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
Kazakh semi-desert in livestock numbers in Kazakhstan is allowing the native plants a greater opportunity to regenerate. The Kazakh semi-desert is an ecotone between the Kazakh Steppe to the north and the Central Asian northern desert to the south, running in a band across central Kazakhstan. The climate here is semi-arid and highly continental. Precipitation averages between and annually. Mean temperatures in January range from and , while July means are between and . Annual average temperatures are around . The region's topography consists of vast, flat plains and salt flats broken by dissected plateaus (known locally as ""melkosopochniki""). As a transition