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High-resolution pollen sequence from Lop Nur, Xinjiang, China: Implications on environmental changes during the late Pleistocene to the early Holocene | |
Yang, Dong1,2; Peng, Zicheng2,3; Luo, Chao3; Liu, Yi3; Zhang, Zhaofeng4; Liu, Weiguo2; Zhang, Pengxi5 | |
2013-05-15 | |
发表期刊 | REVIEW OF PALAEOBOTANY AND PALYNOLOGY
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卷号 | 192页码:32-41 |
关键词 | Lop Nur Pollen Late Glacial Paleoclimate Paleoenvironment |
摘要 | A 9.35-m long sediment core, CK2, that covers the time span between 31.98 and 9.14 kilo annum before present (ka BP) at the Luobei Depression (Lop Nur, Eastern Xinjiang, Northwest China) was studied by pollen analysis. The pollen assemblages of coniferous trees, temperate deciduous trees, herbs, and shrubs can be divided into the following four stages: Zone I (31.98 ka BP to 19.26 ka BP) corresponds to a steppe or desert steppe landscape, which conforms to the cold-wet climatic environment of the Last Glacial Maximum; Zone II (19.26 ka BP to 13.67 ka BP) corresponds to a steppe desert or desert landscape, which conforms to the warm-arid climatic environment of the transient interglacial period; Zones III (13.67 ka BP to 12.73 ka BP) and IV (12.73 ka BP to 9.14 ka BP) are similar to Zones I and II, respectively, corresponding to the late last glacial and post last glacial, i.e., Early Holocene, respectively. The climatic environment in Lop Nur was increasingly getting drier based on Artemisia/Chenopodiaceae ratios of <= 0.5 in Subzones IVa and IVc. The Heinrich cold events (H3, H2, H1, and YD) and the Dansgaard-Oeschger warm events (IS4, IS3, IS2, IS1) with millennial-scale changes appearing at high latitudes can also be found in the pollen records of Lop Nur. Results show that the climate characteristics of the Lop Nur region are mainly controlled by the westerly belt, as displayed in mainly cold-wet or warm-arid synchronization. These climate characteristics differ from those of the monsoon area, which are mainly displayed in cold-arid and warm-wet synchronization but also restricted by the atmospheric circulation at high latitudes. (C) 2013 Elsevier B.V. All rights reserved. |
语种 | 英语 |
引用统计 | |
文献类型 | 期刊论文 |
条目标识符 | http://ir.isl.ac.cn/handle/363002/4462 |
专题 | 青海盐湖研究所知识仓储 中国科学院青海盐湖研究所 |
作者单位 | 1.Northwest Normal Univ, Coll Geog & Environm Sci, Lanzhou 730070, Peoples R China 2.Chinese Acad Sci, State Key Lab Loess & Quaternary Geol, Xian 710054, Peoples R China 3.Univ Sci & Technol China, Sch Earth & Space Sci, Hefei 230026, Peoples R China 4.Chinese Acad Sci, Guangzhou Inst Geochem, State Key Lab Isotope Geochem, Guangzhou 510640, Peoples R China 5.Chinese Acad Sci, Inst Salt Lake Res, Xian 710043, Peoples R China |
推荐引用方式 GB/T 7714 | Yang, Dong,Peng, Zicheng,Luo, Chao,et al. High-resolution pollen sequence from Lop Nur, Xinjiang, China: Implications on environmental changes during the late Pleistocene to the early Holocene[J]. REVIEW OF PALAEOBOTANY AND PALYNOLOGY,2013,192:32-41. |
APA | Yang, Dong.,Peng, Zicheng.,Luo, Chao.,Liu, Yi.,Zhang, Zhaofeng.,...&Zhang, Pengxi.(2013).High-resolution pollen sequence from Lop Nur, Xinjiang, China: Implications on environmental changes during the late Pleistocene to the early Holocene.REVIEW OF PALAEOBOTANY AND PALYNOLOGY,192,32-41. |
MLA | Yang, Dong,et al."High-resolution pollen sequence from Lop Nur, Xinjiang, China: Implications on environmental changes during the late Pleistocene to the early Holocene".REVIEW OF PALAEOBOTANY AND PALYNOLOGY 192(2013):32-41. |
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