*Plain text denotes geological ‘eras’, some of which are typically broken into shorter ‘epochs’, which are named in italics.
When |
Geological time* |
What happened |
~100 million years ago (mya) |
Cretaceous period |
Afrotheria lineage, which includes elephants, splits from other mammalian lineages, including the branch that led to humans and other primates. This is the date of the last common ancestor between humans and elephants. |
65mya |
Cretaceous period |
Extinction of the dinosaurs. |
~65–55mya |
Palaeocene epoch of Paleogene period |
Evolution of first proboscideans, when the lineage that resulted in elephants split from that of the hyraxes and manatees. These early proboscideans were all extinct by ~30mya. |
~30–25mya |
Late Oligocene |
Evolution of deinotheres in Africa, which subsequently colonised southern Asia and Europe. The deinothere group died out ~1mya. |
~25mya |
Late Oligocene |
Evolution of mastodons in Africa, which colonised most of the northern hemisphere. The last of the mastodons died out around 10,000 years ago. |
~24mya |
Late Oligocene or early Miocene |
Evolution of gomphotheres, which colonised North, Central, and South America, and Eurasia. Extinction less than 10,000 years ago. |
~12–10mya |
Miocene |
Evolution of elephantoids, the super-family that contains today’s elephant species. |
~8–6mya |
Late Miocene |
Last common ancestor between Loxodonta lineage and Asian elephant/mammoth lineage. |
~7–6mya |
Late Miocene |
Last common ancestor between humans and our closest living relative, the chimpanzees. |
~7–5.5mya |
Late Miocene |
Mammoth and Asian elephant lineages split. |
~5.5–5mya |
Late Miocene |
Loxodonta africana (savannah elephant) and Loxodonta cyclotis (forest elephant) lineages split. |
~5mya |
Start of Pliocene |
Earth cools and becomes drier, forest cover shrinks. |
~3mya |
End of Pliocene |
Migration of Elephas species from Africa to Asia. |
~2mya |
Start of Pleistocene epoch of Quaternary period |
Rapid cooling of Earth. |
Appearance of human lineage, Homo. |
||
~500,000 years ago |
Pleistocene |
Clear evidence from stone tools that Homo species were hunting proboscids. |
~195,000 years ago |
Pleistocene |
Earliest known fossils of our own species – anatomically modern humans – Homo sapiens. |
50–30,000 years ago |
Pleistocene |
Extinction of Palaeoloxodons (straight-tusked elephants) from mainland Europe and Britain. |
15–10,000 years ago |
Late Pleistocene to early Holocene |
Extinction of most proboscids across the Americas, Europe and Asia. Homo sapiens settles most parts of the planet. |
~6,000 years ago |
Holocene |
Extinction of last gomphotheres in South America, and last Palaeoloxodons in Greek islands. |
~5,000 years ago (3000 BC) |
Holocene |
First evidence of Asian elephants being captured and trained in India. |
~4,000 years ago (2000 BC) |
Holocene |
Extinction of last woolly mammoths from Wrangel Island in Siberia. |
~2,000 years ago (218 BC) |
Holocene |
Hannibal crosses the Alps with an army of African elephants. |
~1,500 years ago (AD 500) |
Holocene |
The last elephants disappear in North Africa. |
~500-100 years ago (1500–1920) |
Holocene |
Expansion of agriculture in Africa; European colonisation and ivory trade grows; the demise of Africa’s elephants begins. |
1920–2019 |
Holocene |
Massive boom in human population. Elephant numbers drop from 12 million to less than 415,000. |