中国科学院青藏高原研究所机构知识库
Advanced  
ITPCAS OpenIR  > 图书馆  > 期刊论文
学科主题: 地球科学::地质学
题名: Late Cenozoic fire enhancement response to aridification in mid-latitude Asia: Evidence from microcharcoal records
作者: 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
通讯作者: Miao, YF ; Fang, XM
刊名: QUATERNARY SCIENCE REVIEWS
发表日期: 2016
DOI: 10.1016/j.quascirev.2016.02.030
卷: 139, 期:0, 页:53-66
收录类别: SCI
合作性质: 国际
文章类型: Review
英文摘要: Fire 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.
语种: 英语
WOS记录号: WOS:000374606100005
Citation statistics:
内容类型: 期刊论文
URI标识: http://ir.itpcas.ac.cn/handle/131C11/7709
Appears in Collections:图书馆_期刊论文

Files in This Item:
File Name/ File Size Content Type Version Access License
V.139 53-66 2016.pdf(4085KB)期刊论文作者接受稿开放获取View 联系获取全文

作者单位: 1.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:
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.
Service
Recommend this item
Sava as my favorate item
Show this item's statistics
Export Endnote File
Google Scholar
Similar articles in Google Scholar
[Miao, YF (Miao, Yunfa)]'s Articles
[Fang, XM (Fang, Xiaomin)]'s Articles
[Song, CH (Song, Chunhui)]'s Articles
CSDL cross search
Similar articles in CSDL Cross Search
[Miao, YF (Miao, Yunfa)]‘s Articles
[Fang, XM (Fang, Xiaomin)]‘s Articles
[Song, CH (Song, Chunhui)]‘s Articles
Related Copyright Policies
Null
Social Bookmarking
Add to CiteULike Add to Connotea Add to Del.icio.us Add to Digg Add to Reddit
文件名: V.139 53-66 2016.pdf
格式: Adobe PDF
所有评论 (0)
暂无评论
 
评注功能仅针对注册用户开放,请您登录
您对该条目有什么异议,请填写以下表单,管理员会尽快联系您。
内 容:
Email:  *
单位:
验证码:   刷新
您在IR的使用过程中有什么好的想法或者建议可以反馈给我们。
标 题:
 *
内 容:
Email:  *
验证码:   刷新

Items in IR are protected by copyright, with all rights reserved, unless otherwise indicated.

 

 

Valid XHTML 1.0!
Copyright © 2007-2017  中国科学院青藏高原研究所 - Feedback
Powered by CSpace