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Decoupling of stalagmite-derived Asian summer monsoon records from North Atlantic temperature change during marine oxygen isotope stage 5d

Published online by Cambridge University Press:  20 January 2017

Houyun Zhou ,
Jianxin Zhao ,
Pingzhong Zhang ,
Chuan-Chou Shen ,
Baoquan Chi ,
Yuexing Feng ,
Yin Lin ,
Huazheng Guan  and
Chen-Feng You
Houyun Zhou*
Affiliation:
Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China
Jianxin Zhao
Affiliation:
Radiogenic Isotope Laboratory, Centre for Microscopy and Microanalysis, the University of Queensland, Brisbane, Qld 4072, Australia
Pingzhong Zhang
Affiliation:
Key Laboratory of Western China's Environmental Systems of Ministry of Education, College of Earth and Environment Sciences, Lanzhou University, Lanzhou 730000, China
Chuan-Chou Shen
Affiliation:
Department of Geosciences, National Taiwan University, Taipei 106, Taiwan, Republic of China
Baoquan Chi
Affiliation:
Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China The Graduate School, Chinese Academy of Sciences, Beijing 100039, China
Yuexing Feng
Affiliation:
Radiogenic Isotope Laboratory, Centre for Microscopy and Microanalysis, the University of Queensland, Brisbane, Qld 4072, Australia
Yin Lin
Affiliation:
Department of Geosciences, National Taiwan University, Taipei 106, Taiwan, Republic of China
Huazheng Guan
Affiliation:
Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China The Graduate School, Chinese Academy of Sciences, Beijing 100039, China
Chen-Feng You
Affiliation:
The Earth Dynamic System Research Center, National Cheng-Kung University, Tainan 701, Taiwan, Republic of China
*
*Corresponding author. Guangzhou Institute of Geochemistry, Chinese Academy of Sciences. No. 511, Kehua Street, Guangzhou, Guangdong Province, 510640, China. Fax: +86 20 8529 0130. E-mail address:hyzhou@gig.ac.cn (H. Zhou).
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Abstract

The Asian monsoon is an important component of the global climate system. Seasonal variations in wind, rainfall, and temperature associated with the Asian monsoon systems affect a vast expanse of tropical and subtropical Asia. Speleothem-derived summer monsoon variation in East Asia was previously found to be closely associated with millennial-scale change in temperature in the North Atlantic region between 75 and 10 ka. New evidence recovered from East Asia, however, suggests that the teleconnection between summer monsoon in East Asia and temperature change in the North Atlantic region may have significantly reduced during 120 to ~ 110 ka, a period directly after the full last interglaciation and corresponding roughly to marine oxygen isotope stage 5d. This reduction may be due to the low ice volume in the North Hemisphere at that time, which makes the millennial-scale change in temperature in the North Atlantic region less effective in influencing the Asian summer monsoon. This is important for investigating the mechanisms controlling the Asian summer monsoon and the paleoclimatic teleconnection between East Asia and the North Atlantic region, and for predicting monsoon-associated precipitation in East Asia under a global-warming trend.

Keywords

Asian monsoonNorth AtlanticStalagmitePaleoclimateMillennial-scale eventDecouplingTeleconnectionMarine oxygen isotope stage 5d
Type
Original Articles
Information
Quaternary Research , Volume 70 , Issue 2 , September 2008 , pp. 315 - 321
Copyright
University of Washington

