Published April 11, 2022 | Version 2022.1
Dataset Open

Geographical and geological GIS boundaries of the Tibetan Plateau and adjacent mountain regions

Creators

  • 1. Kunming Institute of Botany, Chinese Academy of Sciences

Description

Introduction

Geographical scale, in terms of spatial extent, provide a basis for other branches of science. This dataset contains newly proposed geographical and geological GIS boundaries for the Pan-Tibetan Highlands (new proposed name for the High Mountain Asia), based on geological and geomorphological features. This region comprises the Tibetan Plateau and three adjacent mountain regions: the Himalaya, Hengduan Mountains and Mountains of Central Asia, and boundaries are also given for each subregion individually. The dataset will benefit quantitative spatial analysis by providing a well-defined geographical scale for other branches of research, aiding cross-disciplinary comparisons and synthesis, as well as reproducibility of research results.

The dataset comprises three subsets, and we provide three data formats (.shp, .geojson and .kmz) for each of them. Shapefile format (.shp) was generated in ArcGIS Pro, and the other two were converted from shapefile, the conversion steps refer to 'Data processing' section below. The following is a description of the three subsets:

(1) The GIS boundaries we newly defined of the Pan-Tibetan Highlands and its four constituent sub-regions, i.e. the Tibetan Plateau, Himalaya, Hengduan Mountains and the Mountains of Central Asia. All files are placed in the "Pan-Tibetan Highlands (Liu et al._2022)" folder.

(2) We also provide GIS boundaries that were applied by other studies (cited in Fig. 3 of our work) in the folder "Tibetan Plateau and adjacent mountains (Others’ definitions)". If these data is used, please cite the relevent paper accrodingly. In addition, it is worthy to note that the GIS boundaries of Hengduan Mountains (Li et al. 1987a) and Mountains of Central Asia (Foggin et al. 2021) were newly generated in our study using Georeferencing toolbox in ArcGIS Pro.

(3) Geological assemblages and characters of the Pan-Tibetan Highlands, including Cratons and micro-continental blocks (Fig. S1), plus sutures, faults and thrusts (Fig. 4), are placed in the "Pan-Tibetan Highlands (geological files)" folder.

Note: High Mountain Asia: The name ‘High Mountain Asia’ is the only direct synonym of Pan-Tibetan Highlands, but this term is both grammatically awkward and somewhat misleading, and hence the term ‘Pan-Tibetan Highlands’ is here proposed to replace it. Third Pole: The first use of the term ‘Third Pole’ was in reference to the Himalaya by Kurz & Montandon (1933), but the usage was subsequently broadened to the Tibetan Plateau or the whole of the Pan-Tibetan Highlands. The mainstream scientific literature refer the ‘Third Pole’ to the region encompassing the Tibetan Plateau, Himalaya, Hengduan Mountains, Karakoram, Hindu Kush and Pamir. This definition was surpported by geological strcture (Main Pamir Thrust) in the western part, and generally overlaps with the ‘Tibetan Plateau’ sensu lato defined by some previous studies, but is more specific.

More discussion and reference about names please refer to the paper. The figures (Figs. 3, 4, S1) mentioned above were attached in the end of this document.

 

Data processing

We provide three data formats. Conversion of shapefile data to kmz format was done in ArcGIS Pro. We used the Layer to KML tool in Conversion Toolbox to convert the shapefile to kmz format. Conversion of shapefile data to geojson format was done in R. We read the data using the shapefile function of the raster package, and wrote it as a geojson file using the geojson_write function in the geojsonio package.

 

Version

Version 2022.1.

 

Acknowledgements

This study was supported by the Strategic Priority Research Program of Chinese Academy of Sciences (XDB31010000), the National Natural Science Foundation of China (41971071), the Key Research Program of Frontier Sciences, CAS (ZDBS-LY-7001). We are grateful to our coauthors insightful discussion and comments. We also want to thank professors Jed Kaplan, Yin An, Dai Erfu, Zhang Guoqing, Peter Cawood, Tobias Bolch and Marc Foggin for suggestions and providing GIS files.

 

Citation

Liu, J., Milne, R. I., Zhu, G. F., Spicer, R. A., Wambulwa, M. C., Wu, Z. Y., Li, D. Z. (2022). Name and scale matters: Clarifying the geography of Tibetan Plateau and adjacent mountain regions. Global and Planetary Change, In revision

 

Jie Liu & Guangfu Zhu. (2022). Geographical and geological GIS boundaries of the Tibetan Plateau and adjacent mountain regions (Version 2022.1). https://doi.org/10.5281/zenodo.6432940

 

Contacts

Dr. Jie LIU: E-mail: liujie@mail.kib.ac.cn;

Mr. Guangfu ZHU: zhuguangfu@mail.kib.ac.cn

Institution: Kunming Institute of Botany, Chinese Academy of Sciences

Address: 132# Lanhei Road, Heilongtan, Kunming 650201, Yunnan, China

 

Copyright

This dataset is available under the Attribution-ShareAlike 4.0 International (CC BY-SA 4.0).

