikipedia]