中文摘要：

从在南部的华南海(SCS ) 的面象对象程序设计地点 1143 基于深海的花粉结果(512--76 m ) ，包围的岛和暴露的大陆人架上的气候和植被进化顺序被讨论。花粉记录证明花粉流入是相当低的 before8.15 妈并且以后戏剧性地增加了。流入变化能被归功于，在一个方面上，到在导致的南部的 SCS 附近的 tectonics 变丑快速岛和沉积率和花粉流入并且在另外的方面上的随后的增加高举到气候冷却和季风改进。约 2.63 妈是另一条明显的边界，这次后来增加花粉和孢子流入主要与全球气候冷却有关。花粉流入价值的 Spectrumanalysis 给那 2 妈， 0.67 妈，和 0.19--0.17 看妈周期存在 during12 -- 3.0 妈，当 0.1 个妈 and46.9 ka 周期在 3.0--2.0 期间存在时妈。

英文摘要：

Based on deep-sea pollen results （512-76 m） from ODP Site 1143 in the southern South China Sea （SCS）, the climate and vegetation evolution sequence on the surrounding islands and the exposed continental shelf are discussed. The pollen records show that the pollen influx was quite low before 8.15 Ma and increased dramatically afterwards. The influx changes can be ascribed, on one side, to tectonics deformations around the southern SCS resulting in rapid uplift of islands and subsequent increase of the sediment rates and pollen influx and on the other side to climate cooling and monsoon enhancement. Around 2.63 Ma was another obvious boundary, the increasing of pollen and spores influx since this time was mainly related to global climate cooling. Spectrum analysis of pollen influx values shows that 2 Ma, 0.67 Ma, and 0.19-0.17 Ma cycles existed during 12-3.0 Ma, while 0.1 Ma and 46.9 ka cycles existed during 3.0-2.0 Ma.