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Magnetostratigraphic dating of the Donggutuo and Maliang Paleolithic sites in the Nihewan Basin, North China

Published online by Cambridge University Press:  20 January 2017

Hongqiang Wang ,
Chenglong Deng ,
Rixiang Zhu ,
Qi Wei ,
Yamei Hou  and
Eric Boëda
Hongqiang Wang*
Affiliation:
Paleomagnetism and Geochronology Laboratory (SKL-LTE), Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China
Chenglong Deng
Affiliation:
Paleomagnetism and Geochronology Laboratory (SKL-LTE), Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China
Rixiang Zhu
Affiliation:
Paleomagnetism and Geochronology Laboratory (SKL-LTE), Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China
Qi Wei
Affiliation:
Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences, Beijing 100044, China
Yamei Hou
Affiliation:
Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences, Beijing 100044, China
Eric Boëda
Affiliation:
Maison de L'Archéologie et de l'Ethnologie, Université Paris X, Nanterre 92023, France
*
*Corresponding author. E-mail addresses:[email protected] (H. Wang) [email protected] (C. Deng) [email protected] (R. Zhu) [email protected] (Y. Hou)
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Abstract

A detailed magnetostratigraphic investigation, coupled with rock-magnetic studies, was carried out on a lacustrine sequence in the eastern Nihewan Basin, Northern China, which contains the Donggutuo and Maliang Paleolithic sites. Magnetite and hematite were identified as the main carriers for the characteristic remanent magnetizations. Magnetostratigraphic results show that the lacustrine sequence recorded the late Matuyama and Brunhes chrons. Furthermore, the Maliang artifact layer occurs just below the Brunhes/Matuyama boundary, and the Donggutuo artifact layer is just below the Jaramillo onset. Therefore, the age of the Maliang and Donggutuo artifact layers can be definitely estimated to be about 0.78 myr and 1.1 myr, respectively. These two paleomagnetic ages, coupled with previously obtained paleomagnetic data of the Majuangou, Xiaochangliang, Banshan, Lantian, and Xihoudu Paleolithic sites, suggest an expansion and lengthy flourishing of human groups from northern to north-central China during the entire Early Pleistocene.

Keywords

MagnetostratigraphyPaleolithic sitePleistoceneDonggutuoMaliangNihewan BasinNorth China
Type
Research Article
Information
Quaternary Research , Volume 64 , Issue 1 , July 2005 , pp. 1 - 11
Copyright
University of Washington

