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Decoupling of the East Asian summer monsoon and Indian summer monsoon between 20 and 17 ka

Published online by Cambridge University Press:  20 January 2017

Xiuyang Jiang ,
Yaoqi He ,
Chuan-Chou Shen ,
Shi-Yu Lee ,
Bang Yang ,
Ke Lin  and
Zhizhong Li
Xiuyang Jiang*
Affiliation:
Key Laboratory of Humid Subtropical Eco-geographical Processes, Ministry of Education, College of Geography Science, Fujian Normal University, Fuzhou 350007, China High-Precision Mass Spectrometry and Environment Change Laboratory (HISPEC), Department of Geosciences, National Taiwan University, Taipei 10617, Taiwan
Yaoqi He
Affiliation:
College of Tourism and Air Service, Guizhou Minzu University, Guiyang 550025, China
Chuan-Chou Shen*
Affiliation:
High-Precision Mass Spectrometry and Environment Change Laboratory (HISPEC), Department of Geosciences, National Taiwan University, Taipei 10617, Taiwan
Shi-Yu Lee
Affiliation:
Research Center for Environment Changes, Academia Sinica, Taipei 11529, Taiwan
Bang Yang
Affiliation:
Key Laboratory of Humid Subtropical Eco-geographical Processes, Ministry of Education, College of Geography Science, Fujian Normal University, Fuzhou 350007, China
Ke Lin
Affiliation:
High-Precision Mass Spectrometry and Environment Change Laboratory (HISPEC), Department of Geosciences, National Taiwan University, Taipei 10617, Taiwan
Zhizhong Li
Affiliation:
Key Laboratory of Humid Subtropical Eco-geographical Processes, Ministry of Education, College of Geography Science, Fujian Normal University, Fuzhou 350007, China
*
* Correspondence to: X. Jiang, College of Geography Science, Fujian Normal University, Fuzhou, China.
** Correspondence to: C.-C. Shen, Department of Geosciences, National Taiwan University, Taipei, Taiwan.E-mail addresses: [email protected] (X. Jiang), [email protected] (C.-C. Shen).
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Abstract

Marine Oxygen Isotope Stage (MIS) 2, with its profound environmental and climatic changes from before the last glacial maximum (LGM) to the last deglaciation, is an ideal period for understanding the evolution of the East Asian summer monsoon (EASM) and Indian summer monsoon (ISM), two Asian monsoon sub-systems. With 875 stable oxygen isotope ratios and 43 230Th dates from stalagmites in Sanxing Cave, southwestern China, we construct and interpret a new, replicated, Asian summer monsoon (ASM) record covering 30.9–9.7 ka with decadal resolution. δ18O records from this site and other reported Chinese caves display similar long-term orbitally dominated trends and synchronous millennial-scale strong and weak monsoonal events associated with climate changes in high northern latitudes. Interestingly, Sanxing δ18O and Arabian Sea records show a weakening ISM from 22 to 17 ka, while the Hulu and Qingtian records from East and Central China express a 3-ka intensifying EASM from 20 to 17 ka. This decoupling between EASM and ISM may be due to different sensitivities of the two ASM sub-systems in response to internal feedback mechanisms associated with the complex geographical or land-ocean configurations.

Keywords

East Asian summer monsoonIndian summer monsoonMIS 2DecouplingStalagmite
Type
Articles
Information
Quaternary Research , Volume 82 , Issue 1 , July 2014 , pp. 146 - 153
Copyright
University of Washington

