Abstract
Shuidonggou is one of the most important Upper Paleolithic sites in North China. Due to the presence of rich human remains, animal fossils, abundant sporopollen and unique geological sequence, it is the type site for Late Pleistocene to Holocene human occupation and environmental change in the Ningxia-Inner Mongolia region. Many scholars suggest that the site should be named the “Shuidonggou Formation” of Late Pleistocene in North China. Dating results indicate that ancient human activities at the site took place 30–24 ka (Marine Isotope Stage [MIS] 3). The climate at that time was warmer and moister than present day, and adequate precipitation led to the formation of water pack depressions where broad-leaf trees and sparse forest vegetations, as well as herbivorous animals flourished, making the area suitable for early human hunting, gathering and survival. The Neolithic human occupation happened 9–5 ka at the site, while similar environmental conditions with MIS3 occurred. The absence of human activity record in the region during the Last Glacial Maximum (MIS2) suggests that the environment was too harsh for humans to live there.
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References
Licent E, Teilhard de chardin P., Le Paleolithique, de la Chine. L’Anthropologie, 1925, 25: 201–234
Jia L P, Gai P, Li Y X. New materials from Shuidonggou Paleolithic site. Vertebr. PalAsiatica, 1964, 8(1): 75–83
Wang Y P. A Paleolithic site in the Shuidonggou village. Archaeology (in Chinese), 1962, (11): 601–604
Zhou K S, Hu J L. Environment and stratigraphy at the Shuidonggou site. Acta Anthropol Sin, 1988, 7(3): 263–269
Institute of Archeology of Ningxia Hui Autonomous Region. Shuidonggou—Report on the excavation in 1980. Beijing: Science Press, 2003. 1–233
Gao X, Wang H M, Pei S W, et al. Tracing the footprints of human groups from Shuidonggou. In: Institute of Archeology of Yunnan Province, ed. Collected Works for “The International Conference in Commemoration of the 40th Anniversary of the Discovery of Yunmou Man” (in Chinese). Kunming: Yunnan Science and Technology Press, 2006. 152–158
Gao X, Li J Z, Madsen D B. et al. New 14C dates for Shuidonggou and related discussions. Acta Anthropol Sin (in Chinese), 2001, 21(3): 211–218
Bureau of Geology and Mineral Resouces of Ningxia. Report of Geological and Regional Survey of 1:200000〈Yinchuan〉 (in Chinese). Lanzhou: Printing Factory of China Geological Map. 1983
Teilhard de chardin. Mammiferes Tertiares de Chine et de Mongolia. Ann de Paleon, 1926, 15: 1–51
Yang Z J, Zhou M Z. Latest discoveries in vertebrate Paleontology in China. Acta Palaeontol Sin (in Chinese), 1956, 4(4): 447–459
Sun J Z, Zhao J B. Quaternary Geology in the Loess Plateau (in Chinese). Beijing: Science Press, 1991
Chen T M, Yuan S X, Gao S J. The study on Uranium-series dating of fossil bones and an absolute age sequence for the main Paleolihic sites of North China. Acta Anthropol Sin (in Chinese), 1984, 3(3): 259–269
Li X G, Liu G L, Xu G Y, et al. Dating reports on the 14C dating methodology (PV). In: Radiocarbon Dating Society of Chinese Quaternary Research Association, ed. Contribution to the Quaternary Glaciology and Geology (4) (in Chinese). Beijing: Geological Publishing House, 1987, 16–38
Imbrie J, Hays J D, Martinson D G, et al. The orbital theory of Pleistocene climate: Support from a revised chronology of the marine δ 18O record. In: Berger A, Imbrie J, Hays J D, et al. eds. Milankovitch and Climate. Netherlands: Reidel Dordrent, 1984. 169–305
Ningxia Museum & the Ningxia Geological Survey. A Report on the Excavation of Shuidonggou Site in 1980. Acta Archaeol Sin (in Chinese), 1987, (4): 439–448
Li B C. New understanding on the Paleo-climate at Shuidonggou since 10 ka. J Arid Land Resour Environ, 2006, 20(4): 25–29
Boule M, Breuil H, Licent E, et al. Le Pateolithique de la China. Paris: Archives de l’institut de Paleontologie Humaine, 1928
Lu H Y, Wu N Q, Liu K M, et al. Hydroliths as quantitative indicators for the reconstruction of past environmental conditions in China II: Paleoenvironmental reconstruction in the Loess Plateau. Quat Sci Rev, 2007, 26: 759–772
Wu H B, Guo Z T. Evolution and drought events in arid region of Northern china since the Last Glacial Maximum. Quat Sci (in Chinese), 2000, 20(6): 548–558
Wen X H, Li B S, Zhang D, et al. Megainterstadial climate of the Salawusu valley-Milangouwan stratigraphic section. Acta Geologica Sin (in Chinese). 2007, 81(4): 553–562
Yang X P. Development of landscape and change of precipitation of Badain Jaran Desert since 30000 years ago. Chin Sci Bull, 2000, 45(4): 428–434
Yang X P. Water chemistry of the lakes in the Badain Jaran Desert and their Holocene evolutions. Quat Sci, 2002, 22(2): 97–104
Zhou K S. Shuidonggou site is the standard section in North China since 30 ka. In: Zhong K, Gao X, eds. Paleolithic Essays for the Conference in Commemoration of the 80th Anniversary of the Discovery of the Shuidonggou Site (in Chinese). Beijing: Cultural Relics Press, 2006. 57–58
Yuan B Y, Hou Y M, Budja M, et al. The framework of the prehistory and stratigraphic subdivision of Late Pleistocene in North China. In: Zhong K, Gao X, eds. Paleolithic Essays for the Conference in Commemoration of the 80th Anniversary of the Discovery of the Shuidonggou Site (in Chinese). Beijing: Cultural Relics Press, 2006. 8–16
Geng K, Shan P F. The Yinchuan Area: Past, Present and Future (in Chinese). Beijing: Cultural Relics Press, 1992
Yuan B Y. Sedimentary environment and Stratigraphic subdivision of Salawusu Formation. Sci Geol (in Chinese), 1978, (3): 320–334
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Supported by the Major Basic Research Projects (Grant No. 2006CB806400) of MST of China and the National Natural Science Foundation of China-General Program (Grant No. 40472016)
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Gao, X., Yuan, B., Pei, S. et al. Analysis of sedimentary-geomorphologic variation and the living environment of hominids at the Shuidonggou Paleolithic site. Chin. Sci. Bull. 53, 2025–2032 (2008). https://doi.org/10.1007/s11434-008-0264-y
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DOI: https://doi.org/10.1007/s11434-008-0264-y