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Synchronism of Holocene East Asian monsoon variations and North Atlantic drift-ice tracers

Published online by Cambridge University Press:  20 January 2017

Stephen C. Porter  and
Zhou Weijian
Stephen C. Porter*
Affiliation:
Department of Earth and Space Sciences, University of Washington, Seattle, WA 98195, USA
Zhou Weijian
Affiliation:
Institute of Earth Environment, Chinese Academy of Sciences, 10 Fenghui South Road, Xi'an High-Tech Zone, Xi'an 710054, People's Republic of China
*
*Corresponding author. E-mail address:scporter@u.washington.edu (S.C. Porter).
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Abstract

Eighteen radiocarbon-dated eolian and paleosol profiles within a 1500-km-long belt along the arid to semi-arid transition zone of north-central China record variations in the extent and strength of the East Asian summer monsoon during the Holocene. Dated paleosols and peat layers represent intervals when the zone was dominated by a mild, moist summer monsoon climate that favored pedogenesis and peat accumulation. Brief intervals of enhanced eolian activity that resulted in the deposition of loess and eolian sand were times when strengthened winter monsoon conditions produced a colder, drier climate. The monsoon variations correlate closely with variations in North Atlantic drift-ice tracers that represent episodic advection of drift ice and cold polar surface water southward and eastward into warmer subpolar water. The correspondence of these records over the full span of Holocene time implies a close relationship between North Atlantic climate and the monsoon climate of central China.

Keywords

ChinaMonsoon climateEolian sedimentsPaleosolsNorth Atlantic drift ice
Type
Research Article
Information
Quaternary Research , Volume 65 , Issue 3 , May 2006 , pp. 443 - 449
Copyright
University of Washington

