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Evidence from the Dayao Paleolithic site, Inner Mongolia for human migration into arid northwest China during mid-Pleistocene interglacials

Published online by Cambridge University Press:  05 March 2021

Junyi Ge*
Affiliation:
Key Laboratory of Vertebrate Evolution and Human Origins, Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences, Beijing, China CAS Center for Excellence in Life and Paleoenvironment, Beijing, China University of the Chinese Academy of Sciences, Beijing, China
Yinghua Wang
Affiliation:
Inner Mongolia Museum, Hohhot, China
Mingchao Shan
Affiliation:
Inner Mongolia Museum, Hohhot, China
Xingwu Feng
Affiliation:
Key Laboratory of Vertebrate Evolution and Human Origins, Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences, Beijing, China
Fuyou Chen
Affiliation:
Key Laboratory of Vertebrate Evolution and Human Origins, Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences, Beijing, China
Haibin Wu
Affiliation:
CAS Center for Excellence in Life and Paleoenvironment, Beijing, China University of the Chinese Academy of Sciences, Beijing, China Key Laboratory of Cenozoic Geology and Environment, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, China
Qin Li
Affiliation:
Key Laboratory of Cenozoic Geology and Environment, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, China
Xinying Zhou
Affiliation:
Key Laboratory of Vertebrate Evolution and Human Origins, Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences, Beijing, China CAS Center for Excellence in Life and Paleoenvironment, Beijing, China University of the Chinese Academy of Sciences, Beijing, China
Yan Li
Affiliation:
School of Ocean Sciences, China University of Geosciences (Beijing), Beijing, China
Ruiping Tang
Affiliation:
University of the Chinese Academy of Sciences, Beijing, China
John W. Olsen
Affiliation:
Key Laboratory of Vertebrate Evolution and Human Origins, Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences, Beijing, China School of Anthropology, University of Arizona, Tucson, USA
Chenglong Deng
Affiliation:
University of the Chinese Academy of Sciences, Beijing, China State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, China
Xing Gao
Affiliation:
Key Laboratory of Vertebrate Evolution and Human Origins, Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences, Beijing, China CAS Center for Excellence in Life and Paleoenvironment, Beijing, China University of the Chinese Academy of Sciences, Beijing, China
*
*Corresponding author: (J. Ge) gejunyi@ivpp.ac.cn

Abstract

The Dayao Paleolithic site, located in Inner Mongolia on the eastern margin of China's vast northwestern drylands, was a lithic quarry-workshop utilized by Pleistocene human migrants through the region. Determining the age of this activity has previously yielded controversial results. Our magnetostratigraphic and OSL dating results suggest the two artifact-bearing paleosols are correlated with MIS 5 and 7, respectively. Correlating paleoclimatic data with marine δ18O records leads us to conclude that two sandy gravel layers containing many artifacts in the lower part of the Dayao sequence were formed during MIS 9 and 11, if not earlier. Our results reveal that the earliest human occupation at the Dayao site occurred before ca. 400 ka during a relatively warm and moist interglacial period, similar to several subsequent occupations, documenting the earliest and northernmost archaeological assemblage yet reported in China's arid northwest. We conclude that the northward and southward displacements of the East Asian summer monsoon rain belt during past interglacial-glacial cycles were responsible for the discontinuous human occupation detected at the Dayao site. The penetration of this precipitation regime into dryland ecologies via the Huanghe (Yellow River) Valley effectively created a corridor for hominin migration into China's arid northwest.

