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Mass accumulation rate and monsoon records from Xifeng, Chinese Loess Plateau, based on a luminescence age model
Uppsala University, Disciplinary Domain of Science and Technology, Earth Sciences, Department of Earth Sciences, LUVAL.ORCID iD: 0000-0002-6662-6650
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2016 (English)In: Journal of Quaternary Science, ISSN 0267-8179, E-ISSN 1099-1417, Vol. 31, 391-405 p.Article in journal (Refereed) Published
Abstract [en]

Luminescence dating of loess accumulation in China has raised questions over disturbance and gaps in the record, the magnitude of mass accumulation rates (MARs), and monsoon forcing mechanisms. Here we present a detailed quartz optically stimulated luminescence (OSL) chronology from the Xifeng Chinese Loess Plateau site. We reconstruct MARs and construct an age model for monsoon proxies at the site. The luminescence ages show significant pedogenic and anthropogenic disturbance in material deposited after ca. 20-22 ka. Analysis of other published data suggests that this disturbance may be more common than previously realized. MARs from undisturbed portions of Xifeng vary dramatically, with peaks potentially matching the timing of Heinrich events. The last glacial maximum peak MAR (22-27 ka) matches the Pacific and Greenland dust flux records, although appears earlier than peak MARs seen in many other OSL-dated Loess Plateau sites. East Asian monsoon grain-size and magnetic susceptibility records also show several differences between independently dated loess sites. This complicates our understanding of any lag between insolation forcing and monsoon response. Nevertheless, the Xifeng climate proxy changes show apparent broad agreement with the timing of Heinrich events in the North Atlantic, supporting assertions of a climatic teleconnection between the two areas.

Place, publisher, year, edition, pages
2016. Vol. 31, 391-405 p.
Keyword [en]
Chinese loess; dust MAR; East Asian monsoon; luminescence dating; OSL
National Category
Geosciences, Multidisciplinary
Identifiers
URN: urn:nbn:se:uu:diva-297057DOI: 10.1002/jqs.2848ISI: 000379155600010OAI: oai:DiVA.org:uu-297057DiVA: diva2:940683
Funder
Danish National Research Foundation, 11-104566
Available from: 2016-06-21 Created: 2016-06-21 Last updated: 2016-08-02Bibliographically approved

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Stevens, Thomas
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