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Wang Qiang,Li Yude,Tian Guoqiang,Lin Fang.Quaternary marine ostracoda on the west coast of the Bohai Sea[J].Acta Oceanologica Sinica,1988,(1):94-103
Quaternary marine ostracoda on the west coast of the Bohai Sea
Quaternary marine ostracoda on the west coast of the Bohai Sea
投稿时间:1986-11-02  修订日期:1987-07-15
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作者单位
Wang Qiang Tianjin Institute of Geology and Mineral Resources, Tianjin, China 
Li Yude Second Hydrogeological Team of Shandong Province, Dezhou, China 
Tian Guoqiang Institute of Geomechanics, Beijing, China 
Lin Fang Institute of Hydrogeology-Engineering Geology, Zhengding, China 
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中文摘要:
      According to the results of analysis of the marine ostracoda biofacies from over 160 drilled holes on the west coast of the Bohai Sea, i.e. Hebei and Shandong Provinces, Tianjin, and the east part of Beijing, the present paper is a discussion of their palaeoecological and stratigraphigical significance. The investigation of ostracoda thanatocoenoces in the modern coastal zone suggests that the distribution of marine ostracoda has been controlled by the salinity and depth of water. The study of Quaternary marine ostracoda should be concentrated mainly on the determination of their biofacies and palaeogeographigical conditions, so as to provide evidence for the determination of transgression range, palaeoshoreline and sca-level changes.
英文摘要:
      According to the results of analysis of the marine ostracoda biofacies from over 160 drilled holes on the west coast of the Bohai Sea, i.e. Hebei and Shandong Provinces, Tianjin, and the east part of Beijing, the present paper is a discussion of their palaeoecological and stratigraphigical significance. The investigation of ostracoda thanatocoenoces in the modern coastal zone suggests that the distribution of marine ostracoda has been controlled by the salinity and depth of water. The study of Quaternary marine ostracoda should be concentrated mainly on the determination of their biofacies and palaeogeographigical conditions, so as to provide evidence for the determination of transgression range, palaeoshoreline and sca-level changes.
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