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Late Quaternary lake-level and climate changes in arid central Asia inferred from sediments of Ebinur Lake, Xinjiang, northwestern China

Published online by Cambridge University Press:  24 June 2019

Jianchao Zhou ,
Jinglu Wu ,
Long Ma  and
Mingrui Qiang
Jianchao Zhou
Affiliation:
State Key Laboratory of Lake Science and Environment, Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences, Nanjing 210008, People's Republic of China University of Chinese Academy of Sciences, Beijing 100049, People's Republic of China
Jinglu Wu*
Affiliation:
State Key Laboratory of Lake Science and Environment, Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences, Nanjing 210008, People's Republic of China Research center for Ecology and Environment of Central Asia, Chinese Academy of Sciences, Urumqi 830011, People's Republic of China
Long Ma
Affiliation:
State Key Laboratory of Desert and Oasis Ecology, Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, Urumqi 830011, People's Republic of China
Mingrui Qiang
Affiliation:
School of Geography, South China Normal University, Guangzhou 510631, People's Republic of China
*
*Corresponding author at: State Key Laboratory of Lake Science and Environment, Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences, Nanjing 210008, People's Republic of China. E-mail address: [email protected] (J. Wu).
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Abstract

Arid central Asia plays an important role in global climate dynamics, but large uncertainties remain in our understanding of the region's hydroclimate variability during the Late Quaternary. Here we present a new, high-resolution record of lacustrine sediment grain-size and element chemistry from Ebinur Lake, which was used to infer lake conditions and related climate changes in the study region between ca. 39.2 and 3.6 ka. End-member modeling analysis of grain-size data and PCA of elemental data show that lake level fluctuated dramatically from 39.2 to 34.0 ka. Subsequently, Ebinur Lake experienced a high stand from 34.0 to 28.0 ka, under humid climate conditions. The subsequent period, from 28.0 to 12.0 ka, was characterized by lake regression under dry climate conditions, whereas afterward (12.0–3.6 ka), considerably higher lake levels and humid conditions again prevailed. Millennial-scale abrupt climate changes, such as Heinrich events (H3 and H1) and the Younger Dryas, which are documented in the North Atlantic region, are also detected in the sediment record from Ebinur Lake. Comparisons with other sediment records from arid central Asia generally support the claim that climate change in this region was influenced mainly by variations in North Atlantic sea surface temperatures, through the westerlies.

Keywords

Lake levelClimate changeArid central AsiaGrain sizeElemental compositionEbinur Lake
Type
Research Article
Information
Quaternary Research , Volume 92 , Issue 2 , September 2019 , pp. 416 - 429
Copyright
Copyright © University of Washington. Published by Cambridge University Press, 2019 

