Great Dying

E267699

The Great Dying is the most severe mass extinction event in Earth's history, occurring about 252 million years ago and wiping out the majority of marine and terrestrial species.

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All labels observed (1)

Label Occurrences
Great Dying canonical 1

Statements (48)

Predicate Object
instanceOf Permian–Triassic extinction event
mass extinction event
paleontological event
affects insects
marine invertebrates
plants
terrestrial vertebrates
alsoKnownAs Permian–Triassic mass extinction
surface form: Permian–Triassic extinction event

P–Tr extinction event
Permian–Triassic mass extinction
surface form: end-Permian extinction
associatedWith Siberian Traps large igneous province volcanism
surface form: Siberian Traps large igneous province

prolonged biotic recovery lasting millions of years
sharp negative carbon isotope excursion
widespread coal gap in Early Triassic
deathToll about 57% of all biological families extinct
about 70% of terrestrial vertebrate species extinct
about 81% of all marine genera extinct
about 90–96% of marine species extinct
definedBy abrupt changes in marine fossil assemblages
abrupt changes in terrestrial fossil assemblages
endTime approximately 251 million years ago
fieldOfStudy geology
paleoecology
paleontology
followedBy Triassic biotic recovery
geologicalBoundary Permian–Triassic mass extinction
surface form: Permian–Triassic boundary
hasCause global warming
large-scale release of greenhouse gases
marine anoxia
massive Siberian Traps volcanism
methane release from seafloor (hypothesized)
ocean acidification
ozone layer depletion (hypothesized)
hasEffect collapse of marine ecosystems
collapse of terrestrial ecosystems
end of the Permian period
extinction of majority of marine species
extinction of majority of terrestrial species
location global
partOf Phanerozoic mass extinctions
surface form: Big Five mass extinctions

Phanerozoic Eon
surface form: Phanerozoic eon
precededBy Capitanian (Guadalupian) mass extinction
surface form: Capitanian mass extinction event
recoveryDuration several million years into the Triassic
startTime approximately 252 million years ago
superlative most severe mass extinction in Earth history
temporalLocation boundary between Permian and Triassic periods
timeScaleUnit base of Induan age
end of Lopingian epoch

Referenced by (1)

Full triples — surface form annotated when it differs from this entity's canonical label.