Eolian Dust Deposition in the Last Glacial Stage (43-12ka)in Tanigumi Moor, Gifu Prefecture, Central japan

摘要

The Tanigumi core records the content, grain size of inorganic material, and ESR intensity of fine quartz between 43ka and 12ka and reveals changes in the deposition and trajectory of eolian dust from the Asian continent. The inorganic material content during isotope stage 3 was 0.1 to 1.35g/cm~2, and fluctuated more widely than that of isotope stage 2.