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References

An, Z.S. The history and variability of the East Asian paleomonsoon climate. Quaternary Science Reviews 19, (2000). 171–187.CrossRefGoogle Scholar
Berger, A., and Loutre, M.F. Insolation values for the climate of the last 10 million years. Quaternary Science Reviews 10, (1991). 297–317.Google Scholar
Bond, G., Showers, W., Cheseby, M., Lotti, R., Almasi, P., deMenocal, P., Priore, P., Cullen, H., Hajdas, I., and Bonani, G. A pervasive millennial-scale cycle in North Atlantic Holocene and glacial climates. Science 278, (1997). 1257–1266.CrossRefGoogle Scholar
Cai, Y.J., An, Z.S., Cheng, H., Edwards, R.L., Kelly, M.J., Liu, W., Wang, X., and Shen, C.-C. High-resolution absolute-dated Indian Monsoon record between 53 and 36 ka from Xiaobailong Cave, southwestern China. Geology 34, 8 (2006). 621–624.Google Scholar
Cai, Y.J., Tan, L.C., Cheng, H., An, Z.S., Edwards, R.L., Kelly, M.J., Kong, X.G., and Wang, X.F. The variation of summer monsoon precipitation in central China since the last deglaciation. Earth and Planetary Science Letters 291, (2010). 21–31.Google Scholar
Cheng, H., Edwards, R.L., Hoff, J., Gallup, C.D., Richards, D.A., and Asmerom, Y. The half-lives of uranium-234 and thorium-230. Chemical Geology 169, (2000). 17–33.CrossRefGoogle Scholar
Cheng, H., Edwards, R.L., Broecker, W.S., Denton, G.H., Kong, X.G., Wang, Y.J., Zhang, R., and Wang, X.F. Ice age terminations. Science 326, (2009). 248–252.CrossRefGoogle ScholarPubMed
Cheng, H., Sinha, A., Wang, X.F., Cruz, F.W., and Edwards, R.L. The Global Paleomonsoon as seen through speleothem records from Asia and the Americas. Climate Dynamics 39, 5 (2012). 1045–1062.Google Scholar
Chiang, J.C.H., and Bitz, C.M. Influence of high latitude ice cover on the marine Intertropical Convergence Zone. Climate Dynamics 25, 5 (2005). 477–496.Google Scholar
Clark, P.U., Dyke, A.S., Shakun, J.D., Carlson, A.E., Clark, J., Wohlfarth, B., Mitrovica, J.X., Hostetler, S.W., and McCabe, A.M. The last glacial maximum. Science 325, (2009). 710–714.CrossRefGoogle ScholarPubMed
Clement, A.C., Seager, R., and Cane, M.A. Orbital controls on ENSO and tropical climate. Paleoceanography 14, 4 (1999). 441–456.CrossRefGoogle Scholar
Deplazes, G., Lückge, A., Peterson, L.C., Timmermann, A., Hamann, Y., Hughen, K.A., R öhl, U., Laj, C., Cane, M.A., Sigman, D.M., and Haug, G.H. Links between tropical rainfall and North Atlantic climate during the last glacial period. Nature Geoscience 6, (2013). 213–217.CrossRefGoogle Scholar
Dong, J.G., Wang, Y.J., Cheng, H., Hardt, B., Edwards, R.L., Kong, X.G., Wu, J.Y., Chen, S.T., Liu, D.B., Jiang, X.Y., and Zhao, K. A high-resolution stalagmite record of the Holocene East Asian monsoon from Mt Shennongjia, central China. The Holocene 20, 2 (2010). 257–264.Google Scholar
Dorale, J.A., and Liu, Z.H. Limitations of Hendy test criteria in judging the paleoclimatic suitability of speleothems and the need for replication. Journal of Cave and Karst Studies 71, 1 (2009). 73–80.Google Scholar
Dykoski, C.A., Edwards, R.L., Cheng, H., Yuan, D.X., Cai, Y.J., Zhang, M.L., Lin, Y.S., Qing, J.M., An, Z.S., and Revenaugh, J. A high-resolution, absolute-dated Holocene and deglacial Asian monsoon record from Dongge Cave, China. Earth and Planetary Science Letters 233, (2005). 71–86.Google Scholar
Hong, Y.T., Hong, B., Lin, Q.H., Shibata, Y., Hirota, M., Zhu, Y.X., Leng, X.T., Wang, Y., Wang, H., and Yi, L. Inverse phase oscillations between the East Asian and Indian ocean summer monsoons during the last 12000 years and paleo-El Niño. Earth and Planetary Science Letters 231, (2005). 331–346.CrossRefGoogle Scholar
