Holocene climatic change reconstructed from trace elements of an aeolian deposit in the southeastern Mu Us Desert, northern China

doi:10.3724/SP.J.1226.2019.00126.

Abstract

Abstract:

In semi-arid and arid desert regions of northern China, aeolian deposits document the framework variation of an Asian monsoon during the late Quaternary. However, there is still a lack of detailed data pertaining to Holocene Asian monsoonal variation especial in the modern Asian summer monsoonal boundary belt. In this study, we reconstructed Holocene millennial-scale climatic changes in the Mu Us Desert, northern China, through systematic analysis of the variation of trace elements (324 samples) in different lithological units of the palaeosol-aeolian sand deposit, in combination with ¹⁴C and OSL chronology. Statistical results, correlation and clustering analysis indicate that the high content of 11 trace elements (V, Y, Cr, Nb, P, Mn, Cu, Zr, As, Ni and Rb, represented by P) and lower Sr content corresponding to periods of palaeosol development, marked increase of vegetation, weathering degree, and enhanced Asian summer monsoonal strength. In contrast, their opposed variation are coincident with accumulated aeolian sand layers, implying weaker summer monsoons and less geochemical weathering and degraded vegetation. These associations can be considered as signaling regional humid and dry changes of the Holocene environment. Accordingly, relatively arid conditions dominated the region before 7.2 ka, and there was an optimal humid climate in 7.2?4.6 ka. Afterwards, the climate became obviously dry, accompanied with several cycles of relatively wet and dry, such as relatively wet intervals around 4.1?3.7 ka, 3.5?3.3 ka and 2.5 ka. In addition, six millennial-scale dry events were recorded, and these events were consistent with weaker Asian summer monsoonal intervals in low latitudes, declined palaeosol development and precipitation in middle latitudes, as well as increased winter monsoon and periodic ice-rafting events in high latitudes of the Northern Hemisphere, within limits of accuracy of existing dating ages. This possibly suggests a noteworthy synchronism between millennial-scale climatic changes in this region and on a global scale.

Key words: Holocene climatic change, Mu Us Desert, Aeolian deposit, trace element, synchronism

Bing Liu,HeLing Jin,LiangYing Sun,WenPing Xue,ZhenYu Liu. Holocene climatic change reconstructed from trace elements of an aeolian deposit in the southeastern Mu Us Desert, northern China[J].Sciences in Cold and Arid Regions, 2019, 11(2): 126-138.

