[U-11] Climate change during the Quaternary and Anthropocene

[U11-P10] Hydroclimatic variability during the last deglaciation based on biogenic silica records from Lake Suigetsu, Japan

*Madoka Murai¹, Masayuki Ikeda¹, Takeshi Nakagawa², Ryuji Tada³, Daishi Horiuchi⁴, Tsuyoshi HARAGUCHI^11,5, Ikuko Kitaba², Yoshiaki Suzuki⁶, Katsuya Gotanda⁷, Keitaro Yamada⁸, TAKAAKI ITAI¹, Jonathan TYLER⁹, Alexander FRANCKE⁹, Vanessa NOWINSKI⁹, Ryuhei Sanjo¹⁰, Kazuo Mizoguchi¹⁰ (1. The University of Tokyo, Graduate School of Science, Japan, 2. Ritsumeikan University, Research Center for Palaeoclimatology, Japan, 3. Earth Science Research Center, Chiba Institute of Technology, Japan, 4. Japan Coast Guard Academy, Japan, 5. International Research Institute of Disaster Science (IRIDeS), Tohoku University; STORY Co., Ltd., Japan, 6. Geological Survey of Japan, National Institute of Advanced Industrial Science and Technology (AIST), Japan, 7. Chiba University of Commerce, Faculty of Global and Regional Studies, Japan, 8. Yamagata University, Faculty of Science, Japan, 9. Adelaide University, School of Physics, Chemistry and Earth Science, Australia, 10. Central Research Institute of Electric Power Industry (CRIEPI), Japan, 11. STORY, Ltd.)

Keywords:Chronological correlation, Last deglaciation, climate change, East Asian monsoon, FTIR, lake sediments