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Encyclopedia > Late Pleistocene
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Late Pleistocene (also known as Upper Pleistocene or the Tarantian) is a stage of the Pleistocene Epoch. The beginning of the stage is defined by the base of Eemian interglacial phase before final glacial episode of Pleistocene 126,000 ± 5,000 years ago. The end of the stage is defined exactly at 10,000 Carbon-14 years before present. The stage is followed by Holocene. Faunal stages are a subdivision of geologic time used primarily by paleontologists who study fossils rather than by geologists who study rock formations. ... Jump to: navigation, search The Pleistocene Epoch is part of the geologic timescale, usually dated as 1. ... The word epoch can mean either an interval of time, or a particular point in time used as a reference point. ... Radiocarbon dating is a radiometric dating method that uses the naturally occurring isotope carbon-14 to determine the age of carbonaceous materials up to ca. ... Jump to: navigation, search The Holocene Epoch is a geologic period that extends from the present back about 10,000 radiocarbon years. ...


The Wisconsin glaciation comprises much of the Late Pleistocene Epoch. Many megafauna become extinct over this period, a trend that continued into Holocene. Also, human species other than the modern human died out. Humanity spread to every continent except for Antarctica over the Late Pleistocene. The Wisconsin (in North America), Weichsel (in Scandinavia), Devensian (in the British Isles), Midlandian (in Ireland) or Würm glaciation (in the Alps) is the most recent period of the Ice Age, and ended some 10,000 BC. The Wisconsin/Weichsel/Devensian/Midlandian/Würm glaciation began about 70,000... Jump to: navigation, search It has been suggested that Giant animals be merged into this article or section. ... Jump to: navigation, search Species Homo sapiens See text for extinct species. ... Jump to: navigation, search Binomial name Homo sapiens Linnaeus, 1758 Subspecies Homo sapiens idaltu (extinct) Homo sapiens sapiens For other uses, see Human (disambiguation). ... Jump to: navigation, search Dymaxion map by Buckminster Fuller shows land mass with minimal distortion as only one continuous continent A continent (Latin continere, to hold together) is a large continuous land mass. ...


References

  • GeoWhen Database - Early Pleistocene
Tertiary sub-era Quaternary sub-era
Neogene period
Miocene Pliocene Pleistocene Holocene
Aquitanian Burdigalian Zanclean Early  
Langhian Serravallian Piacenzian Middle
Tortonian Messinian Gelasian Late

 
 

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