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Late Cenozoic fire enhancement response to aridification in mid-latitude Asia: Evidence from microcharcoal records
Miao, YF (Miao, Yunfa)1; Fang, XM (Fang, Xiaomin)2,3; Song, CH (Song, Chunhui)4,5; Yan, XL (Yan, Xiaoli)4,5; Zhang, P (Zhang, Ping)6; Meng, QQ (Meng, Qingquan)4,5; Li, F (Li, Fang)1; Wu, FL (Wu, Fuli)2,3; Yang, SL (Yang, Shengli)7,8; Kang, SY (Kang, Shuyuan)1; Wang, YP (Wang, Yuanping)1; Miao, YF; Fang, XM
Source PublicationQUATERNARY SCIENCE REVIEWS
2016
Volume139Issue:0Pages:53-66
DOI10.1016/j.quascirev.2016.02.030
AbstractFire provides an important indicator of paleoclimatic change. However, little information relating to late Cenozoic fire history has been gathered in mid-latitude Asia (including Inner Asia and East Asia), a key region for understanding the development of the arid-monsoon climate system as well as the driving forces behind it. Here we first report the records of microcharcoal concentrations (MC) covering the Holocene (10-0 Ica) and late Pleistocene (0.8-0 Ma), which we use to analyze the fire activity patterns at an orbital time scale; then we compile the late Cenozoic MC record to investigate the long-term fire history by analyzing four cores from the Yangtze River Delta (YRD) area, East Asia (representing 8-0 Ma) and three sites in Inner Asia (representing 18-2 Ma). The results show that the (i) MC remained higher during the relatively dry late Holocene/glacial stages than that during the humid middle Holocene/interglacial stages at individual sites; (ii) MC increased with time in both Inner Asia and East Asia after 18 and 8 Ma, respectively; and (iii) MC always remained higher in the dry Inner Asia than in the contemporaneous wet East Asia. All these characteristics imply that late Cenozoic fire occurrence in mid-latitude Asia experienced a gradual increasing trend along with the global temperature/ice volume change, and indicates a continuous aridification trend across mid-latitude Asia. The global cooling, rather than the Tibetan Plateau uplift, might have played a key role in this observed trend. (C) 2016 Elsevier Ltd. All rights reserved.
Subject Area地质学
WOS IDWOS:000374606100005
Language英语
Indexed BySCI
KeywordSummer Monsoon Evolution South China Sea Northern Tibetan Plateau Yellowstone-national-park Western United-states Yangtze-river Delta Daihai Lake Region Climate-change Late Miocene Taklimakan Desert
Cooperation Status国际
Department碰撞与隆升
Citation statistics
Cited Times:9[WOS]   [WOS Record]     [Related Records in WOS]
Document Type期刊论文
Identifierhttp://ir.itpcas.ac.cn/handle/131C11/7709
Collection图书馆
Corresponding AuthorMiao, YF; Fang, XM
Affiliation1.Chinese Acad Sci, Key Lab Desert & Desertificat, Cold & Arid Reg Environm & Engn Inst, Lanzhou 730000, Peoples R China
2.Chinese Acad Sci, Key Lab Continental Collis & Plateau Uplift, Inst Tibetan Plateau Res, Beijing 100101, Peoples R China
3.CAS Ctr Excellence Tibetan Plateau Earth Sci, Beijing 100101, Peoples R China
4.Lanzhou Univ, Sch Earth Sci, Lanzhou 730000, Peoples R China
5.Lanzhou Univ, Key Lab Western Chinas Mineral Resources Gansu Pr, Lanzhou 730000, Peoples R China
6.Geol Survey Jiangsu Prov, Key Lab Earth Fissures Geol Disaster, Minist Land & Resources, Nanjing 210018, Peoples R China
7.Lanzhou Univ, MOE Key Lab Western Chinas Environm Syst, Lanzhou 730000, Peoples R China
8.Lanzhou Univ, Res Sch Arid Environm & Climate Change, Lanzhou 730000, Peoples R China
Recommended Citation
GB/T 7714
Miao, YF ,Fang, XM ,Song, CH ,et al. Late Cenozoic fire enhancement response to aridification in mid-latitude Asia: Evidence from microcharcoal records[J]. QUATERNARY SCIENCE REVIEWS,2016,139(0):53-66.
APA Miao, YF .,Fang, XM .,Song, CH .,Yan, XL .,Zhang, P .,...&Fang, XM.(2016).Late Cenozoic fire enhancement response to aridification in mid-latitude Asia: Evidence from microcharcoal records.QUATERNARY SCIENCE REVIEWS,139(0),53-66.
MLA Miao, YF ,et al."Late Cenozoic fire enhancement response to aridification in mid-latitude Asia: Evidence from microcharcoal records".QUATERNARY SCIENCE REVIEWS 139.0(2016):53-66.
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