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References

An, Z.S., (2000). The history and variability of the East Asian paleomonsoon climate. Quaternary Science Reviews 19, 171–187.CrossRefGoogle Scholar
An, Z.S., Porter, S.C., (1997). Millennial-scale climatic oscillations during the last interglaciation in central China. Geology 25, 603–606.Google Scholar
An, Z.S., Kukla, G.J., Porter, S.C., Xiao, J.L., (1991). Magnetic susceptibility evidence of monsoon variations on the Loess Plateau of central China during the last 130,000 years. Quaternary Research 36, 29–36.Google Scholar
An, Z.S., Porter, S.C., Kutzbach, J.E., Wu, X., Wang, X., Liu, X., Li, W., Zhou, W., (2000). Asynchronous Holocene optimum of the East Asian monsoon. Quaternary Science Reviews 19, 743–762.Google Scholar
Bond, G., Kromer, B., Beer, J., Muscheler, R., Evans, M.N., Showers, W., Hoffmann, S., Lotti-Bond, R., Hajdas, I., Bonani, G., (2001). Persistent solar influence on North Atlantic climate during the Holocene. Science 294, 1257–1266.CrossRefGoogle ScholarPubMed
Cui, Z.J., Song, C.Q., (1992). The periglacial phenomenon and environmental evolution during Holocene in Daqingshan (mountain). Glacier and Permafrost 14, 325–331.(in Chinese).Google Scholar
Dong, G.R., Chen, H.Z., Wang, G.R., Li, X.Z., Shao, Y.J., Jing, J., (1995). The evolution of desert and sandy land in North China and their climatic change in the last 150 ka. Science in China Series B 25, 1303–1312.(in Chinese).Google Scholar
Dong, G.R., Gao, Q.Z., Zhou, X.Y., Li, B.S., Yan, M.C., (1996). Climatic changes on southern fringe of the Badain Jaran Desert since the Late Pleistocene. Chinese Science Bulletin 41, 837–842.Google Scholar
Gao, S.Y., Chen, W.N., Jin, H.l., Dong, G.R., Li, B.S., Yang, G.S., Lin, L.Y., Guan, Y.Z., Sun, Z., Jin, J., Zhang, Y.T., Cao, J.S., (1993). Preliminary study on the Holocene evolution of the NW desert margin in the monsoon region of China. Science in China Series B 23, 202–208.(in Chinese).Google Scholar
Gao, Q.G., Gao, G.R., Zhou, X.Y., Li, B.S., Yan, M.C., (1996). The Chagelebulu Section: a strata record of the advances and retreats of the monsoons in East Asia sine Late Pleistocene. Journal of Desert Research 16, 112–119.(in Chinese).Google Scholar
Hong, Y.T., Hong, B., Lin, Q.H., Zhu, Y.K., Shibata, Y., Hirota, M., Uchida, M., Leng, X.T., Jiang, H.B., Xu, H., Wang, H., Yi, L., (2003). Correlation between Indian Ocean summer monsoon and North Atlantic climate during the Holocene. Earth and Planetary Science Letters 211, 371–380.CrossRefGoogle Scholar
Porter, S.C., (2000a). High-resolution paleoclimatic information from Chinese eolian sediments based on grayscale intensity profiles. Quaternary Research 53, 70–77.Google Scholar
Porter, S.C., (2000b). Onset of Neoglaciation in the Southern Hemisphere. Journal of Quaternary Science 15, 395–408.3.0.CO;2-H>CrossRefGoogle Scholar
Porter, S.C., (2001). Chinese loess record of monsoon climate during the last glacial–interglacial cycle. Earth Science Reviews 54, 115–128.Google Scholar
Porter, S.C., An, Z.S., (1995). Correlation between climate events in the North Atlantic and China during the last glaciation. Nature 375, 305–308.CrossRefGoogle Scholar
Stuiver, M., Reimer, P.J., (1993). Extended 14C database and revised CALIB 3.1 14C age calibration program. Radiocarbon 35, 215–230.Google Scholar
Tao, Z., Dong, G.R., (1994). Relation of land desertification and climatic changes sine last-glacial period in Guinan Sandy Land. Journal of Desert Research 14, 42–48.(in Chinese).Google Scholar
Zhou, W.J., An, Z.S., (1994). Stratigraphic division of Holocene loess in China. Radiocarbon 36, 37–45.CrossRefGoogle Scholar
Zhou, W.J., Donahue, D.J., Porter, S.C., Jull, T.A., Li, X.Q., Stuiver, M., An, Z.S., Matsumoto, E., Dong, G.R., (1996). Variability of monsoon climate in East Asia at the end of the last glaciation. Quaternary Research 46, 219–229.Google Scholar
Zhou, W.J., Donahue, D.J., Jull, A.T.J., (1997). Radiocarbon AMS dating of pollen concentrated form aeolian sediments: implications for monsoon climate change since the late Quaternary. Radiocarbon 39, 16–19.Google Scholar
Zhou, W.J., An, Z.S., 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, 905–913.CrossRefGoogle Scholar
Zhou, W.J., Head, M.J., Lu, X.F., An, Z.S., Jull, A.J.T., Donahue, D., (1999). Teleconnection of climatic events between East Asia and polar, high latitude areas during the last deglaciation. Palaeogeography, Palaeoclimatology, Palaeoecology 152, 163–172.Google Scholar
Zhou, W.J., Head, M.J., An, Z.S., De Deckker, P., Liu, Z.Y., Liu, X.D., Lu, X.F., Donahue, D., Jull, A.J.T., Beck, J.W., (2001a). Terrestrial evidence for a spatial structure of tropical–polar interconnections during the Younger Dryas episode. Earth and Planetary Science Letters 191, 231–239.Google Scholar
Zhou, W.J., Head, M.J., Lin, D., (2001b). Climate change in northern China since the late Pleistocene and its response to global change. Quaternary International 83–85, 285–292.CrossRefGoogle Scholar
Zhou, W.J., Wu, Z.J., Jull, A.J.T., Burr, G., Donahue, D.D., Li, B.S., Head, J., (2001c). Environmental and climatic change as recorded in geological sediments from the arid to semi-arid zone of China. Radiocarbon 43, 619–627.CrossRefGoogle Scholar
Zhou, W.J., Dodson, J., Head, M.J., Li, B.S., Hou, Y.J., Lu, X.F., Donahue, D.J., Jull, A.J.T., (2002). Environmental variability within the Chinese desert-loess transition zone over the last 20,000 years. The Holocene 12, 117–122.CrossRefGoogle Scholar