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References

Abbate, E., Albianelli, A., Azzaroli, A., Benvenuti, M., Tesfamariam, B., Bruni, P., Cipriani, N., Clarke, R.J., Ficcarelli, G., Machiarelli, R., Napoleone, G., Papini, M., Rook, L., Sagri, M., Tecle, T.M., Torre, D., and Villa, I. (1998). A one-million year-old Homo cranium from the-Danakil (Afar) Depression of Eritrea. Nature 393, 458–460.Google Scholar
An, Z., and Ho, C.K. (1989). New magnetostratigraphic dates of Lantian Homo erectus . Quaternary Research 32, 213–221.Google Scholar
An, Z., Kutzbach, J.E., Prell, W.L., and Porter, S.C. (2001). Evolution of Asian monsoons and phased uplift of the Himalaya-Tibetan plateau since late Miocene times. Nature 411, 62–66.Google Scholar
Antón, S.C., and Swisher, C.C. ("n and Swisher, 2004). )Early dispersals of Homo from Africa. Annual Review of Anthropology 33, 271–296.Google Scholar
Barbour, G.B. (1924). Preliminary observation in Kalgan Area. Bulletin of Geological Society of China 3, 167–168.Google Scholar
Barbour, G.B. (1925). The deposits of the Sankanho Valley. Bulletin of Geological Society of China 4, 53–55.Google Scholar
Barbour, G.B., Licent, E., and de Chardin, P. (1927). Geological study of the deposits of the Sangkanho basin. Bulletin of Geological Society of China 5, 2-4 263–278.Google Scholar
Bar-Yosef, O., and Belfer-Cohen, A. (2001). From Africa to Eurasia–early dispersals. Quaternary International 75, 19–28.Google Scholar
Chen, M.N. (1988). Study on the Nihewan Beds. China Ocean Press, Beijing.1–143.In Chinese with English abstractGoogle Scholar
Clark, P.U., Alley, R.B., and Pollard, D. (1999). Northern Hemisphere ice-sheet influences on global climate change. Science 286, 1104–1111.Google Scholar
Deng, C., Zhu, R., Verosub, K.L., Singer, M.J., and Yuan, B. (2000). Paleoclimatic significance of the temperature-dependent susceptibility of Holocene loess along a NW-SE transect in the Chinese loess plateau. Geophysical Research Letters 27, 3715–3718.Google Scholar
Deng, C., Zhu, R., Jackson, M.J., Verosub, K.L., and Singer, M.J. (2001). Variability of the temperature-dependent susceptibility of the Holocene Eolian deposits in the Chinese Loess Plateau: a pedogenesis indicator. Physics and Chemistry of the Earth (A) 26, 873–878.Google Scholar
Deng, C., Zhu, R., Verosub, K.L., Singer, M.J., and Vidic, N.J. (2004). Mineral magnetic properties of loess/paleosol couplets of the central loess plateau of China over the last 1.2 Myr. Journal of Geophysical Research 109, B01103 10.1029/2003JB002532Google 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, 421–440.Google Scholar
Dunlop, D.J., and Özdemir, Ö. ("zdemir, 1997). )Rock Magnetism: Fundamentals and Frontiers. Cambridge University Press, New York.573 pp.Google Scholar
Feng, X.W., and Hou, Y.M. (1998). Huojiadi–A new Paleolithic site discovered in the Nihewan basin. Acta Anthropologica Sinica 17, 4 310–316.In Chinese with English abstractGoogle Scholar
Florindo, F., Zhu, R., Guo, B., Yue, L., Pan, Y., and Speranza, F. (1999). Magnetic proxy climate results from the Duanjiapo loess section, southernmost extremity of the Chinese loess plateau. Journal of Geophysical Research 104, B1 645–659.Google Scholar
Gabunia, L., and Vekua, A. (1995). A Plio-Pleistocene hominid from Dmanisi, East Georgia, Caucasus. Nature 373, 509–512.Google Scholar
Gabunia, L., Vekua, A., Lordkipanidze, D., Swisher III, C.C., Ferring, R., Justus, A., Nioradze, M., Tvalchrelidze, M., Antón, S.C., Bosinski, G., Jöris, O., Lumley, M., Majsuradze, G., and Mouskhelishvili, A. (2000). Earliest Pleistocene hominid cranial remains from Dmanisi, Republic of Georgia: taxonomy, geological setting, and age. Science 288, 1019–1025.CrossRefGoogle ScholarPubMed
Goren-Inbar, N., Feibei, C.S., Verosub, K.L., Melamed, Y., Kislev, M.E., Tchernov, E., and Saragusti, I. (2000). Pleistocene milestones on the out-of-Africa corridor at Gesher Benot Ya'aqov, Israel. Science 289, 944–947.Google Scholar
Y.M., Hou. (2000). Donggutuo lithic industry of the Nihewan basin, North China.IVPP (Institute of Vertebrate Paleontology and Paleoanthropology). Chinese Academy of Sciences, Beijing, PhD thesis., 112 pp. (In Chinese with English abstract).Google Scholar
