Karoo Ice Age Karoo Ice Age The Karoo Ice Age, more commonly referred to as the Late Paleozoic Ice Age, from 360–260 million years ago (Mya) was the second major ice age of the Phanerozoic Eon. It is named after the tillite (Dwyka Group) found in the Karoo Basin of South Africa, where evidence for this ice age was first clearly identified in the 19th century. The tectonic assembly of the continents of Euramerica (later with the Uralian orogeny, into Laurasia) and Gondwana into Pangaea, in the Hercynian-Alleghany Orogeny, made a major continental land mass within the Antarctic region, and the closure of
Karoo Desert National Botanical Garden such as the succulents of the unique Robertson Karoo vegetation type, and patches of the threatened Breede Shale Renosterveld vegetation type. The cultivated area, with its network of pathways, includes a very large succulent collection. Including the greenhouses it maintains nearly 3,000 species. There are another 400 plant species that are naturally indigenous to the garden's premises. A range of wild animals also naturally occurs in the garden, including the shrub hare, grey mongoose, three tortoises species ("Chersina angulata", "Stigmochelys pardalis" & "Homopus areolatus") and a range of other small mammals, reptiles and amphibians. Karoo Desert National Botanical Garden The