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	The history of the Yangtze River entering sea since the last glacial maximum: a review and look forward
	Xiao, SB; Li, AC; Jiang, FQ; Li, TG; Wan, SM; Huang, P
刊名	JOURNAL OF COASTAL RESEARCH
	2004-03-01
卷号	20期号:2页码:599-604
关键词	Sea-level Change Channel Metamorphosis East China Sea
ISSN号	0749-0208
文献子类	Article
英文摘要	This review paper provides a brief review on the development of ideas in the fields of the sea level change of the ECS (East China Sea), the history of the Yangtze River entering the sea and paleochannels in the shelf of the ECS since the Last Glacial Maximum (LGM). The paper summarizes two opposite theories about the Yangtze River entering the sea during the LGM. One theory is that the Yangtze River input a lacustrine in the north of Jiangsu province which was defunct in middle Holocene, and the river was once dry. The other was that the Yangtze River still existed and entered into the Okinawa Trough during the LGM, but scholars share different opinions on which course the river ran across and which place the river input the trough.; This review paper provides a brief review on the development of ideas in the fields of the sea level change of the ECS (East China Sea), the history of the Yangtze River entering the sea and paleochannels in the shelf of the ECS since the Last Glacial Maximum (LGM). The paper summarizes two opposite theories about the Yangtze River entering the sea during the LGM. One theory is that the Yangtze River input a lacustrine in the north of Jiangsu province which was defunct in middle Holocene, and the river was once dry. The other was that the Yangtze River still existed and entered into the Okinawa Trough during the LGM, but scholars share different opinions on which course the river ran across and which place the river input the trough. This paper concludes future work is to study the evolution of the Yangtze River and the paleoclimate and the corresponding events as a whole from the view of regional and even global change, and more attention should be paid to the study on mud sediment, the Yangtze River's response to the changes in climate and sea-level, and the channel metamorphosis.
学科主题	Environmental Sciences ; Geography, Physical ; Geosciences, Multidisciplinary
语种	英语
WOS记录号	WOS:000222956700018
公开日期	2010-12-22
内容类型	期刊论文
源URL	[http://ir.qdio.ac.cn/handle/337002/3765]
专题	海洋研究所_海洋地质与环境重点实验室
作者单位	Chinese Acad Sci, Inst Oceanol, Qingdao 266071, Peoples R China
推荐引用方式 GB/T 7714	Xiao, SB,Li, AC,Jiang, FQ,et al. The history of the Yangtze River entering sea since the last glacial maximum: a review and look forward[J]. JOURNAL OF COASTAL RESEARCH,2004,20(2):599-604.
APA	Xiao, SB,Li, AC,Jiang, FQ,Li, TG,Wan, SM,&Huang, P.(2004).The history of the Yangtze River entering sea since the last glacial maximum: a review and look forward.JOURNAL OF COASTAL RESEARCH,20(2),599-604.
MLA	Xiao, SB,et al."The history of the Yangtze River entering sea since the last glacial maximum: a review and look forward".JOURNAL OF COASTAL RESEARCH 20.2(2004):599-604.

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