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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Publié dans:Nat Commun
Auteurs principaux: 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
Format: Artigo
Langue:Inglês
Publié: Nature Publishing Group UK 2019
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Article
Accès en ligne:https://ncbi.nlm.nih.gov/pmc/articles/PMC6744502/
https://ncbi.nlm.nih.gov/pubmed/31519899
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/s41467-019-12214-5
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