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References 0

	An ZS, 2000. The history and variability of the East Asian paleomonsoon climate. Quaternary Science Reviews, 191: 171−187. DOI: 10.1016/S0277-3791(99)00060-8. doi: 10.1016/S0277-3791(99)00060-8
	Bianchi GG , McCave IN , 1999. Holocene periodicity in North Atlantic climate and deep-ocean flow south of Iceland. Nature, 397: 513−515. DOI: 10.1038/17362. doi: 10.1038/17362
	Bond G , Kromer B , Beer J , et al . , 2001. Persistent solar influence on north Atlantic climate during the Holocene. Science, 294: 2130−2136. DOI: 10.1126/science.1065680. doi: 10.1126/science.1065680
	Chen FH , Xu QH , Chen JH , et al . , 2015. East Asian summer monsoon precipitation variability since the last deglaciation. Scientific Reports, 5: 11186. DOI: 10.1038/srep11186. doi: 10.1038/srep11186
	Chen FH , Zhu Y , Li JJ , et al . , 2001. Abrupt Holocene changes of the Asian monsoon at millennial-and centennial-scales: Evidence from lake sediment document in Minqin Basin, north China. Chinese Science Bulletin, 46: 1942−1947. DOI: 10.1007/BF02901902. doi: 10.1007/BF02901902
	Chen J , An ZS , Wang YJ , et al . , 1999, Distribution of Rb and Sr in the Luochuan loess-paleosol sequence of China during the last 800 ka: Implications for paleomonsoon variations. Science in China: (Series D), 42(3): 225−232. DOI: 10.1007/BF02878959. doi: 10.1007/BF02878959
	Chen WN , Gao SY , Shao YJ , et al . , 1994. Holocene pollen assemblage and climatic change in the Mu Us sand sea. Journal of Chinese Historical Geography, 1: 39−54. DOI: https://doi.org/10.1007/BF02878959. doi: 10.1007/BF02878959
	Chen WN , Gao SY , Sun Z , 1993. On the Holocene geochemical landscape characteristics and its palaeoclimatic meaning, Mu Us sand sea. Journal of Desert Research, 14(1): 22−30. (in Chinese)
	Dong GR , Gao SY , Jin J , 1993. Desertification and Its Control in Gonghe Basin of Qinghai Province. Beijing,China: Science Press. (in Chinese)
	Du SH , Li BS , Chen MH , et al . , 2012. Kiloyear-scale climate events and evolution during the Last Interglacial, Mu Us Desert, China. Quaternary International, 263: 63−70. DOI: 10.1016/j.quaint.2012.01.004. doi: 10.1016/j.quaint.2012.01.004
	Gao SY , Cheng WN , Jin HL , et al . , 1993. Preliminary study on the desert changes at the northwest edge of China. Science in China (Series B), 23(2): 203−208. (in Chinese)
	Guo LL , Feng ZD , Li XQ , et al . , 2007. Holocene climatic and environmental changes recorded in BaaharNuur Lake core in the Ordos Plateau, Inner Mongolia of China. Chinese Science Bulletin, 52(7): 959−966. DOI: 982006-1191. doi: 982006-1191
	Guo ZT , Nicole PM , Kropelin S , 2000. Holocene non-orbital climatic events in present-day arid area of northern Africa and China. Global and Planetary Change, 26: 97−103. DOI: 10.1016/S0921-8181(00)00037-0. doi: 10.1016/S0921-8181(00)00037-0
	Gupta AK , Anderson DM , Overpeck JT , 2003. Abrupt changes in the Asian southwest monsoon during the Holocene and their links to the Atlantic Ocean. Nature, 421: 354−357. DOI: https://doi.org/10.1038/nature01340. doi: 10.1038/nature01340
	Hong YT , Hong B , Lin QH , et al . , 2003. Correlation between Indian Ocean summer monsoon and North Atlantic climate during the Holocene. Earth and Planetary Science Letters, 211: 371−380. DOI: 10.1016/s0012-821x(03)00207-3. doi: 10.1016/s0012-821x(03)00207-3
	Hu CY , Henderson GM , Huang J , et al . , 2008. Quantification of Holocene Asian monsoon rainfall from spatially separated cave records. Earth and Planetary Science Letters, 266: 221−232. DOI: 10.1016/j.epsl.2007.10.015. doi: 10.1016/j.epsl.2007.10.015
	Huang CQ , Feng ZD , Ma YZ , et al . , 2009. Holocene palaeoenvironmental changes recorded by pollen of the BaharNuur Lake. Journal of Lanzhou University (Natural Sciences), 45(4): 7−12. DOI: 10.1016/j.epsl.2007.10.015. (in Chinese) doi: 10.1016/j.epsl.2007.10.015
	Huang F , Lisa K , Xiong SF , et al . , 2004. Holocene grassland vegetation, climate and human impact in central eastern Inner Mongolia. Science in China (Series D), 48(7): 1025−1039. DOI: 10.1360/03yd0165. doi: 10.1360/03yd0165
	Jia FF , Lu RJ , Gao SY , et al . , 2015. Holocene aeolian activities in the southeastern Mu Us Desert, China. Aeolian Research, 19: 267−274. DOI: 10.1016/j.aeolia.2015.01.002. doi: 10.1016/j.aeolia.2015.01.002
	Jin HL , Dong GR , Su ZZ , et al . , 2001. Reconstruction of the spatial patterns of desert/loess boundary belt in north China during the Holocene. Chinese Science Bulletin, 12: 969−974. DOI: 10.1007/BF03183538. doi: 10.1007/BF03183538
	Jin HL , Sun LY , Sun Z , 2010. Millennial-scale evolution of Hunshandake Desert and climate change during the Holocene in Inner Mongolia, northern China. Sciences in Cold and Arid Regions, 2(6): 505−513. DOI: 10.3724/SP.J. 1226.2010.00505. doi: 10.3724/SP.J. 1226.2010.00505
	Li XQ , Zhou WJ , An ZS , et al . , 2003. The vegetation and monsoon variations at the desert-loess transition belt at Midiwan in northern China for the last 13 ka. The Holocene, 13: 779−784. DOI: 10.1191/0959683603hl664rr. doi: 10.1191/0959683603hl664rr
	Li ZP , Yue LP , Guo L , et al . , 2007. Holocene climatic change and desertification in northern China. Northwest Geology, 40(3): 1−29. (in Chinese)
	Linsley BK, 1996. Oxygen-isotope record of sea level and climate variations in the Sulu Sea over the past 150,000 years. Nature, 380: 234−237. DOI: 10.1038/380234a0. doi: 10.1038/380234a0
	Liu B , Jin HL , Sun Z , et al . , 2014a. Evidence of Holocene millennial-scale climatic change from Gonghe Basin peat deposit, northeastern Qinghai-Tibet Plateau. Journal of Arid Environments, 106: 1−10. DOI: 10.1016/j.jaridenv. 2014. 03.003. doi: 10.1016/j.jaridenv. 2014. 03.003
	Liu B , Jin HL , Sun LY , et al . , 2014b. Holocene moisture change revealed by the Rb/Sr ratio of aeolian deposits in the southeastern Mu Us Desert, China. Aeolian Research, 13: 109−119. DOI: 10.1016/j.aeolia.2014.03.006. doi: 10.1016/j.aeolia.2014.03.006
	Liu B , Jin HL , Sun LY , et al . , 2016. Geochemical characteristics of Holocene aeolian deposits and their environmental significance in the Mu Us Desert, northern China. Geological Journal, 51: 325−337. DOI: 10.1002/gj.2630. doi: 10.1002/gj.2630
	Liu B , Jin HL , Sun Z , et al . , 2012. Geochemical evidences of dry climate in the Mid-Holocene in Gonghe Basin, northeastern Qinghai-Tibetan Plateau. Sciences in Cold and Arid Regions, 4(6): 483−494. DOI: 10.3724/SP.J.1226. 2012. 00472. doi: 10.3724/SP.J.1226. 2012. 00472
	Liu K , Lai ZP , 2012. Chronology of Holocene sediments from the archaeological Salawusu site in the Mu Us Desert in China and its palaeoenvironmental implications. Journal of Asian Earth Sciences, 45: 247−255. DOI: 10.1016/j.jseaes. 2011.11.002. doi: 10.1016/j.jseaes. 2011.11.002
	Lu H , Miao X , Zhou Y , et al . , 2005. Late Quaternary aeolian activity in the Mu Us and Otindag dunefields (north China) and lagged response to insolation forcing. Geophysical Research Letters, 32: L21716. DOI: 10.1029/2005gl024560. doi: 10.1029/2005gl024560
