The paleoclimatic footprint in the soil carbon stock of the Tibetan permafrost region

Data and code availability The authors declare that the majority of the data supporting the findings of this study are available through the links given in the paper. The unpublished data are available from the corresponding author upon request. The new estimate of Tibetan soil carbon stock and R co...

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Bibliographic Details
Published in:Nature Communications
Main Authors: Ding, Jinzhi, Wang, Tao, Piao, Shilong, Smith, Pete, Zhang, Ganlin, Yan, Zhengjie, Ren, Shuai, Liu, Dan, Wang, Shiping, Chen, Shengyun, Dai, Fuqiang, He, Jin-Sheng, Li, Yingnian, Liu, Yongwen, Mao, Jiafu, Arain, Altaf, Tian, Hanqin, Shi, Xiaoying, Yang, Yuanhe, Zeng, Ning, Zhao, Lin
Other Authors: University of Aberdeen.Energy, University of Aberdeen.Environment and Food Security, University of Aberdeen.Biological Sciences
Format: Article in Journal/Newspaper
Language:English
Published: 2019
Subjects:
SDG 13 - Climate Action
carbon cycle
cryospheric science
paleoclimate
STORAGE
MATTER
CATION-EXCHANGE
STABILIZATION
CLIMATE-CHANGE
MECHANISMS
PLATEAU
ORGANIC-CARBON
DEGRADATION
PEDOGENESIS
QH301 Biology
General Physics and Astronomy
General Chemistry
General Biochemistry,Genetics and Molecular Biology
Supplementary Data
QH301
permafrost
Online Access:http://hdl.handle.net/2164/13042
https://doi.org/10.1038/s41467-019-12214-5
http://www.scopus.com/inward/record.url?scp=85072190356&partnerID=8YFLogxK
https://figshare.com/s/4374f28d880f366eff6d
Description
Summary:Data and code availability The authors declare that the majority of the data supporting the findings of this study are available through the links given in the paper. The unpublished data are available from the corresponding author upon request. The new estimate of Tibetan soil carbon stock and R code are available in a persistent repository (https://figshare.com/s/4374f28d880f366eff6d). Acknowledgements This study was supported by the Strategic Priority Research Program (A) of the Chinese Academy of Sciences (XDA20050101), the National Natural Science Foundation of China (41871104), Key Research and Development Programs for Global Change and Adaptation (2017YFA0603604), International Partnership Program of the Chinese Academy of Sciences (131C11KYSB20160061) and the Thousand Youth Talents Plan project in China. Jinzhi Ding acknowledges the General (2017M620922) and the Special Grade (2018T110144) of the Financial Grant from the China Postdoctoral Science Foundation. Peer reviewed

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