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Paleogene

66-23 M.a.

The name refers to the oldest Cenozoic period.
Mapamundi
Sphinx Butterfly
Sphinx Butterfly pollinating a Petunia flower (Angiosperma)

Montserrat Conglomerate (Spain)
Montserrat Conglomerate (Spain)./span>

The separation of the continents continues and leads them to their current position. Europe and Africa separate from the two Americas, India speeds towards Asia and Antarctica stands alone over the South Pole. This distribution of the continental masses creates the Antarctic Circumpolar Current, causing climatic cooling and the formation of the southern polar cap. The northward movement of Africa and India and their collision with Europe and Asia lead to the Alpine orogeny and the building of the mountain ranges in southern Europe (the Alps, Carpathians, Pyrenees, Baetic range) and the Himalayas. The subduction of the Pacific Ocean floor continues with the creation of the Rockies and the Andes. After the Cretaceous extinction and the disappearance of large reptiles, the evolutionary spread of mammals, flowering plants and pollinating insects will colonise virtually all habitats.


Basilosaurus
Basilosaurus (Mammal, Cetacea).

Hadean ~4600-4000 M.a.
Archean 4000-2500 M.a.
Proterozoic 2500-541 M.a.
Cambrian 541-485 M.a.
Ordovician 485-443 M.a.
Silurian 443-419 M.a.
Devonian 419-359 M.a.
Carboniferous 359-299 M.a.
Permian 299-252 M.a.
Triassic 252-201 M.a.
Jurassic 201-145 M.a.
Cretaceous 145-66 M.a.
Paleogene 66-23 M.a.
Neogene 23-2,6 M.a.
Quaternary 2,6 M.a.-act.


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