Hou, Y.M. (2003). Naming and preliminary study on the category of the “Donggutuo core”. Acta Anthropologica Sinica 22, 4 279–292.In Chinese with English abstractGoogle Scholar
Hou, Y.M., Wei, Q., Feng, X.W., and Lin, S.L. (1999). Re-excavation at Donggutuo in the Nihewan Basin, North China. Quaternary Sciences 2, 139–147.In Chinese with English abstractGoogle Scholar
Hou, Y.M., Potts, R., Yuan, B.Y., Guo, Z.T., Deino, A., Wang, W., Clark, J., Xie, G.M., and Huang, W.W. (2000). Mid-Pleistocene Acheulean-like stone technology of the Bose Basin, South China. Science 287, 1622–1626.Google Scholar
HPICR (Hebei Province Institute of Cultural Relics)(1998). Excavations of the Lower Paleolithic site at Majuangou.HPICR, Papers on Archaeology in Hebei Province East Press, Beijing.30–45.In ChineseGoogle Scholar
Hrouda, F. (1982). Magnetic anisotropy of rocks and its application in geology and geophysics. Geophysical Surveys 5, 37–82.Google Scholar
Huang, W.P., Ciochon, R., Gu, Y., Larick, R., Fang, Q., Schwartz, H., Yonge, C., De Vos, J., and Rink, W. (1995). Early Homo and associated artifacts from Asia. Nature 378, 275–278.Google Scholar
Hunt, C.P., Banerjee, S.K., Han, J., Solheid, P.A., Oches, E., Sun, W., and Liu, T. (1995). Rock-magnetic proxies of climate change in the loess-paleosol sequences of the western Loess Plateau of China. Geophysical Journal International 123, 232–244.Google Scholar
Hyodo, M., Nakaya, H., Urabe, A., Saegusa, H., Xue, S., Yin, J., and Ji, X. (2002). Paleomagnetic dates of hominid remains from Yuanmou, China, and other Asian sites. Journal of Human Evolution 43, 27–41.Google Scholar
Jelinek, V. (1978). Statistical processing of anisotropy of magnetic susceptibility measured on groups of specimens. Studia Geophysica et Geodaetica 22, 50–62.CrossRefGoogle Scholar
Kirschvink, J.L. (1980). The least-squares line and plane and the analysis of palaeomagnetic data. Geophysical Journal of the Royal Astronomical Society 62, 699–718.Google Scholar
Li, H.M., and Wang, J.D. (1982). Magnetostratigraphic study of several typical geologic sections in North China.Liu, T.S. Quaternary Geology and Environment of China China Ocean Press, Beijing.33–38.Google Scholar
Oches, E.A., and Banerjee, S.K. (1996). Rock-magnetic proxies of climate change from loess-paleosol sediments of the Czech Republic. Studia Geophysica et Geodaetica 40, 287–300.Google Scholar
Oms, O., Parés, J.M., Martinez-Navarro, B., Agustí, J., Toro, I., Martínez-Fernández, G., and Turq, A. (2000). Early human occupation of Western Europe: paleomagnetic dates for two Paleolithic sites in Spain. Proceedings of the National Academy of Sciences of the United States of America 97, 10666–10670.Google Scholar
Pei, S.W., and Hou, Y.M. (2002). Preliminary study on raw materials exploitation at Donggutuo Site, Nihewan Basin, North China. Acta Anthroplogica Sinica 21, 53–66.Supp.Google Scholar
Potts, R. (2001). Mid-Pleistocene environmental change and human evolution.Barham, L., Robson-Brown, K. Human Roots: Africa and Asia in the Middle Pleistocene Western Academic and Specialist Press Limited, Bristol.5–21.Google Scholar
Radhakrishnamurty, C., and Likhite, S.D. (1970). Hopkinson effect, blocking temperature and Curie point in basalts. Earth and Planetary Science Letters 7, 389–396.Google Scholar
Roberts, A.P., Cui, Y., and Verosub, K.L. (1995). Wasp-waisted hysteresis loops: mineral magnetic characteristics and discrimination of components in mixed magnetic systems. Journal of Geophysical Research 100, 17909–17924.Google Scholar
Sarna-Wojcicki, A.M., Pringle, M.S., and Wijbrans, J. (2000). New 40Ar/39Ar age of the Bishop Tuff from multiple sites and sediment rate calibration for the Matuyama-Brunhes boundary. Journal of Geophysical Research 105, 21431–21443.Google Scholar
Schick, K.D., and Dong, Z. (1993). Early Paleolithic of China and Eastern Asia. Evolutionary Anthropology 2, 22–35.Google Scholar
Schick, K.D., Toth, N., Wei, Q., Clark, J.D., and Etler, D. (1991). Archaeological perspectives in the Nihewan Basin, China. Journal of Human Evolution 21, 13–26.Google Scholar
