Hostname: page-component-cd9895bd7-fscjk Total loading time: 0 Render date: 2024-12-26T19:56:53.322Z Has data issue: false hasContentIssue false
  • English
  • Français

A lacustrine record of East Asian summer monsoon and atmospheric dust loading since the last interglaciation from Lake Xingkai, northeast China

Published online by Cambridge University Press:  23 October 2017

Weiwei Sun ,
Ji Shen ,
Shi-Yong Yu ,
Hao Long ,
Enlou Zhang ,
Enfeng Liu  and
Rong Chen
Weiwei Sun*
Affiliation:
State Key Laboratory of Lake Science and Environment, Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences, Nanjing 210008, China
Ji Shen*
Affiliation:
State Key Laboratory of Lake Science and Environment, Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences, Nanjing 210008, China
Shi-Yong Yu
Affiliation:
School of Geography, Geomatics, and Planning, Jiangsu Normal University, Xuzhou 221116, China
Hao Long
Affiliation:
State Key Laboratory of Lake Science and Environment, Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences, Nanjing 210008, China
Enlou Zhang
Affiliation:
State Key Laboratory of Lake Science and Environment, Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences, Nanjing 210008, China
Enfeng Liu
Affiliation:
College of Geography and Environment, Shandong Normal University, Jinan 250014, China
Rong Chen
Affiliation:
State Key Laboratory of Lake Science and Environment, Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences, Nanjing 210008, China
*
*Corresponding authors at: State Key Laboratory of Lake Science and Environment, Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences, Nanjing 210008, China. E-mail addresses: [email protected] (W. Sun), [email protected] (J. Shen).
*Corresponding authors at: State Key Laboratory of Lake Science and Environment, Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences, Nanjing 210008, China. E-mail addresses: [email protected] (W. Sun), [email protected] (J. Shen).
Get access Rights & Permissions [Opens in a new window]

Abstract

A 336-cm-long sediment core spanning the last 130 ka was recovered from Lake Xingkai on the northeastern margin of the East Asian summer monsoon domain to reveal the linkage between lacustrine depositional processes and environmental changes. Bayesian end member modeling analysis was conducted to partition and interpret the grain-size distributions of Lake Xingkai sediments. Our results suggest that the sedimentary system is characterized by three end members (EMs). EM1 and EM2, with a modal value of 13 and 10 μm, respectively, indicate the variation of local hydraulic conditions. EM3, with a modal value of 5 μm, reflects the background atmospheric dust loading. High atmospheric dust concentration generally occurred during Marine Isotope Stage (MIS) 5d, MIS 4, and early MIS 3, when the climate in the Asian dust source region was cold and dry. In contrast, low dust concentration prevailed during MIS 2, likely due to the southward shift of the westerlies driven by maximum ice volume in the high latitudes.

Keywords

Asian summer monsoonDust loadingWesterliesGrain-sizeEnd member analysisLake Xingkai
Type
Research Article
Information
Quaternary Research , Volume 89 , Issue 1: Tribute to Daniel Livingstone and Paul Colinvaux , January 2018 , pp. 270 - 280
Copyright
Copyright © University of Washington. Published by Cambridge University Press, 2017 

