"Quaternary Asia" typically refers to the Quaternary period concerning the continent of Asia, which is the most recent geological time period spanning from about 2.6 million years ago to the present day. The Quaternary period is characterized by significant climatic changes, the development of modern ecosystems, and the appearance and evolution of human beings. During the Quaternary, Asia saw major changes in its environment and biodiversity due to glaciation and climate fluctuations.
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