Microbial Functional Responses Explain Alpine Soil Carbon Fluxes under Future Climate Scenarios
The warming pace in the Tibetan Plateau, which is predominantly occupied by grassland ecosystems, has been 0.2°C per decade in recent years, dwarfing the rate of global warming by a factor of 2. Many Earth system models project substantial carbon sequestration in Tibet, which has been observed.
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American Society for Microbiology
2021
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oai:doaj.org-article:534fc0b37b2346dda3d1aabe9dad38272021-11-03T18:15:37ZMicrobial Functional Responses Explain Alpine Soil Carbon Fluxes under Future Climate Scenarios2161-21292150-751110.1128/mBio.00761-20https://doaj.org/article/534fc0b37b2346dda3d1aabe9dad38272021-02-01T00:00:00Zhttps://journals.asm.org/doi/10.1128/mBio.00761-20https://doaj.org/toc/2161-2129https://doaj.org/toc/2150-7511 The warming pace in the Tibetan Plateau, which is predominantly occupied by grassland ecosystems, has been 0.2°C per decade in recent years, dwarfing the rate of global warming by a factor of 2. Many Earth system models project substantial carbon sequestration in Tibet, which has been observed.Qi QiYue HaoweiZhenhua ZhangJoy D. Van NostrandLinwei WuXue GuoJiajie FengMengmeng WangSihang YangJianshu ZhaoQun GaoQiuting ZhangMengxin ZhaoChangyi XieZhiyuan MaJin-Sheng HeHaiyan ChuYi HuangJizhong ZhouYunfeng YangAmerican Society for MicrobiologyarticleMicrobiologyQR1-502ENmBio, Vol 12, Iss 1 (2021) |
| institution |
DOAJ |
| collection |
DOAJ |
| language |
EN |
| topic |
Microbiology QR1-502 |
| spellingShingle |
Microbiology QR1-502 Qi Qi Yue Haowei Zhenhua Zhang Joy D. Van Nostrand Linwei Wu Xue Guo Jiajie Feng Mengmeng Wang Sihang Yang Jianshu Zhao Qun Gao Qiuting Zhang Mengxin Zhao Changyi Xie Zhiyuan Ma Jin-Sheng He Haiyan Chu Yi Huang Jizhong Zhou Yunfeng Yang Microbial Functional Responses Explain Alpine Soil Carbon Fluxes under Future Climate Scenarios |
| description |
The warming pace in the Tibetan Plateau, which is predominantly occupied by grassland ecosystems, has been 0.2°C per decade in recent years, dwarfing the rate of global warming by a factor of 2. Many Earth system models project substantial carbon sequestration in Tibet, which has been observed. |
| format |
article |
| author |
Qi Qi Yue Haowei Zhenhua Zhang Joy D. Van Nostrand Linwei Wu Xue Guo Jiajie Feng Mengmeng Wang Sihang Yang Jianshu Zhao Qun Gao Qiuting Zhang Mengxin Zhao Changyi Xie Zhiyuan Ma Jin-Sheng He Haiyan Chu Yi Huang Jizhong Zhou Yunfeng Yang |
| author_facet |
Qi Qi Yue Haowei Zhenhua Zhang Joy D. Van Nostrand Linwei Wu Xue Guo Jiajie Feng Mengmeng Wang Sihang Yang Jianshu Zhao Qun Gao Qiuting Zhang Mengxin Zhao Changyi Xie Zhiyuan Ma Jin-Sheng He Haiyan Chu Yi Huang Jizhong Zhou Yunfeng Yang |
| author_sort |
Qi Qi |
| title |
Microbial Functional Responses Explain Alpine Soil Carbon Fluxes under Future Climate Scenarios |
| title_short |
Microbial Functional Responses Explain Alpine Soil Carbon Fluxes under Future Climate Scenarios |
| title_full |
Microbial Functional Responses Explain Alpine Soil Carbon Fluxes under Future Climate Scenarios |
| title_fullStr |
Microbial Functional Responses Explain Alpine Soil Carbon Fluxes under Future Climate Scenarios |
| title_full_unstemmed |
Microbial Functional Responses Explain Alpine Soil Carbon Fluxes under Future Climate Scenarios |
| title_sort |
microbial functional responses explain alpine soil carbon fluxes under future climate scenarios |
| publisher |
American Society for Microbiology |
| publishDate |
2021 |
| url |
https://doaj.org/article/534fc0b37b2346dda3d1aabe9dad3827 |
| work_keys_str_mv |
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| _version_ |
1718445455709306880 |