Type
Thematic Set: Eurasian Climate and Environment
Copyright
Copyright © University of Washington. Published by Cambridge University Press, 2021

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References

Aitken, M.J., 1985. Thermoluminescence Dating. Academic Press, London, Orlando, Montreal.Google Scholar
An, Z.S., Liu, T.S., Lu, Y.C., Porter, S.C., Kukla, G., Wu, X.H., Hua, Y.M., 1990. The long-term paleomonsoon variation recorded by the loess-paleosol sequence in central China. Quaternary International 7–8, 9195.Google Scholar
Arnold, L.J., Bailey, R.M., Tucker, G.E., 2007. Statistical treatment of fluvial dose distributions from southern Colorado arroyo deposits. Quaternary Geochronology 2, 162167.CrossRefGoogle Scholar
Barker, G., Gilbertson, D., 2003. The Archaeology of Drylands: Living at the Margin. Routledge, London, New York.CrossRefGoogle Scholar
Bøtter-Jensen, L., Andersen, C.E., Duller, G.A., Murray, A.S., 2003. Developments in radiation, stimulation and observation facilities in luminescence measurements. Radiation Measurements 37, 535541.CrossRefGoogle Scholar
Breeze, P.S., Groucutt, H.S., Drake, N.A., White, T.S., Jennings, R.P., Petraglia, M.D., 2016. Palaeohydrological corridors for hominin dispersals in the Middle East ~250–70,000 years ago. Quaternary Science Reviews 144, 155185.CrossRefGoogle Scholar
Buylaert, J.P., Jain, M., Murray, A.S., Thomsen, K.J., Thiel, C., Sohbati, R., 2012. A robust feldspar luminescence dating method for middle and late Pleistocene sediments. Boreas 41, 435451.CrossRefGoogle Scholar
Buylaert, J.P., Murray, A.S., Huot, S., 2008. Optical dating of an Eemian site in northern Russia using K-feldspar. Radiation Measurements 43, 715720.CrossRefGoogle Scholar
Buylaert, J.P., Vandenberghe, D., Murray, A.S., Huot, S., De Corte, F., Van den Haute, P., 2007. Luminescence dating of old (>70 ka) Chinese loess: a comparison of single-aliquot OSL and IRSL techniques. Quaternary Geochronology 2, 914.CrossRefGoogle Scholar
Castañeda, I.S., Mulitza, S., Schefuß, E., dos Santos, R.A.L., Damsté, J.S.S., Schouten, S., 2009. Wet phases in the Sahara/Sahel region and human migration patterns in North Africa. Proceedings of the National Academy of Sciences 106, 2015920163.CrossRefGoogle ScholarPubMed
Chen, F.H., Fan, Y.X., Madsen, D.B., Chun, X., Zhao, H., Yang, L.P., 2008. Preliminary study on the formation mechanism of the “Jilantai-Hetao” megalake and the lake evolutionary history in Hetao region. Quaternary Sciences 28, 866873. [in Chinese]Google Scholar
Cheng, J., Tian, M.Z., Cao, B.X., Zhao, Z.Z., 1997. New Quaternary mammalian faunas and cave deposits in the Zhoukoudian area, Beijing. Acta Geologica Sinica (English Edition) 71, 231243.Google Scholar
Chen, J., Tian, M.Z., Cao, B.X., Li, L.Y., 1996. Evolution of Quaternary mammalian assemblages and environmental changes in Zhoukoudian Area, Beijing. Geoscience-Journal of Graduate School, China University of Geosciences 10, 202212.Google Scholar
Clark, P.U., Archer, D., Pollard, D., Blum, J.D., Rial, J.A., Brovkin, V., Mix, A.C., Pisias, N.G., Roy, M., 2006. The middle Pleistocene transition: characteristics, mechanisms, and implications for long-term changes in atmospheric pCO2. Quaternary Science Reviews 25, 31503184.CrossRefGoogle Scholar
Coulthard, T.J., Ramirez, J.A., Barton, N., Rogerson, M., Brücher, T., 2013. Were rivers flowing across the Sahara during the last interglacial? Implications for human migration through Africa. PloS ONE 8, e74834. https://doi.org/10.1371/journal.pone.0074834.CrossRefGoogle ScholarPubMed
