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Distinct climate change synchronous with Heinrich event one, recorded by stable oxygen and carbon isotopic compositions in stalagmites from China

Published online by Cambridge University Press:  20 January 2017

Houyun Zhou ,
Jianxin Zhao ,
Yuexing Feng ,
Michael K. Gagan ,
Guoqing Zhou  and
Jun Yan
Houyun Zhou*
Affiliation:
Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Wushan, Guangzhou 510640, P. R. China
Jianxin Zhao
Affiliation:
Radiogenic Isotope Laboratory, Centre for Microscopy and Microanalysis, University of Queensland, Brisbane, Qld 4072, Australia
Yuexing Feng
Affiliation:
Radiogenic Isotope Laboratory, Centre for Microscopy and Microanalysis, University of Queensland, Brisbane, Qld 4072, Australia
Michael K. Gagan
Affiliation:
Research School of Earth Sciences, The Australian National University, Canberra, ACT 0200, Australia
Guoqing Zhou
Affiliation:
Department of Earth Sciences, Nanjing University, Nanjing 210093, China
Jun Yan
Affiliation:
School of Resources and Environmental Engineering, Hefei University of Technology, Hefei 230009, China
*
*Corresponding author. Fax: +86 20 85290130.E-mail address:[email protected] (H. Zhou).
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Abstract

Uranium-series dating of oxygen and carbon isotope records for stalagmite SJ3 collected in Songjia Cave, central China, shows significant variation in past climate and environment during the period 20–10 ka. Stalagmite SJ3 is located more than 1000 km inland of the coastal Hulu Cave in East China and more than 700 km north of the Dongge Cave in Southwest China and despite minor differences, displays a clear first-order similarity with the Hulu and Dongge records. The coldest climatic phase since the Last Glacial Maximum, which is associated with the Heinrich Event 1 in the North Atlantic region, was clearly recorded in SJ3 between 17.6 and 14.5 ka, in good agreement in timing, duration and extent with the records from Hulu and Dongge caves and the Greenland ice core. The results indicate that there have been synchronous and significant climatic changes across monsoonal China and strong teleconnections between the North Atlantic and East Asia regions during the period 20–10 ka. This is much different from the Holocene Optimum which shows a time shift of more than several thousands years from southeast coastal to inland China. It is likely that temperature change at northern high latitudes during glacial periods exerts stronger influence on the Asian summer monsoon relative to insolation and appears to be capable of perturbing large-scale atmospheric/oceanic circulation patterns in the Northern Hemisphere and thus monsoonal rainfall and paleovegetation in East Asia. Climatic signals in the North Atlantic region propagate rapidly to East Asia during glacial periods by influencing the winter land–sea temperature contrast in the East Asian monsoon region.

Keywords

Speleothemδ18Oδ13CThe H1 cold phaseSynchronicityEast AsiaTeleconnectionAtmospheric circulation
Type
Research Article
Information
Quaternary Research , Volume 69 , Issue 2 , March 2008 , pp. 306 - 315
Copyright
University of Washington

