Paleohydrological Changes in the Western Tibetan Plateau over the Past 16,000 years Based on Sedimentary Records of n‐Alkanes and Grain Size
Both monsoons and westerlies have exerted influence on climate dynamics over the Tibetan Plateau (TP) since the last deglaciation, producing complex patterns of paleohydroclimatic conditions. Diverse proxy records are essential to forge a robust understanding of the climate system on the TP. Current...
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Published in | Acta geologica Sinica (Beijing) Vol. 94; no. 3; pp. 707 - 716 |
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Main Authors | , , , |
Format | Journal Article |
Language | English |
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01.06.2020
CAS Center for Excellence in Tibetan Plateau Earth Sciences,Chinese Academy of Sciences,Beijing 100101,China Key Laboratory of Alpine Ecology,Institute of Tibetan Plateau Research,Chinese Academy of Sciences,Beijing 100101,China%Key Laboratory of Western China's Environmental System(Ministry of Education),College of Earth and Environmental Sciences,Lanzhou University,Lanzhou 730000,China%Key Laboratory of Alpine Ecology,Institute of Tibetan Plateau Research,Chinese Academy of Sciences,Beijing 100101,China |
Edition | English ed. |
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Abstract | Both monsoons and westerlies have exerted influence on climate dynamics over the Tibetan Plateau (TP) since the last deglaciation, producing complex patterns of paleohydroclimatic conditions. Diverse proxy records are essential to forge a robust understanding of the climate system on the TP. Currently, there is a general lack of understanding of the response of inland lakes over the TP to climate change, especially glacier‐fed lakes. Paleohydrological reconstructions of such lakes could deepen our understanding of the history of lake systems and their relationship to regional climate variability. Here we use records of n‐alkanes and grain size from the sediments of Bangong Co in the western TP to reconstruct paleohydrological changes over the past 16,000 years. The Paq record (the ratio of non‐emergent aquatic macrophytes versus emergent aquatic macrophytes and terrestrial plants) is generally consistent with the variations in summer temperature and precipitation isotopes. The changes in grain‐size distributions show a similar trend to Paq but with less pronounced fluctuations in the early‐middle Holocene. The new data combined with previous results from the site demonstrate that: 1) Bangong Co experienced relatively large water‐level fluctuations during the last deglaciation, with a steadily high lake‐level during the early‐middle Holocene and a decreasing lake‐level in the late Holocene; 2) The lake level fluctuations were driven by both high summer temperatures via the melting water and monsoon precipitation. However, the dominant factor controlling lake level changed over time. The lake‐level history at Bangong Co deduced from the n‐alkanes and grain‐size records reveals the past hydrological changes in the catchment area, and stimulates more discussion about the future of glacier‐fed lakes under the conditions of unprecedented warming in the region. |
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AbstractList | Both monsoons and westerlies have exerted influence on climate dynamics over the Tibetan Plateau (TP) since the last deglaciation, producing complex patterns of paleohydroclimatic conditions. Diverse proxy records are essential to forge a robust understanding of the climate system on the TP. Currently, there is a general lack of understanding of the response of inland lakes over the TP to climate change, especially glacier‐fed lakes. Paleohydrological reconstructions of such lakes could deepen our understanding of the history of lake systems and their relationship to regional climate variability. Here we use records of n‐alkanes and grain size from the sediments of Bangong Co in the western TP to reconstruct paleohydrological changes over the past 16,000 years. The Paq record (the ratio of non‐emergent aquatic macrophytes versus emergent aquatic macrophytes and terrestrial plants) is generally consistent with the variations in summer temperature and precipitation isotopes. The changes in grain‐size distributions show a similar trend to Paq but with less pronounced fluctuations in the early‐middle Holocene. The new data combined with previous results from the site demonstrate that: 1) Bangong Co experienced relatively large water‐level fluctuations during the last deglaciation, with a steadily high lake‐level during the early‐middle Holocene and a decreasing lake‐level in the late Holocene; 2) The lake level fluctuations were driven by both high summer temperatures via the melting water and monsoon precipitation. However, the dominant factor controlling lake level changed over time. The lake‐level history at Bangong Co deduced from the n‐alkanes and grain‐size records reveals the past hydrological changes in the catchment area, and stimulates more discussion about the future of glacier‐fed lakes under the conditions of unprecedented warming in the region. Abstract Both monsoons and westerlies have exerted influence on climate dynamics over the Tibetan Plateau (TP) since the last deglaciation, producing complex patterns of paleohydroclimatic conditions. Diverse proxy records are essential to forge a robust understanding of the climate system on the TP. Currently, there is a general lack of understanding of the response of inland lakes over the TP to climate change, especially glacier‐fed lakes. Paleohydrological reconstructions of such lakes could deepen our understanding of the history of lake systems and their relationship to regional climate variability. Here we use records of n ‐alkanes and grain size from the sediments of Bangong Co in the western TP to reconstruct paleohydrological changes over the past 16,000 years. The P aq record (the ratio of non‐emergent aquatic macrophytes versus emergent aquatic macrophytes and terrestrial plants) is generally consistent with the variations in summer temperature and precipitation isotopes. The changes in grain‐size distributions show a similar trend to P aq but with less pronounced fluctuations in the early‐middle Holocene. The new data combined with previous results from the site demonstrate that: 1) Bangong Co experienced relatively large water‐level fluctuations during the last deglaciation, with a steadily high lake‐level during the early‐middle Holocene and a decreasing lake‐level in the late Holocene; 2) The lake level fluctuations were driven by both high summer temperatures via the melting water and monsoon precipitation. However, the dominant factor controlling lake level changed over time. The lake‐level history at Bangong Co deduced from the n ‐alkanes and grain‐size records reveals the past hydrological changes in the catchment area, and stimulates more discussion about the future of glacier‐fed lakes under the conditions of unprecedented warming in the region. |
