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Holocene variations in the Asian monsoon inferred from the geochemistry of lake sediments in central Tibet

Bibliographic Data

ID24088914
AuthorsCarrie Morrill (0000-0002-1635-5469, NSF National Center for Atmospheric Research), Jonathan T Overpeck (0000-0002-3843-9313, University of Arizona), Julia E Cole (0000-0002-3389-7809, University of Arizona), Kam‐biu Liu (0000-0002-0038-2198, Louisiana State University), Kam-biu Liu, Caiming Shen (0000-0002-8126-8775, Louisiana State University), LINGYU TANG (Chinese Academy of Sciences)
Year2006
Volume65
Issue02
Pages232-243
Publication date2006-03-01
Peer ReviewedYes
Open AccessYes
TypeARTICLE
VenueQuaternary Research (JOURNAL)
Journal identifiersISSN: 0033-5894 • E-ISSN: 1096-0287
PublisherCambridge University Press (CUP) (PUBLISHER)
DOI10.1016/j.yqres.2005.02.014
OpenAlexW1968552973
LanguageEN
Citations received49
References cited43

We present a record of monsoon variations for the early and middle Holocene that is inferred from the geochemistry of sediment cores from Ahung Co, a lake in central Tibet. The resolution of this record is better than 50 yr and the age model is derived from radiocarbon ages of terrestrial charcoal, which eliminates errors associated with the lake hard-water effect. We made down-core geochemical measurements of % carbonate, % organic carbon, C/N and δ 13 C of bulk organic matter, δ 13 C and δ 18 O of carbonate, and % dolomite. Proxy calibration and modern water-balance reconstruction show that these are proxies for lake depth and the amount of monsoon precipitation. We find that lake level and monsoon precipitation have been decreasing at Ahung Co since the early Holocene (∼7500 cal yr B.P.). Superimposed on this trend are rapid declines in monsoon rainfall at 7000–7500 and 4700 cal yr B.P. and seven century-scale wet–dry oscillations. The cores do not contain sediment from the last ∼4000 yr. Surface sediments from the lake accumulated during the 20th century, however. From this, we argue that lake levels have risen again recently following a late Holocene dry period.

Carbonate · Climatology · Geochemistry · Holocene · Monsoon · Precipitation · Radiocarbon dating · Sediment · Archaeology and ancient environmental studies · Geology · Geology and Paleoclimatology Research · Isotope Analysis in Ecology · Oceanography · Paleontology

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Unique citing works49
Citations per year2,58
Citation span2007 - 2026 (20)
Citation velocitycurrent
Highly citedNo
Citation typesNeutral: 38
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