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Desiccation cracks in Zhoushan Archipelago, East China Sea, developed during Heinrich event 3

Published online by Cambridge University Press:  20 January 2017

Nan Jia ,
Yuhong Wang  and
Liguang Sun
Nan Jia
Affiliation:
Institute of Polar Environment, School of Earth and Space Sciences, University of Science and Technology of China, Hefei, Anhui 230026, China CAS Key Laboratory of Crust–Mantle Materials and Environments, School of Earth and Space Sciences, University of Science and Technology of China, Hefei, Anhui 230026, China
Yuhong Wang
Affiliation:
Advanced Management Research Center, Ningbo University, Ningbo, Zhejiang 315211, China
Liguang Sun*
Affiliation:
Institute of Polar Environment, School of Earth and Space Sciences, University of Science and Technology of China, Hefei, Anhui 230026, China CAS Key Laboratory of Crust–Mantle Materials and Environments, School of Earth and Space Sciences, University of Science and Technology of China, Hefei, Anhui 230026, China
*
*Corresponding author at: Institute of Polar Environment, School of Earth and Space Sciences, University of Science and Technology of China, Hefei, Anhui 230026, China. Fax: + 86 551 3607583. E-mail address:[email protected] (L. Sun).
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Abstract

Large desiccation cracks were discovered in the intertidal zone of Zhoushan archipelago, East China Sea. Radiocarbon dating showed that desiccation cracks were formed around 31.2–30.4 cal ka BP. Palynological, mineralogical, and elemental geochemical analyses indicated that the cracks were formed as the result of an abrupt climate shift event. The climate changed from warm and humid, to cold and arid, and back to warm and humid again. This climate event is quite likely linked to Heinrich event 3 via the East Asian Monsoon. Desiccation cracks may provide a new proxy material for studying paleoclimate and paleoenvironment in the Quaternary.

Keywords

Zhoushan archipelagoDesiccation cracksHeinrich event 3Climate event
Type
Original Articles
Information
Quaternary Research , Volume 77 , Issue 2 , March 2012 , pp. 258 - 263
Copyright
University of Washington

