...
机译:精确的过时的AMS〜(14)C海洋核心揭示了南海北部千禧年尺度的亚洲季风变化的复杂性(MD972146,MD972148)
Institute of Applied Geosciences, National Taiwan Ocean University, Keelung, Taiwan,Center for Marine Bioenvironment and Biotechnology, National Taiwan Ocean University, Keelung, Taiwan;
Institute of Applied Geosciences, National Taiwan Ocean University, Keelung, Taiwan,Center for Marine Bioenvironment and Biotechnology, National Taiwan Ocean University, Keelung, Taiwan;
Faculty of Environmental Earth Science, Hokkaido University, Sapporo, Japan;
Department of Ocean Floor Ceoscience and Center for Earth Surface System Dynamics, Atmosphere and Ocean Research Institute, University of Tokyo, Kashiwa, Japan,Department of Earth and Planetary Sciences, University of Tokyo, Japan,Institute of Biogeosciences, Japan Agency for Marine-Earth Science and Technology, Yokosuka, Japan;
AMS ~(14)C dating; Oxygen isotope; Carbonate; Monsoon; Cave sediment; South China Sea;
机译:由东海北部海域盐度(ECS)推断的东亚夏季风的千年尺度变化及其在海洋同位素阶段(MIS)对日本海的影响3
机译:在过去的45,000年中,南海北部的水文变异性:基于U-37(k')和TEX86H代理从海洋沉积物芯中重建温度的新见解(MD972146)
机译:过去45,000年南海北部千禧年烯酮海表温度变化(MD972146)
机译:马六甲海峡北部海藻叶绿素a的季节和年际变化与亚洲季风的关系
机译:南亚季风的季节内变化
机译:晚第四纪南海东亚夏季风演化的粘土矿物学和地球化学代理
机译:Evolution of asian monsoon variability revealed by oxygen isotopic record of middle Holocene massive coral in the northern south China sea