Supplementary Materials

Supplementary Materials

Supplementary Materials Spatial and temporal variations in prehistoric human settlement and their influencing factors on the south bank of the Xar Maron River, Northeastern China Xin JIA1*, Shuangwen YI1, Yonggang SUN2, Shuangye WU1, 3 Harry F. LEE4, Lin WANG5, & Huayu LU1 Supplementary References S1: Supplementary references to the 14C chronological dating 1. 14C laboratory, Archaeological Science and Techniques Experiment and Research Center, IA, CASS (1993). Dating report on radiocarbon dates (20). Archaeology, (7): 645‒649 (in Chinese) 2. 14C laboratory, Archaeological Science and Techniques Experiment and Research Center, IA, CASS (1994). Dating report on radiocarbon dates (21). Archaeology, (7): 662‒664 (in Chinese) 3. 14C laboratory, Archaeological Science and Techniques Experiment and Research Center, IA, CASS (1997). Dating report on radiocarbon dates (24). Archaeology, (7): 611‒614 (in Chinese) 4. 14C laboratory, Archaeological Science and Techniques Experiment and Research Center, IA, CASS (1999). Dating report on radiocarbon dates (25). Archaeology, (7): 656‒659 (in Chinese) 5. 14C laboratory, Archaeological Science and Techniques Experiment and Research Center, IA, CASS (2000). Dating report on radiocarbon dates (26). Archaeology, (7): 754‒758 (in Chinese) 6. 14C laboratory, Archaeological Science and Techniques Experiment and Research Center, IA, CASS (2001). Dating report on radiocarbon dates (27). Archaeology, (7): 662‒666 (in Chinese) 7. 14C laboratory, Archaeological Science and Techniques Experiment and Research Center, IA, CASS (2004). Dating report on radiocarbon dates (30). Archaeology, (7): 642‒647 (in Chinese)1. Institute of Archaeology, CASS (1992). 14C chronological data set from Chinese archaeology (1965‒1991). Cultural Relics Publishing House, Beijing, pp. 54‒65 (in Chinese) 8. Liu XY, John M K, Zhao Z J, Liu G X, Connell T C O (2012). The Earliest Evidence of Millet as a Staple Crop: New Light on Neolithic Foodways in North China. American Journal of Physical Anthropology, 149(2): 283‒290 S2: Supplementary references to the chronological dating on Horqin Dunefield evolution. 1. Chronology Laboratory in Department of Geography at Lanzhou University (1987). Data Report on 14C dating from geological samples (LuG) I. In: 14C Group of China Quaternary Research Committee (Eds.), Symposium of Quaternary glacier and Quaternary Geology (4). Geological Publishing House, Beijing, pp. 102 (in Chinese) 2. Dong G R, Jin J, Li B S, Gao S Y, Shao Y J (1994). Several problems on the desertification of Horqin sandy land, Northeast China-a case study on its south area. Journal of Desert Research, 14(1): 1‒9 (in Chinese with English abstract) 3. Joseph A M, Lu H Y, Zhou Y L, Miao X D, James B S, Liu Z Y, Ronald J G, Yi S W (2009). Dune mobility and aridity at the desert margin of northern China at a time of peak monsoon strength. Geology, 37(10): 947‒950 4. Liu B, Jin H L, Sun Z (2013). Desert Evolution and Climate Change in the Horqin Sandy Land in Middle and Late Holocene. Journal of Desert Research, 33(1): 1398‒1405 (in Chinese with English abstract) 5. Lu H Y, Miao X D, Zhou Y L, Joseph M, Zhang J F, Zhou L P, Yi S W (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): 2465‒2481 6. Lu H Y, Zhou Y L, Liu W G, Joseph M (2012). Organic stable carbon isotopic composition reveals late quaternary vegetation changes in the dune fields of northern China. Quaternary Research, 77(3): 433‒444 7. Qiu SW (1989). Study on the formation and evolution of Horqin sandy land. Scientia Geographica Sinica, 9(4): 317‒328 (in Chinese with English abstract) 8. Qiu S W, Li Q S, Xia Y M (1992). Paleosols of sandy lands and environmental changes in the Western Plain of Northeast China during Holocene. Quaternary Sciences, 12(3): 224‒232 (in Chinese with English abstract) 9. Yang L H, Wang T, Zhou J, Lai Z P, Long H (2012). OSL chronology and possible forcing mechanisms of dune evolution in the Horqin Dunefield in northern China since the Last Glacial Maximum. Quaternary Research, 78(2): 185‒196 10. Yang L R, Yue L P (2013). Horqin Dunefield in Notheastern China in the Last late Glacial and Holocene as revealed by OSL dating. Quaternary Sciences, 33(2): 260‒268 (in Chinese with English abstract) 11. Yi S W, Lu H Y, Zeng L, Xu Z W (2013). Paleoclimate changes and reconstruction of the border of Horqin Dunefield (Northeastern China)since the last Giacial Maximum. Quaternary Sciences, 33(2): 206‒217 (in Chinese with English abstract) 12. Zhang W S, Liu J F, Tian J L (1994). The Palaeomagnetic Event and Regional Geology of Loess at the top of south maintain, Chifeng. Journal of Hebei College of Geology, 17(3): 236‒244 (in Chinese with English abstract) 13. Zhao H, Lu Y C, Yin J H (2007). Optical dating of Holocene sand dune activities in the Horqin sand-fields in Inner Mongolia, China, using the SAR protocol. Quaternary Geochronology, 2(1‒4): 29‒33 14. Zhao S, Xia D S, Jin H L, Wen Y L, Liu J B, Liu B, Li G H (2013). High-resolution climate evolution record of the Horqin sandy land since about 5000cal.yr B.P.. Quaternary Sciences, 33(2): 281‒292 (in Chinese with English abstract) .

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