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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Cited
14 citations as recorded by crossref.
- A reconstructed PDO history from an ice core isotope record on the central Tibetan Plateau S. Li et al. 10.1038/s41612-024-00814-y
- Abrupt climate fluctuations in Tibet as imprints of multiple meltwater events during the early to mid-Holocene H. Pang et al. 10.1016/j.scib.2023.12.007
- A high-resolution refractory black carbon (rBC) record since 1932 deduced from the Chongce ice core, Tibetan plateau K. Liu et al. 10.1016/j.atmosenv.2022.119480
- Ice-core based assessment of nitrogen deposition in the central Tibetan Plateau over the last millennium X. Zou et al. 10.1016/j.scitotenv.2021.152692
- On the chronology of Tibetan ice cores S. Hou 10.1016/j.scib.2022.10.009
- δ18O of O2 in a Tibetan Ice Core Constrains Its Chronology to the Holocene H. Hu et al. 10.1029/2022GL098368
- A quantitative method of resolving annual precipitation for the past millennia from Tibetan ice cores W. Zhang et al. 10.5194/tc-16-1997-2022
- Ice Core Methane Analytical Techniques, Chronology and Concentration History Changes: A Review J. Song 10.3390/su15129346
- Environmental and human history in the hyper-arid eastern Tarim Basin (Lop Nur), northwest China: A critical review for sustaining the natural and cultural landscapes K. Li et al. 10.1016/j.quaint.2024.04.001
- Orbital-scale hydroclimate variations in the southern Tibetan Plateau over the past 414,000 years H. Wang et al. 10.1016/j.quascirev.2022.107658
- Late Holocene human population change revealed by fecal stanol records and its response to environmental evolution at Xiada Co on the western Tibetan Plateau X. Li et al. 10.1016/j.palaeo.2023.111993
- High-resolution climate change during the Marine Isotope Stage 3 revealed by Zhouqu loess in the eastern margin of the Tibetan Plateau Z. Chen et al. 10.1177/03091333241236394
- A Tibetan ice core covering the past 1,300 years radiometrically dated with 39 Ar F. Ritterbusch et al. 10.1073/pnas.2200835119
- Radiocarbon dating of alpine ice cores with the dissolved organic carbon (DOC) fraction L. Fang et al. 10.5194/tc-15-1537-2021
13 citations as recorded by crossref.
- A reconstructed PDO history from an ice core isotope record on the central Tibetan Plateau S. Li et al. 10.1038/s41612-024-00814-y
- Abrupt climate fluctuations in Tibet as imprints of multiple meltwater events during the early to mid-Holocene H. Pang et al. 10.1016/j.scib.2023.12.007
- A high-resolution refractory black carbon (rBC) record since 1932 deduced from the Chongce ice core, Tibetan plateau K. Liu et al. 10.1016/j.atmosenv.2022.119480
- Ice-core based assessment of nitrogen deposition in the central Tibetan Plateau over the last millennium X. Zou et al. 10.1016/j.scitotenv.2021.152692
- On the chronology of Tibetan ice cores S. Hou 10.1016/j.scib.2022.10.009
- δ18O of O2 in a Tibetan Ice Core Constrains Its Chronology to the Holocene H. Hu et al. 10.1029/2022GL098368
- A quantitative method of resolving annual precipitation for the past millennia from Tibetan ice cores W. Zhang et al. 10.5194/tc-16-1997-2022
- Ice Core Methane Analytical Techniques, Chronology and Concentration History Changes: A Review J. Song 10.3390/su15129346
- Environmental and human history in the hyper-arid eastern Tarim Basin (Lop Nur), northwest China: A critical review for sustaining the natural and cultural landscapes K. Li et al. 10.1016/j.quaint.2024.04.001
- Orbital-scale hydroclimate variations in the southern Tibetan Plateau over the past 414,000 years H. Wang et al. 10.1016/j.quascirev.2022.107658
- Late Holocene human population change revealed by fecal stanol records and its response to environmental evolution at Xiada Co on the western Tibetan Plateau X. Li et al. 10.1016/j.palaeo.2023.111993
- High-resolution climate change during the Marine Isotope Stage 3 revealed by Zhouqu loess in the eastern margin of the Tibetan Plateau Z. Chen et al. 10.1177/03091333241236394
- A Tibetan ice core covering the past 1,300 years radiometrically dated with 39 Ar F. Ritterbusch et al. 10.1073/pnas.2200835119
1 citations as recorded by crossref.
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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...
