Spatiotemporal evolution and environmental change of ancient sites in Hexi Corridor
The data set is stored in Excel format, which includes two worksheets: "longitude and latitude table obtained from place names" and "longitude and latitude table obtained from information provided in books". The contents of the longitude and latitude table obtained according to the place names are "number, place, site name, latitude"/ ° N. Longitude/ ° E. Altitude / m, archaeological culture, age, area (M2), cultural layer (m) ". According to the information provided in the book, the contents of the longitude and latitude table are "number, location, site name, latitude"/ ° N. Longitude/ ° E. Altitude / m, archaeological culture, age, area (M2), cultural layer (m), vegetation. Data files can be opened with office software or imported into relational database system.
Hou, G. (2021). Spatiotemporal evolution and environmental change of ancient sites in Hexi Corridor. A Big Earth Data Platform for Three Poles, DOI: 10.11888/Paleoenv.tpdc.271278. CSTR: 18406.11.Paleoenv.tpdc.271278. (Download the reference: RIS | Bibtex )
Using this data, the data citation is required to be referenced and the related literatures are suggested to be cited.
1.An, C. B., Wang, L., Ji, D. X., et al. (2006). The temporal and spatial changes of Neolithic culturesin Gansu-Qinghai region and possible environmentalforcing. Quaternary Sciences, 26(6): 923-927. (View Details )
2.An, C. B., Wang, W., Duan, F. T., et al. (2017). Environmental changes and cultural exchangebetween East and West along the Silk Road in aridCentral Asia. Acta Geographica Sinica, 72(5), 875-891. (View Details )
3.Chai, Y. (1999). Millet. Beijing: China Agriculture Press. (View Details )
4.Chen, F. H., An, C. B., Dong, G. H., et al. (2017). Human activities, environmentalchanges, and rise and decline of Silk Road Civilization in Pan-Third Pole Region. Bulletin of Chinese Academy of Sciences, 32(9), 967-975. (View Details )
5.Chen, F. H., Zhang, J. W.,Cheng, B., et al. (2012). Late Quaternary high lake levels and environmental changes since last deglacial in Dalianhai Gonghe Basin in Qinghai Province. QuaternarySciences, 32(1), 122-131. (View Details )
6.Chen, G.K., Wang, H., LiY, X., et al. (2014). Xicheng Station site in Zhangye City Gansu Province. Archaeology, 59(7), 2-17. (View Details )
7.Dong, G.R., Jin, H.L., Chen, H.Z. (1997). Desert-loess boundary belt shift and climatic changesince the last interglacial period. Quaternary Sciences, 17(2), 158-167. (View Details )
8.Dong, G.H., Yang, Y.S., Han, J.Y., et al. (2017). Exploring the history of cultural exchangein prehistoric Eurasia from the perspectives of cropdiffusion and consumption. Scientia Sinica Terrae,47(5), 530-543. (View Details )
9.Duan, K.Q., Yao, T.D., Wang, N.L., et al. (2012). The unstable Holocene climaticchange recorded in an ice core from the central Tibetan Plateau. Scientia Sinica Terrae, 42(9), 1441-1449. (View Details )
10.Gansu Institute of Cultural Relics and Archaeology,School of Archaeology and Museology, PekingUniversity. (2011). Report on prehistoric archaeologicalsurvey in Hexi Corridor. Beijing, Cultural RelicsPublishing House. (View Details )
11.Han, J.Y. (2013). The polychromeceramic road and early Sino-Western culturalexchanges. Archaeology and Cultural Relics, 33(1),28-37. (View Details )
12.Hou, G.L., Xu, C.J., Xiao, J.Y. (2012). Comparative analysis ofprehistoric sites distribution around 4 ka BP in Gansu-Qinghairegion based on GIS. Scientia Geographica Sinica, 32(1),116–120. (View Details )
13.Li, J.J. (2006). Holocenevegetation and environmental change at Qingtu Lakein the Shiyang river drainage. Lanzhou, LanzhouUniversity. (View Details )
14.Dong,G.H., Jia,X., An, C.B., Ma, MM.(2012).Mid-Holocene climate change and its effect on prehistoric cultural evolution in eastern Qinghai Province China. Quaternary Research, 77,23-30. (View Details )
15.Dong, G. H., Yang, Y. S., Liu, X. Y., Li, H. M., Cui, Y. F., Wang, H., Chen, G. K., Dodson, J., & Chen, F. H. (2018). Prehistoric trans-continental cultural exchange in the Hexi Corridor, northwest China. The Holocene, 28(4), 621–628. (View Details )
16.Huang, C.C., Su, H.X. (2009). Climate change and Zhourelocations in early Chinese history. Journal of Historical Geography, 35(2), 297-310. (View Details )
17.Li, Y., Wang, N.A., Li, Z.L., et al. (2011). Holocene palynologicalrecords and their responses to the controversies ofclimate system in the Shiyang River drainage basin.Chinese Science Bulletin, 56(6), 535-546. (View Details )
18.Li, Y., Wang, N.A., Morril, C., et al. (2012). Millennial-scaleerosion rates in three inland drainage basins and theircontrolling factors since the Last Deglaciation aridChina. Palaeogeography, Palaeoclimatology, Palaeoecology, 365(1), 263-275. (View Details )
19.Liu, F.G., Zhang, Y.L., Feng, Z.D., et al. (2010). The impacts of climate change on the Neolithic cultures of Gansu-Qinghai region during the late Holocene Megathermal. Journalof Geographical Science, 20(3), 417–430. (View Details )
Natural Science Foundation Project of Qinghai Provincial Science and Technology Department (No:2017-ZJ-903)
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East: 104.45 | West: 92.21 |
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South: 37.15 | North: 41.30 |
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