Articles | Volume 13, issue 6
https://doi.org/10.5194/tc-13-1743-2019
© Author(s) 2019. 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-13-1743-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
28 Jun 2019
Research article |
| 28 Jun 2019
| 28 Jun 2019
Apparent discrepancy of Tibetan ice core δ18O records may be attributed to misinterpretation of chronology
School of Geographic and Oceanographic Sciences, Nanjing
University, Nanjing, 210023, China
Wangbin Zhang
School of Geographic and Oceanographic Sciences, Nanjing
University, Nanjing, 210023, China
Hongxi Pang
School of Geographic and Oceanographic Sciences, Nanjing
University, Nanjing, 210023, China
Shuang-Ye Wu
Department of Geology, University of Dayton, Dayton, OH 45469, USA
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
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
Yetang Wang
College of Geography and Environment, Shandong Normal University,
Jinan, China
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27 citations as recorded by crossref.
- Westerlies effect in Holocene paleoclimate records from the central Qinghai-Tibet Plateau H. Chen et al. 10.1016/j.palaeo.2022.111036
- Aeolian process and climatic changes in loess records from the eastern Tibetan Plateau: Implications for paleoenvironmental dynamics since MIS 3 Q. Li et al. 10.1016/j.catena.2023.107361
- Extreme precipitation stable isotopic compositions reveal unexpected summer monsoon incursions in the Qilian Mountains L. Zhao et al. 10.1016/j.scitotenv.2023.165743
- 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
- Late Holocene brGDGTs-based quantitative paleotemperature reconstruction from lacustrine sediments on the western Tibetan Plateau X. Li et al. 10.1007/s11707-022-1082-2
- MIS 3 climate transitions revealed by high-resolution loess records from the eastern margin of the Tibetan Plateau X. Wei et al. 10.1016/j.palaeo.2025.112874
- Quantitative estimates of Holocene glacier meltwater variations on the Western Tibetan Plateau C. Li et al. 10.1016/j.epsl.2021.116766
- On the chronology of Tibetan ice cores S. Hou 10.1016/j.scib.2022.10.009
- 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
- Climate change, vegetation history, and landscape responses on the Tibetan Plateau during the Holocene: A comprehensive review F. Chen et al. 10.1016/j.quascirev.2020.106444
- Weathering and pedogenesis of the late Pleistocene and Holocene aeolian loess-paleosol sections in the Yellow River source area, NE Tibetan Plateau Y. Jia et al. 10.1016/j.palaeo.2022.111065
- 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
- 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
- δ18O of O2 in a Tibetan Ice Core Constrains Its Chronology to the Holocene H. Hu et al. 10.1029/2022GL098368
- Decadal Temperature Variations Over the Northwestern Tibetan Plateau Deduced From a 489‐Year Ice Core Stable Isotopic Record W. Zhang et al. 10.1029/2021JD036087
- Ice core evidence for an orbital-scale climate transition on the Northwest Tibetan Plateau L. Thompson et al. 10.1016/j.quascirev.2023.108443
- Southward shift of the westerly jet intensified late Holocene dust storms on the Tibetan Plateau J. Liu et al. 10.1016/j.gloplacha.2024.104461
- The Siberian High drove increasing dust storm activity on the Tibetan Plateau on the centennial scale during the past 2000 years Z. Chen et al. 10.1016/j.gloplacha.2024.104525
- Tracing the isotopic signatures of cryospheric water and establishing the altitude effect in Central Himalayas: A tool for cryospheric water partitioning N. Pant et al. 10.1016/j.jhydrol.2021.125983
- Peat brGDGTs-based Holocene temperature history of the Altai Mountains in arid Central Asia D. Wu et al. 10.1016/j.palaeo.2019.109464
- Ice core evidence of rapid climate and environmental changes on the Tibetan plateau Y. Zhang & S. Kang 10.1016/j.atmosenv.2025.121483
- Potential winter-season bias of annual temperature variations in monsoonal Tibetan Plateau since the last deglaciation Z. Sun et al. 10.1016/j.quascirev.2022.107690
- Relative paleointensity correction of radiocarbon reservoir effect for lacustrine sediments on the northeast Tibetan Plateau H. Ma et al. 10.1016/j.quageo.2021.101193
- Proglacial lake response to Late-Holocene glacial fluctuations in Southeast Tibet F. Lemot et al. 10.1016/j.gloplacha.2023.104347
- Brief communication: New evidence further constraining Tibetan ice core chronologies to the Holocene S. Hou et al. 10.5194/tc-15-2109-2021
- Ice Core Methane Analytical Techniques, Chronology and Concentration History Changes: A Review J. Song 10.3390/su15129346
- Significant greening in the western Tibetan Plateau and surroundings occurred after the 1970s R. Huang et al. 10.1038/s43247-025-02061-2
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Short summary
The apparent discrepancy between the Holocene δ18O records of the Guliya and the Chongce ice cores may be attributed to a possible misinterpretation of the Guliya ice core chronology.
The apparent discrepancy between the Holocene δ18O records of the Guliya and the Chongce ice...
