66 Million Years Ago – Present
Cenozoic Era
The Cenozoic Era, the 'Age of Mammals,' encompasses the last 66 million years and continues to the present day. After the extinction of non-avian dinosaurs, mammals underwent a dramatic adaptive radiation, filling ecological niches left vacant. Horses, whales, elephants, primates, and countless other groups evolved and diversified. Grasslands spread across continents, reshaping herbivore evolution and driving the development of running adaptations. The era's later stages were marked by dramatic climate oscillations — the Pleistocene ice ages — that drove cycles of glaciation and profoundly influenced the distribution and evolution of life. The emergence of Homo sapiens in the late Cenozoic has had an unprecedented impact on the biosphere.
Milestones
Key Events
Adaptive radiation of mammals (Paleocene–Eocene)
India collides with Asia, forming the Himalayas (~50 Mya)
Spread of grasslands (Miocene, ~20 Mya)
Evolution of hominins (~7 Mya)
Pleistocene ice ages (~2.6 Mya–11,700 years ago)
Emergence of modern humans (~300,000 years ago)
Environment
Climate & Environment
The Cenozoic began warm, then experienced a long-term cooling trend. The formation of the Antarctic ice sheet (~34 Mya) and later the Arctic ice cap (~3 Mya) drove the Pleistocene glacial cycles.
Collection
Cenozoic Era Specimens (26)

Ambulocetus
paleogene

Andrewsarchus
paleogene

Australopithecus
Neogene

Basilosaurus
paleogene

Cave Bear
quaternary

Darwinius (Ida)
paleogene

Deinotherium
neogene

Dire Wolf
quaternary

Dodo
quaternary

Gastornis
paleogene

Glyptodon
quaternary

Homo erectus
quaternary

Hyracotherium
paleogene

Insect in amber
Eocene

Irish Elk
quaternary

Megalodon
neogene
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Megalodon (Carcharocles megalodon) tooth
Miocene, Pliocene

Megatherium
quaternary

Paraceratherium
neogene

Smilodon
quaternary

Thylacosmilus
neogene

Titanoboa
Paleogene

Uintatherium
paleogene
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Ursus spelaeus (Cave Bear)
Pleistocene

Woolly Mammoth
quaternary

Woolly Rhinoceros
quaternary