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While the progressive elongation of the neck and limbs can be found throughout the giraffid lineage, it became more pronounced in genera such as Giraffokeryx, Palaeotragus ( possible ancestor of the okapi ), Samotherium and Bohlinia.
Bohlinia entered China and northern India in response to climate change.
From here, the genus Giraffa evolved and, around 7 mya, entered Africa.
Further climate changes caused the extinction of the Asian giraffes, while the African ones survived and radiated into several new species.
G. camelopardalis arose around 1 mya in eastern Africa during the Pleistocene.
Some biologists suggest that the modern giraffe descended from G. jumae ; others find G. gracilis a more likely candidate.
It is believed that the main driver for the evolution of the giraffes was the change from extensive forests to more open habitats, which began 8 mya.

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