A glacial relict is a population of a species that was common in the Northern Hemisphere prior to the onset of glaciation in the late Tertiary that was forced by climate change to retreat into refugia
The Franklin tree is an example of a glacial relict species from the Southeastern USA. It went extinct in the wild in the early 19th century due to a changing climate, inability to spread outside of its limited range, and limited environmental tolerance. The species survives today as a cultivated garden plant.