Elemental carbon record of paleofire history on the Chinese Loess Plateau during the last 420 ka and its response to environmental and climate changes
Zhou, Bin; Shen, Chengde; Sun, Weidong; Zheng, Hongbo; Yang, Ying; Sun, Youbin; An, Zhisheng
刊名PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY
2007-09-03
卷号252期号:3-4页码:617-625
关键词Elemental Carbon Paleofire Biomass Chinese Loess Plateau Environmental And Climate Changes
ISSN号0031-0182
DOI10.1016/j.palaeo.2007.05.014
文献子类Article
英文摘要An elemental carbon (EC) record, covering the last 420 ka, was reconstructed using chemical oxidation method on a loess and paleosol sequence from the Lingtai section on the Chinese Loess Plateau. The EC record reveals the paleofire history and its relationship with climate and vegetation changes on the Chinese Loess Plateau. Our results show that the EC abundance is generally higher in the paleosols than in the loess layers, showing a glacial/interglacial pattern, which is coincident with biomass changes. This variation pattern indicates that paleofires were intensified when biomass accumulated and climate changed abruptly especially from wet to dry conditions. The EC abundance increases sharply at similar to 130 kaB.P., indicating a dramatic change in the vegetation and climate variation patterns. The occurrence of a peak value with the highest average EC abundance in the Holocene may reflect the occurrence of a major climate event at similar to 6 kaB.P., and may also be partly due to more frequent anthropogenic fire usages. (c) 2007 Elsevier B.V. All rights reserved.; An elemental carbon (EC) record, covering the last 420 ka, was reconstructed using chemical oxidation method on a loess and paleosol sequence from the Lingtai section on the Chinese Loess Plateau. The EC record reveals the paleofire history and its relationship with climate and vegetation changes on the Chinese Loess Plateau. Our results show that the EC abundance is generally higher in the paleosols than in the loess layers, showing a glacial/interglacial pattern, which is coincident with biomass changes. This variation pattern indicates that paleofires were intensified when biomass accumulated and climate changed abruptly especially from wet to dry conditions. The EC abundance increases sharply at similar to 130 kaB.P., indicating a dramatic change in the vegetation and climate variation patterns. The occurrence of a peak value with the highest average EC abundance in the Holocene may reflect the occurrence of a major climate event at similar to 6 kaB.P., and may also be partly due to more frequent anthropogenic fire usages. (c) 2007 Elsevier B.V. All rights reserved.
学科主题Geography, Physical ; Geosciences, Multidisciplinary ; Paleontology
URL标识查看原文
语种英语
WOS记录号WOS:000249412300017
公开日期2010-12-24
内容类型期刊论文
源URL[http://ir.qdio.ac.cn/handle/337002/5407]  
专题海洋研究所_海洋生态与环境科学重点实验室
海洋研究所_深海极端环境与生命过程研究中心
作者单位1.Chinese Acad Sci, Guangzhou Inst Geochem, Key Lab Isotope Geochronol, Guangzhou 510640, Peoples R China
2.Tongji Univ, Sch Ocean & Earth Sci, Shanghai 200092, Peoples R China
3.Chinese Acad Sci, Inst Oceanol, Qingdao 266071, Peoples R China
4.Chinese Acad Sci, Inst Earth Environm, State Key Lab Loess & Quaternary Geol, Xian 710075, Peoples R China
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Zhou, Bin,Shen, Chengde,Sun, Weidong,et al. Elemental carbon record of paleofire history on the Chinese Loess Plateau during the last 420 ka and its response to environmental and climate changes[J]. PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY,2007,252(3-4):617-625.
APA Zhou, Bin.,Shen, Chengde.,Sun, Weidong.,Zheng, Hongbo.,Yang, Ying.,...&An, Zhisheng.(2007).Elemental carbon record of paleofire history on the Chinese Loess Plateau during the last 420 ka and its response to environmental and climate changes.PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY,252(3-4),617-625.
MLA Zhou, Bin,et al."Elemental carbon record of paleofire history on the Chinese Loess Plateau during the last 420 ka and its response to environmental and climate changes".PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY 252.3-4(2007):617-625.
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