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YANG Qian,SONG Xianli,SUN Yao,HUANG Jiansheng.Application of biologic silicon in modern sedimentary section to reconstruction of phytoplankton changes in the East China Sea and the Huanghai Sea during last 200 years[J].Acta Oceanologica Sinica,2012,(2):70-77
Application of biologic silicon in modern sedimentary section to reconstruction of phytoplankton changes in the East China Sea and the Huanghai Sea during last 200 years
Application of biologic silicon in modern sedimentary section to reconstruction of phytoplankton changes in the East China Sea and the Huanghai Sea during last 200 years
投稿时间:2011-03-15  修订日期:2011-11-07
DOI:10.1007/s13131-012-0193-0
中文关键词:  typical sea areas of the East China Sea and the Huanghai Sea  sediment  BSi  productivity reconstruction
英文关键词:typical sea areas of the East China Sea and the Huanghai Sea  sediment  BSi  productivity reconstruction
基金项目:The National Key Basic Research Program of China under contract No.2006CB400007;the National Natural Science Foundation of China under contract No.40876088.
作者单位E-mail
YANG Qian Key Laboratory of Marine Chemistry Theory and Technology, Ministry of Education, Ocean University of China, Qingdao 266100, China
Yellow Sea Fisheries Research Institute, Chinese Fisheries Science Academy, Qingdao 266071, China 
 
SONG Xianli Key Laboratory of Marine Chemistry Theory and Technology, Ministry of Education, Ocean University of China, Qingdao 266100, China
Yellow Sea Fisheries Research Institute, Chinese Fisheries Science Academy, Qingdao 266071, China
Mariculture Institute of Shandong Province, Qingdao 266002, China 
 
SUN Yao Yellow Sea Fisheries Research Institute, Chinese Fisheries Science Academy, Qingdao 266071, China sunyao@ysfri.ac.cn 
HUANG Jiansheng Yellow Sea Fisheries Research Institute, Chinese Fisheries Science Academy, Qingdao 266071, China
Xiamen University, Xiamen 361005, China 
 
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中文摘要:
      Biomarkers had been widely used to reconstruct phytoplankton productivity,and this method was applied in the East China Sea and the Huanghai Sea (Yellow Sea).In this study,Biologic Silicon (BSi) was used as productivity proxy to reconstruct productivity change of phytoplankton during last 200 years.The results show that the BSi contents of surficial sediments were in the range of 0.018%-2.516%,averaging 0.726%,and had a similar variation trend with phytoplankton biomass.The vertical distribution profiles revealed that BSi contents were relatively stable,in accordance with the variations of the contemporary phytoplankton standing crop index.According to the stability analysis of BSi in sediments,BSi was not degradaded for the past two hundred years and remained in sediments steadily.Thus,BSi in sediments had the potential to invert paleoproductivity.To conduct further survey,the linear regression equation between BSi contents and phytoplankton biomass index could be used to calculate the phytoplankton productivity by BSi,so that paleoproductivity may be reconstructed during last 200 years.
英文摘要:
      Biomarkers had been widely used to reconstruct phytoplankton productivity,and this method was applied in the East China Sea and the Huanghai Sea (Yellow Sea).In this study,Biologic Silicon (BSi) was used as productivity proxy to reconstruct productivity change of phytoplankton during last 200 years.The results show that the BSi contents of surficial sediments were in the range of 0.018%-2.516%,averaging 0.726%,and had a similar variation trend with phytoplankton biomass.The vertical distribution profiles revealed that BSi contents were relatively stable,in accordance with the variations of the contemporary phytoplankton standing crop index.According to the stability analysis of BSi in sediments,BSi was not degradaded for the past two hundred years and remained in sediments steadily.Thus,BSi in sediments had the potential to invert paleoproductivity.To conduct further survey,the linear regression equation between BSi contents and phytoplankton biomass index could be used to calculate the phytoplankton productivity by BSi,so that paleoproductivity may be reconstructed during last 200 years.
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