The paleoclimatic events and cause in the Okinawa Trough during 50 kaBP | |
Liu, ZX; Li, TG; Li, PY; Huang, QY; Berne, S; Saito, Y; Cheng, ZB; Wei, GJ; Liu, LJ; Li, Z | |
2001 | |
发表期刊 | CHINESE SCIENCE BULLETIN |
ISSN | 1001-6538 |
卷号 | 46期号:2页码:153-157 |
文章类型 | Article |
摘要 | Planktonic foraminiferal delta O-18 record for core DGKS9603 from the Okinawa Trough shows a series of climatic fluctuations and sudden cooling events in short time scale during 50 kaBP, which appear to correlate closely to the Younger Dryas and Heinrich events H1-5 recorded in Chinese loess, the South China Sea, the North Atlantic cores and the Greenland ice cores. Three polarity reversal events, correlating to Gothenburg, Mungo and Laschamp events, approximately correspond to Heinrich events H1, H3 and H5 respectively, which could be a cause of global climate changes. The delta O-18 curve of the Okinawa Trough is well associated with the grain size record of the Lijiayuan loess profile in northwestern China and is somewhat different from the climate fluctuations documented in the Greenland ice cores. These correlation results indicate that regional factors play an important role in controlling the climate changes in the East Asia, and the East Asian Monsoon could be the prominent regional controlling factor.; Planktonic foraminiferal delta O-18 record for core DGKS9603 from the Okinawa Trough shows a series of climatic fluctuations and sudden cooling events in short time scale during 50 kaBP, which appear to correlate closely to the Younger Dryas and Heinrich events H1-5 recorded in Chinese loess, the South China Sea, the North Atlantic cores and the Greenland ice cores. Three polarity reversal events, correlating to Gothenburg, Mungo and Laschamp events, approximately correspond to Heinrich events H1, H3 and H5 respectively, which could be a cause of global climate changes. The delta O-18 curve of the Okinawa Trough is well associated with the grain size record of the Lijiayuan loess profile in northwestern China and is somewhat different from the climate fluctuations documented in the Greenland ice cores. These correlation results indicate that regional factors play an important role in controlling the climate changes in the East Asia, and the East Asian Monsoon could be the prominent regional controlling factor. |
关键词 | Okinawa Trough Sudden Paleoclimatic Change Events Polarity Reversal Events Late Quaternary |
学科领域 | Multidisciplinary Sciences |
收录类别 | SCI |
语种 | 英语 |
WOS记录号 | WOS:000167010200015 |
引用统计 | |
文献类型 | 期刊论文 |
条目标识符 | http://ir.qdio.ac.cn/handle/337002/3816 |
专题 | 海洋地质与环境重点实验室 |
作者单位 | 1.SOA, Key Lab Marine Sci & Numer Modeling, Qingdao 266003, Peoples R China 2.SOA, Inst Oceanog 1, Qingdao 266003, Peoples R China 3.Chinese Acad Sci, Inst Oceanol, Qingdao 266003, Peoples R China 4.Taiwan Natl Univ, Taibei, Taiwan 5.IFREMER, French Oceanog Inst, F-29280 Plouzane, France 6.Geol Survey Japan, Tsukuba, Ibaraki 3058567, Japan |
推荐引用方式 GB/T 7714 | Liu, ZX,Li, TG,Li, PY,et al. The paleoclimatic events and cause in the Okinawa Trough during 50 kaBP[J]. CHINESE SCIENCE BULLETIN,2001,46(2):153-157. |
APA | Liu, ZX.,Li, TG.,Li, PY.,Huang, QY.,Berne, S.,...&Li, Z.(2001).The paleoclimatic events and cause in the Okinawa Trough during 50 kaBP.CHINESE SCIENCE BULLETIN,46(2),153-157. |
MLA | Liu, ZX,et al."The paleoclimatic events and cause in the Okinawa Trough during 50 kaBP".CHINESE SCIENCE BULLETIN 46.2(2001):153-157. |
条目包含的文件 | ||||||
文件名称/大小 | 文献类型 | 版本类型 | 开放类型 | 使用许可 | ||
liu-The paleoclimati(148KB) | 限制开放 | -- | 浏览 |
个性服务 |
推荐该条目 |
保存到收藏夹 |
查看访问统计 |
导出为Endnote文件 |
谷歌学术 |
谷歌学术中相似的文章 |
[Liu, ZX]的文章 |
[Li, TG]的文章 |
[Li, PY]的文章 |
百度学术 |
百度学术中相似的文章 |
[Liu, ZX]的文章 |
[Li, TG]的文章 |
[Li, PY]的文章 |
必应学术 |
必应学术中相似的文章 |
[Liu, ZX]的文章 |
[Li, TG]的文章 |
[Li, PY]的文章 |
相关权益政策 |
暂无数据 |
收藏/分享 |
除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。
修改评论