Karoo Karoo biome. The number of mainly succulent plant species is very high for an arid area of this size anywhere in the world. The Nama Karoo biome is located entirely on the central plateau mostly at altitudes between 1000 and 1500 m. It incorporates nearly the whole of the historical and geographical Great Karoo, but also includes a portion of southern Namibia's Namaqualand, and South Africa's Bushmanland" (both local geographical names, not names of biomes). It is the second-largest biome in South Africa, and forms the botanical transition between the Fynbos biome to the south and the savannah biome to
Karoo National Park Karoo paleontologically famous. Their fossils have been found all over the Karoo. Some of these fossils are on display in the Park, though none of them have been found there. About 60 million years after the Beaufort sediments had been laid down and topped with a thick layer of desert sands, there was an outpouring of lava on to Southern Africa on a titanic scale. The entire area was covered within a very short space of time with a 1.5 km thick layer of lava, the remnants of which form the Drakensberg. In addition to flooding the African surface with