	Lu HY , Yi SW , Xu ZW , et al . , 2013. Chinese deserts and sand fields in Last Glacial Maximum and Holocene Optimum. Chinese Science Bulletin, 58(23): 2775−2783. DOI: 10. 1007/s11434-013-5919-7. doi: 10. 1007/s11434-013-5919-7
	Lu YX , Li BS , Wen XH , et al . , 2010. Millennial-centennial scales climate changes of holocene indicated by magnetic susceptibility of high-resolution section in Salawusu River Valley, China. Chinese Geographical Science, 20(3): 243−251. DOI: 10.1007/s11769-010-0243-5. doi: 10.1007/s11769-010-0243-5
	Ma J , Yue LP , Yang LR , et al . , 2011. OSL dating of Holocene sequence and palaeoclimate change record in southeastern margin of Mu us desert, north China. Quaternary Sciences, 31(1): 120−129. DOI: 10.3969/j.issn.1001-7410.2011. 01.16. (in Chinese) doi: 10.3969/j.issn.1001-7410.2011. 01.16
	Mason JA , Lu H , Zhou Y , et al . , 2009. Dune mobility and aridity at the desert margin of northern China at a time of peak monsoon strength. Geology, 37(10): 947−950. DOI: 10.1 130/g30240a.1. doi: 10.1 130/g30240a.1
	Mayewski PA , Meeker LD , Twickler MS , et al . , 1997. Major features and forcing of high-latitude northern hemisphere atmospheric circulation using a 110,000-year-long glaciochemical series. Journal of Geophysical Research, 102(12): 26345−26366. DOI: https://doi.org/10.1029/96JC03365. doi: 10.1029/96JC03365
	McLennan SM, 1993. Weathering and global denudation. Journal of Geology, 101: 295−303. DOI: 10.1086/648222. doi: 10.1086/648222
	Nesbitt HW , Young GM , 1982. Early Proterozoic climates and plate motions inferred from major element chemistry of lutites. Nature, 299: 715−717. DOI: 10.1038/299715a0. doi: 10.1038/299715a0
	Niu DF , Li BS , Wang FN , et al . , 2015. Holocene climate fluctuations from the record of trace elements in the Mu Us Desert: evidence from the DGS 1 SEGMENT OF THE Salawusu river valley. Acta Sedimentological Sinica, 33(4): 735−743. (in Chinese)
	Niu DF , Li BS , Du SH , et al . , 2008. Cold events of Holocene indicated by primary elements distribution of the high-resolution sand dunes in the Salawusu River Valley. Journal of Geographical Sciences, 18: 26−36. DOI: 10.1007/s11442-008-0026-4. doi: 10.1007/s11442-008-0026-4
	O'Brien SR , Mayewski PA , Meeker LD , et al . , 1995. Complexity of Holocene climate as reconstructed from a Greenland ice core. Science, 270(5244): 1962−1964. DOI: 10.1126/science.270.5244.1962. doi: 10.1126/science.270.5244.1962
	Overpeck J , Anderson DM , Trumbore S , 1996. The southeast Indian monsoon over the last 18000 years. Climate Dynamics, 12: 213−255. DOI: 10.1007/bf00211619. doi: 10.1007/bf00211619
	Steinhilber F , Abreu JA , Beer J , et al . , 2012. 9,400 years of cosmic radiation and solar activity from ice cores and tree rings. Proceedings of the National Academy of Sciences, 109: 5967−5971. DOI: 10.1073/pnas.1118965109. doi: 10.1073/pnas.1118965109
	Stott L , Cannariato K , Thunell R , et al . , 2004. Decline of surface temperature and salinity in the western tropical Paciﬁc Ocean in the Holocene epoch. Nature, 431: 56−59. DOI:10.1038/nature02903. doi: 10.1038/nature02903
	Sun AZ , Feng ZD , 2013. Holocene climatic reconstructions from the fossil pollen record at QigaiNuur in the southern Mongolian Plateau. The Holocene, 23(10): 1391−1402. DOI: 10.1177/0959683613489581. doi: 10.1177/0959683613489581
	Sun JM , Li SH , Han P , et al . , 2006. Holocene environment changes in the central inner Monglia, based on the signle-aliquot-quartz optical dating and muti-proxy study of dune sands. Palaeogeography, Palaeoclimatology, Palaeoecology, 233: 51−62. DOI: 10.1016/j.palaeo.2005.09.016. doi: 10.1016/j.palaeo.2005.09.016
	Wang HP , Chen JH , Zhang XJ , et al . , 2014. Palaeosol development in the Chinese Loess Plateau as an indicator of the strength of the East Asian summer monsoon: Evidence for a mid-Holocene maximum. Quaternary International, 334−335: 155−164. DOI: 10.1016/j.quaint.2014.03.013. doi: 10.1016/j.quaint.2014.03.013
	Wang T, 2011. Deserts and Aeolian Desertification in China. Beijing: Science Press, pp. 1−819.
	Wang YJ , Cheng H , Edwards RL , et al . , 2005. The Holocene Asian Monsoon: link to solar changes and North Atlantic Climate. Science, 308: 854−857. DOI: 10.1126/science. 1106296. doi: 10.1126/science. 1106296
	Wang YJ , Cheng H , Edwards RL , et al . , 2008. Millennial- and orbital-scale changes in the East Asian monsoon over the past 224,000 years. Nature, 451: 1090−1093. DOI: 10.1038/nature06692. doi: 10.1038/nature06692
	Wen XH , Li BS , Zheng YM , et al . , 2016. Early Holocene multi-centennial moisture change reconstructed from lithology, grain-size and chemical composition data in the eastern Mu Us desert and potential driving forces. Palaeogeography, Palaeoclimatology, Palaeoecology, 459: 440−452. DOI: 10.10 16/j.palaeo.2016.07.035. doi: 10.10 16/j.palaeo.2016.07.035
	Xiao JL , Xu QH , Nakamura T , et al . , 2004. Holocene vegetation variation in the Daihai Lake region of north-central China: a direct indication of the Asian monsoon climatic history. Quaternary Science Reviews, 23: 1669−1679. DOI: 10.1016/j.quascirev.2004.01.005. doi: 10.1016/j.quascirev.2004.01.005
	Xu QH , Xiao JL , Nakamura T , et al . , 2003. Quantitative reconstructed climatic changes of Daihai Basin by pollen data. Marine Geology & Quaternary Geology, 23(4): 99−108. DOI: 10.1007/s11769-003-0089-1. doi: 10.1007/s11769-003-0089-1
	Yu YT , Yang TB , Li JJ , et al . , 2006. Millennial-scale Holocene climate variability in the NW China drylands and links to the tropical Pacific and the North Atlantic. Palaeogeography, Palaeoclimatology, Palaeoecology, 233: 149−162. DOI: 10.1016/j.palaeo.2005.09.008. doi: 10.1016/j.palaeo.2005.09.008
	Zhao H , Lu YC , Wang CM , et al . , 2010. ReOSL dating of aeolian and ﬂuvial sediments from Nihewan Basin, northern China and its environmental application. Quaternary Geochronology, 5: 159−163. DOI: 10.1016/j.quageo.2009. 03.008. doi: 10.1016/j.quageo.2009. 03.008
	Zhao H , Shen YW , Li B , et al . , 2016. Holocene environment changes around the Sara Us River, northern China, revealed by optical dating of lacustrine−aeolian sediments. Journal of Asian Earth Sciences, 120: 184−191. DOI: 10. 1016/j.jseaes.2016.02.002. doi: 10. 1016/j.jseaes.2016.02.002
	Zhou TR , Zhang LS , 1992. Holocene Environmental Evolution and Prediction in the Farming and Pastoral Transition Belt, Northern China. Beijing: Geological Publishing House. (in Chinese)
	Zhou WJ , Dodson J , Head MJ , et al . , 2002b. Environmental variability within the Chinese desert-loess transition zone over the last 20,000 years. The Holocene, 12(1): 107−112. DOI: 10.1191/0959683602hl525rr. doi: 10.1191/0959683602hl525rr
	Zhou WJ , Lu XF , Wu ZK , et al . , 2002a. Peat record reflecting Holocene climatic change in the Zoige Plateau and AMS radiocarbon dating. Chinese Science Bulletin, 47: 66−70. DOI: 10.1360/02tb9013. doi: 10.1360/02tb9013
	Zhou YL , Lu HY , Zhang JF , et al . , 2009. Luminescence dating of sand−loess sequences and response of Mu Us and Otindag sand fields (north China) to climatic changes. Journal of Quaternary Sciences, 24(4): 336−344. DOI: 10.1002/jqs.1234. doi: 10.1002/jqs.1234