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

REFERENCES

An, Z., Colman, S.M., Zhou, W., Li, X., Brown, E.T., Jull, A.J.T., Cai, Y., et al 2012. Interplay between the Westerlies and Asian monsoon recorded in Lake Qinghai sediments since 32 ka. Scientific Reports 2: A619. http://dx.doi.org/10.1038/srep00619.Google Scholar
An, Z., Kukla, G.J., Porter, S.C., Xiao, J., 1991. Magnetic susceptibility evidence of monsoon variation on the Loess Plateau of central China during the last 130,000 years. Quaternary Research 36, 29–36.Google Scholar
Berger, A., Loutre, M.-F., 1991. Insolation values for the climate of the last 10 million years. Quaternary Science Reviews 10, 297–317.Google Scholar
Chen, F., Qiang, M., Zhou, A., Xiao, S., Chen, J., Sun, D., 2013. A 2000-year dust storm record from Lake Sugan in the dust source area of arid China. Journal of Geophysical Research: Atmospheres 118, 2149–2160.Google Scholar
Chen, J.A., Wan, G., Zhang, D., Zhang, F., Huang, R., 2004. Environmental records of lacustrine sediments in different time scales: sediment grain size as an example. Science in China Series D: Earth Sciences 47, 954–960.Google Scholar
Chu, G., Sun, Q., Zhaoyan, G., Rioual, P., Qiang, L., Kaijun, W., Han, J., Liu, J., 2009. Dust records from varved lacustrine sediments of two neighboring lakes in northeastern China over the last 1400 years. Quaternary International 194, 108–118.CrossRefGoogle Scholar
Dietze, E., Hartmann, K., Diekmann, B., Ijmker, J., Lehmkuhl, F., Opitz, S., Stauch, G., Wünnemann, B., Borchers, A., 2012. An end-member algorithm for deciphering modern detrital processes from lake sediments of Lake Donggi Cona, NE Tibetan Plateau, China. Sedimentary Geology 243–244, 169–180.CrossRefGoogle Scholar
Dietze, E., Maussion, F., Ahlborn, M., Diekmann, B., Hartmann, K., Henkel, K., Kasper, T., Lockot, G., Opitz, S., Haberzettl, T., 2014. Sediment transport processes across the Tibetan Plateau inferred from robust grain-size end members in lake sediments. Climate of the Past 10, 91–106.Google Scholar
Finney, B.P., Johnson, T.C., 1991. Sedimentation in Lake Malawi (East Africa) during the past 10,000 years: a continuous paleoclimatic record from the southern tropics. Palaeogeography, Palaeoclimatology, Palaeoecology 85, 351–366.Google Scholar
Jones, R.T., Cook, C.G., Zhang, E., Langdon, P.G., Jordan, J., Turney, C., 2012. Holocene environmental change at Lake Shudu, Yunnan Province, southwestern China. Hydrobiologia 693, 223–235.CrossRefGoogle Scholar
Kang, S., Roberts, H.M., Wang, X., An, Z., Wang, M., 2015. Mass accumulation rate changes in Chinese loess during MIS 2, and asynchrony with records from Greenland ice cores and North Pacific Ocean sediments during the Last Glacial Maximum. Aeolian Research 19, Part B. 251–258.Google Scholar
Kitoh, A., Murakami, S., Koide, H., 2001. A simulation of the Last Glacial Maximum with a coupled atmosphere-ocean GCM. Geophysical Research Letters 28, 2221–2224.CrossRefGoogle Scholar
Lai, Z., Mischke, S., Madsen, D., 2014. Paleoenvironmental implications of new OSL dates on the formation of the “Shell Bar” in the Qaidam Basin, northeastern Qinghai-Tibetan Plateau. Journal of Paleolimnology 51, 197–210.Google Scholar
Li, G., Jin, M., Duan, Y., Madsen, D.B., Li, F., Yang, L., Wei, H., Chen, F., 2015. Quartz and K-feldspar luminescence dating of a Marine Isotope Stage 5 megalake in the Juyanze Basin, central Gobi Desert, China. Palaeogeography, Palaeoclimatology, Palaeoecology 440, 96–109.Google Scholar
