Mesozoic–Cenozoic radiation
id:
mesozoic-cenozoic-radiation-234-1912365
title:
Mesozoic–Cenozoic radiation
text:
The Mesozoic–Cenozoic Radiation is the third major extended increase of biodiversity in the Phanerozoic, after the Cambrian Explosion and the Great Ordovician Biodiversification Event, which appeared to exceeded the equilibrium reached after the Ordovician radiation. Made known by its identification in marine invertebrates, this evolutionary radiation began in the Mesozoic, after the Permian extinctions, and continues to this date. This spectacular radiation affected both terrestrial and marine
brand slug:
wiki
category slug:
encyclopedia
description:
Increase in biodiversity since the Permian extinction
original url:
https://en.wikipedia.org/wiki/Mesozoic%E2%80%93Cenozoic_radiation
date created:
date modified:
2024-03-27T12:31:49Z
main entity:
{"identifier":"Q17113740","url":"https://www.wikidata.org/entity/Q17113740"}
image:
{"content_url":"https://upload.wikimedia.org/wikipedia/commons/4/4d/Phanerozoic_Biodiversity.svg","width":784,"height":464}
fields total:
13
integrity:
15