Cunningham, A.C., Wallinga, J., 2010. Selection of integration time intervals for quartz OSL decay curves. Quaternary Geochronology 5, 657666.CrossRefGoogle Scholar
Dennell, R., 2003. Dispersal and colonisation, long and short chronologies: how continuous is the early Pleistocene record for hominids outside East Africa? Journal of Human Evolution 45, 421440.CrossRefGoogle ScholarPubMed
Dennell, R., 2013a. Hominins, deserts, and the colonisation and settlement of continental Asia. Quaternary International 300, 1321.CrossRefGoogle Scholar
Dennell, R.W., 2013b. The Nihewan Basin of North China in the early Pleistocene: continuous and flourishing, or discontinuous, infrequent and ephemeral occupation? Quaternary International 295, 223236.CrossRefGoogle Scholar
Dennell, R.W. 2016. Life without the Movius Line. Quaternary International 400, 1422.CrossRefGoogle Scholar
Dennell, R.W., Martinón-Torres, M., Bermudez de Castro, J.M. and Gao, X., 2020. A demographic history of late Pleistocene China. Quaternary International 559, 413. https://doi.org/10.1016/j.quaint.2020.03.014.CrossRefGoogle Scholar
Ding, Z.L., Derbyshire, E., Yang, S.L., Yu, Z.W., Xiong, S.F., Liu, T., 2002. Stacked 2.6-Ma grain size record from the Chinese loess based on five sections and correlation with the deep-sea δ18O record. Paleoceanography 17, 5–15–21.CrossRefGoogle Scholar
Dong, H.M., Zhao, J.B., Song, Y.G., 2010. Geochemical components and paleoenvironment implication for S4 paleosol in Shaolingyuan, Chang'an County. Scientia Geographica Sinica 30, 904909.Google Scholar
Drake, N.A., Blench, R.M., Armitage, S.J., Bristow, C.S., White, K.H., 2011. Ancient watercourses and biogeography of the Sahara explain the peopling of the desert. Proceedings of the National Academy of Sciences 108, 458462.CrossRefGoogle ScholarPubMed
Duller, G.A.T., 2008. Single-grain optical dating of Quaternary sediments: why aliquot size matters in luminescence dating. Boreas 37, 589612.CrossRefGoogle Scholar
Durcan, J.A., King, G.E., Duller, G.A.T., 2015. DRAC: dose rate and age calculator for trapped charge dating. Quaternary Geochronology 28, 5461.CrossRefGoogle Scholar
Faegri, K., Iversen, J., 1975. Textbook of Pollen Analysis. Blackwell Scientific, Oxford.Google Scholar
Feng, X.W., 2008. Lithic Industry of the Sidaogou Locality, Dayao, Inner Mongolia. Ph.D. thesis, Beijing, Chinese Academy of Science, 180 pp.Google Scholar
Fick, S.E., Hijmans, R.J., 2017. WorldClim 2: new 1-km spatial resolution climate surfaces for global land areas. International Journal of Climatology 37, 43024315.CrossRefGoogle Scholar
Finlayson, C., 2013. The Water Optimisation Hypothesis and the human occupation of the mid-latitude belt in the Pleistocene. Quaternary International 300, 2231.CrossRefGoogle Scholar
Foley, R.A., Maíllo-Fernández, J.M., Lahr, M.M., 2013. The Middle Stone Age of the central Sahara: biogeographical opportunities and technological strategies in later human evolution. Quaternary International 300, 153170.CrossRefGoogle Scholar
Galbraith, R.F., Roberts, R.G., Laslett, G.M., Yoshida, H., Olley, J.M., 1999. Optical dating of single and multiple grains of quartz from Jinmium rock shelter, northern Australia: Part I, experimental design and statistical models. Archaeometry 41, 339364.CrossRefGoogle Scholar
