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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Format: | article |
Langue: | EN |
Publié: |
American Society for Microbiology
2021
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Accès en ligne: | https://doaj.org/article/534fc0b37b2346dda3d1aabe9dad3827 |
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