View source for Cretaceous–Paleogene extinction event

== Introduction ==
The [[Cretaceous–Paleogene extinction event]] (K–Pg event), also known as the Cretaceous–Tertiary (K–T) extinction, was a sudden mass extinction of some three-quarters of the plant and animal species on Earth, approximately 66 million years ago. With the exception of some [[ectothermic]] species such as the leatherback sea turtle and crocodiles, no tetrapods weighing more than 25 kilograms (55 lb) survived. It marked the end of the [[Cretaceous]] period and with it, the entire [[Mesozoic]] Era, opening the [[Cenozoic]] Era that continues today.

[[Image:Detail-69183.jpg|thumb|center|A depiction of a meteorite impact that caused a mass extinction.|class=only_on_mobile]]
[[Image:Detail-69184.jpg|thumb|center|A depiction of a meteorite impact that caused a mass extinction.|class=only_on_desktop]]

== Causes ==
In the [[geologic record]], the K–Pg event is marked by a thin layer of sediment called the [[K–Pg boundary]], which can be found throughout the world in marine and terrestrial rocks. The boundary clay shows high levels of the metal [[iridium]], which is rare in the Earth's crust but abundant in asteroids.

== Impact Hypothesis ==
The [[Alvarez hypothesis]], widely accepted as the most plausible explanation, posits that the mass extinction resulted from the impact of a large asteroid or comet on the Earth. The hypothesis is named after the father-and-son team of scientists Luis and Walter Alvarez, who first suggested it in 1980.

== Deccan Traps Volcanism ==
An alternate hypothesis, originally proposed by Dewey McLean, suggests that the K–Pg extinction was caused by the [[Deccan Traps]] volcanic eruptions in what is now India. Large-scale volcanism could have led to a "nuclear winter" scenario, similar to the Alvarez impact hypothesis.

== Consequences ==
The K–Pg extinction had a profound effect on the evolution of life on Earth. The elimination of large, terrestrial animals altered the distribution of ecosystems, allowing new groups to evolve. In the oceans, the extinction of large marine animals led to the evolution of modern, smaller marine fauna.

== Recovery and Radiation ==
Life on Earth took a long time to recover from the environmental disruptions which likely lasted for thousands of years after the K–Pg event. The [[Chicxulub crater]], in the Yucatán Peninsula of Mexico, is the impact crater associated with the K–Pg event. The recovery of life forms was relatively fast on a geological scale, but slow by human standards.

== See Also ==
* [[End-Cretaceous extinction event]]
* [[Alvarez Hypothesis]]
* [[Chicxulub Crater]]
* [[Deccan Traps]]

[[Category:Cretaceous–Paleogene extinction event]]
[[Category:Prehistoric events]]
[[Category:Extinction events]]