| Chen Wenrui,Lan Dongzhao,Chen Chenghui.Late Quaternary diatom and sea level changes in estuarine plain of the Jiulong River[J].Acta Oceanologica Sinica,1998,(4):509-518 |
| Late Quaternary diatom and sea level changes in estuarine plain of the Jiulong River |
| Late Quaternary diatom and sea level changes in estuarine plain of the Jiulong River |
| 投稿时间：1997-09-23 修订日期：1997-11-15 |
| DOI： |
| 中文关键词: Late Quaternary diatom sea level change estuarine plain the Jiulong River |
| 英文关键词:Late Quaternary diatom sea level change estuarine plain the Jiulong River |
| 基金项目:This study was supported by the Natural Science Funds of Fujian Province (D95008). Project coding:SCIEL 21197132. |
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| 中文摘要: |
| Four units and twenty-four zones of diatom have been discerned in the Borehole ZKS in the estuarine plain of the)iulong River,Fujian Province.Comprehensive analysis of these,together with microbiological assemblages and age determinations in some other boreholes,shows that during the Late Wiirm Glacial,sea level of the study area rose and fell frequently,but had principally been in the environments of estuary-bay.This mainly resulted from the tectonic subduction.In this period 3 low sea levels occurred,at 18,16 and 12 kaBP respectively.During Hokx"ene,sea water intruded massively and the sea level over the transgression maximum had been 5-10 m higher than that of the present. |
| 英文摘要: |
| Four units and twenty-four zones of diatom have been discerned in the Borehole ZKS in the estuarine plain of the)iulong River,Fujian Province.Comprehensive analysis of these,together with microbiological assemblages and age determinations in some other boreholes,shows that during the Late Wiirm Glacial,sea level of the study area rose and fell frequently,but had principally been in the environments of estuary-bay.This mainly resulted from the tectonic subduction.In this period 3 low sea levels occurred,at 18,16 and 12 kaBP respectively.During Hokx"ene,sea water intruded massively and the sea level over the transgression maximum had been 5-10 m higher than that of the present. |
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