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

Tibetan permafrost largely formed during the late Pleistocene glacial period and shrank in the Holocene Thermal Maximum period. Quantifying the impacts of paleoclimatic extremes on soil carbon stock can shed light on the vulnerability of permafrost carbon in the future. Here, we synthesize data from...

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Detalles Bibliográficos
Autores principales: Ding, Jinzhi, Wang, Tao, Piao, Shilong, Smith, Pete, Zhang, Ganlin, Yan, Zhengjie, Ren, Shuai, Liu, Dan, Wang, Shiping, Chen, Shengyun, Dai, Fuqiang, He, Jinsheng, Li, Yingnian, Liu, Yongwen, Mao, Jiafu, Arain, Altaf, Tian, Hanqin, Shi, Xiaoying, Yang, Yuanhe, Zeng, Ning, Zhao, Lin
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2019
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6744502/
https://www.ncbi.nlm.nih.gov/pubmed/31519899
http://dx.doi.org/10.1038/s41467-019-12214-5

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