Singer, B.S., Hoffman, K.A., Chauvin, A., Coe, R.S., and Pringle, M.S. (1999). Dating transitionally magnetized lavas of the late Matuyama Chron: toward a new 40Ar/39Ar timescale of reversals and events. Journal of Geophysical Research 104, B1 679–693.Google Scholar
Stacey, F.D., and Banerjee, S.K. (1974). The Physical Principles of Rock Magnetism. Elsevier, Amsterdam.195 pp.Google Scholar
Swisher, C.C., Curtis, G.H., Jacob, T., Getty, A.G., Suprijo, A., Widiasmoro, (1994). Age of the earliest known hominids in Java, Indonesia. Science 263, 1118–1121.Google Scholar
Tang, Y.J., Li, Y., and Chen, W.Y. (1995). Mammalian fossils and the age of Xiaochangliang Paleolithic site of Yangyuan, Hebei. Vertebrata Palasiatica 33, 1 74–83.In Chinese with English abstractGoogle Scholar
Teilhard de Chardin, P., and Piveteau, J. (1930). Les mammiferes fossils de Nihowan (China). Annales de Paleontologie 19, 3–132.Google Scholar
Vekua, A., Lordkipanidze, D., Philip Rightmire, G., Agusti, J., Ferring, R., Maisuradze, G., Mouskhelishvili, A., Nioradze, M., Ponce de Leon, M., Tappen, M., Tvalchrelidze, M., and Zollikofer, C. (2002). A new skull of early Homo from Dmanisi, Georgia. Science 297, 85–89.Google Scholar
Wang, X.S., Yang, Z.Y., Løvlie, R., and Min, L.R. (2004). High-resolution magnetic stratigraphy of fluvio-lacustrine succession in the Nihewan Basin, China. Quaternary Science Reviews 23, 1187–1198.CrossRefGoogle Scholar
Wei, Q. (1985). Preliminary observation of Donggutuo Palaeolithics. Acta Anthropologica Sinica 4, 4 289–300.In ChineseGoogle Scholar
Wei, Q. (1991). Geologic sequence of the archaeological sites in the Nihewan Basin, North China.In: IVPP (Institute of Vertebrate Paleontology and Paleoanthropology)(Ed.), Contributions to the XIII INQUA. Beijing Scientific and Technological Publishing House, Beijing., pp. 61-73. In Chinese with English abstract.Google Scholar
Wei, Q. (1994). Banshan Paleolithic site from the Lower Pleistocene in the Nihewan Basin in Northern China. Acta Anthropologica Sinica 13, 3 223–238.In Chinese with English abstractGoogle Scholar
Wei, Q. (1997). The framework of archaeological geology of the Nihewan basin.Tong, Y.S. Evidence of Evolution–Essays in Honor of Prof. Chungchien Young on the Hundredth Anniversary of His Birth China Ocean Press, Beijing.193–207.In Chinese with English abstractGoogle Scholar
Wei, Q., Meng, H., and Cheng, S.Q. (1985). New Paleolithic site from the Nihewan beds. Acta Anthroplogica Sinica 4, 3 223–232.In ChineseGoogle Scholar
You, Y.Z., Tang, Y.J., and Li, Y. (1980). New discovery of palaeoliths in the Nihewan formation. Quaternaria Sinica 5, 1 1–13.In ChineseGoogle Scholar
Young, C.C. (1950). The Plio-Pleistocene boundary in China. Report on 18th International Geological Congress, London 115–125.Google Scholar
Yuan, B.Y., Zhu, R.X., Tian, W.L., Cui, J.X., Li, R.Q., Wang, Q., and Yan, F.H. (1996). The age, subdivision and correlation of Nihewan Group. Science in China (Series D) 26, 67–73.In ChineseGoogle Scholar
Zhu, R.X., Deng, C.L., and Jackson, M.J. (2001a). )A magnetic investigation along a NW-SE transect of the Chinese Loess Plateau and its implications. Physics and Chemistry of the Earth (A) 26, 867–872.Google Scholar
Zhu, R.X., Hoffman, K.A., Potts, R., Deng, C.L., Pan, Y.X., Guo, B., Shi, C.D., Guo, Z.T., Yuan, B.Y., Hou, Y.M., and Huang, W.W. (2001b). )Earliest presence of humans in northeast Asia. Nature 413, 413–417.Google Scholar
Zhu, R.X., An, Z.S., Potts, R., and Hoffman, K.A. (2003). Magnetostratigraphic dating of early humans in China. Earth-science Reviews 61, 341–359.Google Scholar
Zhu, R.X., Potts, R., Xie, F., Hoffman, K.A., Deng, C.L., Shi, C.D., Pan, Y.X., Wang, H.Q., Shi, R.P., Wang, Y.C., Shi, G.H., and Wu, N.Q. (2004). New evidence on the earliest human presence at high northern latitudes in Northeast Asia. Nature 431, 559–562.Google Scholar
Zijderveld, J.D.A. (1967). A.C. demagnetization of rocks: analysis of results.Collinson, D.W., Creer, K.M., Runcorn, S.K. Methods on Palaeomagnetic Elsevier, New York.254–286.Google Scholar