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References

Barnett, T.P., Dümenil, L., Schlese, U., Roeckner, E., Latif, M., (1989). The effect of Eurasian snow cover on regional and global climate variations.. J. Atmos. Sci. 46, 661–685.Google Scholar
Berger, A.L., (1978). Long-term variations of caloric insolation resulting from the Earth's orbital elements.. Quat. Res. 9, 139–167.Google Scholar
Bureau of Geology and Mineral Resources of Sichuan Province (1991). Regional Geology of Sichuan Province.. Geological Publishing House, Beijing.Google Scholar
Chappellaz, J., Brook, E., Blunier, T., Malaize, B., (1997). CH4 and δ18O of O2 records from Antarctic and Greenland ice: a clue for stratigraphic disturbance in the bottom part of the Greenland Ice Core Project and Greenland Ice Sheet Project 2 ice cores.. J. Geophys. Res. 102, 26547–26557.Google Scholar
Dansgaard, W., (1964). Stable isotopes in precipitation.. Tellus 16, (4) 436–468.Google Scholar
Dansgaard, W., Johnsen, S.J., Clausen, H.B., Dahl-Jensen, D., Gundestrup, N.S., Hammer, C.U., Hvidberg, C.S., Steffensen, J.P., Sveinbjörnsdottir, A.E., Jouzel, J., Bond, G., (1993). Evidence for general instability of past climate from a 250-kyr ice-core record.. Nature 364, 218–220.Google Scholar
Drysdale, R.N., Zanchetta, G., Hellstrom, J.C., Fallick, A.E., McDonald, J., Cartwright, I., (2007). Stalagmite evidence for the precise timing of North Atlantic cold events during the early last glacial.. Geology 35, 77–80.Google Scholar
Dykoski, C.A., Edwards, R.L., Cheng, H., Yuan, D.X., Cai, Y.J., Zhang, M.L., Lin, Y.S., Qin, J.M., An, Z.S., Revenauh, J., (2005). A high-resolution, absolute-dated Holocene and deglacial Asian monsoon record from Dongge Cave, China.. Earth Planet. Sci. Lett. 233, 71–86.Google Scholar
Grootes, P.M., Stuiver, M., White, J.W.C., Johnsen, S.J., Jouzel, J., (1993). Comparison of oxygen isotope records from the GISP2 and GRIP Greenland ice cores.. Nature 366, 552–554.Google Scholar
Hendy, C.H., (1971). The isotopic geochemistry of speleothems 1: the calculation of the effects of the different modes of formation on the isotopic composition of speleothems and their applicability as palaeoclimatic indicators.. Geochim. Cosmochim. Acta 35, 801–824.Google Scholar
Hu, C.Y., Huang, J.H., Fang, N.Q., Xie, S.C., Henderson, G.M., Cai, Y.J., (2005). Adsorbed silica in stalagmite carbonate and its relationship to past rainfall.. Geochim. Cosmochim. Acta 69, 2285–2292.Google Scholar
Hu, C.Y., Henderson, G.M., Huang, J.H., Xie, S.C., Sun, Y., Johnson, K.R., (2008). Quantification of Holocene Asian monsoon rainfall from spatially separated cave records.. Earth Planet. Sci. Lett. 266, 221–232.Google Scholar
Johnsen, S.J., Clausen, H.B., Dansgaard, W., Gundestrup, N.S., Hammer, C.U., Andersen, U., Andersen, K.K., Hvidberg, C.S., Dahl-Jensen, D., Steffensen, J.P., Shoji, H., Sveinbjörnsdóttir, Á.E., White, J., Jouzel, J., Fishe, D., (1997). The δ18O record along the Greenland Ice Core Project deep ice core and the problem of possible Eemian climatic instability.. J. Geophys. Res. 102, 26397–26410.Google Scholar
Johnson, K.R., Ingram, B.L., Sharp, W.D., Zhang, P.Z., (2006). East Asian summer monsoon variability during Marine Isotope Stage 5 based on speleothem δ18O records from Wanxiang Cave, Central China.. Palaeogeogr. Palaeoclimatol. Palaeoecol. 236, 5–19.Google Scholar
Kelly, M.J., Edwards, R.L., Cheng, H., Yuan, D.X., Cai, Y.J., Zhang, M.L., Lin, Y.S., An, Z.S., (2006). High resolution characterization of the Asian Monsoon between 146,000 and 99,000 years B.P. from Dongge Cave, China and global correlation of events surrounding Termination II.. Palaeogeogr. Palaeoclimatol. Palaeoecol. 236, 20–38.Google Scholar