Green, R.E., Krause, J., Briggs, A.W., Maricic, T., Stenzel, U., Kircher, M., Patterson, N., Li, H., Zhai, W., Fritz, M.H.-Y., 2010. A draft sequence of the Neandertal genome. Science 328, 710722.CrossRefGoogle ScholarPubMed
Guérin, G., Mercier, N., Adamiec, G., 2011. Dose-rate conversion factors: update. Ancient TL 29, 58.Google Scholar
Guiot, J., 1990. Methodology of the last climatic cycle reconstruction in France from pollen data. Palaeogeography, Palaeoclimatology, Palaeoecology 80, 4969.CrossRefGoogle Scholar
Guiot, J., Goeury, C., 1996. PPPBASE, a software for statistical analysis of paleoecological and paleoclimatological data. Dendrochronologia 14, 295300.Google Scholar
Guo, Z.T., Liu, T.S., Fedoroff, N., Wei, L.Y., Ding, Z.L., Wu, N.Q., Lu, H.Y., Jiang, W.Y., An, Z.S., 1998. Climate extremes in loess of China coupled with the strength of deep-water formation in the North Atlantic. Global and Planetary Change 18, 113128.CrossRefGoogle Scholar
Guo, Z.T., Sun, B., Zhang, Z.S., Peng, S.Z., Xiao, G.Q., Ge, J.Y., Hao, Q.Z., et al. , 2008. A major reorganization of Asian climate by the early Miocene. Climate of the Past 4, 153174.CrossRefGoogle Scholar
Hao, Q., Wang, L., Oldfield, F., Guo, Z., 2015. Extra-long interglacial in Northern Hemisphere during MISs 15–13 arising from limited extent of Arctic ice sheets in glacial MIS 14. Nature Scientific Reports 5, 12103. https://doi.org/10.1038/srep12103.CrossRefGoogle ScholarPubMed
Hao, Q.Z., Guo, Z.T., 2005. Spatial variations of magnetic susceptibility of Chinese loess for the last 600 kyr: implications for monsoon evolution. Journal of Geophysical Research: Solid Earth 110, B12101. https://doi.org/10.1029/2005JB003765.CrossRefGoogle Scholar
Hao, Q.Z., Wang, L., Oldfield, F., Peng, S.Z., Qin, L., Song, Y., Xu, B., Qiao, Y.S., Bloemendal, J., Guo, Z.T., 2012. Delayed build-up of Arctic ice sheets during 400,000-year minima in insolation variability. Nature 490, 393396.CrossRefGoogle ScholarPubMed
Head, M.J., Pillans, B., Farquhar, S.A., 2008. The early–middle Pleistocene transition: characterization and proposed guide for the defining boundary. Episodes 31, 255259.CrossRefGoogle Scholar
Hublin, J.-J., Roebroeks, W., 2009. Ebb and flow or regional extinctions? On the character of Neandertal occupation of northern environments. Comptes Rendus Palevol 8, 503509.CrossRefGoogle Scholar
Huntley, D.J., Baril, M.R., 1997. The K content of the K-feldspars being measured in optical dating or in thermoluminescence dating. Ancient TL 15, 1113.Google Scholar
Imbrie, J., Berger, A., Boyle, E.A., Clemens, S.C., Duffy, A., Howard, W.R., Kukla, G., Kutzbach, J., Martinson, D.G., McIntyre, A., 1993. On the structure and origin of major glaciation cycles 2. The 100,000-year cycle. Paleoceanography 8, 699735.CrossRefGoogle Scholar
Jain, M., Murray, A.S., Bøtter-Jensen, L., 2003. Characterisation of blue-light stimulated luminescence components in different quartz samples: implications for dose measurement. Radiation Measurements 37, 441449.CrossRefGoogle Scholar
Jones, C.H., 2002. User-driven integrated software lives: “Paleomag” paleomagnetics analysis on the Macintosh. Computers & Geosciences 28, 11451151.CrossRefGoogle Scholar
Kirschvink, J.L., 1980. The least-squares line and plane and the analysis of palaeomagnetic data. Geophysical Journal International 62, 699718.CrossRefGoogle Scholar
