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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...

詳細記述

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書誌詳細
出版年:Nat Commun
主要な著者: 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
フォーマット: Artigo
言語:Inglês
出版事項: Nature Publishing Group UK 2019
主題:
オンライン・アクセス: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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