Climate and Geography
Paleogene period witnessed a steady cooling of the earth's climate from the hothouse conditions of the preceding Cretaceous period. Ice began to form at both the North and South poles and seasonal changes were more pronounced in the northern and southern hemispheres, which had a significant impact on plant and animal life. The northern supercontinent of Laurasia gradually broke apart into North America in the west and Eurasia in the east, while its southern counterpart Gondwana continued to fracture into South America, Africa, Australia and Antarctica, all of which began drifting to their present positions.
Paleogene period witnessed a steady cooling of the earth's climate from the hothouse conditions of the preceding Cretaceous period. Ice began to form at both the North and South poles and seasonal changes were more pronounced in the northern and southern hemispheres, which had a significant impact on plant and animal life. The northern supercontinent of Laurasia gradually broke apart into North America in the west and Eurasia in the east, while its southern counterpart Gondwana continued to fracture into South America, Africa, Australia and Antarctica, all of which began drifting to their present positions.
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