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	JJ profile		Palaeosol		Aeolian sand		Weakly developed palaeosol
	Range	Average	Range	Average	Range	Average	Range	Average
P	219.66?410.82	286.18	256.82?382.54	307.17	219.66?332.03	258.19	271.01?410.82	333.11
V	9.08?37.14	22.51	36.85?16.59	24.28	9.08?33.54	19.74	21.64?37.14	29.83
Cr	10.58?32.68	20.11	13.62?32.68	21.63	10.58?31.93	17.80	19.10?30.75	25.57
Mn	87.64?299.43	181.92	137.63?299.43	204.85	87.64?241.78	154.26	163.64?258.24	212.46
Ni	13.17?21.54	16.91	13.75?21.54	17.36	13.17?20.73	16.50	13.96?19.23	16.62
Cu	4.01?10.99	6.60	4.45?10.99	7.38	4.01?8.20	5.71	5.57?8.99	7.27
As	2.73?6.01	4.27	3.32?6.01	4.45	2.73?5.57	4.06	3.54?5.43	4.40
Rb	76.55?86.66	80.07	78.18?86.66	81.70	76.55?81.42	78.56	77.86?80.00	79.00
Sr	293.81?373.07	331.88	293.81?357.13	320.73	315.42?373.07	344.32	300.31?347.28	324.29
Y	5.64?13.21	8.97	7.10?13.21	9.58	5.64?11.55	8.11	8.16?13.11	10.65
Zr	6.144?188.20	111.56	87.22?182.22	111.24	61.44?180.99	107.01	113.70?188.20	146.44
Nb	2.83?8.36	4.50	3.90?7.72	5.23	2.83?7.20	4.58	4.71?8.36	6.23
Ba	796.47?980.90	911.13	796.47?940.97	903.07	826.20?980.90	925.77	799.27?917.37	865.29

