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Chen Wenrui,Lan Dongzhao,Chen Chenghui. 1998. Late Quaternary diatom and sea level changes in estuarine plain of the Jiulong River. Acta Oceanologica Sinica, (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
Received:September 23, 1997  Revised:November 15, 1997
DOI：
Key words:Late Quaternary  diatom  sea level change  estuarine plain  the Jiulong River
中文关键词:  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.
Author NameAffiliation
Chen Wenrui State Pilot Laboratory of Coast and Island Exploitation, Naning University, Naning 210093, China 
Lan Dongzhao Third Institute of Oceanography, State Oceanic Administration, Xiamen 361005, China 
Chen Chenghui Third Institute of Oceanography, State Oceanic Administration, Xiamen 361005, China 
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Abstract:
      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.
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.
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