Lea, D.W., Pak, D.K., Spero, H.J., (2000). Climate impact of Late Quaternary equatorial Pacific sea surface temperature variations.. Science 289, 1719–1724.Google Scholar
Martinson, D.G., Pisias, N.G., Hays, J.D., Imbrie, J., (1987). Age dating and the orbital theory of the ice ages: development of a high-resolution 0 to 300,000-year chronostratigraphy.. Quat. Res. 27, 1–29.Google Scholar
NGRIP Project members (2004). High-resolution record of Northern Hemisphere climate extending into the last interglacial period.. Nature 431, 147–151.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.Google Scholar
Shackleton, N.J., (1987). Oxygen isotopes, ice volume and sea level.. Quat. Sci. Rev. 6, 183–190.Google Scholar
Shao, X.H., Wang, Y.J., Cheng, H., Kong, X.G., Wu, J.Y., (2006). Long-term trend and abrupt events of the Holocene Asian monsoon inferred from a stalagmite δ18O record from Shennongjia in Central China.. Chin. Sci. Bull. 51, (2) 221–228.Google Scholar
Sinomaps Press (1984). Atlas of the People's Republic of China.. Sinomaps Press, Beijing.Google Scholar
Tan, M., Cai, B.G., (2005). Preliminary calibration of stalagmite oxygen isotopes from eastern monsoon China with Northern Hemisphere temperatures.. Pages News 13, (2) 16–17.Google Scholar
Wang, Z., Mysak, L.A., (2006). Glacial abrupt climate changes and Dansgaard–Oeschger oscillations in a coupled climate model.. Paleoceanography 21, PA2001 10.1029/2005PA001238.Google Scholar
Wang, Y.J., Cheng, H., Edwards, R.L., An, Z.S., Wu, J.Y., Shen, C.C., Dorale, J.A., (2001). A high-resolution absolute-dated late Pleistocene monsoon record from Hulu Cave, China.. Science 294, 2345–2348.Google Scholar
Wang, Y.J., Cheng, H., Edwards, R.L., He, Y.Q., Kong, X.G., An, Z.S., Wu, J.Y., Kelly, M.J., Dykoski, C.A., Li, X.D., (2005). The Holocene Asian monsoon: links to solar changes and North Atlantic climate.. Science 308, 854–857.Google Scholar
Wang, Y.J., Cheng, H., Edwards, R.L., Kong, X.G., Shao, X.H., Chen, S.T., Wu, J.Y., Jiang, X.Y., Wang, X.F., An, Z.S., (2008). Millennial- and orbital-scale changes in the East Asian monsoon over the past 224,000 years.. Nature 451, 1090–1093.Google Scholar
Wu, W.X., Liu, T.S., (2004). Possible role of the “Holocene Event 3” on the collapse of Neolithic cultures around the central plain of China.. Quat. Int. 117, 153–166.Google Scholar
Yuan, D.X., Cheng, H., Edwards, R.L., Dykoski, C.A., Kelly, M.J., Zhang, M.L., Qing, J.M., Lin, Y.S., Wang, Y.J., Wu, J.Y., Dorale, J.A., An, Z.S., Cai, Y.J., (2004). Timing, duration, and transitions of the Last Interglacial Asian monsoon.. Science 304, 575–578.Google Scholar
Zhang, X.P., Yao, T.D., (1998). Distributional features of δ18O in precipitation in China.. Acta Geogr. Sin. 53, (4) 356–364. (in Chinese).Google Scholar
Zhao, J.X., Hu, K., Collerson, K.D., Xu, H.K., (2001). Thermal ionization mass spectrometry U-series dating of a hominid site near Nanjing, China.. Geology 29, 27–30.Google Scholar
Zhou, H.Y., Li, T.G., Jia, G.D., Zhu, Z.Y., Chi, B.Q., Cao, Q.Y., Sun, R.T., Peng, P.A., (2007). Sea surface temperature reconstruction for the middle Okinawa Trough during the last glacial–interglacial cycle using C37 unsaturated alkenones.. Palaeogeogr. Palaeoclimatol. Palaeoecol. 240, 440–453.Google Scholar
Zhou, H.Y., Zhao, J.X., Feng, Y.X., Gagan, M.K., Zhou, G.Q., Yan, J., (2008). Distinct climate change synchronous with Heinrich event one, recorded by stable oxygen and carbon isotopic compositions in stalagmites from China.. Quat. Res. 69, 306–315.Google Scholar