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  Millennial-scale East Asian monsoon variability of the last glacial deduced from annually laminated sediments from Lake Sihailongwan, N.E. China

Mingram, J., Stebich, M., Schettler, G., Hu, Y., Rioual, P., Nowaczyk, N., Dulski, P., You, H., Opitz, S., Liu, Q., Liu, J. (2018): Millennial-scale East Asian monsoon variability of the last glacial deduced from annually laminated sediments from Lake Sihailongwan, N.E. China. - Quaternary Science Reviews, 201, 57-76.
https://doi.org/10.1016/j.quascirev.2018.09.023

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Mingram, J.1, Autor              
Stebich, Martina2, Autor
Schettler, Georg1, Autor              
Hu, Yaqin1, Autor              
Rioual, Patrick2, Autor
Nowaczyk, N.1, Autor              
Dulski, Peter1, Autor              
You, Haitao2, Autor
Opitz, Stephan2, Autor
Liu, Qiang2, Autor
Liu, Jiaqi2, Autor
Affiliations:
15.2 Climate Dynamics and Landscape Evolution, 5.0 Geoarchives, Departments, GFZ Publication Database, Deutsches GeoForschungsZentrum, ou_146046              
2External Organizations, ou_persistent22              

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Schlagwörter: Paleoclimatology, East Asian monsoon, Lake sediments, Varves, Pleistocene, Dansgaard-Oeschger cycles, Heinrich events
 Zusammenfassung: Lake Sihailongwan in Jilin province, NE China, provides the first continuous and almost entirely seasonally laminated sediment record on the East Asian mainland comprising the complete Holocene, the Late-glacial period, and large parts of the Last Glacial. Sediment and palynological proxy data provide a finely resolved regional environmental history of the East Asian monsoon. A varve-based chronology (shl-vc2) has been established for the last 65,000 years and allows a detailed comparison with other long regional and global palaeoclimate records. Vegetation density of the study area depends, on the long run, on precessionally forced insolation changes, with superimposed millennial-scale variability during the Last Glacial. Periodic increase of organic carbon content and thermophilous tree species like Ulmus and Fraxinus and contemporary decrease of shrub Alnus precisely mirror millennial-scale climatic variations primarily known from Greenland ice-cores as Dansgaard-Oeschger cycles, as well as Late-glacial period climate changes. Percentages of trees & shrubs pollen and in particular lake productivity-related data reveal substantial differences between interstadial intensities, with those between 50 and 60 ka BP being more pronounced than the following ones.

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Sprache(n): eng - Englisch
 Datum: 2018
 Publikationsstatus: Final veröffentlicht
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 Ort, Verlag, Ausgabe: -
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 Art der Begutachtung: -
 Identifikatoren: DOI: 10.1016/j.quascirev.2018.09.023
GFZPOF: p3 PT3 Earth Surface and Climate Interactions
 Art des Abschluß: -

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Titel: Quaternary Science Reviews
Genre der Quelle: Zeitschrift, SCI, Scopus
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Ort, Verlag, Ausgabe: -
Seiten: - Band / Heft: 201 Artikelnummer: - Start- / Endseite: 57 - 76 Identifikator: CoNE: https://gfzpublic.gfz-potsdam.de/cone/journals/resource/journals418