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References

Biscaye, P.E. Grousset, F.E. Revel, M. Van der Gaast, S. Zielinski, G.A. Vaars, A. Kukla, G. 1997, Asian provenance of glacial dust (stage 2) in the Greenland Ice Sheet Project2 Ice Core, Summit, Greenland. Journal of Geophysical Research 102, 26765–26781.Google Scholar
Cox, R. Lowe, D.R. Cullers, R.L. 1995, The influence of sediment recycling and basement composition on evolution of mudrock chemistry in the southwestern United States. Geochimica et Cosmochimica Acta 59, 2919–2940.CrossRefGoogle Scholar
Danzeglocke, U. Jöris, O. Weninger, B. 2007, CalPal-2007. onlinehttp://www.calpal-online.de/accessed 2007-06-27.Google Scholar
Deconinck, J.F. Blanc-Valleron, M.M. Rouchy, J.M. Gamoin, G. Badaut-Trauth, D. 2000, Palaeoenvironmental and diagenetic control of the mineralogy of Upper Cretaceous–Lower Tertiary deposits of the Central Palaeo-Andean basin of Bolivia (Potosi area). Sedimentary Geology 132, 263–278.CrossRefGoogle Scholar
Ducloux, J. Meunier, A. Velde, B. 1976, Smectite, chlorite and a regular interlayered chlorite–vermiculite in soils developed on a small serpentinite body, Massif Central, France. Clay Minerals 11, 121–135.Google Scholar
Goehring, L. Conroy, R. Akhter, A. Clegg, W.J. Routh, A.F. 2010, Evolution of mud-crack patterns during repeated drying cycles. Soft Matter 6, 3562–3567.Google Scholar
Grimm, E.C. Jacobson, G.L. Watts, W.A. Hansen, B.C.S. Maasch, K.A. 1993, A 50000-year record of climate oscillations from Florida and its temporal correlation with the Heinrich events. Science 261, 198–200.Google Scholar
Guo, Z. Liu, T. Guiot, J. Wu, N. Lü, H. Han, J. Liu, J. Gu, Z. 1996, High frequency pulses of East Asian monsoon climate in the last two glaciations: link with the North Atlantic. Climate Dynamics 12, 701–709.Google Scholar
Heinrich, H. 1988, Origin and consequences of cyclic ice rafting in the Northeast Atlantic Ocean during the past 130000 years. Quaternary Research 29, 142–152.Google Scholar
Holtzapffel, T. 1985, Les minérauxargileux, préparation, analysediffractométriqueetdétermination. 12. Societal Géologique du Nord 136 pp.Google Scholar
Li, T. Liu, Z. Hall, M.A. Berne, S. Saito, Y. Cang, S. Cheng, Z. 2001, Heinrich event imprints in the Okinawa Trough: evidence from oxygen isotope and planktonic foraminifera. Palaeoecolology 176, 133–146.Google Scholar
Mack, G.H. James, W.C. Monger, H.C. 1993, Classification of paleosols. Bulletin of the Geological Society of America 105, 129–136.2.3.CO;2>CrossRefGoogle Scholar
Marriott, S.B. Wright, V.P. 1993, Paleosols as indicators of geomorphic stability in two old red sandstone alluvial suites. Journal of the Geological Society 150, 1109–1120.Google Scholar
Mayewski, P.A. Meeker, L.D. Whitlow, S. Twickler, M.S. Morrison, M.C. Bloomfield, P. Bond, G.C. Alley, R.B. Gow, A.J. Meese, D.A. Grootes, P.M. Ram, M. Taylor, K.C. Wumkes, W. 1994, Changes in atmospheric circulation and ocean ice cover over the north Atlantic during the last 41000 a. Science 263, 1741–1751.CrossRefGoogle Scholar
Paik, I.S. Lee, Y.I. 1998, Desiccation cracks in verticpalaeosols of the Cretaceous Hasandong Formation, Korea: genesis and palaeoenvironmental implications. Sedimentary Geology 119, 161–179.Google Scholar
Porter, S.C. An, Z.S. 1995, Correlation between climate events in the North Atlantic and China during the last glaciations. Nature 375, 305–308.Google Scholar
Sun, L.G. Xie, Z.Q. Shen, X.S. Zhu, Q.S. 2000, Ancient-wood layer at Guanyin Bay in Zhujiajian, Zhejiang Province being discovered and its significance. Chinese Journal of Nature 22, 354–357(in Chinese).Google Scholar
Sun, Y.B. Clemens, S.C. Morrill, C. Lin, X.P. Wang, X.L. An, Z.S. 2011, Influence of Atlantic meridional overturning circulation on the East Asian winter monsoon. Nature Geoscience 10.1038/ngeo 1326 Google Scholar
Tang, Y.J. Jia, J.Y. Xie, X.D. 2002, Environmental significance of clay minerals. Earth Science Frontiers 9, 337–344(in Chinese with English abstract).Google Scholar
Thiry, M. 2000, Palaeoclimatic interpretation of clay minerals in marine deposits: an outlook from the continental origin. Earth-Science Reviews 49, 201–221.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. Wu, J.Y. Liu, D.B. Wu, J.Q. Cai, Y.J. Cheng, H. 2002, The abrupt changing information of H1 event of East Asia monsoon recorded by stalagmite. China Science: D 32, 227-223(in Chinese).Google Scholar
Wu, Z.J. Yuan, L.X. Jia, N. Wang, Y.H. Sun, L.G. 2009, Microbial Biomineralization of iron seepage water: implication for the iron ores formation in intertidal zone of Zhoushan Archipelago, East China Sea. Geochemical Journal 43, 167–177.CrossRefGoogle Scholar
Yang, X.Q. Li, H.M. Zhou, Y.Z. 2002, The character of magnetic susceptibility of NS93-5 sediment at the south of South China Sea and its record of global climate change. Marine Geology and Quaternary Geology 22, 31–36(in Chinese with English abstract).Google Scholar
Zhao, M. Beveridge, N.A.S. Skackleton, N.J. Sarnthein, M. Eglinton, G. 1995, Molecular Stratigraphy of cores off northwest Africa: sea surface temperature history over the last 80 ka. Paleoceanography 10, 661–675.Google Scholar