Paleontology
The Quaternary is the most recent geological period in the Earth's history, spanning from about 2.58 million years ago to the present. It is characterized by significant climate changes, including the onset of glaciations, and the evolution of modern humans and many other species. This period is divided into two epochs: the Pleistocene, marked by repeated ice ages, and the Holocene, which is the current interglacial period.
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