Be-10 signature of the Matuyama-Brunhes transition from the Heqing paleolake basin
文献类型:期刊论文
作者 | Xie, XJ (Xie, Xingjun)[ 1,3,4 ]; Fu, YC (Fu, Yunchong)[ 1,3,4 ]; Zhou, WJ (Zhou, Weijian)[ 1,3,4,5 ]; Xian, F (Xian, Feng)[ 1,3,4 ]; Qiang, XK (Qiang, Xiaoke)[ 1 ]; Kong, XH (Kong, Xianghui)[ 1,3,4 ]; Du, YJ (Du, Yajuan)[ 1,2,3,4 ]; Zhao, GQ (Zhao, Guoqing)[ 1,3,4 ] |
刊名 | QUATERNARY SCIENCE REVIEWS |
出版日期 | 2018-11-01 |
卷号 | 199页码:41-48 |
关键词 | Heqing Paleolake 10be Cosmogenic Isotopes Matuyama-brunhes Transition |
DOI | 10.1016/j.quascirev.2018.09.020 |
文献子类 | 期刊论文 |
英文摘要 | We present a new 10Be record spanning the Matuyama-Brunhes (M-B) reversal from the Heqing paleolake basin in southern China. It provides a robust proxy for past geomagnetic variations that can be compared with paleomagnetic records. The M-B transition is identified as a pronounced maximum of authigenic 10Be/9Be ratio between 768.6 and 778.5 ka, that is consistent with all other available 10Be-proxy records from marine, ice and loess archives. However, it is offset by approximately 0–60 cm depth from the magnetic signature of the polarity transition recorded in the same sediments. We attribute this offset to the lock-in effect of the remanence acquisition process, which is similar to the phenomenon that exists in marine sediments. We suggest that after eliminating the climatic-hydrological signal, the Heqing sediments may be used as an archive for atmospheric 10Be production rate changes. The combination of magnetic remanence measurements and the cosmogenic 10Be allows for a more precise geochronology of geomagnetic polarity reversals. |
语种 | 英语 |
源URL | [http://ir.ieecas.cn/handle/361006/9581] |
专题 | 地球环境研究所_古环境研究室 |
通讯作者 | Zhou, WJ (Zhou, Weijian)[ 1,3,4,5 ] |
作者单位 | 1.University of Chinese Academy of Sciences, Beijing, 100049, China; 2.Open Studio for Oceanic-Continental Climate and Environment Changes (OCCEC), Qingdao National Laboratory for Marine Science and Technology,Qingdao, China 3.State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi'an, 710061, China; 4.Shaanxi Key Laboratory of Accelerator Mass Spectrometry Technology and Application, Xi'an AMS Center of IEECAS & Xi'an Jiaotong University, Xi'an,710061, China; |
推荐引用方式 GB/T 7714 | Xie, XJ ,Fu, YC ,Zhou, WJ ,et al. Be-10 signature of the Matuyama-Brunhes transition from the Heqing paleolake basin[J]. QUATERNARY SCIENCE REVIEWS,2018,199:41-48. |
APA | Xie, XJ .,Fu, YC .,Zhou, WJ .,Xian, F .,Qiang, XK .,...&Zhao, GQ .(2018).Be-10 signature of the Matuyama-Brunhes transition from the Heqing paleolake basin.QUATERNARY SCIENCE REVIEWS,199,41-48. |
MLA | Xie, XJ ,et al."Be-10 signature of the Matuyama-Brunhes transition from the Heqing paleolake basin".QUATERNARY SCIENCE REVIEWS 199(2018):41-48. |
入库方式: OAI收割
来源:地球环境研究所
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