该研究通过对南大西洋ODP 1263和1265站位进行多指标联合分析，揭示了极热气候时期海洋最小含氧层（ODZs）与氮循环的耦合演变机制。

Slab dehydration and potassium-lithium recycling in the forearc indicated by potassium and lithium isotope compositions of exhumed metabasites

Oxygenated deep waters fed early Atlantic overturning circulation upon Antarctic glaciation

Petrogenesis of High-Alumina Basalts: Implications for Magmatic Processes Associated with the Opening of the South China Sea