Huang, R., Huang, G., and Wei, Z.G. Climate variations of the summer monsoon over China. Chang, C.-P. East Asian Monsoon. (2004). World Scientific Publishing Co. Pte. Ltd, Singapore. 213–268.Google Scholar
IAEA/WMO Global Network of Isotopes in Precipitation. The GNIP Database. (Accessible at: http://www.iaea.org/water) (2006). Google Scholar
Jaffey, A.H., Flynn, K.F., Glendenin, L.E., Bentley, W.C., and Essling, A.M. Precision measurement of half-lives and specific activities of U-235 and U-238. Physical Review 4, (1971). 1889–1906.Google Scholar
Lisiecki, L.E., and Raymo, M.E. A Pliocene–Pleistocene stack of 57 globally distributed benthic δ18O records. Paleoceanography 20, (2005). PA1003 http://dx.doi.org/10.1029/2004PA001071 Google Scholar
Liu, J., Wang, B., and Yang, J. Forced and internal modes of variability of the East Asian summer monsoon. Climate of Past 4, (2008). 225–233.CrossRefGoogle Scholar
Maher, B.A., and Hu, M. A high-resolution record of Holocene rainfall variations from the western Chinese Loess Plateau: antiphase behavior of the African/Indian and East Asian summer monsoons. The Holocene 16, 3 (2006). 309–319.Google Scholar
Partin, J.W., Cobb, K.M., Adkins, J.F., Clark, B., and Fernandez, D.P. Millennial-scale trends in west Pacific warm pool hydrology since the Last Glacial Maximum. Nature 449, (2007). 452–455.CrossRefGoogle ScholarPubMed
Rasmussen, S.O., Seierstad, I.K., Andersen, K.K., Bigler, M., Dahl-Jensen, D., and Johnsen, S.J. Synchronization of the NGRIP, GRIP, and GISP2 ice cores across MIS2 and palaeoclimatic implications. Quaternary Science Reviews 27, (2008). 18–28.CrossRefGoogle Scholar
Rosenthal, Y., Oppo, D.W., and Linsley, K. The amplitude and phasing of climate change during the last deglaciation in the Sulu Sea, western equatorial Pacific. Geophysical Research Letters 30, 8 (2003). 1428 http://dx.doi.org/10.1029/2002GL016612 Google Scholar
Schulz, H., Rad, U.V., and Erlenkeuser, H. Correlation between Arabian Sea and Greenland climate oscillation of the past 110,000 years. Nature 393, (1998). 54–57.Google Scholar
Shen, C.-C., Edwards, R.L., Cheng, H., Dorale, J.A., Thomas, R.B., Moran, S.B., Weinstein, S.E., and Edmonds, H.N. Uranium and thorium isotopic and concentration measurements by magnetic sector inductively coupled plasma mass spectrometry. Chemical Geology 185, (2002). 165–178.CrossRefGoogle Scholar
Shen, C.-C., Cheng, H., Edwards, R.L., Moran, S.B., Edmonds, H.N., Hoff, J.A., and Thomas, R.B. Measurement of attogram quantities of 231Pa in dissolved and particulate fractions of seawater by isotope dilution thermal ionization mass spectroscopy. Analytical Chemistry 75, (2003). 1075–1079.Google Scholar
Shen, C.-C., Li, K.-S., Sieh, K., Natawidjaja, D., Cheng, H., Wang, X.F., Edwards, R.L., Lam, D.D., Hsieh, U.-T., Fan, T.-Y., Meltzner, A.J., Taylor, F.W., Quinn, T.M., Chiang, H.-W., and Kilbourne, K.H. Variation of initial 230Th/232Th and limits of high precision U–Th dating of shallow-water corals. Geochimica et Cosmochimica Acta 72, (2008). 4201–4223.Google Scholar
Shen, C.-C., Wu, C.-C., Cheng, H., Edwards, R.L., Hsieh, Y.-T., Gallet, S., Chang, C.-C., Li, T.Y., Lam, D.D., Kano, A., Hori, M., and Spötl, C. High-precision and high-resolution carbonate 230Th dating by MC-ICP-MS with SEM protocols. Geochimica et Cosmochimica Acta 99, (2012). 71–86.Google Scholar
Sun, Y.B., Clemens, S.C., Morrill, C., Lin, X.P., Wang, X.L., and An, Z.S. Influence of Atlantic meridional overturning circulation on the East Asian winter monsoon. Nature Geoscience 5, (2012). 46–49.Google Scholar
Tao, S.Y., and Chen, L. A review of recent research on East Asian summer monsoon in China. Chang, C.P., and Krishnamurti, T.N. Monsoon Meteorology. (1987). Oxford University Press, London. 60–92.Google Scholar
