Àsíkò Ìgbéàtijọ́

The Paleozoic or Palaeozoic Era (from the Greek palaios (παλαιός), "old" and zoe (ζωή), "life", meaning "ancient life") is the earliest of three geologic eras of the Phanerozoic Eon. The Paleozoic spanned from roughly 542 to 251 ẹgbẹgbẹ̀rún ọdún sẹ́yìn (ICS, 2004), and is subdivided into six geologic periods; from oldest to youngest they are: the Cambrian, Ordovician, Silurian, Devonian, Carboniferous, and Permian. Fish populations exploded in the Devonian. During the late Paleozoic, great forests of primitive plants throve on land forming the great coal beds of Europe and eastern North America. By the end of the era, the first large, sophisticated reptiles and the first modern plants, (conifers) had developed.

Àsíkò Ìgbéàtijọ́

Àsíkò Ìgbéàtijọ́ 542 - 251 ẹgbẹgbẹ̀rún ọdun sẹ́yìn

Key events in the Paleozoic view • discuss •  -550 — – -500 — – -450 — – -400 — – -350 — – -300 — – -250 — – Neoproterozoic Mesozoic Cambrian Ordovician Silurian Devonian Carboniferous Permian           P a l e o z o i c  Phanerozoic  Proterozoic An approximate timescale of key Paleozoic events. Axis scale: millions of years ago.

The Paleozoic Era ended with the largest mass extinction in Earth's history, the Permian-Triassic Extinction Event. The effects of this catastrophe were so devastating that it took life on land 30 million years to recover. Recovery of life in the sea may have been much faster.

Itokasi

Preceded by Proterozoic Eon	542 Ma - Phanerozoic Eon - Present
	542 Ma - Paleozoic Era - 251 Ma						251 Ma - Mesozoic Era - 65 Ma			65 Ma - Cenozoic Era - Present
	Kámbríà	Ọ̀rdòfísíà	Sílúríà	Dẹfoníà	Eléèédú	Pẹ́rmíà	Tríásíkì	Jùrásíkì	Ẹlẹ́fun	Ìbíniàtijọ́	Ìbíniọ̀tun	Quaternary