Evidence for the 8,200 a BP cooling event in the middle Okinawa Trough

doi:10.1007/s00367-007-0095-x

	Evidence for the 8,200 a BP cooling event in the middle Okinawa Trough
	Yu, Hua 1; Xiong, Yingqian 2; Liu, Zhenxia 3; Berne, Serge 4; Huang, Chi-Yue 5; Jia, Guodong 6
刊名	GEO-MARINE LETTERS
	2008-06
卷号	28 期号:3 页码:131-136
ISSN号	0276-0460
DOI	10.1007/s00367-007-0095-x
英文摘要	Based on new and existing data on oxygen isotopes, alkenone-surface seawater temperature trends, planktonic foraminifers, lithology, and clay mineral composition of piston cores, a distinct cooling event has been identified around 8,200 cal a B.P. in the middle Okinawa Trough, northwest Pacific. This corresponds to the 8,200 a B.P. cooling event recorded in many places of the Northern Hemisphere. During this event, the local temperature decreased by 1 degrees C, and the delta O-18 value increased by 0.6%omicron. A strengthened Asian winter monsoon is the most probable cause for this event, which thus adds further credibility to the contention that we are dealing here with a global phenomenon.
WOS研究方向	Geology ; Oceanography
语种	英语
出版者	SPRINGER
WOS记录号	WOS:000255255000001
内容类型	期刊论文
源URL	[http://ir.fio.com.cn/handle/2SI8HI0U/4479]
专题	自然资源部第一海洋研究所
作者单位	1.Rice Univ, Dept Earth Sci, Houston, TX 77005 USA; 2.Univ Houston, Dept Geosci, Houston, TX 77204 USA; 3.SOA, Inst Oceanog 1, Marine Geol Div, Qingdao, Peoples R China; 4.IFREMER, F-29280 Plouzane, France; 5.Natl Cheng Kung Univ, Dept Earth Sci, Tainan 701, Taiwan; 6.Chinese Acad Sci, Guangzhou Inst Geochem, Guangzhou 510640, Peoples R China
推荐引用方式 GB/T 7714	Yu, Hua,Xiong, Yingqian,Liu, Zhenxia,et al. Evidence for the 8,200 a BP cooling event in the middle Okinawa Trough[J]. GEO-MARINE LETTERS,2008,28(3):131-136.
APA	Yu, Hua,Xiong, Yingqian,Liu, Zhenxia,Berne, Serge,Huang, Chi-Yue,&Jia, Guodong.(2008).Evidence for the 8,200 a BP cooling event in the middle Okinawa Trough.GEO-MARINE LETTERS,28(3),131-136.
MLA	Yu, Hua,et al."Evidence for the 8,200 a BP cooling event in the middle Okinawa Trough".GEO-MARINE LETTERS 28.3(2008):131-136.