Microbial Functional Responses Explain Alpine Soil Carbon Fluxes under Future Climate Scenarios

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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Detalles Bibliográficos
Autores principales: 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
Formato: article
Lenguaje:EN
Publicado: American Society for Microbiology 2021
Materias:
Microbiology
QR1-502
Acceso en línea:https://doaj.org/article/534fc0b37b2346dda3d1aabe9dad3827
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