Paleoenvironmental Changes in the Northern Okinawa Trough since 25 ka BP:REE and Organic Carbon Evidence
文献类型:CNKI期刊论文
作者 | Xu ZK(徐兆凯); Li TG(李铁刚)![]() |
发表日期 | 2012-06-15 |
出处 | Journal of Earth Science
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关键词 | paleoenvironmental change,the northern Okinawa trough,Tsushima Warm Current,REE,discriminant function |
英文摘要 | 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. |
文献子类 | CNKI期刊论文 |
资助机构 | 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) |
卷 | v.23期:03页:49-62 |
语种 | 英文; |
分类号 | P595 |
ISSN号 | 1674-487X |
源URL | [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. |
入库方式: OAI收割
来源:海洋研究所
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