Ìgbà Ìbíniọ̀tun

The Neogene is a geologic period and system in the International Commission on Stratigraphy (ICS) Geologic Timescale starting 23.03 ± 0.05 million years ago and ending 2.588 million years ago. The Neogene Period follows the Paleogene Period as the 2nd period within the Cenozoic Era and is succeeded by the Quaternary Period.

Ìgbà Ìbíniọ̀tun
Ìgbà Ìbíniọ̀tun
23.03–2.588 ẹgbẹgbẹ̀rún ọdun sẹ́yìn
Mean atmospheric O2 content over period durationca. 21.5 Vol %[1]
(108 % of modern level)
Mean atmospheric CO2 content over period durationca. 280 ppm[2]
(1 times pre-industrial level)
Mean surface temperature over period durationca. 14 °C[3]
(0 °C above modern level)
Àdàkọ:Ìgbà Ìbíniọ̀tun graphical timeline

The last epoch into which the Paleogene Period is subdivided is its Oligocene Epoch. The Neogene Period is subdivided into 2 epochs, the earlier Miocene Epoch and its succeeding Pliocene Epoch. The first epoch into which the Quaternary Period is subdivided is its Pleistocene Epoch.[4]


Itokasi


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MiocenePliocene
Aquitanian | Burdigalian
Langhian | Serravallian
Tortonian | Messinian
Zanclean | Piacenzian
Preceded by Proterozoic Eon542 Ma - Phanerozoic Eon - Present
542 Ma - Paleozoic Era - 251 Ma251 Ma - Mesozoic Era - 65 Ma65 Ma - Cenozoic Era - Present
KámbríàỌ̀rdòfísíàSílúríàDẹfoníàEléèédúPẹ́rmíàTríásíkìJùrásíkìẸlẹ́funÌbíniàtijọ́Ìbíniọ̀tunQuaternary