Li, G., Rao, Z., Duan, Y., Xia, D., Wang, L., Madsen, D.B., Jia, J., Wei, H., Qiang, M., Chen, J., Chen, F., 2016. Paleoenvironmental changes recorded in a luminescence dated loess/paleosol sequence from the Tianshan Mountains, arid central Asia, since the Penultimate Glaciation. Earth and Planetary Science Letters 448, 1–12.CrossRefGoogle Scholar
Lim, J., Matsumoto, E., 2006. Bimodal grain-size distribution of aeolian quartz in a maar of Cheju Island, Korea, during the last 6500 years: its flux variation and controlling factor. Geophysical Research Letters 33, L21816. http://dx.doi.org/10.1029/2006GL027432.CrossRefGoogle Scholar
Liu, X., Dong, H., Yang, X., Herzschuh, U., Zhang, E., Stuut, J.-B.W., Wang, Y., 2009. Late Holocene forcing of the Asian winter and summer monsoon as evidenced by proxy records from the northern Qinghai–Tibetan Plateau. Earth and Planetary Science Letters 280, 276–284.CrossRefGoogle Scholar
Long, H., Lai, Z., Fuchs, M., Zhang, J., Li, Y., 2012. Timing of Late Quaternary palaeolake evolution in Tengger Desert of northern China and its possible forcing mechanisms. Global and Planetary Change 92–93, 119–129.Google Scholar
Long, H., Shen, J., 2017. Sandy beach ridges from Xingkai Lake (NE Asia): Timing and response to palaeoclimate. Quaternary International 430 (B), 21–31.Google Scholar
Long, H., Shen, J., Wang, Y., Gao, L., Frechen, M., 2015. High-resolution OSL dating of a late Quaternary sequence from Xingkai Lake (NE Asia): chronological challenge of the “MIS 3a Mega-paleolake” hypothesis in China. Earth and Planetary Science Letters 428, 281–292.Google Scholar
Lu, H., Yi, S., Xu, Z., Zhou, Y., Zeng, L., Zhu, F., Feng, H., et al 2013. Chinese deserts and sand fields in Last Glacial Maximum and Holocene Optimum. Chinese Science Bulletin 58, 2775–2783.CrossRefGoogle Scholar
Maher, B.A., Prospero, J.M., Mackie, D., Gaiero, D., Hesse, P.P., Balkanski, Y., 2010. Global connections between aeolian dust, climate and ocean biogeochemistry at the present day and at the last glacial maximum. Earth-Science Reviews 99, 61–97.Google Scholar
Middleton, N.J., Sternberg, T., 2013. Climate hazards in drylands: a review. Earth-Science Reviews 126, 48–57.Google Scholar
Nagashima, K., Tada, R., Matsui, H., Irino, T., Tani, A., Toyoda, S., 2007. Orbital- and millennial-scale variations in Asian dust transport path to the Japan Sea. Palaeogeography, Palaeoclimatology, Palaeoecology 247, 144–161.Google Scholar
Peng, Y., Xiao, J., Nakamura, T., Liu, B., Inouchi, Y., 2005. Holocene East Asian monsoonal precipitation pattern revealed by grain-size distribution of core sediments of Daihai Lake in Inner Mongolia of north-central China. Earth and Planetary Science Letters 233, 467–479.Google Scholar
Pigati, J.S., Quade, J., Wilson, J., Jull, A.J.T., Lifton, N.A., 2007. Development of low-background vacuum extraction and graphitization systems for 14C dating of old (40–60 ka) samples. Quaternary International 166, 4–14.Google Scholar
Porter, S.C., An, Z., 1995. Correlation between climate events in the North-Atlantic and China during last glaciation. Nature 375, 305–308.Google Scholar
Rades, E.F., Hetzel, R., Xu, Q., Ding, L., 2013. Constraining Holocene lake-level highstands on the Tibetan plateau by 10Be exposure dating: a case study at Tangra Yumco, southern Tibet. Quaternary Science Reviews 82, 68–77.CrossRefGoogle Scholar
Rea, D.K., Hovan, S.A., 1995. Grain size distribution and depositional processes of the mineral component of abyssal sediments: Lessons from the North Pacific. Paleoceanography 10, 251–258.Google Scholar
Schiemann, R., Lüthi, D., Schär, C., 2009. Seasonality and interannual variability of the westerly jet in the Tibetan Plateau region. Journal of Climate 22, 2940–2957.Google Scholar
