delta C-13(org) and n-alkane evidence for changing wetland conditions during a stable mid-late Holocene climate in the central Tibetan Plateau

doi:10.1016/j.palaeo.2015.08.007

GIG OpenIR

	Cheung, Man-Ching 1; Zong, Yongqiang 1; Wang, Ning 2; Aitchison, Jonathan C.3; Zheng, Zhuo 4
	delta C-13(org) and n-alkane evidence for changing wetland conditions during a stable mid-late Holocene climate in the central Tibetan Plateau
Source Publication	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY
ISSN	0031-0182
	2015-11-15
Volume	438 Pages:203-212
DOI	10.1016/j.palaeo.2015.08.007
Language	英语
WOS Research Area	Physical Geography ; Geology ; Paleontology
WOS ID	WOS:000362613300017
Indexed By	SCI
Citation statistics
Document Type	期刊论文
Identifier	http://ir.gig.ac.cn/handle/344008/53687
Corresponding Author	Zong, Yongqiang
Affiliation	1.Univ Hong Kong, Dept Earth Sci, Hong Kong, Hong Kong, Peoples R China 2.Chinese Acad Sci, Guangzhou Inst Geochem, Guangzhou, Guangdong, Peoples R China 3.Univ Queensland, Sch Geog Planning & Environm Management, Brisbane, Qld, Australia 4.Sun Yat Sen Univ, Dept Earth Sci, Guangzhou 510275, Guangdong, Peoples R China
Recommended Citation GB/T 7714	Cheung, Man-Ching,Zong, Yongqiang,Wang, Ning,et al. delta C-13(org) and n-alkane evidence for changing wetland conditions during a stable mid-late Holocene climate in the central Tibetan Plateau[J]. PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY,2015,438:203-212.
APA	Cheung, Man-Ching,Zong, Yongqiang,Wang, Ning,Aitchison, Jonathan C.,&Zheng, Zhuo.(2015).delta C-13(org) and n-alkane evidence for changing wetland conditions during a stable mid-late Holocene climate in the central Tibetan Plateau.PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY,438,203-212.
MLA	Cheung, Man-Ching,et al."delta C-13(org) and n-alkane evidence for changing wetland conditions during a stable mid-late Holocene climate in the central Tibetan Plateau".PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY 438(2015):203-212.

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