Glacial advances in Tibet during the Younger Dryas? Evidence from cosmogenic Be-10, Al-26, and Ne-21
Tschudi, S; Schafer, JM; Zhao, ZZ; Wu, XH; Ivy-Ochs, S; Kubik, PW; Schluchter, C
刊名JOURNAL OF ASIAN EARTH SCIENCES
2003-10
卷号22期号:4页码:301-306
关键词younger dryas cosmogenic nuclides Tibet
DOI10.1016/S1367-9120(03)00035-X
文献子类Article
英文摘要Was the abrupt climate cold reversal called the Younger Dryas (YD) a global climate excursion? This study presents the first evidence for YD glacial advances on the Tibetan Plateau, derived from Be-10, Al-26, and Ne-21 exposure ages of two erratics with a weighted mean age of about 11,600 years BP from a moraine at the eastern margin of the Tibetan Plateau. This implies that the YD climate signal, commonly thought to be initiated by decreased North Atlantic Deep Water Formation and transferred by ocean circulation, was even recorded at the inner-continental, high-altitude site of Tibet, implying atmospheric transport and thus a global character for this abrupt climatic change. (C) 2003 Elsevier Ltd. All rights reserved.
学科主题Geology
WOS关键词NUCLIDE PRODUCTION-RATES ; QUATERNARY GLACIATIONS ; SOUTHERN ALPS ; NANGA PARBAT ; NEW-ZEALAND ; ICE CORE ; CLIMATE ; QUARTZ ; EVENT ; RADIONUCLIDES
WOS研究方向Geosciences, Multidisciplinary
语种英语
出版者PERGAMON-ELSEVIER SCIENCE LTD
WOS记录号WOS:000187843700001
内容类型期刊论文
源URL[http://ir.ieecas.cn/handle/361006/11962]  
专题黄土与第四纪地质国家重点实验室(1985-2004)
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GB/T 7714
Tschudi, S,Schafer, JM,Zhao, ZZ,et al. Glacial advances in Tibet during the Younger Dryas? Evidence from cosmogenic Be-10, Al-26, and Ne-21[J]. JOURNAL OF ASIAN EARTH SCIENCES,2003,22(4):301-306.
APA Tschudi, S.,Schafer, JM.,Zhao, ZZ.,Wu, XH.,Ivy-Ochs, S.,...&Schluchter, C.(2003).Glacial advances in Tibet during the Younger Dryas? Evidence from cosmogenic Be-10, Al-26, and Ne-21.JOURNAL OF ASIAN EARTH SCIENCES,22(4),301-306.
MLA Tschudi, S,et al."Glacial advances in Tibet during the Younger Dryas? Evidence from cosmogenic Be-10, Al-26, and Ne-21".JOURNAL OF ASIAN EARTH SCIENCES 22.4(2003):301-306.
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