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Reinterpretation of Late Quaternary Sediment Chronology of Lake Biwa, Japan, from Correlation with Marine Glacial-Interglacial Cycles

Published online by Cambridge University Press:  20 January 2017

Philip A. Meyers ,
Keiji Takemura  and
Shoji Horie
Philip A. Meyers
Affiliation:
Department of Geological Sciences and Center for Great Lakes and Aquatic Sciences, University of Michigan, Ann Arbor, Michigan 48109-1063
Keiji Takemura
Affiliation:
Beppu Geophysical Research Laboratory, Kyoto University, Noguchibaru, Beppu 874, Japan
Shoji Horie
Affiliation:
Beppu Geophysical Research Laboratory, Kyoto University, Noguchibaru, Beppu 874, Japan
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Abstract

A review of published stratigraphic records of pollen, sediment grain size, diatoms, and organic matter composition from Lake Biwa, Japan, identifies four pre-Holocene episodes of milder climate, increased surface runoff, and enhanced aquatic productivity, indicating intervals of warmer and wetter conditions which are interpreted as being interglacial. Correlation of these episodes to times of marine interglacial periods revises the age scale of the Lake Biwa sediment sequence which has been based on fission-track dating. The revised chronostratigraphic scale proposes an age of ca. 430,000 yr B.P. for the base of the 250-m-thick T Bed instead of the former age of ca. 700,000 yr B.P.

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Quaternary Research , Volume 39 , Issue 2 , March 1993 , pp. 154 - 162
Copyright
University of Washington

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