Time runs left (older) → right (younger) · Hover a card for details
The eon of visible life — Cambrian explosion to present (539 Ma-now).
538.80 Ma – Present · 538.80 Ma duration
Axis labels in Ma (millions of years ago) ·
Click a card for details
Phanerozoic Eon 28
538.8 Ma – 521 MaCambrian ExplosionMost animal body plans appearRapid diversification of complex multicellular life with hard body parts.
470 MaFirst Coral ReefsOrdovician reef systemsFirst significant coral-stromatoporoid reef systems in shallow Ordovician seas.
443.8 MaEnd-Ordovician ExtinctionFirst major mass extinctionTwo-phase extinction driven by glaciation and sea level fall; ~85% of marine species lost.
430 MaFirst Vascular PlantsLife colonises the landEarly plants like Cooksonia spread onto land.
385 MaFirst ForestsDevonian tree evolutionArchaeopteris and Wattieza form first forests, dramatically altering the carbon cycle.
375 MaFirst TetrapodsFish crawl onto landTiktaalik and relatives develop limbs and begin exploiting terrestrial environments.
372 Ma – 358.9 MaLate Devonian ExtinctionKellwasser and Hangenberg eventsSeries of pulses over ~20 Ma; reef ecosystems collapse; ~75% of species lost.
335 Ma – 270 MaPangaea AssemblesSupercontinent formsAll major landmasses collide to form Pangaea.
312 MaFirst ReptilesAmniote egg evolvesEvolution of the amniotic egg frees vertebrates from dependency on water.
252.5 Ma – 251.5 MaSiberian Traps VolcanismTriggers Great DyingMassive flood basalt volcanism releases CO2 and SO2, causing runaway climate change.
251.902 MaEnd-Permian ExtinctionThe Great Dying — 96% of marine species lostLargest mass extinction; caused by Siberian Traps volcanism, ocean acidification and anoxia.
231 MaFirst DinosaursTriassic origin of dinosaursEarliest dinosaurs appear in South America after the P-T extinction recovery.
201.4 MaEnd-Triassic ExtinctionCAMP volcanismMassive volcanism as Pangaea rifts apart; ~80% of species lost; clears way for dinosaur dominance.
201 Ma – 140 MaPangaea Breaks ApartAtlantic Ocean opensPangaea rifts apart; Atlantic begins to open.
150.8 MaArchaeopteryxFirst known birdTransitional fossil combining dinosaur and bird features; Jurassic Solnhofen limestone, Germany.
130 MaFirst Flowering PlantsAngiosperms diversifyFlowering plants appear and co-evolve with insects, eventually dominating terrestrial ecosystems.
120 Ma – 90 MaOcean Anoxic EventsCretaceous dead zonesRepeated episodes of ocean-wide anoxia during the Cretaceous.
66.5 Ma – 65.5 MaDeccan Traps VolcanismContributes to K-Pg extinctionLarge volcanic province erupting around Chicxulub impact, compounding extinction pressures.
66 MaChicxulub ImpactAsteroid ends the Mesozoic10 km asteroid strikes Yucatan; triggers mass extinction.
66 MaEnd-Cretaceous ExtinctionK-Pg event — dinosaurs go extinctChicxulub asteroid impact ends the Mesozoic. Non-avian dinosaurs, mosasaurs and ammonites disappear.
56 Ma – 55.8 MaPaleocene-Eocene Thermal MaximumPETM — rapid global warmingGlobal temperatures rise 5-8 C in under 20,000 years; closest ancient analogue to modern climate change.
53 MaFirst WhalesReturn to the seaPakicetus and relatives begin transitioning from land to aquatic life.
33.9 Ma – 33.7 MaAntarctic Ice Sheet FormsEocene-Oligocene transitionDrake Passage opens; cold circumpolar current drives Antarctic glaciation.
6 Ma – 4 MaFirst HominidsApes walk uprightEarly hominins appear in Africa; bipedal locomotion evolves.
3 Ma – 2.8 MaPanama Land Bridge ClosesAtlantic and Pacific separateCentral American seaway closes; alters ocean circulation and intensifies glaciation.
2.58 Ma – 0.012 MaPleistocene Ice AgesRepeated glacial cyclesGlacials and interglacials driven by Milankovitch cycles; ice sheets cover North America and Europe.
0.3 Ma – presentHomo sapiensModern humans evolveAnatomically modern Homo sapiens appears in Africa, eventually spreading to every continent.