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OSL chronology and palaeoclimatic implications of aeolian sediments inthe eastern Qaidam Basin of the northeastern Qinghai-Tibetan Plateau
Yu, LuPeng; Lai, ZhongPing
2012
发表期刊PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY
ISSN0031-0182
卷号337期号:*页码:120-129
摘要Aeolian sediments are widely distributed in the hyper-arid Qaidam Basin and are good palaeoclimatic records. Due to limited age control, aeolian processes and their relevance to palaeoclimatic change are poorly understood. In this study, we present 28 optically stimulated luminescence (OSL) ages for both loess (14 samples) and aeolian sand (14 samples) from 8 profiles in eastern Qaidam Basin (EQB) in order to provide a detailed chronology for understanding the timing of aeolian processes and associated environmental conditions. We reconstructed the history of aeolian activity in the EQB since deglaciation by combining OSL chronologies, lithologic stratigraphy and grain-size analysis. The results indicate that (1) aeolian sand underlying the loess accumulated at ca. 12.4-11.5 ka and 10-8 ka, but not during the Last Glacial Maximum, (2) loess accumulation started at 10 ka and lasted to 0.45 ka at least, while most of the loess was deposited during 8-4.5 ka, (3).palaeoclimates in the EQB are inferred to be arid during 12.4-11.5 ka, (relatively) humid during 10-8 ka, humid during 8-4.5 ka and relatively arid during 4.5-0.45 ka, and (4) evolution of aeolian sediments were mainly controlled by effective moisture, and also affected by local topography. (C) 2012 Elsevier B.V. All rights reserved. Aeolian sediments are widely distributed in the hyper-arid Qaidam Basin and are good palaeoclimatic records. Due to limited age control, aeolian processes and their relevance to palaeoclimatic change are poorly understood. In this study, we present 28 optically stimulated luminescence (OSL) ages for both loess (14 samples) and aeolian sand (14 samples) from 8 profiles in eastern Qaidam Basin (EQB) in order to provide a detailed chronology for understanding the timing of aeolian processes and associated environmental conditions. We reconstructed the history of aeolian activity in the EQB since deglaciation by combining OSL chronologies, lithologic stratigraphy and grain-size analysis. The results indicate that (1) aeolian sand underlying the loess accumulated at ca. 12.4-11.5 ka and 10-8 ka, but not during the Last Glacial Maximum, (2) loess accumulation started at 10 ka and lasted to 0.45 ka at least, while most of the loess was deposited during 8-4.5 ka, (3).palaeoclimates in the EQB are inferred to be arid during 12.4-11.5 ka, (relatively) humid during 10-8 ka, humid during 8-4.5 ka and relatively arid during 4.5-0.45 ka, and (4) evolution of aeolian sediments were mainly controlled by effective moisture, and also affected by local topography. (C) 2012 Elsevier B.V. All rights reserved.
关键词Luminescence Dating Aeolian Activity Palaeoclimate During Deglaciation
收录类别SCI
文献类型期刊论文
条目标识符http://ir.isl.ac.cn/handle/363002/2047
专题青海盐湖研究所知识仓储
推荐引用方式
GB/T 7714
Yu, LuPeng,Lai, ZhongPing. OSL chronology and palaeoclimatic implications of aeolian sediments inthe eastern Qaidam Basin of the northeastern Qinghai-Tibetan Plateau[J]. PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY,2012,337(*):120-129.
APA Yu, LuPeng,&Lai, ZhongPing.(2012).OSL chronology and palaeoclimatic implications of aeolian sediments inthe eastern Qaidam Basin of the northeastern Qinghai-Tibetan Plateau.PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY,337(*),120-129.
MLA Yu, LuPeng,et al."OSL chronology and palaeoclimatic implications of aeolian sediments inthe eastern Qaidam Basin of the northeastern Qinghai-Tibetan Plateau".PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY 337.*(2012):120-129.
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