Files

Pan-Tibetan Highlands.zip

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Additional details

References

  • Bolch, T., Kulkarni, A., Kääb, A., Huggel, C., Paul, F., Cogley, J. G., Stoffel, M. (2012). The state and fate of Himalayan glaciers. Science, 336, 310-314. https://doi.org/10.1126/science.1215828
  • Bolch, T., Shea, J. M., Liu, S., Azam, F. M., Gao, Y., Gruber, S., Zhang, Y. (2019). Status and change of the cryosphere in the extended Hindu Kush Himalaya region. In P. Wester, A. Mishra, A. Mukherji, & A. B. Shrestha (Eds.), The Hindu Kush Himalaya Assessment: Mountains, Climate Change, Sustainability and People (pp. 209-255). Cham, Switzerland: Springer Nature.
  • Cawood, P. A., Zhao, G., Yao, J., Wang, W., Xu, Y., & Wang, Y. (2018). Reconstructing South China in Phanerozoic and Precambrian supercontinents. Earth-Science Reviews, 186, 173-194. https://doi.org/10.1016/j.earscirev.2017. 06.001
  • Foggin, J. M., Lechner, A. M., Emslie-Smith, M., Hughes, A. C., Sternberg, T., & Dossani, R. (2021). Belt and Road Initiative in Central Asia: Anticipating socioecological challenges from large-scale infrastructure in a global biodiversity hotspot. Conservation Letters, 14, e12819. https://doi.org/10.1111/conl.12819
  • Jolivet, M., Heilbronn, G., Robin, C., Barrier, L., Bourquin, S., Guo, Z., . . . Fu, B. (2013). Reconstructing the Late Palaeozoic – Mesozoic topographic evolution of the Chinese Tian Shan: available data and remaining uncertainties. Adv. Geosci., 37, 7-18. https://doi.org/10.5194/adgeo-37-7-2013
  • Körner, C., Jetz, W., Paulsen, J., Payne, D., Rudmann-Maurer, K., & M. Spehn, E. (2017). A global inventory of mountains for bio-geographical applications. Alpine Botany, 127, 1-15. https://doi.org/10.1007/s00035-016-0182-6
  • Li, B. Y. (1987a). On the boundaries of the Hengduan Mountains. Journal of Mountain Research, 5, 74-82.
  • Li, B. Y. (1987b). On the extent of the Qinghai-Xizang (Tibet) Plateau. Geographical Research, 6, 57-64.
  • Li, J. Y. (2006). Permian geodynamic setting of Northeast China and adjacent regions: Closure of the Paleo-Asian Ocean and subduction of the Paleo-Pacific Plate. Journal of Asian Earth Sciences, 26, 207-224. https://doi.org/10.1016/j.jseaes.2005.09.001
  • McRivette, M. W., Yin, A., Chen, X., & Gehrels, G. E. (2019). Cenozoic basin evolution of the central Tibetan plateau as constrained by U-Pb detrital zircon geochronology, sandstone petrology, and fission-track thermochronology. Tectonophysics, 751, 150-179. https://doi.org/10.1016/j.tecto.2018.12.015
  • Mittermeier, R. A., Gil, P. R., Hoffman, M., Pilgrim, J., Brooks, T., Mittermeier, C., Saligmann, P. A. (2004). Hotspots revisited: Earth's biologically richest and most endangered ecoregions (2nd ed.). Mexico City, Mexico: CEMEX.
  • Rana, S. K., Price, T. D., & Qian, H. (2019). Plant species richness across the Himalaya driven by evolutionary history and current climate. Ecosphere, 10, e02945. https://doi.org/10.1002/ecs2.2945
  • Ren, J., Niu, B., Wang, J., Jin, X., Zhao, L., & Liu, R. (2013). Advances in research of Asian geology—A summary of 1: 5M International Geological Map of Asia project. Journal of Asian Earth Sciences, 72, 3-11. https://doi.org/10.1016/j.jseaes.2013.02.006
  • Taylor, M., & Yin, A. (2009). Active structures of the Himalayan-Tibetan orogen and their relationships to earthquake distribution, contemporary strain field, and Cenozoic volcanism. Geosphere, 5, 199-214. https://doi.org/10.1130/GES00217.1
  • Wang, Y., Dai, E., Yin, L., & Ma, L. (2018). Land use/land cover change and the effects on ecosystem services in the Hengduan Mountain region, China. Ecosystem Services, 34, 55-67. https://doi.org/10.1016/j.ecoser.2018.09.008
  • Yin, A., & Harrison, T. M. (2000). Geologic evolution of the Himalayan-Tibetan orogen. Annual Review of Earth and Planetary Sciences, 28, 211-280. https://doi.org/10.1146/annurev.earth.28.1.211
  • Zhang, G., Yao, T., Xie, H., Kang, S., & Lei, Y. (2013). Increased mass over the Tibetan Plateau: From lakes or glaciers? Geophysical Research Letters, 40, 2125-2130. https://doi.org/10.1002/grl.50462
  • Zhang, Y., Li, B., & Zheng, D. (2002). A discussion on the boundary and area of the Tibetan Plateau in China. Geographical Research, 21, 1-8. https://doi.org/10.11821/yj2002010001