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The Late Pleistocene is an unofficial age in the international geologic timescale in chronostratigraphy, also known as the Upper Pleistocene from a stratigraphic perspective. It is intended to be the fourth division of the Pleistocene Epoch within the ongoing Quaternary Period.
Glaciation in the Pleistocene was a series of glacials and interglacials, stadials and interstadials, mirroring periodic climate changes. The main factor at work in climate cycling is now believed to be Milankovitch cycles. These are periodic variations in regional and planetary solar radiation reaching the Earth caused by several repeating ...
Pleistocene Epoch, earlier and major of the two epochs of the Quaternary Period of Earth’s history, an epoch during which a succession of glacial and interglacial climatic cycles occurred. It ended 11,700 years ago.
The Late Pleistocene refers to a period of significant climatic and faunal changes in North America, marked by the extinction of most of the continent's megafauna at the end of this epoch. AI generated definition based on: Reference Module in Earth Systems and Environmental Sciences, 2023. About this page.
The best-known are those that occurred from the time of the last interglaciation, about 125,000 years ago, to the present. The growth of large ice sheets, ice caps, and long valley glaciers was among the most significant events of the Pleistocene. During times of extensive glaciation, more than 45 million square km.
The late Pleistocene is a geological epoch that spans from approximately 126,000 to about 11,700 years ago, marked by significant climatic fluctuations and the emergence of modern Homo sapiens.
1 sty 2022 · Late Pleistocene orbital and millennial-to-centennial climate changes strongly affected European ecosystems, leading to a contrasted vegetation response following north–south and east–west gradients.