	P	V	Cr	Mn	Ni	Cu	As	Rb	Sr	Y	Zr	Nb	Ba
P	1	0.858**	0.902**	0.934**	0.550**	0.882**	0.589**	0.655**	-0.873**	0.895**	0.524**	0.781**	-0.738**
V		1	0.941**	0.864**	0.533**	0.713**	0.674**	0.324**	-0.772**	0.953**	0.932**	0.929**	-0.909**
Cr			1	0.893**	0.554**	0.776**	0.620**	0.418**	-0.774**	0.941**	0.751**	0.891**	-0.850**
Mn				1	0.596**	0.902**	0.630**	0.665**	-0.839**	0.915**	0.540**	0.787**	-0.698**
Ni					1	0.580**	0.584**	0.379**	-0.540**	0.553**	0.350**	0.509**	-0.420**
Cu						1	0.527**	0.750**	-0.843**	0.784**	0.323**	0.627**	-0.550**
As							1	0.375**	-0.561**	0.643**	0.478**	0.589**	-0.552**
Rb								1	-0.780**	0.429**	-0.170**	0.209**	-0.119*
Sr									1	-0.781**	-0.341**	-0.627**	0.620**
Y										1	0.770**	0.909**	0.878**
Zr											1	0.868**	-0.885**
Nb												1	-0.898**
Ba													1

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