Permian–Triassic mass extinction

E53623

The Permian–Triassic mass extinction was the most severe biodiversity crisis in Earth's history, wiping out the majority of marine and terrestrial species around 252 million years ago and marking the boundary between the Paleozoic and Mesozoic eras.

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Observed surface forms (3)


Statements (62)

Predicate Object
instanceOf mass extinction event
paleontological event
alsoKnownAs Great Dying
Permian–Triassic mass extinction
surface form: Permian–Triassic extinction event

Permian–Triassic mass extinction
surface form: P–Tr extinction
associatedWith carbon cycle disruption
collapse of marine ecosystems
collapse of terrestrial ecosystems
extreme greenhouse warming
global euxinia
global warming of more than 5–10 °C
massive flood basalt eruptions
ocean acidification
ocean anoxia
rapid CO₂ increase
severe climate change
strong negative carbon isotope excursion
durationEstimate on the order of tens of thousands to hundreds of thousands of years
ecologicalConsequence long recovery time for biodiversity
reset of marine trophic structures
estimatedRecoveryTime 5–10 million years for many ecosystems
followedBy Triassic–Jurassic mass extinction
generaLoss about 80–90% of marine genera extinct
geochemicalEvidence evidence for widespread anoxia in sedimentary rocks
large negative δ13C excursion
geochronologyMethod U–Pb zircon dating of volcanic ash beds
invertebrateFamilyLoss about 57% of marine invertebrate families extinct
isBoundaryLevel Permian–Triassic mass extinction self-linksurface differs
surface form: Permian–Triassic boundary
keyStudyRegion Meishan section, South China
majorVictimGroup many brachiopod groups
many fusulinid foraminifera
many insect orders
many synapsid (therapsid) lineages
rugose corals (extinct)
tabulate corals (extinct)
trilobites (completely extinct)
marineSpeciesLoss about 80–96% of marine species extinct
marksBoundaryBetween Mesozoic Era
surface form: Mesozoic era

Paleozoic Era
surface form: Paleozoic era

Permian Period
surface form: Permian period

Triassic
surface form: Triassic period
paleontologicalEvidence abrupt faunal turnover in fossil record
global extinction horizon in marine strata
plantImpact major turnover in terrestrial floras
possibleContributingCause continental aridification
impact event (hypothesized, not widely accepted)
methane release from seafloor or permafrost
ocean stratification
ozone layer depletion
sea-level changes
wildfires
precededBy Capitanian (Guadalupian) mass extinction
primarySuspectedCause Siberian Traps large igneous province volcanism
recognizedAs one of the “Big Five” Phanerozoic mass extinctions
relativeSeverity most severe mass extinction in Earth history
survivorGroup ammonoids (severely reduced but later radiated)
archosaur lineages
bivalves
early ancestors of mammals
gastropods
terrestrialVertebrateSpeciesLoss about 70% or more of terrestrial vertebrate species extinct
timePeriod around 252 million years ago

Referenced by (9)

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

Permian–Triassic mass extinction alsoKnownAs Permian–Triassic mass extinction
this entity surface form: P–Tr extinction
Permian–Triassic mass extinction alsoKnownAs Permian–Triassic mass extinction
this entity surface form: Permian–Triassic extinction event
Triassic beginsAfter Permian–Triassic mass extinction
Permian Period endedWith Permian–Triassic mass extinction
this entity surface form: Permian–Triassic extinction event
Paleozoic Era endsWith Permian–Triassic mass extinction
this entity surface form: Permian–Triassic extinction event
Phanerozoic Eon includesEvent Permian–Triassic mass extinction
Permian–Triassic mass extinction isBoundaryLevel Permian–Triassic mass extinction self-linksurface differs
this entity surface form: Permian–Triassic boundary
Paleozoic Era majorEvent Permian–Triassic mass extinction
Mesozoic Era precededByEvent Permian–Triassic mass extinction