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References

REFERENCES

Albéric, P., Jézéquel, D., Bergonzini, L., Chapron, E., Viollier, E., Massault, M., Michard, G., 2013. Carbon cycling and organic radiocarbon reservoir effect in a meromictic crater lake (Lac Pavin, Puy-de-Dôme, France). Radiocarbon 55, 1029–1042.Google Scholar
An, C.B., Zhao, J.J., Tao, S.C., Lv, Y.B., Dong, W.M., Li, H., Jin, M., Wang, Z.L., 2011. Dust variation recorded by lacustrine sediments from arid Central Asia since ~15 cal ka BP and its implication for atmospheric circulation. Quaternary Research 75, 566–573.Google Scholar
An, Z.S., Colman, S.M., Zhou, W.J., Li, X.Q., Brown, E.T., Jull, A.J.T., Cai, Y.J, et al. , 2012. Interplay between the westerlies and Asian monsoon recorded in Lake Qinghai sediments since 32 ka. Scientific Reports 2, 1–7.Google Scholar
Bard, E., 2002. Climate shock: abrupt changes over millennial time scales. Physics Today 55, 32–38.Google Scholar
Bigg, G.R., Levine, R.C., Green, C.L., 2011. Modelling abrupt glacial North Atlantic freshening: rates of change and their implications for Heinrich events. Global and Planetary Change 79, 176–192.Google Scholar
Blyakharchuk, T.A., Wright, H.E., Borodavko, P.S., Knaap, W.O.V.D., Ammann, B., 2004. Late glacial and Holocene vegetational changes on the Ulagan high-mountain plateau, Altai Mountains, southern Siberia. Palaeogeography, Palaeoclimatology, Palaeoecology 209, 259–279.Google Scholar
Boomer, I., Aladin, N., Plotnikov, I., Whatley, R., 2000. The palaeolimnology of the Aral Sea: a review. Quaternary Science Reviews 19, 1259–1278.Google Scholar
Bøtter-Jensen, L., Thomsen, K.J., Jain, M., 2010. Review of optically stimulated luminescence (OSL) instrumental developments for retrospective dosimetry. Radiation Measurements 45, 253–257.Google Scholar
Bouchez, J., Gaillardet, J., France-Lanord, C., Maurice, L., Dutra-Maia, P., 2011. Grain size control of river suspended sediment geochemistry: clues from Amazon River depth profiles. Geochemistry, Geophysics, Geosystems 12, 1–24.Google Scholar
Cai, Y.J., Chiang, J.C.H., Breitenbach, S.F.M., Tan, L.C., Cheng, H., Edwards, R.L., An, Z.S, 2017. Holocene moisture changes in western China, Central Asia, inferred from stalagmites. Quaternary Science Reviews 158, 15–28.Google Scholar
Chen, F.H., Yu, Z.C., Yang, M.L., Ito, E., Wang, S.M., Madsen, D.B., Huang, X.Z., et al. , 2008. Holocene moisture evolution in arid central Asia and its out-of-phase relationship with Asian monsoon history. Quaternary Science Reviews 27, 351–364.Google Scholar
Colman, S.M., Rosenbaum, J.G., Kaufman, D.S., Dean, W.E., McGeehin, J.P., 2009. Radiocarbon ages and age models for the past 30,000 years in Bear Lake, Utah and Idaho. Geological Society of America, Special Papers 450, 133–144.Google Scholar
Dietze, M., Dietze, E., 2013. EMMAgeo: End-Member Modelling Algorithm and Supporting Functions for Grain-Size Analysis. R package version 0.9.0. http://CRAN.Rproject.org/package=EMMAgeo (accessed 10.09.2014).Google 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, 169–180.Google Scholar
Duller, G., 2003. Distinguishing quartz and feldspar in single grain luminescence measurements. Radiation Measurements 37, 161–165.Google Scholar
Grunert, J., Lehmkuhl, F., Walther, M., 2000. Paleoclimatic evolution of the Uvs Nuur basin and adjacent areas (western Mongolia). Quaternary International 65–66, 171–192.Google Scholar
Grygar, T.M., Mach, K., Schnabl, P., Pruner, P., Laurin, J., Martinez, M., 2014. A lacustrine record of the early stage of the Miocene Climatic Optimum in central Europe from the Most Basin, Ohře (Eger) Graben, Czech Republic. Geological Magazine 151, 1013–1033.Google Scholar
Hemming, S.R., 2004. Heinrich events: massive late Pleistocene detritus layers of the North Atlantic and their global climate imprint. Reviews of Geophysics 42, 1–43.Google Scholar
Herzschuh, U., Zhang, C.J., Mischke, S., Herzschuh, R., Mohammadi, F., Mingram, B., Kürschner, H., Riedel, F., 2005. A late Quaternary lake record from the Qilian Mountains (NW China): evolution of the primary production and the water depth reconstructed from macrofossil, pollen, biomarker, and isotope data. Global and Planetary Change 46, 361–379.Google Scholar