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References

An, Z.S., Porter, S.C., Kutzbach, J.E., Wu, X.H., Wang, S.M., Liu, X.D., Li, X.Q., Zhou, W.J., (2000). Asynchronous Holocene optimum of the East Asian monsoon. Quaternary Science Reviews 19, 743–762.Google Scholar
Araguas-Araguas, L., Froehlich, K., (1998). Stable isotope composition of precipitation over southeast Asian. Journal of Geophysical Research 103, D22, 28721–28742.Google Scholar
Baker, A., Ito, E., Smart, P.L., McEwan, R.F., (1997). Elevated and variable values of C-13 in speleothems in a British cave system. Chemical Geology 136, 263–270.Google Scholar
Banner, J.L., Musgrove, M., Asmerom, Y., (1996). High-resolution temporal record of Holocene ground-water chemistry: tracing links between climate and hydrology. Geology 24, 1049–1052.Google Scholar
Baskaran, M., Krishnamurthy, R.V., (1993). Speleothems as proxy for the carbon isotope composition of atmospheric CO2 . Geophysical Research Letters 20, 2905–2908.Google Scholar
Beck, J.W., Recy, J., Taylor, F., Edwards, R.L., Cabioch, G., (1997). Abrupt changes in early Holocene tropical sea surface temperature derived from coral records. Nature 385, 705–707.Google Scholar
Benson, L., Burdett, J., Lund, S., Kashgarian, M., Mensing, S., (1997). Nearly synchronous climate change in the Northern Hemisphere during the last glacial termination. Nature 388, 263–265.Google Scholar
Broecker, W.S., (1994). Massive iceberg discharges as triggers for global climate change. Nature 372, 421–424.Google Scholar
Bureau of Geology and Mineral Resources of Sichuan Province, , (1991). Regional Geology of Sichuan Province. Geological Publishing House, Beijing., .Google Scholar
Cao, J., Yang, J.Y., (2005). Characteristics of Geological Vestiges Landscape in the Nuoshuihe Geopark, Sichuan. Geological Acta of Sichuan Province vol. 25 (2), (in Chinese with English abstract).Google Scholar
CLIMAP Project Members, , (1976). The surface of the ice-age earth. Science 191, 1131–1137.Google Scholar
Dansgaard, W., (1964). Stable isotopes in precipitation. Tellus 16, 436–468.CrossRefGoogle Scholar
Dorale, J.A., Edwards, R.L., Ito, E., Gonzàlez, L.A., (1998). Climate and vegetation history of the midcontinent from 75 to 25 ka: a Speleothem record from Crevice Cave, Missouri, USA. Science 282, 1871–1874.Google Scholar
Dykoski, C.A., Edwards, R.L., Cheng, H., Yuan, D., Cai, Y., Zhang, M., Lin, Y., Qin, J., An, Z., Revenauh, J., (2005). A high-resolution, absolute-dated Holocene and deglacial Asian monsoon record from Dongge Cave, China. Earth and Planetary Science Letters 233, 71–86.Google Scholar
Fleitmann, D., Burns, S.J., Neff, U., Mudelsee, M., Mangini, A., Matter, A., (2004). Palaeoclimatic interpretation of high-resolution oxygen isotope profiles derived from annually laminated speleothems from Southern Oman. Quaternary Science Reviews 23, 935–945.Google Scholar
Gascoyne, M., (1992). Palaeoclimate determination from cave calcite deposits. Quaternary Science Reviews 11, 609–632.Google Scholar
Genty, D., Blamart, D., Ouahdi, R., Gilmour, M., Baker, A., Jouzel, J., van Exter, S., (2003). Precise dating of Dansgaard–Oeschger climate oscillations in western Europe from stalagmite data. Nature 421, 833–837.Google Scholar
Grootes, P.M., Stuiver, M., White, J.W.C., Johnsen, S., Jouzel, J.J., (1993). Comparison of oxygen isotope records from the GISP2 and GRIP Greenland ice cores. Nature 366, 552–554.Google Scholar
He, Y., Theakstone, W.H., Zhonglin, Z., Dian, Z., Tandong, Y., Tuo, C., Yongping, S., Hongxi, P., (2004). Asynchronous Holocene climatic change across China. Quaternary Research 61, 52–63.CrossRefGoogle Scholar
Heinrich, H., (1988). Origin and consequences of cyclic ice rafting in the Northeast Atlantic Ocean during the past 130,000 years. Quaternary Research 29, 142–152.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. Geochimica et Cosmochimica Acta 35, 801–824.Google Scholar
