9:00 AM - 9:15 AM
*Shunsuke KUROKAWA1, Ryuji TADA1, Takuya ITAKI2, Satoshi TAKAHASHI1 (1.Department of Earth and Planetary Science, University of Tokyo, 2.Geological Survey of Japan, AIST)
Oral
Symbol M (Multidisciplinary and Interdisciplinary) » M-IS Intersection
Thu. May 28, 2015 9:00 AM - 10:45 AM 202 (2F)
Convener:*Ryuji Tada(Department of Earth and Planetary Science, Graduate School of Science, The Univeristy of Tokyo), Takeshi Nakagawa(Ritsumeikan University), Ken Ikehara(Institute of Geology and Geoinformation, National Institute of Advanced Industrial Science and Technology), Masanobu Yamamoto(Faculty of Environmental Earth Science, Hokkaido University), Chair:Masanobu Yamamoto(Faculty of Environmental Earth Science, Hokkaido University)
With increasing awareness of human impact on global climate change, people pay more attention to the changes in spatial pattern, magnitude, and periodicity of climatic changes, as well as intensity and frequency of extreme weather, which are all relevant to near future regional-scale climatic changes and natural disasters. Having robust knowledge on magnitudes, frequencies, spatial patterns, and mechanisms of past climatic changes is a prerequisite to understand near future climatic changes. However, existing paleo-climatic records do not have sufficient spatio-temporal resolutions and age precision to address key questions. In addition, types of proxies as well as their precisions are variable and not inter-calibrated to each other. Recently, high-resolution absolute time scale back to 50 ka was established using varved sediments of Lake Suigetsu that enables us to reconstruct paleo-climatic changes in such high resolution as decadal or even annual. Likewise, continuous sediment records back to more than 2.5 Ma were recovered from the Sea of Japan by IODP Exp. 346, which has potential to provide a reference time scale for the entire Quaternary in East Asia-NW Pacific region. We aim to extend these reference time scales to paleo-observatory sites in East Asia-NW Pacific region using various stratigraphic correlation techniques and standardized protocols. The paleo-climate observatory network would allow us to interrogate causal links between components of the climate system.
9:00 AM - 9:15 AM
*Shunsuke KUROKAWA1, Ryuji TADA1, Takuya ITAKI2, Satoshi TAKAHASHI1 (1.Department of Earth and Planetary Science, University of Tokyo, 2.Geological Survey of Japan, AIST)
9:15 AM - 9:30 AM
*Kaori AOKI1 (1.Faculty of Geo-Environmental Science, Rissho University)
9:30 AM - 9:45 AM
*Ken IKEHARA1, Kazuko USAMI1, Toshiya KANAMATSU2 (1.Geological Survey of Japan, AIST, 2.CEAT, JAMSTEC)
9:45 AM - 10:00 AM
*Keita SAITO1, Ryuji TADA1, Hongbo Zheng2, Tomohisa IRINO3, Ke WANG3, Chao Luo4, Yuya TSUNAZAWA1, Saiko SUGISAKI1 (1.University of Tokyo, 2.Nanjing Normal University, 3.Hokkaido University, 4.Nanjing University)
10:00 AM - 10:15 AM
*Ke WANG1, Ryuji TADA2, Tomohisa IRINO1, Hongbo ZHENG3, Keita SAITO2, Saiko SUGISAKI2, Masao UCHIDA4 (1.Hokkaido University, 2.The University of Tokyo, 3.Nanjing Normal Univ., 4.National Institute for Environmental Studies)
10:15 AM - 10:30 AM
*Saiko SUGISAKI1, Jan-Pieter Buylaert2, Andrew Murray3, Ryuji TADA1, Hongbo Zheng4, Ke WANG5, Keita SAITO1, Tomohisa IRINO5, Masao UCHIDA6 (1.University of Tokyo, 2.Aarhus University, 3.Technical University of Denmark, 4.Nanjing Normal University, 5.Hokkaido University, 6.National Institute for Environmental Studies)
10:30 AM - 10:45 AM
*Yoshiaki SUZUKI1, Ryuji TADA1, Kana NAGASHIMA2, Tomohisa IRINO3, Kazuyoshi YAMADA4, Takeshi NAKAGAWA5, Hideaki KOJIMA6, Project members SG12/067 (1.Univ. Tokyo, 2.JAMSTEC, 3.Hokkaido University, 4.Museum of Natural and Environmental history, Shizuoka, 5.Ritsumeikan University, 6.Wakasa-Mikata Jomon Museum, 7.none)