Cosmogenic 10Be and 26Al Chronology of the Last Glaciation of the Palaeo-Daocheng Ice Cap, Southeastern Qinghai-Tibetan Plateau
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This work was supported by the National Natural Science Foundation of China (Grant No. 40572097), the Priority Academic Program Development of Jiangsu Higher Education Institutions (PAPD) (Grant No. 164320H116), and by the Yulong Mountain tourism development and management committee special project. We are also grateful to the two anonymous reviewers for their constructive comments.


Cosmogenic 10Be and 26Al Chronology of the Last Glaciation of the Palaeo-Daocheng Ice Cap, Southeastern Qinghai-Tibetan Plateau
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This work was supported by the National Natural Science Foundation of China (Grant No. 40572097), the Priority Academic Program Development of Jiangsu Higher Education Institutions (PAPD) (Grant No. 164320H116), and by the Yulong Mountain tourism development and management committee special project. We are also grateful to the two anonymous reviewers for their constructive comments.

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    摘要:

    The glacial landforms of the Qinghai-Tibetan Plateau (QTP) provide a unique opportunity to research hemispheric and global environmental changes. In this study, we focus on the glacial history of the palaeo-Daocheng Ice Cap (p-DIC) in the southeastern QTP during the last glacial cycle. Based on field investigations, morphostratigraphy, and surface exposure dating of roche moutonnée, polished surface and moraine debris through the terrestrial cosmogenic nuclides (TCN) 10Be and 26Al. We identify glacial deposits of the last deglaciation, with minimum ages of 14.9±1.3–18.7±1.7 ka, the Last Glacial Maximum (LGM) of 24.7±2.2 ka, and the early part of the last glacial period (marine oxygen isotope stage (MIS) 3) of 37.1±3.4–45.2±3.9 ka. Our results show that in this region, the extent of the glacial advance during MIS 3 was larger than that during the traditional LGM (MIS 2). These ages are consistent with prior chronologies, and the 10Be age is consistent with the 26Al age for the same sample. Thus, these data provide reliable constraints on climate change in the QTP, during the last glaciation.

    Abstract:

    The glacial landforms of the Qinghai-Tibetan Plateau (QTP) provide a unique opportunity to research hemispheric and global environmental changes. In this study, we focus on the glacial history of the palaeo-Daocheng Ice Cap (p-DIC) in the southeastern QTP during the last glacial cycle. Based on field investigations, morphostratigraphy, and surface exposure dating of roche moutonnée, polished surface and moraine debris through the terrestrial cosmogenic nuclides (TCN) 10Be and 26Al. We identify glacial deposits of the last deglaciation, with minimum ages of 14.9±1.3–18.7±1.7 ka, the Last Glacial Maximum (LGM) of 24.7±2.2 ka, and the early part of the last glacial period (marine oxygen isotope stage (MIS) 3) of 37.1±3.4–45.2±3.9 ka. Our results show that in this region, the extent of the glacial advance during MIS 3 was larger than that during the traditional LGM (MIS 2). These ages are consistent with prior chronologies, and the 10Be age is consistent with the 26Al age for the same sample. Thus, these data provide reliable constraints on climate change in the QTP, during the last glaciation.

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ZHANG Zhigang, WANG Jian, XU Xiaobin, BAI Shibiao, CHANG ZhiYang.2015. Cosmogenic 10Be and 26Al Chronology of the Last Glaciation of the Palaeo-Daocheng Ice Cap, Southeastern Qinghai-Tibetan Plateau[J]. ACTA GEOLOGICA SINICA(English edition),89(2):575~584

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  • 收稿日期:2014-05-18
  • 最后修改日期:2014-10-24
  • 在线发布日期: 2015-04-14
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