Natural ecosystem response and recovery after the 8.2 ka cold event: Evidence from slope sediments on the northeastern Tibetan Plateau (SCI)
Miao Y. F. ; Jin H. L. ; Liu B. ; Wang Y. P.
刊名Journal of Arid Environments
2014
卷号104期号:17-22
英文摘要On the Tibetan Plateau, mountain slope sediments provide a sensitive record of the 8.2 ka cold event and suggest possible strategies for restoration of grasslands degraded by human activities. Based on a grain-size study of slope sediments of the KE section on the northeastern Tibetan Plateau, climate changes at 8.3-8.0 ka evidenced by a high content of coarse grains are connected with the 8.2 ka cold event. The compiled records of pollen and non-pollen palynomorphs show that, during this event, most plant species suffered serious setbacks characterized by an immediate and obvious reduction of pollen and spore production, and it took similar to 1.5 ka (from 8.0 to 6.5 ka) to recover to normal levels, occurring at different rates for different taxa. (C) 2014 Elsevier Ltd. All rights reserved.
收录类别SCI
公开日期2015-12-24
内容类型期刊论文
源URL[http://ir.casnw.net/handle/362004/24884]  
专题寒区旱区环境与工程研究所_中科院寒区旱区环境与工程研究所(未分类)_期刊论文
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GB/T 7714
Miao Y. F.,Jin H. L.,Liu B.,et al. Natural ecosystem response and recovery after the 8.2 ka cold event: Evidence from slope sediments on the northeastern Tibetan Plateau (SCI)[J]. Journal of Arid Environments,2014,104(17-22).
APA Miao Y. F.,Jin H. L.,Liu B.,&Wang Y. P..(2014).Natural ecosystem response and recovery after the 8.2 ka cold event: Evidence from slope sediments on the northeastern Tibetan Plateau (SCI).Journal of Arid Environments,104(17-22).
MLA Miao Y. F.,et al."Natural ecosystem response and recovery after the 8.2 ka cold event: Evidence from slope sediments on the northeastern Tibetan Plateau (SCI)".Journal of Arid Environments 104.17-22(2014).
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