Reappraisal of Chinese Loess Plateau stratigraphic sequences over the last 30,000 years: Precursors of an important Holocene monsoon climatic event

IEECAS OpenIR > 黄土与第四纪地质国家重点实验室（1985-2004）

	Reappraisal of Chinese Loess Plateau stratigraphic sequences over the last 30,000 years: Precursors of an important Holocene monsoon climatic event
	Zhou, WJ; An, ZS; Tjull, AJ; Donahue, DJ; Head, MJ
	1998
发表期刊	RADIOCARBON
卷号	40 期号:2 页码:905-913
文章类型	Article; Proceedings Paper
摘要	Through the establishment of radiocarbon chronozones relating common geological events within lacustrine and eolian sediments from five profiles representative of loess yuan (tablelands), river valley and northwest margin features of the Loess Plateau, we propose a series of stratigraphic divisions within the last 30 ka. The focus of this detailed study involves stratigraphic relationships contributing to evidence of Younger Dryas events, with the recognition of cold-dry, cool-wet and cold-dry periods represented within the Heiheze silt, Midiwan pest and Liushuwan eolian sand. The stratigraphic profiles reflect century-scale fluctuations of the East Asian monsoons. The precursor events enable us to place the Pleistocene/Holocene boundary at 10,000 BP.
学科领域	Geochemistry & Geophysics
关键词[WOS]	SEDIMENTS
收录类别	SCI ; SCIE
语种	英语
WOS研究方向	Geochemistry & Geophysics
WOS记录号	WOS:000075550800038
出版者	UNIV ARIZONA DEPT GEOSCIENCES
引用统计	被引频次：31[WOS] [WOS记录] [WOS相关记录]
文献类型	期刊论文
条目标识符	http://ir.ieecas.cn/handle/361006/11979
专题	黄土与第四纪地质国家重点实验室（1985-2004）
推荐引用方式 GB/T 7714	Zhou, WJ,An, ZS,Tjull, AJ,et al. Reappraisal of Chinese Loess Plateau stratigraphic sequences over the last 30,000 years: Precursors of an important Holocene monsoon climatic event[J]. RADIOCARBON,1998,40(2):905-913.
APA	Zhou, WJ,An, ZS,Tjull, AJ,Donahue, DJ,&Head, MJ.(1998).Reappraisal of Chinese Loess Plateau stratigraphic sequences over the last 30,000 years: Precursors of an important Holocene monsoon climatic event.RADIOCARBON,40(2),905-913.
MLA	Zhou, WJ,et al."Reappraisal of Chinese Loess Plateau stratigraphic sequences over the last 30,000 years: Precursors of an important Holocene monsoon climatic event".RADIOCARBON 40.2(1998):905-913.