| PALYNOLOGICAL ASSEMBLAGES FROM THE QUATERNARY SEDIMENTS OF THE CHANGJIANG RIVER DELTA AND THE AGE OF STRATA AND PALEOGEOGRAPHY |
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| 作者姓名： | 王开发 张玉兰 蒋辉 韩信斌 |
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| 作者单位： | Department of Marine Geolopy, Tongji University, Shanghai;Department of Marine Geolopy, Tongji University, Shanghai;Department of Marine Geolopy, Tongji University, Shanghai;First Hydrogeologic Crew, Jiangsu, Nanjing |
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| 摘 要： | Through the palynological research of Quaternary sediments in Changjiang River Delta, 14 spores and - pollen zones might be distinguished, reflecting the vegetation succession and climate fluctuation of Quaternary, which conforms to the climate of the world.Zones 1-9 are thought of as Pleistocene and Zones 10-14 as Holocene based on the climatic fluctuation reflected by these zones and the comparison with the climatic stage at home and abroad.The marine facies sediments of Quaternary in the Changjiang River Delta contain abundant fossil spores and pollen and have obvious characters. Because the warm and humid climate reflected by the palynological assemblages of marine facies sediments often fittes with the transgression, the curve line of the climate fluctuation of Quaternary in the Delta coincides with that of sea level changes.
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| 收稿时间： | 1984/9/13 0:00:00 |
| 修稿时间： | 8/4/1985 12:00:00 AM |
PALYNOLOGICAL ASSEMBLAGES FROM THE QUATERNARY SEDIMENTS OF THE CHANGJIANG RIVER DELTA AND THE AGE OF STRATA AND PALEOGEOGRAPHY |
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| WANG KAIFA,ZHANG YULAN,JIANG HUI and HAN XINBIN.PALYNOLOGICAL ASSEMBLAGES FROM THE QUATERNARY SEDIMENTS OF THE CHANGJIANG RIVER DELTA AND THE AGE OF STRATA AND PALEOGEOGRAPHY[J].Acta Oceanologica Sinica,1986,5(2):257-270. |
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| Authors: | WANG KAIFA ZHANG YULAN JIANG HUI and HAN XINBIN |
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| Institution: | 1.Department of Marine Geolopy, Tongji University, Shanghai2.First Hydrogeologic Crew, Jiangsu, Nanjing |
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| Abstract: | Through the palynological research of Quaternary sediments in Changjiang River Delta,14 spores and-pollen zones might be distinguished,reflecting the vegetation succession and climate fluctuation of Quaternary,which conforms to the climate of the world.Zones 1-9 are thought of as Pleistocene and Zones 10-14 as Holocene based on the climatic fluctuation reflected by these zones and the comparison with the climatic stage at home and abroad.The marine facies sediments of Quaternary in the Changjiang River Delta contain abundant fossil spores and pollen and have obvious characters.Because the warm and humid climate reflected by the palynological assemblages of marine facies sediments often fittes with the transgression,the curve line of the climate fluctuation of Quaternary in the Delta coincides with that of sea level changes. |
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