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A proposed Global Stratotype Section and Point (GSSP) for the base of the Upper (Late) Pleistocene Subseries (Quaternary System/Period)
作者姓名:Thomas Litt  ;Philip Gibbard
作者单位:[1]Steinmann Institute for Geology, Mineralogy and Palaeontology, University of Bonn, Germany.; [2]Godwin Institute of Quatemagy Research, Department of Geography, University of Cambridge, Downing Street Cambridge CB2 3EN, England.
摘    要:Following the precedence already established during the INQUA Congress in 1932, the Middle/Upper (Late) Pleistocene boundary is defined at the base of the Last Interglacial, the Eemian Stage. It is proposed that a high-resolution core sequence from the Amsterdam Terminal (the Eemian Stage parastratotype) should constitute the Global Stratotype Section and Point (GSSP) for the base of the Upper (Late) Pleistocene Subseries (Quaternary System/Period).

关 键 词:地球  洪积世  间冰期  边界
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