Kukla, G., An, Z.S., 1989. Loess stratigraphy in central China. Palaeogeography, Palaeoclimatology, Palaeoecology 72, 203225.CrossRefGoogle Scholar
Li, F., Kuhn, S.L., Chen, F.Y., Wang, Y.H., Southon, J., Peng, F., Shan, M.C., Wang, C.X., Ge, J.Y., Wang, X.M., 2018. The easternmost Middle Paleolithic (Mousterian) from Jinsitai Cave, North China. Journal of Human Evolution 114, 7684.CrossRefGoogle ScholarPubMed
Li, F., Kuhn, S.L., Gao, X., Chen, F.Y., 2013. Re-examination of the dates of large blade technology in China: a comparison of Shuidonggou Locality 1 and Locality 2. Journal of Human Evolution 64, 161168.CrossRefGoogle ScholarPubMed
Lisiecki, L.E., Raymo, M.E., 2005. A Pliocene–Pleistocene stack of 57 globally distributed benthic δ18O records. Paleoceanography 20, PA1003. https://doi.org/10.1029/2004PA001071.Google Scholar
Liu, T.S., Ding, Z.L., 1998. Chinese loess and the paleomonsoon. Annual Review of Earth and Planetary Sciences 26, 111145.CrossRefGoogle Scholar
Madsen, D.B., Li, J.Z., Brantingham, P.J., Gao, X., Elston, R.G., Bettinger, R.L., 2001. Dating Shuidonggou and the Upper Palaeolithic blade industry in North China. Antiquity 75, 706716.CrossRefGoogle Scholar
Maher, B.A., Thompson, R., Zhou, L.P., 1994. Spatial and temporal reconstructions of changes in the Asian palaeomonsoon: a new mineral magnetic approach. Earth and Planetary Science Letters 125, 461471.CrossRefGoogle Scholar
Members of China Quaternary Pollen Data Base (MCQPD), 2000. Pollen-based biome reconstruction at middle Holocene (6 ka BP) and Last Glacial Maximum (18 ka BP) in China. Acta Botanica Sinica 42, 12011209. [in Chinese with English Abstract]Google Scholar
Moore, P.D., Webb, J.A., Collison, M.E., 1991. Pollen Analysis. Blackwell Scientific, Oxford.Google Scholar
Mu, H.S., Xu, Q.H., Zhang, S.R., Hun, L.Y., Li, M.Y., Li, Y., Hu, Y.N., Xie, F., 2015. Pollen-based quantitative reconstruction of the paleoclimate during the formation process of Houjiayao Relic Site in Nihewan Basin of China. Quaternary International 374, 7684.CrossRefGoogle Scholar
Murray, A.S., Wintle, A.G., 2000. Luminescence dating of quartz using an improved single-aliquot regenerative-dose protocol. Radiation Measurements 32, 5773.CrossRefGoogle Scholar
Murray, A.S., Wintle, A.G., 2003. The single aliquot regenerative dose protocol: potential for improvements in reliability. Radiation Measurements 37, 377381.CrossRefGoogle Scholar
Nie, Z.S., 2019. Stratigraphic division of the upper Pleistocene, environmental change and formation of the Yellow River in the Hetao Basin, Inner Mongolia. Earth Science Frontiers 26, 259272.Google Scholar
Olley, J.M., Caitcheon, G.G., Roberts, R.G., 1999. The origin of dose distributions in fluvial sediments, and the prospect of dating single grains from fluvial deposits using optically stimulated luminescence. Radiation Measurements 30, 207217.CrossRefGoogle Scholar
Olley, J.M., Pietsch, T., Roberts, R.G., 2004. Optical dating of Holocene sediments from a variety of geomorphic settings using single grains of quartz. Geomorphology 60, 337358.CrossRefGoogle Scholar
Osborne, A.H., Vance, D., Rohling, E.J., Barton, N., Rogerson, M., Fello, N., 2008. A humid corridor across the Sahara for the migration of early modern humans out of Africa 120,000 years ago. Proceedings of the National Academy of Sciences 105, 1644416447.CrossRefGoogle ScholarPubMed
Overpeck, J.T., Webb, T., Prentice, I.C., 1985. Quantitative interpretation of fossil pollen spectra: dissimilarity coefficients and the method of modern analogs. Quaternary Research 23, 87108.CrossRefGoogle Scholar