Jiang, D.B., Lang, X.M., Tian, Z.P., Guo, D.L., 2011. Last glacial maximum climate over China from PMIP simulations. Palaeogeography, Palaeoclimatology, Palaeoecology 309, 347–357.Google Scholar
Kislov, A.V., Panin, A., Toropov, P., 2014. Current status and palaeostages of the Caspian Sea as a potential evaluation tool for climate model simulations. Quaternary International 345, 48–55.Google Scholar
Lai, Z.P., 2010. Chronology and the upper dating limit for loess samples from Luochuan section in the Chinese Loess Plateau using quartz OSL SAR protocol. Journal of Asian Earth Sciences 37, 176–185.Google Scholar
Li, X.Q., Zhao, K.L., Dodson, J., Zhou, X.Y., 2011. Moisture dynamics in central Asia for the last 15 kyr: new evidence from Yili Valley, Xinjiang, NW China. Quaternary Science Reviews 30, 3457–3466.Google Scholar
Li, Y., Morrill, C., 2013. Lake levels in Asia at the Last Glacial Maximum as indicators of hydrologic sensitivity to greenhouse gas concentrations. Quaternary Science Reviews 60, 1–12.Google Scholar
Li, Y., Song, Y.G., Lai, Z.P., Han, L., An, Z.S., 2016. Rapid and cyclic dust accumulation during MIS 2 in Central Asia inferred from loess OSL dating and grain-size analysis. Scientific Reports 6, 32365.Google Scholar
Liu, C.L., Zhang, J.F., Jiao, P.C., Mischke, S., 2016. The Holocene history of Lop Nur and its palaeoclimate implications. Quaternary Science Reviews 148, 163–175.Google Scholar
Liu, W., Wu, J.L., Ma, L., Zeng, H.A., 2014. A 200-year sediment record of environmental change from Lake Sayram, Tianshan Mountains in China. GFF 136, 548–555.Google Scholar
Liu, X.Q., Herzschuh, U., Shen, J., Jiang, Q.F., Xiao, X.Y., 2008. Holocene environmental and climatic changes inferred from Wulungu Lake in northern Xinjiang, China. Quaternary Research 70, 412–425.Google Scholar
Lockot, G., Ramisch, A., Wünnemann, B., Hartmann, K., Haberzettl, T., Chen, H., Diekmann, B., 2015. A process-and provenance-based attempt to unravel inconsistent radiocarbon chronologies in lake sediments: an example from Lake Heihai, north Tibetan Plateau (China). Radiocarbon 57, 1003–1019.Google Scholar
Long, H., Lai, Z.P., Wang, N.A., Zhang, J.R., 2011. A combined luminescence and radiocarbon dating study of Holocene lacustrine sediments from arid northern China. Quaternary Geochronology 6, 1–9.Google Scholar
Long, H., Shen, J., 2015. Underestimated 14C-based chronology of late Pleistocene high lake-level events over the Tibetan Plateau and adjacent areas: evidence from the Qaidam Basin and Tengger Desert. Science China: Earth Sciences 58, 183–194.Google Scholar
Ma, L., Wu, J.L., Abuduwaili, J., Liu, W., 2016. Geochemical responses to anthropogenic and natural influences in Ebinur Lake sediments of arid northwest China. PLoS ONE 11, e0155819.Google Scholar
Murray, A.S., Wintle, A.G., 2003. The single aliquot regenerative dose protocol: potential for improvements in reliability. Radiation Measurements 37, 377–381.Google Scholar
Narisma, G.T., Foley, J.A., Licker, R., Ramankutty, N., 2007. Abrupt changes in rainfall during the twentieth century. Geophysical Research Letters 34, 306–316.Google Scholar
North Greenland Ice Core 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
Qiang, M.R., Chen, F.H., Zhang, J.W., Zu, R.P., Jin, M., Zhou, A.F., Xiao, S., 2007. Grain size in sediments from Lake Sugan: a possible linkage to dust storm events at the northern margin of the Qinghai–Tibetan Plateau. Environmental Geology 51, 1229–1238.Google Scholar
Quiroz-Jimenez, J.D, Roy, P.D, Lozano-Santacruz, R., Giron-García, P., 2017. Hydrological responses of the Chihuahua Desert of Mexico to possible Heinrich Stadials. Journal of South American Earth Sciences 73, 1–9.Google Scholar
Reimer, P.J., Baillie, M.G.L., Bard, E., Bayliss, A., Beck, J.W., Blackwell, P.G., Bronk Ramsey, C., et al. , 2013. IntCal13 and Marine13 radiocarbon age calibration curves 0–50,000 years cal BP. Radiocarbon 55, 1869–1887.Google Scholar
Rhodes, T.E., Gasse, F., Lin, R.F., Fontes, J.C., Wei, K.Q., Bertrand, P., Gibert, E., et al. , 1996. A late Pleistocene-Holocene lacustrine record from Lake Manas, Zunggar (northern Xinjiang, western China). Palaeogeography, Palaeoclimatology, Palaeoecology 120, 105–121.Google Scholar
