| Wang Qiang,Li Xiuwen,Zhang Zhiliang,Li Fenglin,Shao Jun,Bai Dezhong,Shang Xuexi,Tang Ruolu.Palaeoceanological significance of Holocene ostracean banks in Tianjin area[J].Acta Oceanologica Sinica,1991,(2):249-262 |
| Palaeoceanological significance of Holocene ostracean banks in Tianjin area |
| Palaeoceanological significance of Holocene ostracean banks in Tianjin area |
| 投稿时间：1990-10-24 修订日期：1990-11-14 |
| DOI： |
| 中文关键词: |
| 英文关键词: |
| 基金项目:The subject was funded by Xi'an Laboratory of Loess and Quaternary Geology, Academia Sinica. |
| 作者 | 单位 | | Wang Qiang | Tian jin Institute of Geology and Mineral Resources, Chinese Academy of Geological Sciences, Tianjin, 300170, China | | Li Xiuwen | Tian jin Institute of Geology and Mineral Resources, Chinese Academy of Geological Sciences, Tianjin, 300170, China | | Zhang Zhiliang | Tian jin Institute of Geology and Mineral Resources, Chinese Academy of Geological Sciences, Tianjin, 300170, China | | Li Fenglin | Tian jin Institute of Geology and Mineral Resources, Chinese Academy of Geological Sciences, Tianjin, 300170, China | | Shao Jun | Tianjin, Municipica Bureau of Geology and Mineral Resources, Tianjin, China | | Bai Dezhong | Tianjin, Municipica Bureau of Geology and Mineral Resources, Tianjin, China | | Shang Xuexi | Tianjin, Municipica Bureau of Geology and Mineral Resources, Tianjin, China | | Tang Ruolu | The Cultural Museum of Ninghe County, Tianjin Municipality, Tianjin, China |
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| 中文摘要: |
| On the basis of the study of ostracean banks in Tianjin area,the present study recognized that the ostracean banks at Ninghe County in Tianjin area are well developed along the west coast of the Bohai Sea; they consist of thanato-coenose and taphocoenose from Crassistrea gigars and C.revularis.From the 14C datings it can be known that the banks had formed from early Middle-Holocene and continued up to over 2 ka BP (14C age).The top has different reliefs.Although there is an effect of spatial shift of estuary position,the top is only distributed in the range of -0.50~-2.50 m(Huanghai elevation minus National elevation system).The banks cannot explain the sea-level fluctuation.As the string ostracean banks are distributed near E-W direction,it suggests that the direction of tidal currents was then similar to that of the present day. |
| 英文摘要: |
| On the basis of the study of ostracean banks in Tianjin area,the present study recognized that the ostracean banks at Ninghe County in Tianjin area are well developed along the west coast of the Bohai Sea; they consist of thanato-coenose and taphocoenose from Crassistrea gigars and C.revularis.From the 14C datings it can be known that the banks had formed from early Middle-Holocene and continued up to over 2 ka BP (14C age).The top has different reliefs.Although there is an effect of spatial shift of estuary position,the top is only distributed in the range of -0.50~-2.50 m(Huanghai elevation minus National elevation system).The banks cannot explain the sea-level fluctuation.As the string ostracean banks are distributed near E-W direction,it suggests that the direction of tidal currents was then similar to that of the present day. |
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