Hendy, C.H., Wilson, A.T., (1968). Palaeoclimatic data from speleothem. Nature 216, 48–51.Google Scholar
Hendy, I.L., Kennett, J.P., (1999). Latest Quaternary North Pacific surface-water responses imply atmosphere-driven climate instability. Geology 27, 291–294.2.3.CO;2>CrossRefGoogle Scholar
Holmgren, K., Karlén, W., Shaw, P.A., (1995). Paleoclimatic significance of the stable isotopic composition and petrology of a late Pleistocene stalagmite from Botswana. Quaternary Research 43, 320–328.Google Scholar
Hu, C.-Y., Huang, J.-H., Fang, N.-Q., (2005). Adsorbed silica in stalagmite carbonate and its relationship to past rainfall. Geochimica et Cosmochimica Acta 69, 2285–2292.Google Scholar
Ijiri, A., Wang, L., Oba, T., Kawahata, H., Huang, C.-Y., Huang, C.-Y., (2005). Paleoenvironmental changes in the northern area of the East China Sea during the past 42,000 years. Palaeogeography, Palaeoclimatology, Palaeoecology 219, 239–261.Google Scholar
Johnson, K.R., Ingram, B.L., Sharp, W.D., (2006). East Asian summer monsoon variability during Marine Isotope Stage 5 based on speleothem δ 18O records from Wanxiang Cave, central China. Palaeogeography, Palaeoclimatology, Palaeoecology 236, 5–19.Google Scholar
Jouzel, J., Lorius, C., Petit, J.R., (1987). Vostok ice core: a continuous isotope temperature record over the last climatic cycle (160000 years). Nature 329, 403–408.Google Scholar
Kienast, M., Steinke, S., Stattegger, K., Calvert, S.E., (2001). Synchronous tropical South China Sea SST change and Greenland warming during deglaciation. Science 291, 2132–2134.Google Scholar
Kim, S.T., O'Neil, J.R., (1997). Equilibrium and nonequilibrium oxygen isotope effects in synthetic carbonates. Geochimica et Cosmochimica Acta 61, 3461–3475.Google Scholar
Kucera, M., Weinelt, M., Kiefer, T., (2005). Reconstruction of sea-surface temperatures from assemblages of planktonic foraminifera: multi-technique approach based on geographically constrained calibration data sets and its application to glacial Atlantic and Pacific Oceans. Quaternary Science Reviews 24, 951–998.Google Scholar
Liu, T.S., Ding, Z.L., (1998). Chinese loess and the paleomonsoon. Annual Review of Earth and Planetary Sciences 26, 111–145.Google Scholar
Martinson, D.G., Pisias, N.G., Hays, J.D., Imbrie, J., Moore, T.C. Jr., Shackletion, N.J., (1987). Age dating and the orbital theory of the ice ages: Development of a high-resolution 0 to 300000-year chronostratigraphy. Quaternary Research 27, 1–29.Google Scholar
McDermott, F., (2004). Palaeo-climate reconstruction from stable isotope variations in speleothems: A review. Quaternary Science Reviews 23, 901–918.Google Scholar
Porter, S.C., An, Z.S., (1995). Correlation between climate events in the North Atlantic and China during last glaciation. Nature 375, 305–308.Google Scholar
Rozanski, K., (1985). Deuterium and Oxygen-18 in European Groundwaters-Links to Atmospheric circulation in the past. Chemical Geology 52, 349–363.Google Scholar
Rozanski, K., Araguás-Araguás, L., Gonfiantini, R., (1992). Relation between long-term trends of Oxygen-18 isotope composition of precipitation and climate. Science 258, 981–985.Google Scholar
Rozanski, K., Araguás-Araguás, L., Gonfiantini, R., (1993). Isotopic patterns in modern global precipitation. Swart, P.K., Lohmann, K.C., McKenzie, L., Savin, , Climate changes in continental isotopic records. Geophysical Monograph vol. 78, American Geophysical Union, Washington DC., 1–36.Google Scholar
Schwarcz, H.P., (1986). Geochronology and isotopic geochemistry of speleothems. Fritz, P., Fontes, J.Ch., Handbook of Environmental Isotope Geochemistry. Elsevier, Amsterdam., 271–303.Google Scholar
Shao, X.H., Wang, Y.J., Cheng, H., Kong, X.G., Wu, J.Y., (2006). Holocene monsoonal climate and arid events recorded by a stalagmite from Shenlongjia, Hubei Province. Chinese Science Bulletin 51, 80–86.,(in Chinese).Google Scholar