Ricketts, R.D., Johnson, T.C., Brown, E.T., Rasmussen, K.A., Romanovsky, V.V., 2001. The Holocene paleolimnology of Lake Issyk-Kul, Kyrgyzstan: trace element and stable isotope composition of ostracodes. Palaeogeography, Palaeoclimatology, Palaeoecology 176, 207–227.Google Scholar
Shi, Y.F., Yu, G., Liu, X.Q., Li, B.Y., Yao, T.D., 2001. Reconstruction of the 30–40 ka BP enhanced Indian monsoon climate based on geological records from the Tibetan Plateau. Palaeogeography, Palaeoclimatology, Palaeoecology 169, 69–83.Google Scholar
Song, Y.G., Zeng, M.X., Chen, X.L., Li, Y., Chang, H., An, Z.S., 2018. Abrupt climatic events recorded by the Ili loess during the last glaciation in Central Asia: evidence from grain-size and minerals. Journal of Asian Earth Sciences 155, 58–67.Google Scholar
Sorg, A., Bolch, T., Stoffel, M., Solomina, O., Beniston, M., 2012. Climate change impacts on glaciers and runoff in Tien Shan (Central Asia). Nature Climate Change 2, 725–731.Google Scholar
Stockhecke, M., Timmermann, A., Kipfer, R., Haug, G.H., Kwiecien, O., Friedrich, T., Menviel, L., Litt, T., Pickarski, N., Anselmetti, F.S., 2016. Millennial to orbital-scale variations of drought intensity in the eastern Mediterranean. Quaternary Science Reviews 133, 77–95.Google Scholar
Tjallingii, R., Röhl, U., Kölling, M., Bickert, T., 2007. Influence of the water content on X-ray fluorescence core-scanning measurements in soft marine sediments. Geochemistry, Geophysics, Geosystems 8, 1–12.Google Scholar
Tudryn, A., Tucholka, P., Gibert, E., Gasse, F., Wei, K., 2010. A late Pleistocene and Holocene mineral magnetic record from sediments of Lake Aibi, Dzungarian Basin, NW China. Journal of Paleolimnology 44, 109–121.Google Scholar
Wu, J.L., Shen, J., Wang, S.M., Jin, Z.D., Yang, X.D., 2005. Characteristics of an early Holocene climate and environment from lake sediments in Ebinur region, NW China. Science China: Earth Sciences 48, 258–265.Google Scholar
Wu, J.L., Wang, S.M., Wu, Y.H., 1996. The Holocene sedimental characteristic and paleoclimatic evolution of Ebinur Lake, Xinjiang. Chinese Geographical Science 6, 78–88.Google Scholar
Wu, J.L., Yu, Z.C., Zeng, H.A., Wang, N.L., 2009. Possible solar forcing of 400-year wet-dry climate cycles in northwestern China. Climatic Change 96, 473–482.Google Scholar
Xiao, J.L., Zhang, S.R., Fan, J.W., Wen, R.L., Zhai, D.Y., Tian, Z.P., Jiang, D.B., 2018. The 4.2 ka event: multi-proxy records from a closed lake in the northern margin of the East Asian summer monsoon. Climate of the Past 14, 1417–1425.Google Scholar
Xiao, X.Y., Haberle, S.G., Shen, J., Yang, X.D., Han, Y., Zhang, E.L., Wang, S.M., 2014. Latest Pleistocene and Holocene vegetation and climate history inferred from an alpine lacustrine record, northwestern Yunnan Province, southwestern China. Quaternary Science Reviews 86, 35–48.Google Scholar
Yang, X.P., Preusser, F., Radtke, U., 2006. Late Quaternary environmental changes in the Taklamakan Desert, western China, inferred from OSL-dated lacustrine and aeolian deposits. Quaternary Science Review 25, 923–932.Google Scholar
Yang, X.P., Scuderi, L.A., 2010. Hydrological and climatic changes in deserts of China since the late Pleistocene. Quaternary Research 73, 1–9.Google Scholar
Yang, X.P., Wang, X.L., Liu, Z.T., Li, H.W., Ren, X.Z., Zhang, D.G., Ma, Z.B., Rioual, P., Jin, X.D., Scuderi, L., 2013. Initiation and variation of the dune fields in semi-arid China – with a special reference to the Hunshandake Sandy Land, Inner Mongolia. Quaternary Science Reviews 78, 369–380.Google Scholar
Zhang, H.C., Wünnemann, B., Ma, Y.Z., Peng, J.L., Pachur, H.J., Li, J.J., Qi, Y., Chen, G.J., Fang, H.B., Feng, Z.D., 2002. Lake level and climate changes between 42,000 and 18,000 14C yr B.P. in the Tengger Desert, northwestern China. Quaternary Research 58, 62–72.Google Scholar
Zhao, Y.T., An, C.B., Mao, L.M., Zhao, J.J., Tang, L.Y., Zhou, A.F., Li, Y., Dong, W.M., Duan, F.T., Chen, F.H., 2015. Vegetation and climate history in arid western China during MIS 2: new insights from pollen and grain-size data of the Balikun Lake, eastern Tien Shan. Quaternary Science Reviews 126, 112–125.Google Scholar
Zhou, W.J., Liu, T.B., Wang, H., An, Z.S., Cheng, P., Zhu, Y.Z., Burr, G.S., 2016. Geological record of meltwater events at Qinghai Lake, China from the past 40 ka. Quaternary Science Reviews 149, 279–287.Google Scholar