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Conference Paper: An examination of organic molecular compounds of a lake sediment sequence to help explain organic carbon records of climate and environmental changes

TitleAn examination of organic molecular compounds of a lake sediment sequence to help explain organic carbon records of climate and environmental changes
Authors
Wang, NZong, YBrodie, CR
KeywordsEarth sciences
Issue Date2012
PublisherCopernicus GmbH. The Journal's web site is located at http://www.geophysical-research-abstracts.net
Citation
The 9th General Assembly of the European Geosciences Union (EGU 2012), Vienna, Austria, 22-27 April 2012. In Geophysical Research Abstracts, 2012, v. 14, no. EGU2012-4936 How to Cite?
AbstractStable organic carbon isotope ratios (ð13C) of bulk organic matter (OM) are commonly used for environmental reconstructions in lacustrine sediment sequences as a tool for reconstructing palaeovegetation. This interpretation is underpinned by the assumption that variations of bulk _13C can discriminate between C3 and C4 plant materials and thus infer palaeoclimate change. However, when organic matters are mainly from C3 and freshwater aquatic plants, this method becomes less effective. Therefore, we have conducted a research to analyse organic molecular compounds of a lacustrine sedimentary seq…
Persistent Identifierhttp://hdl.handle.net/10722/149317
ISSN
1607-7962

 

DC FieldValueLanguage
dc.contributor.authorWang, Nen_US
dc.contributor.authorZong, Yen_US
dc.contributor.authorBrodie, CRen_US
dc.date.accessioned2012-06-22T06:38:27Z-
dc.date.available2012-06-22T06:38:27Z-
dc.date.issued2012en_US
dc.identifier.citationThe 9th General Assembly of the European Geosciences Union (EGU 2012), Vienna, Austria, 22-27 April 2012. In Geophysical Research Abstracts, 2012, v. 14, no. EGU2012-4936en_US
dc.identifier.issn1607-7962-
dc.identifier.urihttp://hdl.handle.net/10722/149317-
dc.description.abstractStable organic carbon isotope ratios (ð13C) of bulk organic matter (OM) are commonly used for environmental reconstructions in lacustrine sediment sequences as a tool for reconstructing palaeovegetation. This interpretation is underpinned by the assumption that variations of bulk _13C can discriminate between C3 and C4 plant materials and thus infer palaeoclimate change. However, when organic matters are mainly from C3 and freshwater aquatic plants, this method becomes less effective. Therefore, we have conducted a research to analyse organic molecular compounds of a lacustrine sedimentary seq…-
dc.languageengen_US
dc.publisherCopernicus GmbH. The Journal's web site is located at http://www.geophysical-research-abstracts.net-
dc.relation.ispartofGeophysical Research Abstractsen_US
dc.rightsAuthor holds the copyright-
dc.subjectEarth sciences-
dc.titleAn examination of organic molecular compounds of a lake sediment sequence to help explain organic carbon records of climate and environmental changesen_US
dc.typeConference_Paperen_US
dc.identifier.emailZong, Y: yqzong@hku.hken_US
dc.identifier.authorityZong, Y=rp00846en_US
dc.description.naturepublished_or_final_version-
dc.identifier.hkuros200179en_US
dc.identifier.volume14-
dc.publisher.placeGermany-
dc.identifier.issnl1029-7006-

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