| 中国南海沉积物中有孔虫的氧同位素研究 |
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| 引用本文： | 顾兆炎, 刘东生, 陈明扬, 郑淑蕙, 陈成业, 刘妍. 中国南海沉积物中有孔虫的氧同位素研究[J]. 第四纪研究, 1991, 11(1): 55-63. |
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| 作者姓名： | 顾兆炎 刘东生 陈明扬 郑淑蕙 陈成业 刘妍 |
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| 作者单位： | 1. 中国科学院地质研究所;; 2. 北京大学地质系 |
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| 摘 要： | 317-82-25和NS86-43孔岩芯分别取自南海北部和南海南部海底表层沉积物,V24-134孔岩芯取自菲律宾东苏禄海。通过对浮游有孔虫Pulleniatina obliquiloc(?)-late、Globorotalia menardii 和Neogloboquadrina dutertrei 的氧同位素分析,建立了氧同位素阶段,表明约60000年以来南海沉积物中有孔虫的氧同位素变化与世界各大洋相似,但有较大的变化幅度。这种差异可能是南海海水温度在冰期—间冰期较大幅度变化的结果。南海沉积速率明显大于远洋沉积速率,说明南海沉积物主要是陆源的。
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| 关 键 词： | 南海 有孔虫 氧同位素阶段 |
THE OXYGEN ISOTOPIC COMPOSITION OF THE FORAMINIFERA IN THE SEDIMENTS FROM THE SOUTH CHINA SEA |
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| Gu Zhaoyan, Liu Tungsheng, Chen Mingyang, Zheng Shuhui, Chen Chengye, Liu Yan. THE OXYGEN ISOTOPIC COMPOSITION OF THE FORAMINIFERA IN THE SEDIMENTS FROM THE SOUTH CHINA SEA[J]. Quaternary Sciences, 1991, 11(1): 55-63. |
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| Authors: | Gu Zhaoyan Liu Tungsheng Chen Mingyang Zheng Shuhui Chen Chengye Liu Yan |
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| Affiliation: | 1. Institute of Geology, Chinese Academy of Sciences;; 2. Department of Geology, Pcking University |
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| Abstract: | The core 317-82-25 （19°30.13′N,117°53.02′E,3205m） and NS86-43 （07°01.39′N,110°23.78′E,1763m） were derived from the north and south of the South China Sea respectively,andthe core V24-134 （08°50′N,119°14′E,2019m） was derived from the Sulu Sea.The coresmainly consist of foraminiferal calcareous clay and silts.Oxygen isitopic inalysis was sarriedout on the planktonic foraminifera Pulleniatina obliquiloculata,Globorotalia menardii and Neo-globoquadrina dutertrei.The oxygen isotopic records of three planktonic species in each corehave a similar variation.Three oxygen isotopic stages （1 to 3） have been recognized in theisotopic records of the core 317-82-25 and NS86-43.The bottom ages of the core 317-82-25 andNS 86-43 are about 53000 a B.P.and 65000 a B.P.respectively.The fact that averages ofthe sedimentation rates in the sites of the core 317-82-25 and NS86-43 which are estimated as5.5 and 4.6 cm/103a since about 60000a B.P.respectively are greater than that in pelagicregions reflects that the sediments in the South China Sea have mainly been derived from ter-restrial sources.The foraminiferal oxygen isotopic records of two cores from South ChinaSea are in general agreement with that of the cores from the deep-sea since about 60000a B.P.But the amplitudes of δ18O variatiins are greater than that in the pelagic cores from the Trop-ical Pacific Ocean.It might be resulted in that the amplitude of the temperature changesof the South China Sea was greater than one of the Tropical Pacific Ocean during glacial-interglacial because of the strong winter monsoon during glacial period. |
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