Serno, S., Winckler, G., Anderson, R.F., Hayes, C.T., McGee, D., Machalett, B., Ren, H., Straub, S.M., Gersonde, R., Haug, G.H., 2014. Eolian dust input to the Subarctic North Pacific. Earth and Planetary Science Letters 387, 252–263.Google Scholar
Shen, J., 2013. Spatiotemporal variations of Chinese lakes and their driving mechanisms since the Last Glacial Maximum: a review and synthesis of lacustrine sediment archives. Chinese Science Bulletin 58, 17–31.CrossRefGoogle Scholar
Steffensen, J.P., 1997. The size distribution of microparticles from selected segments of the Greenland Ice Core Project ice core representing different climatic periods. Journal of Geophysical Research: Oceans 102, 26755–26763.CrossRefGoogle Scholar
Sun, D., 2004. Monsoon and westerly circulation changes recorded in the late Cenozoic aeolian sequences of Northern China. Global and Planetary Change 41, 63–80.Google Scholar
Sun, D., Bloemendal, J., Rea, D.K., Vandenberghe, J., Jiang, F., An, Z., Su, R., 2002. Grain-size distribution function of polymodal sediments in hydraulic and aeolian environments, and numerical partitioning of the sedimentary components. Sedimentary Geology 152, 263–277.Google Scholar
Sun, D., Su, R., Bloemendal, J., Lu, H., 2008. Grain-size and accumulation rate records from Late Cenozoic aeolian sequences in northern China: implications for variations in the East Asian winter monsoon and westerly atmospheric circulation. Palaeogeography, Palaeoclimatology, Palaeoecology 264, 39–53.Google Scholar
Sun, Y., An, Z., 2005. Late Pliocene-Pleistocene changes in mass accumulation rates of eolian deposits on the central Chinese Loess Plateau. Journal of Geophysical Research: Atmospheres 110, D23101. http://dx.doi.org/10.1029/2005JD006064.CrossRefGoogle Scholar
Sun, Y., Clemens, S.C., Morrill, C., Lin, X., Wang, X., An, Z., 2012. Influence of Atlantic meridional overturning circulation on the East Asian winter monsoon. Nature Geoscience 5, 46–49.Google Scholar
Thomas, D.S.G., Bailey, R., Shaw, P.A., Durcan, J.A., Singarayer, J.S., 2009. Late Quaternary highstands at Lake Chilwa, Malawi: frequency, timing and possible forcing mechanisms in the last 44 ka. Quaternary Science Reviews 28, 526–539.Google Scholar
Tsoar, H., Pye, K., 1987. Dust transport and the question of desert loess formation. Sedimentology 34, 139–153.Google Scholar
Uno, I., Eguchi, K., Yumimoto, K., Takemura, T., Shimizu, A., Uematsu, M., Liu, Z., Wang, Z., Hara, Y., Sugimoto, N., 2009. Asian dust transported one full circuit around the globe. Nature Geoscience 2, 557–560.Google Scholar
Waelbroeck, C., Labeyrie, L., Michel, E., Duplessy, J.C., McManus, J.F., Lambeck, K., Balbon, E., Labracherie, M., 2002. Sea-level and deep water temperature changes derived from benthic foraminifera isotopic records. Quaternary Science Reviews 21, 295–305.Google Scholar
Wan, B., Zhong, Y., 1997. Features analysis and divisions of new tectonic movement in northeast China. [In Chinese.] Seismological Research of Northeast China 13, 64–75.Google Scholar
Wang, P.X., Wang, B., Cheng, H., Fasullo, J., Guo, Z.T., Kiefer, T., Liu, Z.Y., 2014. The global monsoon across timescales: coherent variability of regional monsoons. Climate of the Past 10, 2007–2052.Google Scholar
Wang, Y., Cheng, H., Edwards, R.L., Kong, X., Shao, X., Chen, S., Wu, J., Jiang, X., Wang, X., An, Z., 2008. Millennial- and orbital-scale changes in the East Asian monsoon over the past 224,000 years. Nature 451, 1090–1093.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, 2345–2348.CrossRefGoogle ScholarPubMed
