IOCAS-IR
Paleoenvironmental Changes in the Northern Okinawa Trough since 25 ka BP:REE and Organic Carbon Evidence
Xu ZK(徐兆凯); Li TG(李铁刚); Nan QY(南青云); Yu XK(于心科); Li AC(李安春); Jinyong Choi
发表期刊Journal of Earth Science
ISSN1674-487X
2012-06-15
出版年2012
卷号v.23期号:03页码:49-62
文献类型CNKI期刊论文
摘要Paleoenvironmental changes in the northern Okinawa trough covering the last 25 ka were synthetically reconstructed using REE and organic carbon indices of core CSH1.Variations of these parameters revealed three distinct intervals of major sediment provenance changes that can be related to sea-level fluctuation and Tsushima Warm Current evolution.Interval 1(16-24.7 ka BP) is characterized by dominantly fluvial discharge from the Changjiang(Yangtze River) and Huanghe(Yellow River) as well as high primary productivity.In Interval 2(7.3-16 ka BP),the Changjiang and Huanghe mouths regressed with sea-level rising.The newly formed Tsushima Warm Current could carry some sediment loads of Taiwan to the study core,especially during its late phase(7.3-8.2 ka BP).Modern oceanographic conditions were finally established since the beginning of Interval 3,leading to more terrigenous contribution from Taiwan,whereas low sea-surface productivity in the study area.
关键词paleoenvironmental change,the northern Okinawa trough,Tsushima Warm Current,REE,discriminant function
CNKI专辑号A;
CNKI专辑名称基础科学;
CNKI专题号A011;
CNKI专题名称地质学;
分类号P595
收录类别中科院核心
语种英文;
资助项目(基金)supported by the Open Fund of the Key Laboratory of Marine Geology and Environment,Chinese Academy of Sciences,the Innovative Program of Chinese Academy of Sciences(No.KZCX2-YW-221) ; the National Basic Research Program of China(No.2007CB815903) ; the National Natural Science Foundation of China(Nos. 41106043 and 40906038)
文献类型CNKI期刊论文
条目标识符http://ir.qdio.ac.cn/handle/337002/191232
专题中国科学院海洋研究所
作者单位1.KeyLaboratoryofMarineGeologyandEnvironment,InstituteofOceanology,ChineseAcademyofSciences
2.DepartmentofOceanography,KunsanNationalUniversity,Kunsan573-701,Korea
推荐引用方式
GB/T 7714
Xu ZK,Li TG,Nan QY,et al. Paleoenvironmental Changes in the Northern Okinawa Trough since 25 ka BP:REE and Organic Carbon Evidence. 2012.
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