Science

Mass Extinction Events

Mass Extinction Events is a structured science dataset with 16 entries. Its fields include Event, When (mya), Species Lost (est.). The source values are preserved as a structured reference table.

Every row is shown below and is also available as CSV, JSON, or Excel.

16rows
5columns
42views
0downloads
Updated:4/9/2026

Dataset details

Table scope
All 16 rows
Fields
5 columns
Source
Not provided
Data updated
Apr 9, 2026

Included fields: Event, When (mya), Species Lost (est.), Likely Cause, Known For.

The table contains every record in this dataset; the same records are available in each download format.

Preview observations

No reliable range or grouping can be calculated from the loaded rows without interpreting the source data.

Useful for

  • Comparing Event, When (mya), and Species Lost (est.) across science entries
  • Building reference tables, charts, or analyses from 16 downloadable records
16/16
Event
When (mya)
Species Lost (est.)
Likely Cause
Known For
End-Ediacaran extinction
~542Unknown, most Ediacaran biotaOxygenation, predation, environmental changeWiped out the strange soft-bodied Ediacaran fauna right before the Cambrian explosion
Cambrian-Ordovician extinction
~488~40% generaCooling, anoxiaEnded the Cambrian, reset marine ecosystems
Ordovician-Silurian extinction
~445-444~85% speciesGlaciation and sea level dropSecond-largest mass extinction, triggered by sudden ice age and reef collapse
Lau event
~420Major reef lossesOcean anoxiaOne of several Silurian carbon-cycle perturbations
Late Devonian (Kellwasser)
~372~75% speciesAnoxia, cooling, land plant expansionCrippled reef-building corals, started the 'Devonian reef gap'
End-Devonian (Hangenberg)
~359~50% generaAnoxia and sea level changeWiped out placoderms (armored fish), reset vertebrate evolution
Carboniferous rainforest collapse
~305Massive plant turnoverClimate dryingFragmented equatorial rainforests, set up reptile dominance
End-Capitanian (Guadalupian)
~260~35-47% marine generaEmeishan Traps volcanismPre-quel to the Great Dying, killed off huge brachiopods and reef fauna
End-Permian ('Great Dying')
~252~96% marine species, ~70% terrestrialSiberian Traps volcanism, CO2, anoxiaLargest extinction ever, came within a hair of ending complex life
Triassic-Jurassic extinction
~201~80% speciesCentral Atlantic Magmatic Province volcanismCleared competitors from dinosaurs, enabling their dominance
Toarcian extinction
~183Major marine lossKaroo-Ferrar volcanism, anoxiaOceanic anoxic event, blackened ocean floors, hit marine invertebrates
Cenomanian-Turonian event
~94~27% marine invertebratesOcean anoxiaCreated widespread black shales that are now major oil source rocks
Cretaceous-Paleogene (K-Pg)
~66~75% species, all non-avian dinosaursChicxulub asteroid impact, Deccan TrapsThe one that killed the dinosaurs, opened the way for mammals
Eocene-Oligocene (Grande Coupure)
~33.9Major European mammal turnoverClimate cooling, Antarctic glaciationBirth of modern icehouse climate, major mammal faunal turnover
Quaternary megafauna extinction
~0.05-0.01Most large mammals in Americas, AustraliaClimate change + human huntingWiped out mammoths, saber cats, giant ground sloths, thylacoleo
Holocene (current) extinction
0 to present100-1000x background rateHuman activity, habitat loss, climate changeOngoing sixth mass extinction, driven entirely by humans

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Frequently asked questions

How is Mass Extinction Events organized?

The table starts in the source data's default order. You can sort and filter the loaded rows by the displayed fields.

How much data is available on this page?

This dataset contains 16 entries, and every row is available in the table and in the downloadable files.

Can I download the complete dataset?

Yes. CSV, JSON, and Excel downloads contain all 16 rows. Before republishing the data, review the source and any usage terms listed on this page; dtbse does not replace the original source's licensing terms.

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