【摘 要】
：
A detailed stable isotopic study based on benthic foraminifera from 1165 samples of ODP Site 1148 (18° 50.17.3′N, 116° 33.93′E, water depth 3308.3 m), north
【机 构】
：
Key Laboratory of Marine Geology
论文部分内容阅读
A detailed stable isotopic study based on benthic foraminifera from 1165 samples of ODP Site 1148 (18° 50.17.3′N, 116° 33.93′E, water depth 3308.3 m), northern South China Sea,provides an excellent oxygen isotopic record with an average resolution of 30 ka. It contains the most continuous δ18O data with highest resolution for the whole Neogene sequence in the world.The δ 18O curve shows a step-like increasing upwards and records 5 increases, 3 decreases and 2stable stages during the Neogene, reflecting the general trend of global coolin9. Among these events the δ18O decrease at 17.2-14.5 Ma, and two δ18O increases at 14.5-13.6 and 3.0-2.4Ma are most marked and globally comparable. The intervals at 13.6-10.2 and 6.0-3.0 Ma with the lowest-amplitude and least fluctuation in δ18O represent the most stable bottom water periods for the South China Sea.
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