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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spelling oai:doaj.org-article:40671f7f6fe345d0906e484b1c58379c2021-12-02T16:51:00ZThe paleoclimatic footprint in the soil carbon stock of the Tibetan permafrost region10.1038/s41467-019-12214-52041-1723https://doaj.org/article/40671f7f6fe345d0906e484b1c58379c2019-09-01T00:00:00Zhttps://doi.org/10.1038/s41467-019-12214-5https://doaj.org/toc/2041-1723There 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.Jinzhi DingTao WangShilong PiaoPete SmithGanlin ZhangZhengjie YanShuai RenDan LiuShiping WangShengyun ChenFuqiang DaiJinsheng HeYingnian LiYongwen LiuJiafu MaoAltaf ArainHanqin TianXiaoying ShiYuanhe YangNing ZengLin ZhaoNature PortfolioarticleScienceQENNature Communications, Vol 10, Iss 1, Pp 1-9 (2019)
institution DOAJ
collection DOAJ
language EN
topic Science
Q
spellingShingle Science
Q
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
The paleoclimatic footprint in the soil carbon stock of the Tibetan permafrost region
description 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.
format article
author 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
author_facet 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
author_sort Jinzhi Ding
title The paleoclimatic footprint in the soil carbon stock of the Tibetan permafrost region
title_short The paleoclimatic footprint in the soil carbon stock of the Tibetan permafrost region
title_full The paleoclimatic footprint in the soil carbon stock of the Tibetan permafrost region
title_fullStr The paleoclimatic footprint in the soil carbon stock of the Tibetan permafrost region
title_full_unstemmed The paleoclimatic footprint in the soil carbon stock of the Tibetan permafrost region
title_sort paleoclimatic footprint in the soil carbon stock of the tibetan permafrost region
publisher Nature Portfolio
publishDate 2019
url https://doaj.org/article/40671f7f6fe345d0906e484b1c58379c
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