*Jumpei Yoshioka1, Yusuke Suganuma1,2, Takuya Itaki3, TAKAAKI ITAI4
(1. National Institute of Polar Research, Research Organization of Information and Systems, 2. The Graduate University for Advanced Studies (SOKENDAI), 3. Geological Survey of Japan, National Institute of Advanced Industrial Science and Technology, 4. Department of Earth and Planetary Science, Graduate School of Science, the University of Tokyo)
Keywords:East Antarctic coastal margins, siliceous microfossils, silicon stable isotope ratios, silicon cycle, surface sediment