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dc.contributor.authorZhou, Weijian
dc.contributor.authorAn, Zhisheng
dc.contributor.authorJull, A. J. T.
dc.contributor.authorDonahue, D. J.
dc.contributor.authorHead, M. J.
dc.date.accessioned2021-02-11T21:33:01Z
dc.date.available2021-02-11T21:33:01Z
dc.date.issued1998-01-01
dc.identifier.citationZhou, W., An, Z., Jull, A. J. T., Donahue, D. J., & Head, M. J. (1998). Reappraisal of Chinese Loess Plateau stratigraphic sequences over the last 30,000 years: Precursors of an important Holocene monsoon climatic event. Radiocarbon, 40(2), 905-913.
dc.identifier.issn0033-8222
dc.identifier.doi10.1017/S0033822200018877
dc.identifier.urihttp://hdl.handle.net/10150/654622
dc.descriptionFrom the 16th International Radiocarbon Conference held in Gronigen, Netherlands, June 16-20, 1997.
dc.description.abstractThrough the establishment of radiocarbon chronozones relating common geological events within lacustrine and eolian sediments from five profiles representative of loess yuan (tablelands), river valley and northwest margin features of the Loess Plateau, we propose a series of stratigraphic divisions within the last 30 ka. The focus of this detailed study involves stratigraphic relationships contributing to evidence of Younger Dryas events, with the recognition of cold-dry, cool-wet and cold-dry periods represented within the Heiheze silt, Midiwan peat and Liushuwan eolian sand. The stratigraphic profiles reflect century-scale fluctuations of the East Asian monsoons. The precursor events enable us to place the Pleistocene/Holocene boundary at 10,000 BP.
dc.language.isoen
dc.publisherDepartment of Geosciences, The University of Arizona
dc.relation.urlhttp://radiocarbon.webhost.uits.arizona.edu/
dc.rightsCopyright © by the Arizona Board of Regents on behalf of the University of Arizona. All rights reserved.
dc.rights.urihttp://rightsstatements.org/vocab/InC/1.0/
dc.subjecteolian features
dc.subjectLoess Plateau
dc.subjectsand
dc.subjectstratigraphic boundary
dc.subjectloess
dc.subjectmonsoons
dc.subjectPaleosols
dc.subjectChina
dc.subjectsilt
dc.subjectlacustrine environment
dc.subjectaccelerator mass spectra
dc.subjectupper Weichselian
dc.subjectWeichselian
dc.subjectYounger Dryas
dc.subjectmass spectra
dc.subjectspectra
dc.subjectHolocene
dc.subjectmicrofossils
dc.subjectmiospores
dc.subjectpalynomorphs
dc.subjectpollen
dc.subjectFar East
dc.subjectstratigraphy
dc.subjectpaleoclimatology
dc.subjectPleistocene
dc.subjectupper Pleistocene
dc.subjectpeat
dc.subjectsediments
dc.subjectAsia
dc.subjectCenozoic
dc.subjectcharcoal
dc.subjectQuaternary
dc.subjectwood
dc.subjectclastic sediments
dc.subjectC 14
dc.subjectcarbon
dc.subjectdates
dc.subjectisotopes
dc.subjectradioactive isotopes
dc.subjectabsolute age
dc.titleReappraisal of Chinese Loess Plateau Stratigraphic Sequences Over the Last 30,000 Years: Precursors of an Important Holocene Monsoon Climatic Event
dc.typeProceedings
dc.typetext
dc.identifier.journalRadiocarbon
dc.description.noteThis material was digitized as part of a cooperative project between Radiocarbon and the University of Arizona Libraries.
dc.description.collectioninformationThe Radiocarbon archives are made available by Radiocarbon and the University of Arizona Libraries. Contact lbry-journals@email.arizona.edu for further information.
dc.eprint.versionFinal published version
dc.description.admin-noteMigrated from OJS platform February 2021
dc.source.volume40
dc.source.issue2
dc.source.beginpage905
dc.source.endpage913
refterms.dateFOA2021-02-11T21:33:01Z


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