Articles | Volume 15, issue 4
https://doi.org/10.5194/tc-15-2109-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/tc-15-2109-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Brief communication
| 
28 Apr 2021
Brief communication |
| 28 Apr 2021
| 28 Apr 2021
Brief communication: New evidence further constraining Tibetan ice core chronologies to the Holocene
School of Oceanography, Shanghai Jiao Tong University, Shanghai 200240, China
School of Geographic and Oceanic Sciences, Nanjing University, Nanjing 210023, China
Wangbin Zhang
School of Geographic and Oceanic Sciences, Nanjing University, Nanjing 210023, China
Ling Fang
Laboratory of Environmental Chemistry, Paul Scherrer Institute, 5232 Villigen PSI, Switzerland
Oeschger Centre for Climate Change Research, University of Bern, Sidlerstrasse 5, 3012 Bern, Switzerland
Theo M. Jenk
Laboratory of Environmental Chemistry, Paul Scherrer Institute, 5232 Villigen PSI, Switzerland
Oeschger Centre for Climate Change Research, University of Bern, Sidlerstrasse 5, 3012 Bern, Switzerland
Shuangye Wu
Department of Geology, University of Dayton, Dayton, OH 45469, USA
Hongxi Pang
School of Geographic and Oceanic Sciences, Nanjing University, Nanjing 210023, China
Margit Schwikowski
Laboratory of Environmental Chemistry, Paul Scherrer Institute, 5232 Villigen PSI, Switzerland
Oeschger Centre for Climate Change Research, University of Bern, Sidlerstrasse 5, 3012 Bern, Switzerland
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Short summary
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±0.57/0.56 ka and 7.46±1.46/1.79 ka for the ZK and SLNS ice core respectively, constraining the time range accessible by Tibetan ice cores to the Holocene.
We present ages for two new ice cores reaching bedrock, from the Zangser Kangri (ZK) glacier in...