Author | ZHANG, Jiawu YANG, Yaping WANG, Mingda HOU, Juzhi |
AuthorAffiliation | Key Laboratory of Alpine Ecology,Institute of Tibetan Plateau Research,Chinese Academy of Sciences,Beijing 100101,China%Key Laboratory of Western China's Environmental System(Ministry of Education),College of Earth and Environmental Sciences,Lanzhou University,Lanzhou 730000,China%Key Laboratory of Alpine Ecology,Institute of Tibetan Plateau Research,Chinese Academy of Sciences,Beijing 100101,China;CAS Center for Excellence in Tibetan Plateau Earth Sciences,Chinese Academy of Sciences,Beijing 100101,China |
AuthorAffiliation_xml | – name: Key Laboratory of Alpine Ecology,Institute of Tibetan Plateau Research,Chinese Academy of Sciences,Beijing 100101,China%Key Laboratory of Western China's Environmental System(Ministry of Education),College of Earth and Environmental Sciences,Lanzhou University,Lanzhou 730000,China%Key Laboratory of Alpine Ecology,Institute of Tibetan Plateau Research,Chinese Academy of Sciences,Beijing 100101,China;CAS Center for Excellence in Tibetan Plateau Earth Sciences,Chinese Academy of Sciences,Beijing 100101,China |
Author_xml | – sequence: 1 givenname: Mingda surname: WANG fullname: WANG, Mingda email: mdwang@itpcas.ac.cn organization: Chinese Academy of Sciences – sequence: 2 givenname: Yaping surname: YANG fullname: YANG, Yaping organization: Lanzhou University – sequence: 3 givenname: Jiawu surname: ZHANG fullname: ZHANG, Jiawu organization: Lanzhou University – sequence: 4 givenname: Juzhi surname: HOU fullname: HOU, Juzhi email: houjz@itpcas.ac.cn organization: Chinese Academy of Sciences |
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Copyright | 2020 Geological Society of China Copyright © Wanfang Data Co. Ltd. All Rights Reserved. |
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GrantInformation_xml | – fundername: We thank Mr. Wenjing Zhang, Dr. Yue He and Mr. Li Lei for their assistance in the field and Mr. Shaopeng Gao from the Key Laboratory of Tibetan Environment Changes and Land Surface Processes, ITPCAS, who conducted the 210Pb/137Cs analyses. We also thank Dr. Asif Khan for providing the shape files of the Bangong Co catchment area and Dr. Junbo Wang for the bathymetric data of Bangong Co. We thank the editors and reviewers for their helpful comments and Jan Bloemendal for English improvement. This research was financially supported by the Natural Science Foundation of China (41601205, 41772178, 41072120) |
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Notes | houjz@itpcas.ac.cn WANG Mingda, male, born in 1983 in Shenyang City, Liaoning Province; graduated from the University of Chinese Academy of Sciences; Postdoctoral researcher at the Institute of Tibetan Plateau Research, Chinese Academy of Sciences. He is interested in organic molecules, called ‘biomarkers’, to understand how climate change impacted the world in the past. Email HOU Juzhi, male, born in 1975 in Xingtai City, Hebei Province; he received his Ph.D. degrees in 2003 from the Institute of Geology and Geophysics, CAS, and in 2008 from Brown University; research professor at the Institute of Tibetan Plateau Research, Chinese Academy of Sciences (CAS) and CAS Center for Excellence in Tibetan Plateau Earth Sciences. His research topic is quantitative reconstruction of Holocene temperature and precipitation on the Tibetan Plateau using biomarkers. Email About the corresponding author About the first author phone: 010‐84097077. mdwang@itpcas.ac.cn phone: 18600498031. Current address: School of Geography, Liaoning Normal University, Dalian 116029, Liaoning. |
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Publisher | Wiley Subscription Services, Inc CAS Center for Excellence in Tibetan Plateau Earth Sciences,Chinese Academy of Sciences,Beijing 100101,China Key Laboratory of Alpine Ecology,Institute of Tibetan Plateau Research,Chinese Academy of Sciences,Beijing 100101,China%Key Laboratory of Western China's Environmental System(Ministry of Education),College of Earth and Environmental Sciences,Lanzhou University,Lanzhou 730000,China%Key Laboratory of Alpine Ecology,Institute of Tibetan Plateau Research,Chinese Academy of Sciences,Beijing 100101,China |
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Snippet | Both monsoons and westerlies have exerted influence on climate dynamics over the Tibetan Plateau (TP) since the last deglaciation, producing complex patterns... Abstract Both monsoons and westerlies have exerted influence on climate dynamics over the Tibetan Plateau (TP) since the last deglaciation, producing complex... |
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SubjectTerms | Alkanes Aquatic plants Bangong Co Catchment area Catchment areas Climate change Climate system Climate variability Deglaciation Fluctuations Glaciers Grain size Holocene Hydrology Inland waters Isotopes lake level Lakes Macrophytes Meltwater Monsoons n‐alkane Paq Particle size Precipitation Records Sediments Summer Terrestrial environments Tibetan Plateau Water levels Westerlies |
Title | Paleohydrological Changes in the Western Tibetan Plateau over the Past 16,000 years Based on Sedimentary Records of n‐Alkanes and Grain Size |
URI | https://onlinelibrary.wiley.com/doi/abs/10.1111%2F1755-6724.14538 https://www.proquest.com/docview/2417277671 https://d.wanfangdata.com.cn/periodical/dzxb-e202003014 |
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