The Pleistocene epoch is a geological time period that lasted from about 2.6 million to 11,700 years ago. It is also known as the Ice Age, as it was marked by extensive glaciation and the repeated advance and retreat of ice sheets across the Earth's surface.
During the Pleistocene epoch, the Earth experienced dramatic climate fluctuations, with alternating cold glacial periods and warmer interglacial periods. These climatic changes had a profound impact on the Earth's ecosystems and flora and fauna distribution.
One of the defining features of the Pleistocene epoch was the presence of vast ice sheets that covered large portions of the Earth's surface. These ice sheets had a significant impact on shaping the landscape, carving out valleys and shaping mountain ranges.
The Pleistocene epoch was home to a variety of now-extinct megafauna, including mammoths, mastodons, saber-toothed cats, and giant ground sloths. These large animals roamed the Earth during this time period, but many of them went extinct at the end of the Pleistocene, possibly due to a combination of climate change and human activity.
By studying the Pleistocene epoch, we can gain a better understanding of the Earth's past climate dynamics and the impact of environmental changes on ecosystems and species diversity.
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