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DOI10.5194/tc-15-2109-2021
Brief communication: New evidence further constraining Tibetan ice core chronologies to the Holocene
Hou S.; Zhang W.; Fang L.; Jenk T.M.; Wu S.; Pang H.; Schwikowski M.
发表日期2021
ISSN19940416
起始页码2109
结束页码2114
卷号15期号:4
英文摘要There is considerable controversy regarding the age ranges of Tibetan ice cores. The Guliya ice core was reported to reach as far back as ∼ 760 ka (kiloannum, i.e. 1000 years), whereas chronologies of all other Tibetan cores cover at most the Holocene. Here we present ages for two new ice cores reaching bedrock, from the Zangser Kangri (ZK) glacier in the northwestern Tibetan Plateau and the Shulenanshan (SLNS) glacier in the western Qilian Mountains. We estimated bottom ages of 8:90±0 0:56 57 ka and 7:46±1 1:79 46 ka for the ZK and SLNS ice core respectively, further constraining the time range accessible by Tibetan ice cores to the Holocene. © Author(s).
英文关键词bedrock; chronology; Holocene; ice core; China; Guliya Ice Cap; Qilian Mountains; Qinghai-Xizang Plateau; Xizang
语种英语
来源期刊Cryosphere
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/202334
作者单位School of Oceanography, Shanghai Jiao Tong University, Shanghai, 200240, China; School of Geographic and Oceanic Sciences, Nanjing University, Nanjing, 210023, China; Laboratory of Environmental Chemistry, Paul Scherrer Institute, Villigen PSI, 5232, Switzerland; Oeschger Centre for Climate Change Research, University of Bern, Sidlerstrasse 5, Bern, 3012, Switzerland; Department of Geology, University of Dayton, Dayton, OH 45469, United States
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GB/T 7714
Hou S.,Zhang W.,Fang L.,et al. Brief communication: New evidence further constraining Tibetan ice core chronologies to the Holocene[J],2021,15(4).
APA Hou S..,Zhang W..,Fang L..,Jenk T.M..,Wu S..,...&Schwikowski M..(2021).Brief communication: New evidence further constraining Tibetan ice core chronologies to the Holocene.Cryosphere,15(4).
MLA Hou S.,et al."Brief communication: New evidence further constraining Tibetan ice core chronologies to the Holocene".Cryosphere 15.4(2021).
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