Pachur, H.J., Rottinger, F., 1997. Evidence for a large extended paleolake in the Eastern Sahara as revealed by spaceborne radar lab images. Remote Sensing of the Environment 61, 437440.CrossRefGoogle Scholar
Petraglia, M.D., Alsharekh, A.M., Crassard, R., Drake, N.A., Groucutt, H., Parker, A.G., Roberts, R.G., 2011. Middle Paleolithic occupation on a Marine Isotope Stage 5 lakeshore in the Nefud Desert, Saudi Arabia. Quaternary Science Reviews 30, 15551559.CrossRefGoogle Scholar
Porter, S.C., 2001. Chinese loess record of monsoon climate during the last glacial–interglacial cycle. Earth-Science Reviews 54, 115128.CrossRefGoogle Scholar
Prentice, I.C., Guiot, J., Huntley, B., Jolly, D., Cheddadi, R. 1996. Reconstructing biomes from palaeoecological data: a general method and its application to European pollen data at 0 and 6 ka. Climate Dynamics 12, 185194.CrossRefGoogle Scholar
Prescott, J.R., Hutton, J.T., 1994. Cosmic ray contributions to dose rates for luminescence and ESR dating: large depths and long-term time variations. Radiation Measurements 23, 497500.CrossRefGoogle Scholar
Prokopenko, A., Williams, D., Kuzmin, M., Karabanov, E.B., Khursevich, G.K., Peck, J.A., 2002. Muted climate variations in continental Siberia during the mid-Pleistocene epoch. Nature 418, 6568.CrossRefGoogle ScholarPubMed
Rees-Jones, J., 1995. Optical dating of young sediments using fine-grain quartz. Ancient TL 13, 914.Google Scholar
Rightmire, G.P., 1998. Human evolution in the middle Pleistocene: the role of Homo heidelbergensis. Evolutionary Anthropology 6, 218227.3.0.CO;2-6>CrossRefGoogle Scholar
Rightmire, G.P., 2001. Comparison of middle Pleistocene hominids from Africa and Asia. In: Barham, L., Robson-Brown, K. (Eds.), Human Roots: Africa and Asia in the Middle Pleistocene. Western Academic and Specialist Press Ltd., Bristol, pp. 123133.Google Scholar
Roberts, H.M., 2006. Optical dating of coarse-silt sized quartz from loess: evaluation of equivalent dose determinations and SAR procedural checks. Radiation Measurements 41, 923929.CrossRefGoogle Scholar
Shen, G.J., Gao, X., Gao, B., Granger, D.E., 2009. Age of Zhoukoudian Homo erectus determined with 26Al/10Be burial dating. Nature 458, 198200.CrossRefGoogle Scholar
Smith, B.W., Rhodes, E.J., 1994. Charge movements in quartz and their relevance to optical dating. Radiation Measurements 23, 329333.CrossRefGoogle Scholar
Song, Y., Hao, Q.Z., Ge, J.Y., Zhao, D.a., Zhang, Y., Li, Q., Zuo, X.X., , Y.W., Wang, P., 2014. Quantitative relationships between magnetic enhancement of modern soils and climatic variables over the Chinese Loess Plateau. Quaternary International 334–335, 119131.CrossRefGoogle Scholar
Stevens, T., Buylaert, J.P., Thiel, C., Újvári, G., Yi, S., Murray, A.S., Frechen, M., Lu, H.Y., 2018. Ice-volume-forced erosion of the Chinese Loess Plateau global Quaternary stratotype site. Nature Communications 9, 112.CrossRefGoogle ScholarPubMed
Stewart, J.R., Stringer, C.B., 2012. Human evolution out of Africa: the role of refugia and climate change. Science 335, 13171321.CrossRefGoogle ScholarPubMed
Sun, X.F., Lu, H.Y., Wang, S.J., Yi, L., Li, Y.X., Bahain, J.J., Voinchet, P., Hu, X.Z., Zeng, L., Zhang, W.C., 2017. Early human settlements in the southern Qinling Mountains, central China. Quaternary Science Reviews 164, 168186.CrossRefGoogle Scholar
