Geochronology
; Aridification
; Fire occurrences
; Global cooling
; Global temperatures
; Late Cenozoic
; Late Pleistocene
; Microcharcoal
; Yangtze river delta
; Fires
; aridification
; Cenozoic
; charcoal
; cooling
; fire history
; global change
; Holocene
; paleoclimate
; Pleistocene
; China
; Far East
; Qinghai-Xizang Plateau
; Yangtze Delta
We are grateful to Y.D., Duan, Y.Y., Zhao, Y.H., Miao, F.Z., Zhang and X.C., Zheng for assistance in laboratory and field help. This work was co-supported by the (973) National Basic Research Program of China (Grant No. 2013CB956403), the Strategic Priority Research Program of the Chinese Academy of Sciences (Grant No. XDB03020103, XDB03020402) and NSFC Grants (41172153, 41290252, 41272128).
Key Laboratory of Desert and Desertification, Cold and Arid Regions Environmental and Engineering Institute, Chinese Academy of Sciences, Lanzhou, China; Key Laboratory of Continental Collision and Plateau Uplift, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, China; CAS Center for Excellence in Tibetan Plateau Earth Sciences, Beijing, China; School of Earth Sciences and Key Laboratory of Western China's Mineral Resources of Gansu Province, Lanzhou University, Lanzhou, China; Key Laboratory of Earth Fissures Geological Disaster, Ministry of Land and Resources, Geological Survey of Jiangsu Province, Nanjing, China; MOE Key Laboratory of Western China's Environmental Systems, Research School of Arid Environment and Climate Change, Lanzhou University, Lanzhou, China
Recommended Citation:
Miao Y.,Fang X.,Song C.,et al. Late Cenozoic fire enhancement response to aridification in mid-latitude Asia: Evidence from microcharcoal records[J]. Quaternary Science Reviews,2016-01-01,139