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Article: δ13Corg and n-alkane evidence for changing wetland conditions during a stable mid-late Holocene climate in the central Tibetan Plateau

Titleδ13Corg and n-alkane evidence for changing wetland conditions during a stable mid-late Holocene climate in the central Tibetan Plateau
Authors
CHEUNG, MCZong, YWANG, NAitchison, JCZheng, Z
KeywordsAlpine wetland
Monsoon climate change
N-Alkane indices
Organic carbon isotopes
Tibetan Plateau
Issue Date2015
Citation
Palaeogeography, Palaeoclimatology, Palaeoecology, 2015, v. 438, p. 203-212 How to Cite?
DOI: http://dx.doi.org/10.1016/j.palaeo.2015.08.007
Persistent Identifierhttp://hdl.handle.net/10722/231851
ISI Accession Number ID
WOS:000362613300017

 

DC FieldValueLanguage
dc.contributor.authorCHEUNG, MC-
dc.contributor.authorZong, Y-
dc.contributor.authorWANG, N-
dc.contributor.authorAitchison, JC-
dc.contributor.authorZheng, Z-
dc.date.accessioned2016-09-20T05:25:54Z-
dc.date.available2016-09-20T05:25:54Z-
dc.date.issued2015-
dc.identifier.citationPalaeogeography, Palaeoclimatology, Palaeoecology, 2015, v. 438, p. 203-212-
dc.identifier.urihttp://hdl.handle.net/10722/231851-
dc.languageeng-
dc.relation.ispartofPalaeogeography, Palaeoclimatology, Palaeoecology-
dc.subjectAlpine wetland-
dc.subjectMonsoon climate change-
dc.subjectN-Alkane indices-
dc.subjectOrganic carbon isotopes-
dc.subjectTibetan Plateau-
dc.titleδ13Corg and n-alkane evidence for changing wetland conditions during a stable mid-late Holocene climate in the central Tibetan Plateau-
dc.typeArticle-
dc.identifier.emailZong, Y: yqzong@hku.hk-
dc.identifier.authorityZong, Y=rp00846-
dc.identifier.doi10.1016/j.palaeo.2015.08.007-
dc.identifier.scopuseid_2-s2.0-84940421657-
dc.identifier.hkuros266729-
dc.identifier.volume438-
dc.identifier.spage203-
dc.identifier.epage212-
dc.identifier.isiWOS:000362613300017-

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