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Sedimentary and OSL dating evidence for the development of the present Hobq desert landscape, northern China 被引量:11

Sedimentary and OSL dating evidence for the development of the present Hobq desert landscape, northern China
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摘要 The sedimentary sequence and landscape of the Hobq desert was observed through twelve profiles along five N-S sections extending through the entire desert.Aeolian sands were found to overlie the alluvial,diluvial,and lacustrine sediments in this desert.Optically stimulated luminescence(OSL)dating results were obtained from post-IR OSL signals of quartz fractions of sand samples at the bottom of sand dunes and hills by using the Double-SAR protocol.The OSL ages reveal that the latest sand accumulation began around 19 ka in the northwestern part and 9 ka in the eastern part of the Hobq Desert.Around 7 ka,the sand accumulation was strengthened and extended southward and northward 2 ka to develop the present desert landscape.Our study suggests that the aeolian sand accumulation around 19,9 and 7 ka resulted from the weakening of the Asian summer monsoon over this region.However,the rapid development of the present Hobq desert landscape since 2 ka was likely triggered by human activities in this desert. The sedimentary sequence and landscape of the Hobq desert was observed through twelve profiles along five N-S sections ex- tending through the entire desert. Aeolian sands were found to overlie the alluvial, diluvial, and lacustrine sediments in this desert. Optically stimulated luminescence (OSL) dating results were obtained from post-IR OSL signals of quartz fractions of sand samples at the bottom of sand dunes and hills by using the Double-SAR protocol. The OSL ages reveal that the latest sand accumulation began around 19 ka in the northwestern part and 9 ka in the eastern part of the Hobq Desert. Around 7 ka, the sand accumulation was strengthened and extended southward and northward 2 ka to develop the present desert landscape. Our study suggests that the aeolian sand accumulation around 19, 9 and 7 ka resulted from the weakening of the Asian summer monsoon over this region. However, the rapid development of the present Hobq desert landscape since 2 ka was likely trig- gered by human activities in this desert.
出处 《Science China Earth Sciences》 SCIE EI CAS 2013年第12期2037-2044,共8页 中国科学(地球科学英文版)
基金 supported by the National Natural Science Foundation of China(Grant Nos.41172163,40972116) the Chinese National Programs for Fundamental Research and Development(Grant No.2010CB950202) the program for New Century Excellent Talents in University(Grant No.NCET-12-0251) the Fundamental Research Funds for the Central Universities(Grant No.LZUJBKY-2013-K17)
关键词 Hobq Desert OSL dating Last Glacial Maximum HOLOCENE environmental and climatic change 光释光测年 沙漠景观 中国北方 沉积岩 证据 库布齐沙漠 亚洲夏季风 沉积层序
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