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

There was extensive degradation during the warm middle Holocene and permafrost area was reduced substantially. Here the authors synthesize data across the Tibetan permafrost region and find that paleoclimate is more important than modern climate in shaping current permafrost carbon distribution, and...

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Autores principales: Jinzhi Ding, Tao Wang, Shilong Piao, Pete Smith, Ganlin Zhang, Zhengjie Yan, Shuai Ren, Dan Liu, Shiping Wang, Shengyun Chen, Fuqiang Dai, Jinsheng He, Yingnian Li, Yongwen Liu, Jiafu Mao, Altaf Arain, Hanqin Tian, Xiaoying Shi, Yuanhe Yang, Ning Zeng, Lin Zhao
Formato: article
Lenguaje:EN
Publicado: Nature Portfolio 2019
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Acceso en línea:https://doaj.org/article/40671f7f6fe345d0906e484b1c58379c
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Sumario:There was extensive degradation during the warm middle Holocene and permafrost area was reduced substantially. Here the authors synthesize data across the Tibetan permafrost region and find that paleoclimate is more important than modern climate in shaping current permafrost carbon distribution, and its importance increases with soil depth.