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《Marine Geology & Quaternary Geology》 2015-01
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STRATIGRAPHIC SEQUENCE AND DEPOSITIONAL ENVIRONMENT SINCE MARINE ISOTOPE STAGE 6 IN THE CONTINENTAL SHELF OF THE WESTERN SOUTH YELLOW SEA:A CASE OF SYS-0804 CORE

ZHANG Junqiang;LIU Jian;KONG Xianghuai;XU Gang;QIU jiandong;YUE Baojing;WANG Feifei;Institute of geology and paleontology,Linyi University;Key Laboratory of Marine Hydrocarbon Resources and Environmental Geology,Ministry of Land and Resources;Qingdao Institute of Marine Geology;  
A 65.10-m-long core(SYS-0804)recovered at water depth of 38 mfrom the relict sediment area off the South Yellow Sea(SYS),together with high resolution shallow seismic profiles,is analyzed on sedimentary characteristics and foraminiferal assemblages.Dated by AMS 14 C and upon the basis of latest research results both at home and abroad,the stratigraphic and environmental evolution and sea level changes during the MIS 6period are documented in this paper.Results show that the core SYS-0804 can be divided into 6depositional units,i.e.the DU 1and the DU4 to DU 8,deposited in the periods of MIS 6,MIS 5,MIS 4,MIS 3and the early epoch of MIS 1respectively.The DU 2and DU 3formed in MIS 2and MIS 3are absent,and the deposits formed in the later period of MIS 1are also missing.During the period of MIS 6(128~128cal.kaBP),fluvial environment(mainly flood plain)dominated the research area.In the early stage of MIS 5(115~128cal.kaBP),a nearshore shallow sea environment characterized by cold water mass deposition was prevailing.The depositional units from middle MIS 5to MIS 4(60~115cal.kaBP)are interpreted as the sediments deposited in littoral to inner sublittoral and fluvial environments.The sediments deposited in early to middle MIS 3(40~60cal.kaBP),show a succession from coastal and shallow sea environments in the early stage,to tidal channels in the later stage.From the later period of MIS 2to middle MIS 1(11.5~13.0~0.7cal.kaBP),it changed into a coast-shallow environment with a transgressional boundary at 11.5~13.0cal.kaBP.covered by a transgressional sequence formed in the period of sea level rising.
【Fund】: 中国地质调查局地质调查项目(1212010611401);; 国家自然科学基金重点项目(41330964);国家自然科学基金青年基金项目(41106060 41206052);; 国土资源部海洋油气资源与环境地质重点实验室项目(MRE201309)
【CateGory Index】: P736.2
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