Williams, D.F., Kuzmin, M.I., Prokopenko, A.A., Karabanov, E.B., Khursevich, G.K., Bezrukova, E.V., 2001. The Lake Baikal drilling project in the context of a global lake drilling initiative. Quaternary International 80–81, 3–18.Google Scholar
Wu, J., Shen, J., 2009. Paleoenvironmental and paleoclimatic changes reflected by diffuse reflectance spectroscopy and magnetic susceptibility from Xingkai Lake sediments. [In Chinese.] Marine. Geology and Quaternary Geology 29, 123–131.Google Scholar
Wu, J., Shen, J., 2010a. Paleoclimate evolution since 27.7 ka BP reflected by grain size variation of a sediment core from Lake Xingkai, northeastern Asia. [In Chinese.] Journal of Lake Science 22, 110–118.Google Scholar
Wu, J., Shen, J., 2010b. Paleoenvironmental and paleoclimatic changes in Lake Xingkai inferred from stable carbon and nitrogen isotopes of bulk organic matter since 28 ka BP. [In Chinese.] Acta Sedimentologica Sinica 28, 365–372.Google Scholar
Xiao, J., Chang, Z., Fan, J., Zhou, L., Zhai, D., Wen, R., Qin, X., 2012. The link between grain-size components and depositional processes in a modern clastic lake. Sedimentology 59, 1050–1062.Google Scholar
Xiao, J., Chang, Z., Si, B., Qin, X., Itoh, S., Lomtatidze, Z., 2009. Partitioning of the grain-size components of Dali Lake core sediments: evidence for lake-level changes during the Holocene. Journal of Paleolimnology 42, 249–260.Google Scholar
Xiao, J., Fan, J., Zhou, L., Zhai, D., Wen, R., Qin, X., 2013. A model for linking grain-size component to lake level status of a modern clastic lake. Journal of Asian Earth Sciences 69, 149–158.Google Scholar
Xiao, J., Si, B., Zhai, D., Itoh, S., Lomtatidze, Z., 2008. Hydrology of Dali Lake in central-eastern Inner Mongolia and Holocene East Asian monsoon variability. Journal of Paleolimnology 40, 519–528.Google Scholar
Xiao, J.L., An, Z.S., Liu, T.S., Inouchi, Y., Kumai, H., Yoshikawa, S., Kondo, Y., 1999. East Asian monsoon variation during the last 130,000 Years: evidence from the Loess Plateau of central China and Lake Biwa of Japan. Quaternary Science Reviews 18, 147–157.CrossRefGoogle Scholar
Xie, Y., Chi, Y., Meng, J., Guo, L., Wang, Y., 2015. Grain-size and Sr–Nd isotopic compositions of dry- and wet-deposited dusts during the same dust-storm event in Harbin, China: implications for source, transport–deposition modes, dynamic mechanism and formation of aeolian loess. Environmental Earth Sciences 74, 6489–6502.Google Scholar
Yang, L.-R., Yue, L.-P., Li, Z.-P., 2008. The influence of dry lakebeds, degraded sandy grasslands and abandoned farmland in the arid inlands of northern China on the grain size distribution of East Asian aeolian dust. Environmental Geology 53, 1767–1775.CrossRefGoogle Scholar
Yi, S., Buylaert, J.-P., Murray, A.S., Thiel, C., Zeng, L., Lu, H., 2015. High resolution OSL and post-IR IRSL dating of the last interglacial–glacial cycle at the Sanbahuo loess site (northeastern China). Quaternary Geochronology 30, Part B. 200–206.CrossRefGoogle Scholar
Yin, J., Fang, X., Su, Y., 2016. Correlation between climate and grain harvest fluctuations and the dynastic transitions and prosperity in China over the past two millennia. The Holocene 26, 1914–1923.CrossRefGoogle Scholar
Yu, S.-Y., Colman, S.M., Li, L., 2016. BEMMA: A hierarchical Bayesian end-member modeling analysis of sediment grain-size distributions. Mathematical Geosciences 48, 723–741.Google Scholar
Zhu, Y., Shen, J., Lei, G., Wang, Y., 2011. Environmental evolution of Xingkai (Khanka) Lake since 200 ka by OSL dating of sand hills. Chinese Science Bulletin 56, 2604–2612.Google Scholar