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.

Saved in:
Bibliographic Details
Main Authors: 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
Format: article
Language:EN
Published: American Society for Microbiology 2021
Subjects:
Microbiology
QR1-502
Online Access:https://doaj.org/article/534fc0b37b2346dda3d1aabe9dad3827
Tags: Add Tag
No Tags, Be the first to tag this record!

Internet

https://doaj.org/article/534fc0b37b2346dda3d1aabe9dad3827

Similar Items