Spatiotemporal evolution of cultural sites in Qinghai Tibet Plateau since Holocene and its driving forces
The data set is stored in Excel format and contains three worksheets: altitude, density of each stage and zero index. The altitude worksheet includes Paleolithic altitude, Neolithic altitude, bronze altitude, Tubo divide and rule altitude, Tubo Dynasty altitude, Yuan Dynasty altitude, Ming Dynasty altitude, Qing Dynasty altitude, modern altitude and age data; There are three sheets in the density worksheet of each stage, which are quantity + area, quantity, density and the corresponding natural division, respectively representing the number and density of Paleolithic sites, Neolithic sites, bronze sites, Tubo divided period sites, Tubo Dynasty sites, Yuan Dynasty sites The number and density of Ming Dynasty sites, Qing Dynasty sites and modern sites; In the zero point index worksheet, there are two sheet tables representing the zero point index and spatial autocorrelation respectively. In the nearest point index, there are the average observation distance, expected average distance, nearest neighbor ratio and Z score p value of Paleolithic, Neolithic, bronze, Tubo tribe, Tubo Dynasty, yuan, Ming, Qing and modern sites.
Hou, G. (2021). Spatiotemporal evolution of cultural sites in Qinghai Tibet Plateau since Holocene and its driving forces. A Big Earth Data Platform for Three Poles, DOI: 10.11888/Paleoenv.tpdc.271277. CSTR: 18406.11.Paleoenv.tpdc.271277. (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.Li, K.F., Zhu, C., Wang, X.H., et al. (2013).The archaeological sites distribution and its relationship with physical environment from around 260 ka BP to 221 BC in Guizhou Province. Acta Geographica Sinica, 68(1):58-68. (View Details )
3.Hou, G.L., Xu, C.G., Cao, G.C., et al. (2017).The spatial-temporal simulation of mankind’s expansion on the Tibetan Plateau during Last Deglaciation-Middle Holocene. Quaternary Research, 37(4),709-720. (View Details )
4.Cui, Y.F., Liu, Y.J., Ma, M.M.(2018).Spatiotemporal evolution of prehistoric Neolithic-Bronze Age settlements and influencing factors in the Guanting Basin Northeast Tibetan Plateau. China Earth Sciences, 48 (2),152-164. (View Details )
5.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 )
6.Chen, F.H., Wu, D., Chen, J.H.(2016). Holocene moisture and East Asian summer monsoon evolution in the northeastern Tibetan Plateau recorded by Lake Qinghai and its environs: A review of conflicting proxies. Quaternary Science Reviews,5(24),111-129. (View Details )
7.Xie Chuanli, Jian Zhimin, Zhao Quanhong, Wang Pinxian. (1996). The paleogeographic configuration of China seas and its climatic influence during the last glacial maximum. Quaternary studies (01) doi:CNKI :SUN:DSJJ.0.1996-01-000. (View Details )
8.Hou, G.L., Xu, C.G.(2016). The temperature change and its influence for human movement of the Tibet Plateau over the past 2000 years. Journal of Qinghai Normal University(Natural Science Edition) , 3(12),56-62. (View Details )
9.Ma, M.M., Dong, G.H., Jia, X.(2012). Analysis of settlement patterns during Neolithic and Bronze period and its influencing factors in Hualong County Qinghai Province China.Quaternary Research, 32(3) : 209 -218. (View Details )
10.Huang Chunchang, Guo Yongqiang, Zhang Yuzhu, Zhou Yali, Zhao Hui, Zheng Zixing... & Liu Tao. (2019). Holocene sedimentary stratigraphy and pre-historical catastrophes over the Lajia Ruins within the Guanting Basin in Qinghai Province of China. Chinese Science: Geosciences (02), 434-455 (View Details )
11.Yi, X., Liang, y.y., Huerta-Sanchez, E. (2010).Sequencing of 50 human exomes reveals adaptation to high altitude. Science, 329(12),75 -78. (View Details )
12.Lu, H.Y. (2012). Modern pollen distributions in Qinghai-Tibetan Plateau and the development of transfer functions for reconstructing Holocene environmental changes. Quaternary International, 30(12), 947-966. (View Details )
13.Tang, H.S., Zhou, C.L., Li, Y.Q.(2013). A new discovery of microlithic information at the entrance to the Northern Qingzang Plateau of the Kunlun Mountains of Qinghai. Chinese Science Bulletin, 58(3),247 -253. (View Details )
14.Huang,J., Gao, Y., Zhao, Z.Q.,Li, S.C. (2011). Comprehensive physiographic regionalization of China using GIS and SOFM neural network. Geographic research, (09), 1648-1659 (View Details )
15.Zhang, D.E., Li, H.C., Gu, D.L.,Lu, L.H. (2010). On linking climate to Chinese dynastic change: Spatial and temporal variations of monsoonal rain. Science Bulletin,55(01), 60-67. (View Details )
Qinghai Provincial Key Laboratory of Geospatial Information Technology and Application Foundation Project (No:2018-006)
National Natural Science Foundation of China, No.41761018 (No:41761018)
To respect the intellectual property rights, protect the rights of data authors, expand services of the data center, and evaluate the application potential of data, data users should clearly indicate the source of the data and the author of the data in the research results generated by using the data (including published papers, articles, data products, and unpublished research reports, data products and other results). For re-posting (second or multiple releases) data, the author must also indicate the source of the original data.
License: This work is licensed under an Attribution 4.0 International (CC BY 4.0)
1.Physical and chemical index data of deep drilling strata in the middle reaches of Heihe River (2013)
2.Spring hydroclimate reconstruction on the south-central Tibetan Plateau
3.Tree age data sampled from different glacier moraines in the central Himalayas
6.Tree ring width data of Qilian mountains in the East Asian Monsoon region
8.Palynological data of vegetation evolution since the formation of Heihe River
10.The tree ring dataset of populus euphratica in the downstream of the Heihe River
No record
No record
Current page automatically show English comments Show comments in all languages
East: 104.47 | West: 73.19 |
---|---|
South: 26.00 | North: 39.47 |
Contact Support
Northwest Institute of Eco-Environment and Resources, CAS 0931-4967287 poles@itpcas.ac.cnLinks
National Tibetan Plateau Data CenterFollow Us
A Big Earth Data Platform for Three Poles © 2018-2020 No.05000491 | All Rights Reserved | No.11010502040845
Tech Support: westdc.cn