Gondwana - Climate

Climate

During the late Paleozoic, Gondwana extended from a point at or near the south pole to near the equator. Across much of Gondwana, the climate was mild. During the Mesozoic, the world was on average considerably warmer than today. Gondwana was then host to a huge variety of flora and fauna for many millions of years. The laurel forest of Australia, New Caledonia and New Zealand have a number of other related species of the laurissilva de Valdivia, through the connection of the Antarctic flora as gymnosperms and deciduous angiosperm Nothofagus. Corynocarpus laevigatus is called the bay of New Zealand, Laurelia novae-zelandiae belongs to the same genus Laurelia. The sempervirens tree niaouli, it grows in Australia, New Caledonia and New Zealand. New Caledonia and New Zealand ecoregion are separated by continental drift from Australia 85 million years ago. The islands still retain plants and animals that originated in Gondwana and spread to the southern hemisphere continents later. But there is strong evidence of glaciation during Carboniferous to Permian time, especially in South Africa.

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