Team, J.E., 1976. Quaternary mammalian fauna from Jinniushan, Yingkou of Liaoning Province. Vertebrata PalAsiatica 14, 120127. [in Chinese]Google Scholar
Thomas, D.S.G., 2011. Arid Zone Geomorphology: Process, Form and Change in Drylands, Third Edition. John Wiley & Sons, Chichester.CrossRefGoogle Scholar
Veth, P., Smith, M., Hiscock, P., 2008. Desert Peoples: Archaeological Perspectives. John Wiley & Sons, Oxford.Google Scholar
Wang, F.X., Qian, N.F., Zhang, Y.L., Yang, H.Q., 1997. Pollen Flora of China, Second Edition. Science Press, Beijing. [in Chinese]Google Scholar
Wang, Y.H., 2002. Geochronological dating and cultural staging of the site of the Dayao Locality 4 site. Inner Mongolia Cultural Relics and Archaeology (Steppe Cultural Relics) 611. [in Chinese]Google Scholar
Wang, Y.H., Liu, J.X., Shan, M.C., Li, F., Chen, F.Y., 2014. A preliminary report of the stone artifacts from the 27th cave of the Dayao Site. Acta Anthropologica Sinica 33, 5159.Google Scholar
Wang, Y.P., Olsen, J.W., 1985. Aspects of the Inner Mongolian Palaeolithic. In: Wu, R.K., Olsen, J.W. (Eds.), Palaeoanthropology and Palaeolithic Archaeology in the People's Republic of China. Academic Press, New York, London, pp. 243258.Google Scholar
Wintle, A.G., Murray, A.S., 2006. A review of quartz optically stimulated luminescence characteristics and their relevance in single-aliquot regeneration dating protocols. Radiation Measurements 41, 369391.CrossRefGoogle Scholar
Xi, Y.Z., Ning, J.C., 1994. Study on pollen morphology of plants from dry and semidry areas in China. Yushania 11, 119191.Google Scholar
Xu, T., Chen, F.Y., Wang, Y.H., 2013. An analysis of the cores and their flaking technology of the Erdaogou Locality of Dayao Site. Acta Anthropologica Sinica 32, 441453.Google Scholar
Yang, S.L., Ding, Z.L., 2008. Advance-retreat history of the East-Asian summer monsoon rainfall belt over northern China during the last two glacial-interglacial cycles. Earth and Planetary Science Letters 274, 499510.CrossRefGoogle Scholar
Yi, S.W., Buylaert, J.P., Murray, A.S., Lu, H.Y., Thiel, C., Zeng, L., 2016. A detailed post-IR IRSL dating study of the Niuyangzigou loess site in northeastern China. Boreas 45, 644657.CrossRefGoogle Scholar
Zheng, Z., Wei, J.H., Huang, K.Y., Xu, Q.H., Lu, H.Y., Tarasov, P., Luo, C.X., Beaudouin, C., Deng, Y., Pan, A.D., 2014. East Asian pollen database: modern pollen distribution and its quantitative relationship with vegetation and climate. Journal of Biogeography 41, 18191832.CrossRefGoogle Scholar
Zhou, X.Y., Li, X.Q., Dodson, J., Yang, S.L., Long, H., Zhao, K.L., Sun, N., Yang, Q., Liu, H.B., Zhao, C., 2014. Zonal vegetation change in the Chinese Loess Plateau since MIS 3. Palaeogeography, Palaeoclimatology, Palaeoecology 404, 8996.CrossRefGoogle Scholar
Zijderveld, J.D.A., 1967. AC demagnetization of rocks: analysis of results. In: Collinson, D.W., Creer, K.M., Runcorn, S.K. (Eds.), Methods in Paleomagnetism: Proceedings of the NATO Advanced Study Institute on Palaeomagnetic Methods held in the Physics Department of the University of Newcastle upon Tyne, April 1–10, 1964. Elsevier Publishing Company, Amsterdam, London, New York, pp. 254286.Google Scholar
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Evidence from the Dayao Paleolithic site, Inner Mongolia for human migration into arid northwest China during mid-Pleistocene interglacials
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