Wang, H.J., and Chen, H.P. Climate control for southeastern China moisture and precipitation: Indian or East Asian monsoon?. Journal of Geophysical Research 117, (2012). http://dx.doi.org/10.1029/2012JD017734 Google Scholar
Wang, B., and Lin, H. Rainy season of the Asian-Pacific summer monsoon. Journal of Climate 15, (2002). 386–396.Google Scholar
Wang, Y.J., Cheng, H., Edwards, R.L., An, Z.S., Wu, J.Y., Shen, C.-C., and Dorale, J.A. A high-resolution absolute-dated Late Pleistocene monsoon record from Hulu Cave, China. Science 294, (2001). 2345–2348.Google Scholar
Wang, B., Clemens, S.C., and Liu, P. Contrasting the Indian and East Asian monsoons: implications on geologic time scale. Marine Geology 201, (2003). 5–21.Google Scholar
Wang, X.F., Auler, A.S., Edwards, R.L., Cheng, H., Ito, E., Wang, Y.J., Kong, X.G., and Solheid, M. Millennial-scale precipitation changes in southern Brazil over the past 90,000 years. Geophysical Research Letters 34, (2007). http://dx.doi.org/10.1029/2007GL031149 CrossRefGoogle 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., and An, Z.S. Millennial- and orbital-scale changes in the East Asian monsoon over the past 224,000 years. Nature 451, (2008). 1090–1093.Google Scholar
Wang, Y.B., Liu, X.Q., and Herzschuh, U. Asynchronous evolution of the Indian and East Asian Summer Monsoon indicated by Holocene moisture patterns in monsoonal central Asia. Earth-Science Reviews 103, (2010). 135–153.CrossRefGoogle Scholar
Webster, P.J., and Yang, S. Monsoon and ENSO: selectively interactive systems. The Quaternary Journal of Royal Meteorological Society 118, 507 (1992). 877–926.CrossRefGoogle Scholar
Webster, P.J., Magana, V.O., Palmer, T.N., Shukla, J., Tomas, R.A., Yanai, M., and Yasunari, T. Monsoons: processes, predictability, and the prospects for prediction. Journal of Geophysical Research 103, (1998). 14451–14510.CrossRefGoogle Scholar
Wu, J.Y., Wang, Y.J., Cheng, H., and Edwards, R.L. An exceptionally strengthened East Asian summer monsoon event between 19.9 and 17.1 ka recorded in a Hulu stalagmite. Science in China Series D: Earth Sciences 52, (2009). 360–368.Google Scholar
Yang, Y., Yuan, D.X., Cheng, H., Zhang, M.L., Qin, J.M., Lin, Y.S., Zhu, X.Y., and Edwards, R.L. Precise dating of abrupt shifts in the Asian Monsoon during the last deglaciation based on stalagmite data from Yamen Cave, Guizhou Province, China. Science in China Series D: Earth Sciences 53, (2010). 633–641.CrossRefGoogle 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., and Cai, Y.J. Timing, duration, and transitions of the last interglacial Asian monsoon. Science 304, (2004). 575–578.CrossRefGoogle ScholarPubMed
Zhang, R., and Delwroth, T.L. Simulated tropical response to a substantial weakening of the Atlantic thermohaline circulation. Journal of Climate 18, (2005). 1853–1860.Google Scholar
Zhang, W.H., Wu, J.Y., Wang, Y., Wang, Y.J., Cheng, H., Kong, X.G., and Duan, F.C. A detailed East Asian monsoon history surrounding the ‘Mystery Interval’ derived from three Chinese speleothem records. Quaternary Research (2014). http://dx.doi.org/10.1016/j.yqres.2014.01.010 Google Scholar
Zhao, K., Wang, Y.J., Edwards, R.L., Cheng, H., and Liu, D.B. High-resolution stalagmite δ18O records of Asian monsoon changes in central and southern China spanning the MIS3/2 transition. Earth and Planetary Science Letters 298, (2010). 191–198.Google Scholar
Zhou, W.J., Priller, A., Beck, J.W., Wu, Z.K., Chen, M.B., An, Z.S., Walter, K., Xian, F., Yu, H.G., and Liu, L. Disentangling geomagnetic and precipitation signals in an 80-kyr Chinese loess record of 10Be. Radiocarbon 49, (2007). 139–160.Google Scholar
Zhou, H.Y., Zhao, J.X., Wang, Q., Feng, Y.X., and Tang, J. Speleothem-derived Asian summer monsoon variations in Central China, 54–46 ka. Journal of Quaternary Science 26, 8 (2011). 781–790.Google Scholar