K-Pg boundary

Extinction event marker

The K-Pg boundary is the geological boundary marking the mass extinction event 66 million years ago that ended the Cretaceous period and began the Paleogene.

This boundary layer, visible in rock formations worldwide, contains high concentrations of iridium—evidence of the asteroid impact that killed the dinosaurs and roughly three-quarters of all species.

Formerly called the K-T boundary (Cretaceous-Tertiary).

Related

Alvarez · ferns · microfossils · iridium · Yucatan · trace elements · dinosaurs · mass extinction · asteroid · marine reptiles · ejecta · Jurassic · mammals · crater · layer · fireball · sediment · Deccan Traps

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extinction mechanism

K-Pg boundarygradual decline

Slow downward trend

attrition

geological transition type

K-Pg boundaryCambrian explosion

Sudden appearance of complex life

diversification

Family

boundary

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