Shi, Y.F., Kong, Z.C., Wang, S.M., Tang, L.Y., Wang, F.B., Chen, Y.D., Zhao, X.T., Zhang, P.Y., Shi, S.H., (1992). Basic feature of climates and environments during the Holocene Megathermal in China. Science in China. Series B, Chemistry, Life Sciences & Earth Sciences 35, 1300–1308.,(in Chinese).Google Scholar
Sinomaps Press, , (1984). Atlas of the People's Republic of China. Sinomaps Press, Beijing., .Google Scholar
Spötl, C., Fairchild, I.J., Tooth, A.F., (2005). Cave air control on dripwater geochemistry, Obir Caves (Austria): Implications for speleothem deposition in dynamically ventilated caves. Geochimica et Cosmochimica Acta 69, 2451–2468.Google Scholar
Stuiver, M., Grootes, P.M., Braziunas, T.F., (1995). The GISP2 delta 18O climate record of the past 16,500 years and the role of the sun, ocean, and volcanoes. Quaternary Research 44, 341–354.Google Scholar
Tan, M., Cai, B.G., (2005). Preliminary Calibration of Stalagmite Oxygen Isotopes from Eastern Monsoon China with Northern Hemisphere Temperatures. Pages Newsletter 13, 2, 16–17.Google Scholar
Thompson, L.G., Yao, T.D., Davis, M.E., Henderson, K., Mosley-Thompson, A.E., Lin, P.-N., Beer, J., Synal, H.-A., Cole-Dai, J., Bolzan, J.F., (1997). Tropical climate instability: the last glacial cycle from a Qinghai-Tibetan ice core. Science 276, 1821–1825.Google Scholar
Visser, K., Thunell, R., Stott, L., (2003). Magnitude and timing of temperature change in the Indo-Pacific warm pool during deglaciation. Nature 421, 152–155.Google Scholar
Wang, L.J., Sarnthein, M., Erlenkeuser, H., Grimalt, J., Grootes, P., Heilig, S., Ivanova, E., Kienast, M., Pelejero, C., Pflaumann, U., (1999). East Asian monsoon climate during the Late Pleistocene: high-resolution sediment records from the south China Sea. Marine Geology 156, 245–284.CrossRefGoogle 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, 2345–2347.Google Scholar
Webster, J.W., Brook, G.A., Railsback, L.B., (2007). Stalagmite evidence from Belize indicating significant droughts at the time of Preclassic Abandonment, the Maya Hiatus, and the Classic Maya collapse. Palaeogeography, Palaeoclimatology, Palaeoecology 250, 1–17.Google Scholar
Wigley, T.M.L., Brown, M.C., (1976). The physics of caves. Ford, T.D., Cullingford, C.H.D., The Science of Speleology. Academic Press, London., 329–358.Google Scholar
Winograd, I.J., Szabo, B.J., Coplen, T.B., Riggs, A.C., Kolesar, P.T., (1985). Two-million-year record of deuterium depletion in Great Basin ground waters. Science, 227, 519–522.Google Scholar
Yuan, D.X., Cheng, H., Edwards, R.L., (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 δ 18O in precipitation in China. Acta Geographica Sinica 53, 4, 356–364.,(in Chinese with English abstract).Google Scholar
Zhao, J.X., Hu, K., Collerson, K.D., (2001). Thermal ionization mass spectrometry U-series dating of a hominid site near Nanjing, China. Geology 29, 27–30.Google Scholar
Zhao, J.X., Wang, Y.J., Collerson, K.D., Gagan, M.K., (2003). Speleothem U-series dating of semi-synchronous climate oscillations during the last deglaciation. Earth and Planetary Science Letters 216, 155–161.Google Scholar
Zhou, H.Y., (2002). A Comment on "Tree-Ring δD as an indicator of Asian Monsoon intensity". Quaternary Research 58, 210–211.CrossRefGoogle Scholar
Zhou, H.Y., Li, T.G., Jia, G.D., Zhu, Z.Y., Chi, B.Q., (2007). Sea Surface Temperature Reconstruction for the Middle Okinawa Trough during the Last Glacial–Interglacial Cycle Using C37 Unsaturated Alkenones. Palaeogeography, Palaeoclimatology, Palaeoecology 246, 440–453.Google Scholar
Zhou, H.Y., Feng, Y.X., Zhao, J.X., Zhu, Z.Y., Chi, B.Q., et al., in preparation. Strontium contents and isotopic ratios of a stalagmite from Central China and their paleoclimatic implications.Google Scholar