Trace elements and stable isotopic geochemistry of an Early Cambrian chert-phosphorite unit from the lower Yurtus Formation of the Sugetbrak section in the Tarim Basin

作     者：YAO ChunYan MA DongSheng DING HaiFeng ZHANG XiaoYong HUANG Hui 

作者机构：School of Earth Sciences and Engineering State Key Laboratory for Mineral Deposits Research Nanjing University Nanjing CenterChina Geological Survey Institute of Remote Sensing and Digital EarthChinese Academy of Sciences Jiangsu Environment Monitoring Center Guangdong Provincial Key Laboratory of Geological Processes and Mineral Resource Exploration Department of Earth Sciences Sun Yat-sen University 

出 版 物：《Science China Earth Sciences》 (中国科学（地球科学英文版）)

年 卷 期：2014年第57卷第3期

页      面：454-464页

核心收录：

学科分类：070902[理学-地球化学] 0709[理学-地质学] 07[理学] 

基　　金：supported by National Natural Science Foundation of China(Grant No.41203023) National Basic Research Program of China(Grant No.2007CB411301) 

主　　题：redox sensitive element ratios carbon isotope sedimentary environment Early Cambrian Tarim Basin 

摘      要：A chert-phosphorite unit from the Sugetbrak section in the Tarim Basin was analyzed for rare earth elements(Ce,Eu),redox sensitive proxies,and carbon isotopic compositions(??13C carb and??13C org)in the lower Yurtus Formation of the Early Cambrian *** sensitive element ratios(Th/U,V/Cr,Ni/Co,and V/Sc)were employed to determine the palaeoenvironmental conditions during this *** ratios indicated that the depositional environment of the chert-phosphorite-black shale unit ranged from suboxic to *** Ce and positive Eu anomalies in the chert-phosphorite assemblages of the studied Yurtus Formation indicated the existence of a redox-stratified ocean,similar to that of South *** or upward expansion of the deep water-mass probably reached the shallow marine zone after the formation of the Yurtus *** characteristics of the negative Ce anomaly may be due to phosphoritic inheritance from the Ce-depleted signature of the overlying water *** hydrothermal inputs and reduced detrital supplies of the deep water caused by the upwelling affected certain redox sensitive elements in the sedimentary basin.??13C carb and??13C org negative excursions in the Yurtus chert-phosphorite unit may be related to a transgression phase when episodic basinal upwelling moved12C-and P-rich waters from the pelagic basin floor to the continental *** carbon isotopic compositions in the Yurtus chert-phosphorite assemblages may have suffered from diagenetic alteration,they can be used to probe diagenetic ***-proxy geochemical studies indicated that the??13C carb values of the Yurtus chert-phosphorite assemblages might be considered reflections of a predominantly suboxic environment that was subsequently affected by hydrothermal inputs due to the upwelling.