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
Gulf of Oman desert and semi-desert of mangroves at Khor Kalba Nature Reserve on the Gulf of Oman in the UAE near the border with Oman. Gulf of Oman desert and semi-desert The Gulf of Oman desert and semi-desert is a coastal ecoregion on the Persian Gulf and the Gulf of Oman in Oman and the United Arab Emirates at the northeastern tip of the Arabian Peninsula. The climate is hot and dry; the ecoregion contains a mixture of habitats including mangrove swamps, lagoons and mudflats on the coast, and gravelly plains and savanna with thorny acacia trees inland. The mangrove areas are dominated by "Avicennia