Biomarker Records of Phytoplankton Productivity and Community Structure Changes During the Last 14000 Years in the Mud Area Southwest off Cheju Island, East China Sea  

作　　者：YUAN Zineng XING Lei LI Li ZHANG Hailong XIANG Rong ZHAO Meixun 

机构地区：[1]Key Laboratory of Marine Chemistry Theory and Technology (Ocean University of China), Ministry of Education/Qingdao Collaborative Innovation Center of Marine Science and Technology [2]Institute of Marine Organic Geochemistry, Ocean University of China [3]CAS Key Laboratory of Marginal Sea Geology, South China Sea Institute of Oceanology, Chinese Academy of Sciences

出　　处：《Journal of Ocean University of China》2013年第4期611-618,共8页中国海洋大学学报（英文版）

基　　金：supported by the National Basic Research Program of China (973 Program 2010CB428901);the National Natural Science Foundation of China (Grant Nos.41020164005,41221004);the ‘111’ Project

摘　　要：The ecological environment in the East China Sea(ECS)and the Yellow Sea(YS)has changed significantly due to sea-level rising and the Kuroshio incursion since the last deglaciation.In this study,biomarker records of core F10B from the mud area southwest off Cheju Island(MSWCI)were generated to evaluate phytoplankton productivity and community structure changes in response to environmental evolution during the last 14 kyr.The contents of diatom,dinoflagellate and haptophyte biomarkers(brassicasterol,dinosterol and C37alkenones)display similar trends,with increasing phytoplankton productivity during the last 14kyr due to the increased influences of the Kuroshio,and especially due to the eddy-induced upwelling during the late Holocene.On the other hand,the contents of terrestrial biomarkers(C28+C30+C32n-alkanols)and terrestrial organic matter(TOM)proxies(TMBR′and BIT)all reveal decreasing TOM input into the area around the sampling site for the 14 kyr,mostly due to sea-level ris-ing.Phytoplankton biomarker ratios reveal a shift from a haptophyte-dominated community at 6.2 2.5 kyr BP to a diatom-dominated community at 2.5 1.45 kyr BP,likely caused by a stronger cold eddy circulation system at 2.5 1.45 kyr BP in the MSWCI.The ecological environment in the East China Sea （ECS） and the Yellow Sea （YS） has changed significantly due to sea-level rising and the Kuroshio incursion since the last deglaciation. In this study, biomarker records of core F10B from the mud area southwest off Cheju Island （MSWCI） were generated to evaluate phytoplankton productivity and community structure changes in response to environmental evolution during the last 14kyr. The contents of diatom, dinoflagellate and haptophyte biomarkers （brassicasterol, dinosterol and C37 alkenones） display similar trends, with increasing phytoplankton productivity during the last 14 kyr due to the increased influences of the Kuroshio, and especially due to the eddy-induced upwelling during the late Holocene. On the other hand, the contents of terrestrial biomarkers （C28 ＋C30 ＋C32 n-alkanols） and terrestrial organic matter （TOM） proxies （TMBR＇ and BIT） all reveal decreasing TOM input into the area around the sampling site for the 14kyr, mostly due to sea-level rising. Phytoplankton biomarker ratios reveal a shift from a haptophyte-dominated community at 6.2-2.5 kyrBP to a diatom-dominated community at 2.5-1.45 kyr BP, likely caused by a stronger cold eddy circulation system at 2.5-1.45 kyrBP in the MSWCI.

关 键 词：BIOMARKER East China Sea PRODUCTIVITY community structure TMBR BIT 

分 类 号：Q948.8[生物学—植物学]