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《Marine Geology & Quaternary Geology》 1982-02
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LATE CENOZOIC PLANKTONIC FORAMINIFERA AND ZONATIONS IN THE NORTHERN SOUTH CHINA SEA

Qin Guoquan (Comprehensive Research Brigade of Headquarters for Geological Investigation of South China Sea)  
The present paper introduces the geographic distribution of the planktonic foraminifera. collected from drill holes of the northern South China Sea. Basedon the vertical change of the planktonic foraminifera in Lei-Qiong area, Ying-gehai sea area, Xisha Islands, and Basin of Zhujiang river mouth, the late Cenozoic marine layers in the northern South China Sea may be delimited into 7 planktonic foraminiferal zonations: Lower Miocene I . Globorotalia jiaoweiensis-Cassigermella chipolensis zonation Middle Miocene II. Turborolalia siakensis zonation Upper Miocene III. Turborolalia acostaensis-1st left coiling zonation of; Menardiform glo-borotalias Pliocene IV. Globorotalia multicamerata-1st right coiling zouatiou of Menardiform globorotalias V . Globorotalia altispira-2nd left coiling zonation of Menardiform globorotalias VI. Turborotalia tosasnsis-2nd right coiling zonation of Menardiform globorotalias Quaternary VII. Globorotalia truncatulinoides-3rd left coiling zonation of Menardiform globorotalias The above zonations can be compared with the planktonic foraminiferal zonations of adjacent areas and the cosmopolitan. The sedimentory environment of the northern South China Sea in late Cenozoic is infered as bellow: The transgressions occured six times at least, the largest one presented in early Pliocene, The palaeotemperatural changes might be four, in Miocene it seems to be cooler and Pliocene was the coldest in all the late Cenozoic period.
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