Neogene burial of organic carbon in the global ocean

Greigite formation modulated by turbidites and bioturbation in deep-sea sediments offshore Sumatra

Diagenetic priming of submarine landslides in ooze-rich substrates

Persistent high latitude amplification of the Pacific Ocean over the past 10 million years

Obliquity Induced Latitudinal Migration of the Intertropical Convergence Zone During the Past ∼410 kyr

首次定量评估了中中新世时期巽他陆架沉积物和碳封存的总量及速率

晚上新世—中更新世（~3.17-1.07 Ma）高分辨率（~1.53 kyr）印尼穿越流中层水（ITF intermediate water, ITF-IW）古海洋学记录

揭示了海峡闭/开状态对科林斯裂谷盆地沉积和物源演化的控制，为大陆边缘活动裂谷沉积过程研究提供了新思路

揭示类似现代规模的珠江流域形成于约三千万年前，源于青藏高原东南部隆升和中国东部地形倒转

研究团队基于IODP 349、367、368及368X航次在南海的钻探数据，半定量化约束了海盆的沉积过程，探讨了控制因素和可能的沉积物源